Working Report 22-1 Core drilling of deep borehole OL -KR 15 at Olkiluoto in Eurajoki 21 Risto Niinimaki Tauno Rautio January 22 POSIVA OY T6616nkatu 4, FIN-1 HELSINKI, FINLAND Tel. +358-9-228 3 Fax +358-9-228 3719
Working Report 22-1 Core drilling of deep borehole OL -KR 15 at Olkiluoto in Eurajoki 2 1 Risto Niinimaki Tauno Rautio Suomen Malmi Oy anuary 22 Working Reports contain information on work in progress or pending completion. The conclusions and viewpoints presented in the report are those of author(s) and do not necessarily coincide with those of Posiva.
Working Report 22-1 Core drilling of deep borehole OL -KR 15 at Olkiluoto in Eurajoki 21 Risto Niinimaki Tauno Rautio January 22
TEKIJA ORGANISAATIO: SUOMEN MALMI OY PL 1 Juvan teollisuuskatu 16-18 2921 ESPOO TILAAJA: POSIVA OY Toolonkatu 4 1 HELSINKI TILAAJAN YHDYSHENKILO : 2r;;. 2.oz/MH. DI Heikki Hinen Posiva Oy URAKOITSIJAN YHDYSHENKILO : FM Tauno Rautio Smoy RAPORTTI: WORKING REPORT 22-1 CORE DRILLING OF DEEP BOREHOLE OL-KR15 AT OLKILUOTO IN EURAJOKI 21 TEKIJA: r\_: 1 Risto Niinimaki Geologi, Smoy TARKASTAJA : - Tauno Rautio Geologi, Smoy
CORE DRILLING OF DEEP BOREHOLE OL-KR15 AT OLKILUOTO IN EURAJOKI 21 ABSTRACT Posiva Oy submitted an application for the Decision in Principle to the Finnish Government in May 1999. A positive decision was made at the end of 2 by the Government. The Finnish Parliament ratified the Decision in Principle on the final disposal facility for spent nuclear fuel at Olkiluoto, Eurajoki in May 21. The decision makes it possible for Posiva to focus the confirming bedrock investigations at Olkiluoto, where in the next few years an underground rock characterisation facility, ONKALO, will be constructed. As a part of the investigations Suomen Malmi Oy (Smoy) core drilled 233.54 m and 45.14 m deep boreholes with a diameter of 76 mm in October November 21 at Olkiluoto. The identification numbers of the boreholes are OL-KR15 and OL-KR15B, respectively. A set of monitoring measurements and samplings from the drilling and returning water were carried out during the drilling. Both the volume and the electric conductivity of the drilling water and the returning water were recorded as well as the pressure of the drilling water. The objective of these measurements was to obtain more information about bedrock and groundwater properties. Uranine was used as a label agent in the drilling water. The volume of the used drilling water was about 123 m 3 and the measured volume of the returning water was about 59 m 3 At the end of the work the boreholes were flushed by pumping about 3m 3 of water from the bottom ofboreholes. The deviation of the boreholes was measured with the deviation instrument EZ Shot. Additionally inclination was measured separately with an inclination instrument. The results of the EZ Shot measurements indicate that borehole OL-KR15 deviates 17.95 m to the northwest and.63 m up at the borehole depth of 233 m and borehole OL-KR15B deviates.39 m to the east and.1 m up at the borehole depth of 45 m. Uniaxial compressive strength, Young's Modulus and Poisson's ratio were measured from the core samples. The average uniaxial compressive strength is about 152 MPa, the average Young's modulus is 47 GPa and average Poisson's ratio is.24. The main rock types are migmatitic micagneiss and granite. Filled fractures dominate. The average fracture frequency is 1.55 pc/m in borehole OL-KR15 and 3.33 pc/m in borehole OL-KR15B. The average RQD is 97.7% in borehole OL-KR15 and 93,7% in borehole OL-KR15B. One fracture zone was penetrated in both boreholes. The total length of the fracture zones is 1.19 m, which is.5 % of the total core length. Keywords: core drilling, borehole, micagneiss, granite, fracture, monitoring measurements, elastic parameters, deviation measurements.
SYV AKAIRAUS OL-KR15 EURAJOEN OLKILUODOSSA VUONNA 21 TIIVISTELMA Posiva Oy jatti valtioneuvostolle vuonna 1999 periaatepaatoshakemuksen, jolla se haki lupaa rakentaa kaytetyn ydinpolttoaineen loppusijoituslaitos Eurajoen Olkiluotoon. Periaatepaatoshakemuksen mukaisesti paikkatutkimukset keskitetaan Olkiluotoon. Joulukuussa 2 valtioneuvosto teki asiasta myonteisen paatoksen. Toukokuussa 21 eduskunta vahvisti valtioneuvoston paatoksen. Syksylla 21 tehdyilla tutkimuksilla hankittiin tietoa ONKALON sisaanmenopaikaksi suunnitellulta alueelta. Tutkimuksiin liittyen Suomen Malmi Oy kairasi 233,54 m pituisen tutkimusreian OL-KR15 ja marraskuussa 45,14 m:n pituisen reian OL-KR15B Eurajoen Olkiluodossa. Reikien halkaisijat ovat 76 mm. Kairauksien aikana suoritettiin tarkkailumittauksia lisainformaation saamiseksi kallio-olosuhteista. Mittauksia olivat veden sahkonjohtokyvyn ja huuhteluveden paineen mittaukset ja huuhteluveden/palautuvan veden maaran mittaus. Kairauksiin kaytettiin uraniinilla merkittya huuhteluvetta no in 123 m 3 Tyon aikana vetlli palautui rei' ista maaramittarin kautta noin 59 m 3 Tyon lopuksi pumpattiin noin 3 m 3 vetlli reikien pohjalta. Reikien sivupoikkeama ja taipuma mitattiin EZ Shot -mittarilla. Reikien kaltevuus mitattiin lisaksi kaltevuusmittarilla. EZ Shot -mittauksen mukaan reian KR15 taipuma on 233 m:n reikasyvyydessa luoteeseen 17,95 m ja ylospain,63 m ja reian KR15B taipuma on 45 m:n reikasyvyydessa itaan,39 mja ylospain,1 m. Kallionaytteistii maaritettiin yksiaksiaalinen puristusmurtolujuus, kimmomoduli ja Poissonin luku. Yksiaksiaalinen puristusmurtolujuus oli keskimaarin noin 152 MPa, kimmomoduli oli keskimaarin no in 4 7 GPa ja Poissonin luku,24. Kivilajeina esiintyivat migmatiittinen kiillegneissi ja graniitti. Rakoilusta taytteiset raot ovat hallitsevia. Kallion rakoluku on reialla KR15 keskimaarin 1,55 kpllm ja reialla KR15B 3,33 kpllm. Vastaavasti RQD-luku on reialla KR15 keskimaarin 97,7% ja reialla KR 15B 93,7 %. Rikkonaisia, tihearakoisia osuuksia lavistettiin yksi kummallakin reiaila. Rikkonaisia osuuksia on yhteensa 1,19 m. Yhteensa rikkonaisten osuuksien maara on,5 % reian kokonaisnaytemaarasta. A vainsanat: kairaus, kairanreika, migmatiittinen kiillegneissi, graniitti, rako, tarkkailumittaukset, muodonmuutosominaisuudet, sivusuuntamittaus
CORE DRILLING OF DEEP BOREHOLE OL-KR15 AT OLKILUOTO IN EURAJOKI 21 ABSTRACT Posiva Oy submitted an application for the Decision in Principle to the Finnish Government in May 1999. A positive decision was made at the end of 2 by the Government. The Finnish Parliament ratified the Decision in Principle on the final disposal facility for spent nuclear fuel at Olkiluoto, Eurajoki in May 21. The decision makes it possible for Posiva to focus the confirming bedrock investigations at Olkiluoto, where in the next few years an underground rock characterisation facility, ONKALO, will be constructed. As a part of the investigations Suomen Malmi Oy (Smoy) core drilled 233.54 m and 45.14 m deep boreholes with a diameter of 76 mm in October November 21 at Olkiluoto. The identification numbers of the boreholes are OL-KR15 and OL-KR15B, respectively. A set of monitoring measurements and samplings from the drilling and returning water were carried out during the drilling. Both the volume and the electric conductivity of the drilling water and the returning water were recorded as well as the pressure of the drilling water. The objective of these measurements was to obtain more information about bedrock and groundwater properties. Uranine was used as a label agent in the drilling water. The volume of the used drilling water was about 123 m 3 and the measured volume of the returning water was about 59 m 3 At the end of the work the boreholes were flushed by pumping about 3m 3 of water from the bottom ofboreholes. The deviation of the boreholes was measured with the deviation instrument EZ Shot. Additionally inclination was measured separately with an inclination instrument. The results of the EZ Shot measurements indicate that borehole OL-KR15 deviates 17.95 m to the northwest and.63 m up at the borehole depth of 233 m and borehole OL-KR15B deviates.39 m to the east and.1 m up at the borehole depth of 45 m. Uniaxial compressive strength, Young's Modulus and Poisson's ratio were measured from the core samples. The average uniaxial compressive strength is about 152 MPa, the average Young's modulus is 47 GPa and average Poisson's ratio is.24. The main rock types are migmatitic micagneiss and granite. Filled fractures dominate. The average fracture frequency is 1.55 pc/m in borehole OL-KR15 and 3.33 pc/m in borehole OL-KR15B. The average RQD is 97.7% in borehole OL-KR15 and 93,7% in borehole OL-KR15B. One fracture zone was penetrated in both boreholes. The total length of the fracture zones is 1.19 m, which is.5 % of the total core length. Keywords: core drilling, borehole, micagneiss, granite, fracture, monitoring measurements, elastic parameters, deviation measurements.
SYV AKAIRAUS OL-KR15 EURAJOEN OLKILUODOSSA VUONNA 21 TIIVISTELMA Posiva Oy jatti valtioneuvostolle vuonna 1999 periaatepaatoshakemuksen, jolla se haki lupaa rakentaa kaytetyn ydinpolttoaineen loppusijoituslaitos Eurajoen Olkiluotoon. Periaatepaatoshakemuksen mukaisesti paikkatutkimukset keskitetaan Olkiluotoon. Joulukuussa 2 valtioneuvosto teki asiasta myonteisen paatoksen. Toukokuussa 21 eduskunta vahvisti valtioneuvoston paatoksen. Syksylla 21 tehdyilla tutkimuksilla hankittiin tietoa ONKALON sislliinmenopaikaksi suunnitellulta alueelta. Tutkimuksiin liittyen Suomen Malmi Oy kairasi 233,54 m pituisen tutkimusreian OL-KR15 ja marraskuussa 45,14 m:n pituisen reian OL-KR15B Eurajoen Olkiluodossa. Reikien halkaisijat ovat 76 mm. Kairauksien aikana suoritettiin tarkkailumittauksia lisainformaation saamiseksi kallio-olosuhteista. Mittauksia olivat veden sahkonjohtokyvyn ja huuhteluveden paineen mittaukset ja huuhteluveden/palautuvan veden mlliiran mittaus. Kairauksiin kaytettiin uraniinilla merkittya huuhteluvetta noin 123 m 3 Tyon aikana vetta palautui rei'ista mlliiramittarin kautta noin 59 m 3 Tyon lopuksi pumpattiin noin 3 m 3 vetta reikien pohjalta. Reikien sivupoikkeama ja taipuma mitattiin EZ Shot -mittarilla. Reikien kaltevuus mitattiin lisaksi kaltevuusmittarilla. EZ Shot -mittauksen mukaan reian KR15 taipuma on 233 m:n reikasyvyydessa luoteeseen 17,95 m ja ylospain,63 m ja reian KR15B taipuma on 45 m:n reikasyvyydessa itaan,39 mja ylospain,1 m. Kallionaytteista maaritettiin yksiaksiaalinen puristusmurtolujuus, kimmomoduli ja Poissonin luku. Yksiaksiaalinen puristusmurtolujuus oli keskimiliirin noin 152 MPa, kimmomoduli oli keskimaarin no in 4 7 GP a ja Poissonin luku,24. Kivilajeina esiintyivat migmatiittinen kiillegneissi ja graniitti. Rakoilusta taytteiset raot ovat hallitsevia. Kallion rakoluku on reialla KR15 keskimiliirin 1,55 kpl/m ja reialla KR15B 3,33 kpl/m. Vastaavasti RQD-luku on reialla KR15 keskimlliirin 97,7% ja reialla KR15B 93,7 %. Rikkonaisia, tihearakoisia osuuksia lavistettiin yksi kummallakin reialla. Rikkonaisia osuuksia on yhteensa 1, 19 m. Yhteensa rikkonaisten osuuksien mlliira on,5 % reian kokonaisnaytemlliirasta. A vainsanat: kairaus, kairanreika, migmatiittinen kiillegneissi, graniitti, rako, tarkkailumittaukset, muodonmuutosominaisuudet, sivusuuntamittaus
1 CORE DRILLING OF DEEP BOREHOLE OL-KR15 AT OLKILUOTO IN EURAJOKI 21 ABSTRACT TIIVISTELMA CONTENTS 1 1. INTRODUCTION 1.1 Background 1.2 Scope of the work 3 3 3 2. WORK DESCRIPTION 2.1 Diamond core drilling 2.2 Drilling water and the use of label agent 2.3 Monitoring measurements 2.4 Deviation surveys 2.5 Flushing of the borehole 2.6 Engineering geological logging 2.7 Rock mechanical tests on core samples 5 5 6 7 8 8 9 14 3. TECHNICAL DETAILS OF THE BOREHOLES 3.1 Location and deviation 3.2 Structure of the upper part of the borehole 17 17 17 4. ENGINEERING GEOLOGY 4.1 The effects of drilling to the sample quality 4.2 Rock quality 4.3 Fracturing 4.4 Core discing 4.5 Strength and elastic properties 19 19 19 2 22 23 5. MONITORING RESULTS 5.1 Conductivity of drilling and returning water 5.2 Quantities of drilling and returning water 5.3 Drilling water pressure 5.4 Ground water level in the borehole 5. 5 Drilling cuttings yield 5.6 Drilling water and returning water label agent concentrations 25 25 25 26 27 27 28 6. SUMMARY 29 7. REFERENCES 3
2 8. APPENDIXES 8.1 Time schedule 8.2 Drilling equipment 8.3 Constructions of the upper part of the borehole 8.4 Degree of weathering 8.5 Lifts 8.6 List of core boxes 8.7 Rock description 8.8 Foliation 8.9 List of fractures 8.1 Fracture frequency and RQD 8.11 Fractured zones, core loss 8.12 Flushing water samples 8.13 Returning water samples 8.14 Deviation surveys 8.15 Deviation surveys, graphic PHOTOS 31 33 35 39 41 43 45 47 49 63 69 71 73 75 79 91
3 1. INTRODUCTION 1.1 Background In 1999, Posiva Oy filed an application for a policy decision from the council of state for a construction permit to build a final disposal facility for spend fuel at the Olkiluoto area in the Eurajoki municipality. It was applied that the nuclear repository site investigations would be concentrated at the Olkiluoto area. In December 2, the council of state made a positive policy decision and in May 21, the parliament ratified the decision. The policy decision makes it possible to concentrate the research activities at Olkiluoto in the municipality of Eurajoki. One part of the research is to build an underground rock characterisation facility (called "ONKALO"). Investigations during the autumn 21 are aimed to document the ground conditions in the area where the planned facility decline and shaft will be located. Posiva Oy contracted (order number 97/1HH) Suomen Malmi Oy (SMOY) to drill new investigation boreholes in the area. In October and November 21 boreholes OL-KR15 (233.54 m) and OL-KR15B (45.14 m) were core drilled. The location of the boreholes are shown in Figure 1. Borehole OL-KR15 is located about 2 m from the Korvensuo reservoir pump station and the borehole OL-KR15B is located three metres west from the borehole OL-KR15. The boreholes are vertical (initial inclination 9 degrees) and the borehole diameter is 76 mm. 1.2 Scope of the work The aim of the work was to drill about 25 m long borehole to document the geology and the ground conditions (continuity of the rock units, fracture zones and rock quality) in the area. The 4 m precollar for the borehole OL-KR15 was drilled with a down the hole percussion drill. Therefore the 45 m deep borehole OL-KR15B was core drilled next to it. To maximise the recovery yield of an undisturbed and continuous core, a triple tube coring technique was used. In addition to the drilling, work included core logging, rock mechanical testing of the core, in-hole technical measurements, drilling fluid monitoring, flushing of the borehole, borehole deviation surveys and reporting. This report documents the work and sampling done during the drilling of the boreholes. Depth measurements are from the ground surface unless otherwise stated. Distance between the top of casings and the ground level is.4 m and.64 m for the boreholes OL-KR15 and OL-KR15B,
1-Tj 1' - t"--4 (j e - ::s g- r:::r '""'t (D 6 CD Cll t"--4 -Vl.. t"--4 Vl t:o s E?. 2" e; (1) p Location of the boreholes KR1 -KR15, KR15B Coordinate System: Finnish Coordinate System, zone 1 (Projection: Gauss-Kruger) 22.1.22 Saanio & Riekkola Oy/HM, KF llegend: K Core Drilled Borehole KR15B KR15 11 [ R14 _ 1 I 'll' 1...,....,...,...,, I,.. I 8" (i1 Cl.l '" 3 - g- ;J (D g' 6 CD Cll (j 8" 5 CD Cl.l (j CD 8" 1G p ::r CD Cl.l @ ::4.... ;:t> g. (D (D 8. g- : - s- go : ::::: a.. e- (1)
5 2. WORK DESCRIPTION 2.1 Diamond core drilling Thickness of the overburden at the location of the borehole OL-KR15 is 3.6 m. The borehole thh the overburden is cased with a 194/184 mm diameter tube, which is drilled into the bedrock to the depth of3.9 m. From 3.9 m to 4.12 m the borehole was drilled with a 165 mm diameter hammer between 15th and 1 i 11 October 21. This percussion drilled part of the borehole is cased with a stainless steel 141135 mm diameter tube which is grouted into the bedrock. The diamond drill rig, additional casings and air lift pumping pipes were set up at the drilling site on 23rd October 21. Drilling commenced on the next day. On 2nd November 21, drilling depth 233.27 m was reached. During the deviation survey, the centralizer for the survey equipment was stuck in the borehole. It was removed by drilling and the final depth 233.54 m was reached. The time schedule of the work is shown in Appendix 8.1. The diamond drill rig was set up at the drilling site OL-KR15B on 6 1 h November 21. Drilling thh the overburden, which was 2.38 m thick, was done on the same day. Because of the fractured bedrock casing was drilled to the depth of 4.48 m. After the casing was placed, diamond drilling continued normally. The final depth 45.14 m was reached on 8th November 21. Boreholes OL-KR15 and OL-KR15B were core drilled with a hydraulic Diamec 1 drill rig of which drill feed, hydraulic chuck, drill head and mast are reinforced. The core barrel used was a WL-76 triple tube and drill rods used were alu-72 rods. Borehole diameter with W-76 triple tube core barrel is 76 mn1 and drill core diameter is 52 mm. Equipment used is shown in Appendix 8.2. The cutting area of the diamond bit of a triple core barrel is larger than that of a double core barrel. In a triple core barrel the extra innermost tube is of split type. The innermost split tube containing the sample is removed from the core barrel with the aid of a piston working on water pressure. By this way the sample may be removed from the core barrel as undisturbed as possible. The structure of the WL-76 triple tube core barrel is presented in figure of Appendix 8.2 in drawings and photographs. Drilling was continuous shift work (three shifts per day) and the drilling team in a shift consisted of a driller and an assistant. Geologist Tauno Rautio was the project manager, and Ville Teivaala and Esko Hartikainen were drilling supervisors. Geological logging was done by geologist Risto Niinimaki and the final report was written by Tauno Rautio and Risto Niinimaki.
6 Drilling time (which does not include set up and dismantling works) on the borehole OL-KR15 was 189 h which gives the mean drilling efficiency of 1.2 m per rig hour. The drilling time for the borehole OL-KR15B was 39 h. Mean drilling efficiency per rig hour in different depth intervals are tabulated in Table 1. Table 1. Drilling efficiency. Depth interval, Efficiency, m m/rig hour 4-1 1.7 1-2 1.9 2-233.27.67-45.14 1.15 Comments! OL-KR15 OL-KR15 OL-KR15 (end ofborehole 233.54 m) Casing and drilling, OL-KR15B Wear and tear of the drilling equipment was heavier than average due to the hard bedrock. The wear of the drill bit correlates with the mineral composition of the bedrock. In this work, only 33. m was drilled per WL-76 bit compared to a long-term average of 55 m per T-76 and T-56 bits. 2.2 Drilling water and the use of label agent Drilling water for the boreholes OL-KR15 and OL-KR15B was pumped from the pump station of the Korvensuo reservoir. The water line was about 2 m long. Before water was pumped into the mixing tanks (two 3 m 3 fibreglass tanks) it was filtered thh a 5 m filter. All drilling water was marked with the label agent sodiumfluoresceine. Sodiumfluoresceine (uranine) is an organic powdery pigment which is broken down by UV radiation. Therefore the label agent mixing tanks have to be covered. The quality of the label agent was tested by the F ortum Vantaa laboratories in spring 21. At the Rauma chemist, uranine was packed in glass vials in 1.5 g ready to use doses. At the drilling site, contents of a vial was dissolved in one litre of water which was slowly added into the mixing tank at the beginning of pumping. Turbulence caused by pumping ensured mixing of the label agent.
--------------- - 7 2.3 Monitoring measurements During the drilling, several drilling water parameters were monitored and water samples taken. The aim was to get additional information of rock quality and predict possible drilling problems. To find out how much drilling water was leaking into the bedrock, the amounts of ingoing and returning drilling water were monitored. The flow meter for ingoing water was assembled in the waterline coming from the water pump and the amount of returning water was measured from the overflow of the sedimentation tank. Water level in the borehole was measured in the beginning of every morning shift and if there was more than two hour break in the drilling. All drilling water batches made in the mixing tank were sampled. The returning water was sampled once a day as long as water was flowing out of the borehole. Because the sensitivity of uranine to the UV -light, immediately after the sampling the sample bottles were wrapped in aluminium foil immediately after the sampling. Water samples were stored in a fridge until they were sent for analysis to the laboratory ofteollisuuden Voima Oy (TVO) in Olkiluoto. Electric conductivity of the drilling water was measured after the label agent was mixed. The returning water samples were collected for the conductivity measurements as long as water was flowing from the borehole. The returning water contains drilling cuttings of which composition depends on the drilled rock type. If the drilling cuttings was affecting the conductivity, the water samples (2-3 dl) were let to settle and, if needed, filtered thh a 45 Jlm filter to remove the remaining drilling cuttings. The conductivity measurements were done with a Phillips conductivity meter PW9529 which gives the results as ms/m at +25 C. The conductivity meter was calibrated at the laboratory oftvo before the measurements. Drilling water pressure was logged at the beginning of every sample run and when there were pressure changes. The drilling water pressure monitoring was aimed to avoid drilling problems and to recognise anomalously permeable fracture zones. The drilling water pressure has a direct correlation to the level of the water column replaced in the borehole. Increased permeability in the fracture zones reduce the water pressure. Blockages in the sample tube and wearing of the diamond bit increase the drilling water pressure.
8 2.4 Deviation surveys To trace the borehole accurately the dip and azimuth of the borehole were measured with a EZ Shot downhole survey tool, which was lowered into the boreholes with a wire line. In addition, the dip of the borehole was measured separately with a PP-downhole dip meter. EZ-Shot meter measures the borehole dip with an electronic accelerometer and the azimuth with a three component fluxgate magnetometer. According to the manufacturer, if there are no magnetic anomalies, the accuracy of the azimuth is ±.5 degrees and the dip of the borehole.2 degrees. The azimuth is given to the magnetic north and the declination, which is about five degrees in the area,has be added to the results. 2.5 Flushing of the borehole Before the final flushing of the boreholes, the walls of the boreholes were washed with the label agent water to drop all loose material to the bottom of the boreholes. The washing device is a double coupler of which one end is blocked and which has four 5 mm boreholes on its rim 9 degrees apart. Consequently, the water jets are directed in a straight angle to the wall of the boreholes. Washing of the boreholes is done by lowering and rotating the rods while the drilling water pressure is on. About 7 m 3 of label agent water was used during the wash of the borehole OL-KR15 and 1.6 m 3 used during the wash of the borehole OL-KR15B. After the walls of the boreholes were washed the boreholes were cleaned by pumping water thh alu-43 drill rods with a submersible pump. In this method, the lowermost 9 m of the drill rods are perforated and in the upper part alu-72 drill rods are used. A submersible pwnp was lowered to about 35 m inside the drill rods. Consequently, the flushing water circulates by the bottom of the borehole. Pumping was interrupted once and drill rods were moved up and down in the borehole to remove any residual drilling cuttings from the wall of the borehole. The pump was taken out of the drill rods before moving the drill rods, and lowered back after the procedure and the pumping continued. The flushing and pumping was done between 8 pm on 4th November and 7 am on 6th November 21 in the borehole OL-KR15. During the flushing 14.4 m 3 of water was pumped from the borehole OL-KR15 at an average rate of 411 1/h. In the borehole OL-KR15 B the flushing and pumping was done between 8 pm on 8th Noven1ber and 7 am on 9th November 21. During the flushing 16.4 m 3 of water was pumped from the borehole OL-KR15B at an average rate of 713 1/h.
r------------- --- -- 9 2.6 Engineering geological logging Handling of the core is based on the POSIV A work instructions TY--3/ 1 "Core handling procedure with triple tube coring (in Finnish)". Drill core samples were placed in about one metre long \Vooden core boxes immediately after emptying the sample tube. Core boxes were covered with damp proofing quality aluminium paper so that the aluminium surface was against the core. Also the wooden blocks separating the different sample runs were covered by aluminium paper. Drill core during the drilling was handled especially carefully. Core was placed on the boxes avoiding any unnecessary breakage. Broken and clay rich core was wrapped in aluminium foil to avoid breaking it during storage and logging. If loose rock fragments had fallen of the borehole walls, they were placed after the block marking of the end of the previous sample run. Therefore, at the beginning of a sample run there might be rock fragments which do no belong to the sample run itself. Geologist logged the core in a transportable office at the drilling site. Logging was designed for engineering geological purposes (Gardemeister et al. 1976, Korhonen et al. 1974). Following parameters were logged: fracture classification, fracture zones and core loss, artificial break and fracture frequency and RQD, petrography, foliation degree, degree of weathering and core discing. In addition, the lift and core box number were documented. In the list of fractures the fractures were numbered sequentially from the top of the borehole to the bottom of the borehole. Fracture depths were tneasured to the centre line of the core and were given with one centimetre accuracy. If the middle line of an gular fracture did not coincide with the centre line of the core, an appropriate depth was given. If observations were given for a depth interval, the depth was given to the end of a last fracture, for example in the case of crushed zone. Logged depths were corrected to the true core depth, i.e. if there were depth inaccuracies due to the core loss or the core lifter had slipped, the depth written on the wooden block marking the end of a lift was corrected. Inaccuracies due to core loss were also separately logged. The nature of a fracture was described with abbreviations: op =open, rusty/lin1onite covering ti = tight, no filling material fi =filled fisl = filled slickenside grfi = grain filled
1 clti = clay filled. Open used in core logging if fracture with rusty/limonite covering. Angle of a fracture was given relative to the core axis. If a fracture was parallel to the core axis its core angle was and if a fracture was perpendicular to the core axis its core angle was 9. Thickness of the fracture filling was given in millimetres. The colour of the fracture surfaces was logged if it differed from the host rock colour significantly. Most commonly the colour of filled and open fractures differed from the host rock colour. Tight fractures had typically only a slightly different shade from the host rock colour. Fractures which had a clear colour but the core was intact across the fractures were classified as filled fractures. In these cases in the remarks column has been written "" or "partly '' which indicates that the fracture is and its permeability is poor in its natural state. Fractures, which had euhedral or subhedral mineral growth, have"crystals" written in the log. In addition, if there was any smell, it has been logged to the remarks column. Fracture surface colour (minerals) has been described with four letter abbreviations: brow, lbro, dbro (brown, light brown, dark brown) gray, lgra, dgra (gray, light gray, dark gray) gree, lgre, dgre (green, light green, dark green) red, lred,dred (red, light red, dark red) Minerals have been logged only if their recognition was absolutely sure. Mineral names used have been listed in the petrography section of the report. The colour shades of the fracture surface colours were described by adding one letter to the front of the three letter colour abbreviation. For example: rbro (reddish brown) Fracture surface morphology is described with following abbreviations: plan (planar) (gular) (ed)
11 Fracture surface quality was described with a four letter abbreviation. The three step classification used corresponds with the JRC-numbers (Barton & Choubey 1977). (h; JRC 15-1) (semih; JRC 7-14) smoo (smooth; JRC -6) Core loss is the result of geological factors which include strong weathering or fracturing of rock, or technical factors during the drilling. The depth of core loss, amount and reason was logged. If the location was not known exactly, the depth interval where the core loss occurred has been logged. Consequently, the depth measurements following the core loss are marked with notation. Fractured zones were described in the list of the fractured zones and core loss using the following abbreviations: Riiii = fracture-structured, densely fractured, more than 1 fractures per metre RiiV = crush-structured RiV =clay-structured Artificial break and fracture frequency and ROD were logged on full metre depth intervals. Artificial break frequency is the number of core breaks within one metre interval. Artificial breaks include all breaks which are caused of by drilling, core handling, core discing and natural fractures. Fracture frequency is the number of natural fractures within one metre interval. If the artificial break frequency is larger than the fracture frequency the core must have been broken during the drilling or core handling accidentally or by purpose. If the fracture frequency is larger than the artificial break frequency the fractures must be tight and cohesive enough to keep the core together. RQD gives the percentage of over 1 cm long core segments, which are separated by natural fractures, within one metre interval. List of lift depths is given as it has been marked on the spacing wooden blocks separating different sample runs in the core boxes. If the length of the core in the core barrel indicated that sampling depth was different from the drilling depth, the true sample depth has been corrected on the spacing block. Therefore, the sample run depth means the sample depth. The drilling depth might be deeper than the sampling depth if the core lifter slips and part of the core is left in the borehole and is not retrieved until with the next lift. The lifts are listed in Appendix 8.5. List of core boxes lists the start and end depths of the core in each core box. List of core boxes is in Appendix 8.6.
12 Petrographical description is based on the Finnish engineering geological rock classification (Korhonen et al. 1974, Gardemeister et al. 1976). Each rock type has been described at the first occurrence and only the changes are added later if there has been significant differences in the deeper sections. Grain size has been classified as follows: Very fine grained, glassy, grain not visible to Naked eyes << 1 mm Fine grained <1 mm Medium grained 1... 5mm Coarse grained 5... 5mm Very coarse grained >5 mm Texture has been described with following terms (Finnish abbreviations used): Massive Foliated Mixed (migmatitic) M L s Foliation degree has been classified to four categories: unfoliated weak medium strong 1 2 3 Texture and foliation intensity description can have following variations: MO, M1, L1, L2, L3, SO, S1, S2, S3.
Recognition of the mineral composition of the rock is qualitative and the mode has been estimated by eye. Mineral names have been abbreviated using the system used in Saltikoffs (1972) Finnish mineral name catalogue. Same abbreviations have also been used in the fracture descriptions. The most common abbreviations used are: quar = quartz feld = feldspars (Kfeldspar or plagioclase) biot = biotite carb = carbonate (unspecified) talc= talc chlo = chlorite clay= clay minerals (unspecified) sulf = sulphide minerals (unspecified) fehy = Fe-hydrates, (limonite) epid = epidote grap = graphite Foliation degree has been described using the Finnish engineering geological classification. Zones of relatively constant foliation intensity were delineated and the angle of foliation was measured about every 1 metres. In addition, the degree was estimated using the above mentioned four category classification (Korhonen et al. 1974, Gardemeister et al. 1976) Degree of weathering was described with following abbreviations (Korhonen et al. 1974, Gardemeister et al. 1976): RpO = unweathered Rp 1 = slightly weathered Rp2 = strongly weathered Rp3 = completely weathered If there are small changes in the weathering degree within a logged depth interval, for example around fractures, the overall weathering degree is given first and the minor weathering changes in brackets.
14 Core discing has been logged separately. Depth intervals, within which core discing occurs, have been documented. The number of breaks and core discs, the minimum and maximum spacing between discs have been logged. In each break, the geometry of the disc surfaces have been described using the following classification (the core is running from left to right): ( ( = top surface concave, lovver surface convex (I = top surface concave, lower surface planar I( = top surface planar, lower surface convex ) ) = top surface convex, lower surface concave )I = top surface convex, lower surface planar I) = top surface planar, lower surface concave 11 =top surface planar, lower surface planar )( = top surface convex and lower surface convex S =saddle A = incomplete discing All core boxes were photographed (colour) both dry and wet. Core photographs (wet) are presented at the end of the report. In addition, close up photographs were taken from well preserved fracture zones and individual clay filled fractures. These photographs (wet) are presented at the end of the report after the full core box photographs. 2. 7 Rock mechanical tests on core samples Rock strength and strain tests were made with Rock Tester-equipment. Samples for the testing were taken every 3 m, or if the rock type changed. Young's Modulus E, Poisson's ratio v and Modulus of Rupture Smax were measured with a Bend test in which the outer supports (L) were placed 16 mm apart and the lower supports (U) 48 mm apart. The test arrangement is shown in Figure 3.
15 u D L> 3,5D DUL/3 L Figure 3. Bend test Young's Modulus describes the ratio between stress and strain. This is given as Hook's law (equation 2.9.1) (j E =- [Pa] Ea (2.9.1) cr = stress [Pa] Ea = axial strain Poisson's ratio is defined as the ratio of radial strain and axial strain (equation 2.9.2). (2.9.2) Er = radial strain Ea = axial strain Uniaxial compressive strength crc was determined indirectly from the point load test results. The point load tests were made according the ISRM instructions (ISRM 1981 ja ISRM 1985). The point load index lsso, which is determined in the test, is multiplied by 24 and resulting value corresponds with the uniaxial compressive strength.
16 In the point load test the load is increased until the core sample breaks (Fig. 4 ). The point load index is calculated from the load required to break the sample. The test result is valid only if the break surface goes thh the both load points. The point load number Is is calculated from the equation 2.9.3. p I.. =-, J D- (2.9.3) P = point load D = diameter of the core sample Point load number is dependent on the diameter of the core sample and it is corrected to the point load index using the equations 2.9.4 and 2.9.5. The result is not dependent on the sample SIZe. (2.9.4) (2.9.5) 4 D ' L >,5D Figure 4. Point load test
17 3. TEHNICAL DETAILS OF THE BOREHOLES 3.1 Location and deviation The initial dip ofthe boreholes OL-KR15 and OL-KR15B was 9 degrees. The ground surface was the starting level of the borehole and depth measurements are from the ground surface unless otherwise mentioned. The collar coordinates of the borehole are shown in the Table 2. EZ-Shot measurements indicate that at the depth of 233 m the borehole OL-KR15 has deviated 17.95 m to the northwest and.63 m up from the initial azimuth and the borehole OL-KR15B has deviated.39 m to east and.1 m up at the depth of 45 m. The total deviation in the borehole OL-KR15 was 7.7% from the length of the borehole and in the borehole OL-KR15B.8%. The National XYZ coordinates of the boreholes calculated from the EZ-Shot measurements are presented in Table 2. Table 2. Coordinates of the boreholes OL-KR15 and OL-KR15B. Point location, borehole number X y z Ground surface, OL-KR15 92 439.91 25 84.14 8.42 Top of the casing, OL-KR15 8.82 End ofborehole (231 m), OL-KR15 92 453.43 25 828.43-221.84 Ground surface, OL-KR15B 92 442.21 25 838.44 8.35 Top of the casing, OL-KR15B 8.99 End ofborehole (45 m), OL-KR15B 92 442.19 25 838.83-36,65 3.2 Structure of upper part of the borehole Down the hole drilling was used to drill the precollar for the borehole OL-KR15. This borehole was started by drilling a 194/184 mm casing thh the overburden into the bedrock. The casing was drilled to 3. 9 m depth from the surface. The thickness of the soil was estimated to be 3.6 m. The borehole was continued with a 165 mm hammer to 4.12 m and a 14/135 mm stainless steel casing was placed into the borehole and cemented into the bedrock. At the bottom of the casing there is a funnel, which helps to insert instruments into the borehole. Finally the 1941184 mm casing was cut to the ground level.
18 Length of the funnel at the bottom of the 14/135 mm casing is 11 mm. The funnelling part is 53 mm long. The bottom of the funnel is made of a 84/77 mm tube which is 57 mm long. The tube has right hand thread which was used to attach the 84/77 casing during the drilling. The funnel is in the 14/135 mm casing and the end of the tube in the lower part of the funnel is at the depth of 4.9 m. Between the tube and the bedrock is 3 cm of concrete which was cut thh at the beginning of diamond drilling. The funnel and the attached tube are also made of stainless steel. The structure of the funnel and casing is shown in Appendix 8.3. After the drilling was finished, a one square metre concrete slab was cast around the casing. The top of the casing was with a plug, which has a lock. The precollar for the borehole OL-KR15B was done by drilling a 9/77 mm casing thh the overburden into the bedrock. The casing was drilled to 4.48 m depth from the surface. The thickness of the soil was estimated to be 2.38 m. Later the casing, which had a casing shoe, was cemented into the bedrock. The top of the casing was with a plug, which has a lock.
19 4. ENGINEERING GEOLOGY 4.1 The effects of drilling to the sample quality Core loss due to rock breaking or milling did not occur. In places, the ends of core pieces had rotated but there was no significant core loss. The sample quality is better while drilling with triple tube core barrel than drilling with double tube core barrel. In a triple tube core barrel the inner tube is split, it is not necessary to shake the core out of a inner tube and, therefore, it will stay more compact than in a normal double tube core barrel. This advantage is especially noticed when drilling fractured rocks; it is not necessary to fit the ends of the core pieces together. In addition, soft fracture fills will be preserved much better. Furthermore, there is much less drilling cuttings on the core surface, and in the breaks and fractures. 4.2 Rock quality Drill core consisted of rock types which had earlier described from the area. Mica gneiss is typically migmatitic and in places granitic (pegmatitic) material is abundant. In addition, granite has slightly foliated sections and contains mica gneiss enclaves. These two rock types are in many places intercalated and, consequently, in drill core, average intersections are only a few metres thick. Therefore, rock types have been classified by the major rock type and can have thin layers of minor rock type. Drill core is mainly unweathered and narrow weathered zones were intersected only near the surface of the bedrock. In the borehole OL-KR15B there is one narrow strongly weathered zone and one weakly weathered zone. In the borehole OL-KR15 there are two weakly weathered zones. In total, 1.92 m of the drill core had visible signs of weathering. However, in places feldspars are cloudy also in the unweathered parts. The weathering degree of rocks are shown in Appendix 8.4. Migmatic micagneiss comprises mica rich bands and light red coarse grained granitic bands. It is typically moderately foliated, L2. The grain size of the mica gneiss varies from fine grained to medium grained. The main minerals are quartz, feldspars and biotite. In places, occurs and some places occurs small cavities. Granite is equigranular. Its grain size varies from medium grained to coarse grained, in places it is pegmatitic. The texture is typically massive, MO, but there are some weakly foliated mica gneiss enclaves, M 1. The main minerals are feldspars, quartz and biotite.
2 Rock descriptions along the boreholes are presented in Appendix 8. 7. Graphic log showing the rock types and fracture frequency is presented in figure 4. Angle of foliation relative to the core axis was measured. Because the borehole was vertical, core was not oriented. Based on the foliation angle relative to the core axis, the strike and dip of the foliation do not vary much, except some small parts in the mica gneiss. Foliation intensity and foliations angles have been presented in Appendix 8.8. 4.3 Fracturing Fractures in the drill core are tight or filled. Most of them are filled. There were no open fractures. Fracture fill material is most commonly grey or white carbonate and sulphides, mostly, or dark chloritic material. White kaolin was also observed as fracture fill. In most fractures, the fracture filling is very thin layer on the fracture surfaces, and the opposite surfaces of the fracture match perfectly on each other's. Commonly the fracture filling is only a patchy coating on the fracture surfaces but these are still classified as filled fractures. Only a few fractures have a filling, which is more than one millimetre thick. The thickest fracture filling is about three centimetres in the borehole OL-KR15B. Most fractures, which have coloured surfaces, were classified as filled fractures. Tight fractures may also have a colour and, consequently, there is no clear distinction between tight and filled fracture. Some fractures, including some filled fractures, are healed. In total, 58 of the fractures intersected, which are about 13% of all fractures, were healed or partly healed. There are 4 clay filled fractures in the borehole OL-KR15 and 11 in the borehole OL-KR15B. 2 grain filled fractures were observed in the borehole OL-KR15 and 4 in OL-KR15B. 23 slickensided surfaces were intersected in the borehole OL-KR15 and 4 in OL-KR15B. In addition, there is one fracture zone with clay and grain filled fractures, but to prevent the core falling apart the core was left in the box and it was not possible to define the exact nature of these fractures. Some of the slickensided fractures have clay or grain filling and some clay and grain filled fractures have slickensides under the fill. Slickensided fractures occur thh the core but most of them are in or near the zones of higher fracture density. In places, slickensided fractures are in groups. Detailed logs of the fractures are presented in Appendix 8.9.
21 Rock types Fractures, pes/m 5 1 15 OL-KR168 OL-KR16 Mica gneiss Granite Figure 4. Graphic log of the boreholes showing rock types and fracture intensity.
22 Morphology of the fractures varies a lot. Most commonly surfaces are gular and semih (JRC-number 7-14). The second most common morphology is gular or ed with a h surface (JRC-number 15-2). However, different variations are common. Average fracture frequency in the borehole OL-KR15 is 1.55 fractures per metre and 3.33 fractures per metre in OL-KR15B. The mean RQD value for the borehole OL-KR15 is 97.7% and 93.7% for OL-KR15B. Variations of the fracture frequency and RQD are listed in Table 3 and fracture frequency is sho"wn graphically in Figure 4. The full logs of the fracture frequency, artificial breaks and RQD are presented in Appendix 8.1. Table 3. Average fracture frequency and RQD values in different depth intervals in OL-KR15 and OL-KR15B. Depth Average Average Depth Average Average from-to fracture RQD value, from-to fracture RQD value, m-m frequency, % n1-m frequency, % fractures/m fractureslln 3-26 4.6 >89. 147-148 12. 56. 26-66 1.9 96.5 148-167.4 1. 66-119 1.3 99. 167-189 2.1 97.3 119-135 4.1 92.8 189-233,54.7 97.5 135-147 1.3 99. One zone of strongly fractured rock was intersected in each borehole. In the borehole OL KR15B, there is a fracture-structured zone between 3.3 and 3.78 m and a crush-structured zone in OL-KR15 between 148.22 and 148.66 m. The total thickness of fracture zone is 1.19 m which is.5% of the drill core length. Fracture zones are presented in Appendix 8.11. 4.4 Core discing Neither of the drill core shovved evidence of core discing.
23 4.5 Strength and elastic properties Samples for testing the strength and elastic properties of the rock were taken every 3 m and in places where the major rock type changed. In total nine samples were tested, eight from the borehole OL-KR15 and one from the borehole OL-KR15B. This accounts five mica gneiss samples and four granite samples. One bend test and two point load tests were done from each sample. Differences in measurements result from the variability in the foliation intensity and grain size. The uniaxial compressive strength of the rock types is slightly different. The mean uniaxial compressive strengths of the mica gneiss and granite are 141 MPa and 167 MPa, respectively. This indicates that the mica gneiss is 16% weaker than granite. Elastic modulus of the rock types has larger variation. The average elastic modulus of the mica gneiss samples is 51 GPa and granite sample 42 GPa, i.e. the elastic modulus of the granite is 18% smaller than the elastic modulus of the mica gneiss. The rock mechanical test results are presented in Table 4, in which the mean strength and elastic properties are presented for each rock type. Uniaxial compressive strength, Young's Modulus and Modulus of Rupture of each rock type versus depth are shown in Figure 5. CU' 2,.eo.. g, 175, Cl) t/) b ::::s t/) :; 15, CI)"C. 125,...-----------.----------------.- 4, 35,... cu.. 3, :::\!! 25, :::\E... 5 c. t/) t/) en 1, 2, /... E 75, CJ>. -..... - -, 15, 5, --- lr. 1, -6 25, 5,, +-----+-----1------+-----+------+-,, 5, 1, 15, 2, 25, ----------------------------Pth[m] Young's Modulus (GPa] Uniaxial compressive strength [MPa] - -.A- Modulus of Rupture [MPa] -Cl) :::!: Figure 5. Uniaxial compressive strength, elastic modulus, and Modulus of Rupture versus depth. Mica gneiss is shown as black symbols and granite as red symbols.
Table 4. Summary of rock mechanical tests. Elastic modulus (E), Poisson's ratio (v), point load index (Isso), uniaxial compressive strength (crc) and Modulus of Rupture (Smax). 24 Depth E V Is so Is so O"Cl O"cz Smax Rocktype m GP a MP a MP a MP a MP a MP a 32, 34,19,16 7,25 6,29 173,92 15,96 12,82 GRAN (OL-KR15B) 46, 55,17,16 5,47 6,45 q1,17 154,87 11,41 GRAN (OL-KR15) 75,3 37,27,26 6,78 6,16 162,69 147,79 11,2 GRAN (OL-KR15) 13,7 39,93,25 8,7 8,57 28,85 25,68 13,39 GRAN (OL-KR15) 117, 38,53,21 5,48 5,38 131,42 129,22 14,8 MGN (OL-KR15) 144,2 36,75,31 4,76 4,7 114,32 97,71 12,92 MGN (OL-KR15) 171,2 6,26,29 6,32 6,53 151,69 156,82 24,8 MGN (OL-KR15) 2,4 4,72,23 4,87 4,83 116,76 ll6,3 11,74 MGN (OL-KR15) 221,8 77,79,32 7,81 8,87 187,36 212,76 13,18 MGN (OL-KR15) average 46,73,24 6,37 152,78 13,87 median 14,64,6 1,43 34,27 3,95 All together median% 31% 24% 22% 22% 28% average 5,81,27 5,89 141,41 15,2 median 17,8,5 1,5 36,4 5,3 MGN median% 35% 18% 25% 25% 33% average 41,64,21 6,96 166,99 12,21 median 9,32,6 1,15 27,7 1,7 GRAN median% 22% 27% 17% 17% 9%
25 5. MONITORING RESULTS 5.1 Electric conductivity of drilling and returning water During the drilling of the boreholes OL-KR15 and OL-KR15B, the electric conductivity of drilling water and returning water was monitored. The conductivity of each drilling water batch was measured after mixing the label agents. The conductivity of the drilling water batches varied between 14.... 16.2 ms/m. The full results are presented in Appendix 8.14. Electric conductivity of the returning water of the borehole OL-KR15B varied from 16.1 to 28.3 ms/m. Variation of the conductivity of the OL-KR15 returning water was larger and it was from 18.8 to 229. ms/m. The highest conductivity values were measured while drilling at depth 77 m. The results are presented graphically in Figure 6. Electric conductivity 25. 2. E en E 15. 1. 5.. - 2 4 6 8 1 12 14 16 18 2 22 24 Depth m Figure 6. Electric conductivity of returning water from the boreholes OL-KR15 and OL KR15B. 5.2 Quantities of drilling and returning water During the drilling of the borehole OL-KR15, 99.4 m 3 of water was used. After the drilling was finished, the borehole was flushed with 7. m 3 of water. During the drilling and flushing, 53. m 3 of returning water was measured. This is about 5% of the drilling and flushing water. Some water went past the flow meter during the air lift pumping and lifting of the drill rods.
26 During the drilling of the borehole OL-KR15B, 15.5 m 3 of water was used. After the drilling was finished, the borehole was flushed with 1. 7 m 3 of water. During the drilling and flushing, 5.6 m 3 of returning water was measured. This is about 32% of the drilling and flushing water. Some water went past the flow meter during the lifting of the drill rods. The cumulative consumption of drilling water and the amount of measured returning water are shown in Figure 7. :i: Drilling water -Returning water - ---- -----. -------- 12 1 8 G) -Q) E 6 :c ::s 4 2 Drilling and returning water 2 4 6 8 1 12 14 16 18 2 22 24 Depth m - ----- -- - ----- ----- -- --- -- Figure 7. Cumulative consumption of drilling water and amount of returning water during the drilling ofboreholes OL-KR15 and OL-KR15B. 5.3 Drilling water pressure During the drilling of the borehole OL-KR15 the drilling water pressure increased quite steadily with depth. At the beginning of the borehole pressure was.2 MPa and at the end it was 1.2 MPa. The pressure varied between.5 MPa and.8 MPa during the drilling of the borehole OL KR15B. The pressure graphs are presented in Figure 8.
I 27 Pressure of drilling water 1.4 1.2 i---- ---------! 1. i- -------- C. osj V\ T. :;.61- - lj... I.4 j!.21 I. - 2 4 6 8 1 12 14 16 18 2 22 24 Depth m.--- Kuva 8. Drilling water pressure during the drilling of the boreholes OL-KR15 and OL-KR15B. 5.4 Groundwater level in the borehole Groundwater level in the borehole OL-KR15 varied between 1 to 12 m. The result depends strongly on the stabilising time before measurements. The groundwater depth is measured from the ground surface. 5.5 Drilling cuttings yield Drilling cuttings was collected in a sedimentation tank and measured. From the borehole OL KR15, 99 litres of water drilling cuttings mixture was collected. The borehole diameter is 76 mm and the core diameter is 52 mm, 2.47 litres of rock per metre was ground to drilling cuttings by the diamond bit. Consequently, the total drilling cuttings generated was 48 litres. If the expansion factor 1. 7 of wet cuttings is assun1ed, the yield would be about 82 litres. Therefore, it can be speculated that the water content in drilling cuttings was higher, or the additional drilling cuttings was generated from the fractures. However, the result indicates that there cannot be significant amount of drilling cuttings residue in the borehole. From the borehole OL-KR15B, 12 litres of drilling cuttings water mixture was collected. The generated drilling cuttings during drilling was 1 litres and with the expansion factor 1. 7, the
28 yield should have been 17 litres. This indicates that about 3% of the drilling cuttings was left in the fractures intersected in the borehole. 5.6 Drilling water and returning water label agent concentrations The concentration of the label agent is used to estimate the representativeness of the groundwater samples taken from the borehole. The planned label agent concentration of the drilling water was.5 g/m 3 The achieved concentrations were close to this level. However, in the drilling water batch 2, the concentration was slightly lower,.449 g/m 3 It is possible that some of the chemical was left in the vial. The label agent mixings, drilling water samples, electric conductivity and uranine concentrations are listed in Appendix 8.12. Returning water samples were collected once a day as long as water was flowing from the borehole. In total, 1 samples were taken. High uranine concentrations in the returning water indicate that the water is mainly drilling water. At the depth of 16 m uranine concentration dropped indicating increase of groundwater flow into the borehole. Concentrations in the returning water varied from 14 to 435 J.lg/1. The analysis of uranine concentrations are presented in Appendix 8.13.
29 6.SUMMARY Finnish parliament ratified the policy decision and Posiva Oy can concentrate its geological investigations for the underground final disposal facility for spent fuel in the Olkiluoto area in the municipality of Eurajoki. Within next few years, an underground rock characterisation facility, ONKALO, will be built in the area. As a part of the investigations, Suomen Malmi Oy core drilled a 233.54 m deep borehole in the area. The borehole identification is OL-KR15. Because the precollar for the borehole OL-KR15 was done by down the borehole percussion drilling, a second diamond borehole OL-KR15B was drilled next to it. Length of the OL-KR15B is 45.6 m. The core was acquired using a triple tube core barrel with a split inner sample tube. During the drilling, the electric conductivity of drilling and returning water, drilling water pressure and the amounts of drilling and returning water were monitored. The monitoring was aimed to get additional information of the bedrock quality. The electric conductivity of the drilling water and returning water in OL-KR15 varied from 14. to 16.2 ms/m and from 16.1 to 229. ms/m, respectively. The drilling water pressure was at the beginning of the borehole OL-KR15.2 MPa and increased quite linearly with the depth to 1.2 MPa. The drilling water pressure in the borehole OL-KR15B varied from.5 to.8 MPa. Drilling water used was marked with uranine as the label agent. During the drilling of the borehole OL-KR15, about 16 m 3 of water was used. The amount of returning water was about 53 m 3 During the drilling of the borehole OL-KR15B, about 17 m 3 of water was used and 6m 3 returning water was measured. After the drilling, borehole OL-KR15 was flushed by pumping about 14 m 3 of water from the bottom of the borehole. For the flushing of the borehole OL-KR15B, about 16 m 3 of water was used. The deviation of the borehole was measured with EZ-Shot survey tool. Based on the results, at 233 m depth the borehole OL KR15 has deviated 17.95 m to NW and.63 m up from the target. Uniaxial compressive strength, Young's modulus, and Poisson's ratio were determined from the core samples. The average uniaxial compressive strength is 152 MPa, Young's Modulus 47 GPa and Poisson's ratio.24. Rock types intersected in the boreholes are migmatitic mica gneiss and granite. Rocks are unweathered or only weakly weathered. Filled fractures are the most common fracture type. The average fracture frequency in the borehole OL-KR15 is 1.55 fractures per metre and in OL-KR15B 3.33 fractures per metre. Mean RQD values of the boreholes OL-KR15 and OL KR15B are 97.7% and 93.7%, respectively. 27 fractures with slickensides, six grain filled and 15 clay filled fractures were intersected in the boreholes. One strongly fractured zone was intersected in both boreholes. The total thickness of these zones is 1.19 m which is.5% of the core. There was no core discing observed.
3 7. REFERENCES Barton, N & Choubey, V., 1977. The shear strength of rock joints in theory and practice. Teoksessa: Rock Mechanics 1, s. 1-54. Springer-Verlag. Gardemeister, R., Johansson, S., Korhonen, P., Patrikainen, P., Tuisku, T. & Vahasarja, P. 1976. Rakennusgeologisen kallioluokituksen soveltaminen. VTT Julkaisusarja, Tiedonanto 25. ISRM. 1981. Suggested Methods for Determining the Uniaxial Compressive Strength and Deformability of Rock Materials. In Rock Characterization Testing & Monitoring. Oxford, Pergamon Press. s. 113-116. ISRM. 1985. Suggested Method for Determining Point Load Strength. International Journal Rock Mech. Min. Sci. & Geomech. Vol. 22, no 2. S. 51-6. Korhonen, K-H., Gardemeister, R., Jaaskelainen, H., Niini, H. & Vahasarja, P. 1974. Rakennusalan kallioluokitus. VTT Julkaisusarja, Tiedonanto 12. Laurila, T. 1998. The comparison of the deviation survey methods and corrections to results at work sites ofposiva in 1997 (in Finnish). Tyoraportti-98-5. Niinimaki, R. 21. Core drilling of deep borehole OL-KR14 at Olkiluoto in Eurajoki 21 (in Finnish). Tyoraportti 21-24. Saltikoff, B. 1972. Mineraalinimisanasto. Espoo, Geological Survey of Finland. Report of Investigation N:o 11 (in Finnish). 82 pages. ISBN 951-69-44-5.
31 Time schedule Appendix 8.1 Item October!November 42 43 44 45 46 47 Down-the-hole drilling/ casing setting Borehole OL-KR15 Move to the hole Drilling 4-233 m Deviation measurements, borehole flushpumping Borehole OL-KR15B Move to the hole Drilling - 45 m Direction/dip measurements, borehole flushpumping
33 Drilling equip1nent Appendix 8.2 Item Quantity 1. Core drilling equipment - Diamec 1 S 1 pc - Royal Bean -pump, suckfilter CT -I 2 I pc - Alu 72 -drill rods 25m -Triple tube core barrel, WL-76 6 pc - Drill bits, WL-7 6 8 pc - Reamers, WL-7 6 2 pc - Casing 84/77 5 m - Casing 9/77 8m - Casingshoe 9/77 1 pc - Valve equipment I pc -Electric centrale 1 pc -Tools etc. 2. Flushing water equipment - Water container 5 m 3 I pc - Water container 3 m 3 2 pc - Compressor 1 pc - Waterpump 3 pc - Water amount counter 6pc - Sedimentation pool 1 pc - Submersible pump, diameter. 48 mm 1 pc - Pneumatic hose 17m -Water line 3m - Water level measuremant 1 pc 3. Auxiliary equipment - Office container 1 pc - Rest container 1 pc -Storage 1 pc - Mobil phone I pc 4. Accessories -Core boxes 4 pc - Label agent 3 pc 5. Measurement equipment - Conductivity measurement 1 pc - PP-dip inclinometer I pc - EZ Shot - survey tool 1 pc 6. Reporting equipment -Computer 1 pc - Examination instruments 1 serie -Rock Tester -instrument 1 pc
34 Drilling equipment Appendix 8. 2._, -. \... C:i - -- \\== : 1= : LF; (J- -= _-_-jj \j /I \ ) -----,- ----- C.'! \ / / WL-76 triple tube core barrel
Appendix 8. 3 CONSTRUCTION OF THE UPPER PART OF THE HOLE OL-KR15 Z - to of the casing ( center of the casi ) (...)..c.... ) c Q) ttr: Cl. L? Cl. Cl. (j Cl) Cl) Q) c () L? (j ls (j...c.... ) c Q) 1? 1? lj lj DIMENSIONS Z - ground level = +8,42 m Z- top of the casing = +8,82 m (V) or- or- ) c (/) ro (...) a= 3,6 m b= 4,12m c,4 m d = 233,54 m "..c... a. Q) " Q)..c
Appendix 8.3 CONSTRUCTION OF THE UPPER PART OF THE HOLE OL-KR15B Z - to of the casing ( center of the casi ).....c en c Q) L? CJ '''= CJ C:l. C:l. m CfJ CfJ Q) c - '''= L? '''= (j '''= '''=- '''= C:l. CJ CJ L? CJ C:l. [S (j L? CJ.. (j..c +-" ') c Q) C:l. DIMENSIONS Z- ground level= +8,35 m Z - top of the casing = +8,99 m a= 2,4 m b = 4,48 m c =,64 m d = 45,14 m 1'-- 1'-- ) ') c CfJ m u "'...c +-".. Q) "' Q)..c E E < 1'--
casing Is opened at three positions 11 os 2-3mm wide tracks casing RST 139. 7x2.6 25 mox.3 (X) m '$,... --- - - - -... - -- 1'-1- - -- - -1-1-- - - -- s. n.35.....c > c... -- - - V!X) v I") $ w -...) 12 1\.42 I Part I Drawlno number I 1 Name of tile part ar 1 Product code _,bfy crouo Generol toleronoea I Scole I Product 1:2 l::t u 8$- TERRA- TEAM OY rs= INOA Appr. kg I Stonclard I Fonn, model, quantity I Quality arllat Linked RST 1 Cone for 84/77 casing Prev. A/275 l New j Nr " (!) [ ;;:; w
39 Degree of weathering OL-KR15 Appendix 8. 4 Start End \Veathering degree Remarks 4.12 4.95 Rpl partly epidotized 4.95 46.85 RpO 46.85 47.54 Rpl partly epidotized 47.54 233.54 RpO
4 Degree of \veathering L-KR 15 B Appendix 8. 4 Start End Weathering degree Remarks 2.38 6.19 RpO 6.19 6.25 Rp2 6.25 41.66 RpO 41.66 42. Rp1 42. 45.14 RpO
41 Lifts, OL-KR15 Appendix 8.5 Lifts m Lifts, m Lifts, m Lifts, m Lifts, m 41.36 82.64 124.9 165.53 24.8 44.33 85.6 127.6 168.47 27.7 45.7 88.58 13.3 171.45 21.6 5.3 91.56 133. 174.44 21.38 53. 94.48 135.92 177.44 213.32 55.99 97.45 138.8 18.42 216.3 58.97 1.36 141.74 183.42 219.23 61.9 13.36 144.73 186.35 222.23 64.85 16.29 147.67 189.32 224.52 67.79 19.27 15.63 192.27 227.37 7.72 112.23 153.61 195.19 23.29 73.69 115.23 156.61 198.16 233.27 76.66 118.18 159.58 21.13 233.54 79.65 121.14 162.57
42 Lifts, OL-KR15B Appendix 8.5 Lifts, m 5.8 7.75 1.69 13.65 16.61 18.59 21.51 24.53 26.94 27.66 3.61 33.48 36.45 39.41 42.38 45.6
----------------------- - 43 List of coreboxes, OL-KR15 Appendix 8. 6 Number Section, m - m Number Section, m - m 1 4.12-44.47 25. - 142.5 2 44.47-48.87 26 142.5-146.56 3 48.87-53. 27 146.56-15.1 4 53. - 56.71 28 15.1-154.19 5 56.71-6.82 29 154.19-158.74 6 6.82-64.85 3 158.74-162.57 7 64.85-68.78 31 162.57-166.27 8 68.78-72.79 32 166.27-17.5 9 72.79-77.8 33 17.5-174.44 1 77.8-81.29 34 174.44-178.58 11 81.29-85.6 35 178.58-183.22 12 85.6-9.6 36 183.22-187.31 13 9.6-94.48 37 187.31-191.54 14 94.48-99.2 38 191.54-195.27 15 99.2-13. 39 195.27-199.67 16 13. - 16.23 4 199.67-24.8 17 16.23-11.44 41 24.8-28.18 18 11.44-114.71 42 28.18-212.92 19 114.71-118.72 43 212.92-217.4 2 118.72-122.9 44 217.4-222.7 21 122.9-127.6 45 222.7-226.24 22 127.6-13.3 46 226.24-23.29 23 13.3-133.82 47 23.29-233.54 24 133.82-138.21
44 List of coreboxes, OL-KR15B Appendix 8. 6 Number Section, m - m 1 3.28-6.44 2 6.44-1.27 3 1.27-14.45 4 14.45-18.45 5 18.45-22.45 6 22.45-26.29 7 26.29-3.2 8 3.2-34.36 9 34.36-38.3 1 38.3-42.38 11 42.38-45.14
Main rock type Minor subdivisions Start End Start End m m m m 4.12 113.2 113.2 233.54 45.93 47.14 56.56 62.4 68.97 67.1 72.36 72.38 89.13 96.32 111.54 113. 113.97 114.71 127.48 127.65 128.3 169.35 179.44 194.17 189.97 19. 192.2 192.54 223.24 229. 227.93 228.2 229. 233.54 23.37 23.72 Rock type GRAN MGN MGN MGN GRAN Description Medium-grained and coarse-grained granite. Colour varies from gray to reddish bro\\tn. The main minerals of the granite are feldspar group (potassimn feldspar and plagioclase ), quartz and biotite. In the granite occurs mica gneiss sections and restites of granitized mica gneiss. Sulfides () occures in mica gneiss. Son1e pinite grains occures in coarse-grained granite. Mica gneiss with some granite sections. Quartz vein Perthite Mica gneiss with some granite sections. In coarse grained granite occurs some quite big grains of perthite and pinite. Micmatic mica gneiss with some granite sections. The main minerals of the mica gneiss are biotite, feldspar group (potassium feldspar and plagioclase) and quartz. Some sulfide and little coverns (1-2 mm) Little cavern with crystlas (e.q. ) Quartz rich section A little cavern in granite section Amount of granite is quite high. Thin layer which have in both contacts 2-3 mm wide vein. Veins are light gray coloured. Some pertihite grains in coarse grained granite. In granite occurs some sections with light coloured flame texture. Some parts/grains are slightly green colored. Some grains of perthite. Amount of granite is about as same as gneiss In granitic section light/gray coloured flame texture.. tll (") ::L ".-.. g -v. > " "C$ ::s.. ;<.j:;;:. Ut
Main rock type Minor subdivisions Rock type Start End Start End m m m m 2.38 13.57 GRAN 13.57 28.46 MGN 28.46 41.5 GRAN 41.5 45.14 MGN Description Mainly coarse-grained red coloured granite with mica gneiss sections. Core sample starts with about 1 meter wide mica gneiss section. In coarse-grained granite occurs micro fractures. Migmatic mica gneiss with some granite sections. Medium-grained and coarse-grained granite. Colour varies from gray to reddish brov.11. In the granite occurs son1e mica gneiss sections and restites of granitized 1nica gneiss. Gneiss with granite sections Q.. ('t) (IJ (") ::1. 'S s? -VI tx1 -+:-. \ > '" '" ('t) ::s Q.. -...J
-------------------------------- 47 Foliation, OL-KR15 Appendix 8.8 Examination section Rock Foliation Degree of Remarks Start (m) End (m) type angle e) foliation On site core orientation is not possible on vertical boreholes 4,12 113,2 GRAN Granite with mica gneiss sections. Granite -1, gneiss 1-2. 44,7 MGN 55 2 Mica gneiss section in granite 6,5 MGN 4 2 Mica gneiss section in granite 93,7 MGN 6 2 Mica gneiss section in granite 113,2 233,54 MGN Micmatic mica gneiss with granite sections. Gneiss 1-2, granite -1. 118, MGN 6 2 127,45 MGN 7 2 137,8 MGN 7 2 146,3 MGN 5 2 151, MGN 65 2 159,3 MGN 6 2 163,95 MGN 7 2 17,15 MGN 55 2 185,3 MGN 8 2 194,45 MGN 5 2 21,8 MGN 55 2 28,2 MGN 6 2 216,15 MGN 5 2
48 Foliation OL-KR158 Appendix 8.8 Examination section Rock Foliation Degree of Remarks Start (m) End (m) type angle ( ) foliation On site core orientation is not possible on vertical boreholes 2,38 13,57 GRAN Granite with mica gneiss sections. Granite -1, gneiss 1-2. 3,4 MGN 5 2 Mica gneiss section in granite 13,57 28,46 MGN Migmatic mica gneiss. Gneiss 1-2, 16, MGN 55 2 25,45 MGN 5 2 27,5 MGN 5 2 28,46 41,5 GRAN Granite with some mica gneiss sections. Granite -1, gneiss 1-2. 33,95 GRAN 5 1 41,5 45,14 MGN 44,75 MGN 4 2
I 35 Fracture Start End Type Fracture Colour of number depth depth angle fracture m m () surface l 4.65 clfi 35 lgra 2 41.7 fi 3 lgra 3 41.11 fi 4 1gra, whit 4 41.93 fi 7 whit 5 42.46 fi 5 \Vhit 6 43.7 fi 45 lgra 7 43.11 fi 35 whit 8 44.4 fi 65 1gra 9 44.48 fi 7 1 44.9 fisl 3 blac, gray 11 44.96 fisl 3 gray, blac 12 45.77 fi 1 blac, gray 13 46.9 fi 55 gray 14 46.95 fi 1 lgree 15 47.2 fi 7 white 16 47.98 fi 6 whit 17 48.51 fi 65 whit, lgree 18 49.1 ti 6 white 19 49.65 fi 55 gray 2 49.86 fi 7 gray 21 49.88 fi 5 dgre 22 51.1 fi 75 gray 23 51.88 ti 4 24 54.3 ti 35 25 54.49 fi 2 gbro 26 54.88 fi 6 b1ac 27 54.97 fi 7 28 55.2 fi 55 gray 29 55.37 fi 55 lgra 3 55.6 fi 45 whit, gray 1 56.4 ti 5 32 56.16 ti 25 33 56.33 fi 7 dgre 34 56.67 fi 75 whit 56.71 fi 6 blac, gray 36 57.12 ti 6 Fracture Thickness Fracture filling of filled shape fracture clay 1 carb.5 carb, su1f lite carb 1 lite carb, su1f carb carb 1 lite carb, su1f lite sulf clor, carb carb, clor, sulf carb 1 sen carb, su1f carb, sulf lite carb, sulf lite carb lite sulf sulf su1f lite sulf sulf sulf carb, su1f carb, sulf 1 plan carb, sulf 1 plan cl or plan Fracture hness smoo smoo Remarks mainly splitted some crystals c... q-. (") 2 >-I (l; v(.ll r---' VI > ' ' (l; ::l ;;, \.+:-. \.
I Fracture Start End Type Fracture Colour of number depth depth angle fracture m m () surface 37 58.57 fi 65 gray, whit 38 58.7 fi 5 39 59.28 fi 5 blac, gray 4 59.59 fi 7 gray 41 6.16 fi 45 blac 42 6.22 fisl 45 blac, lgra 43 6.83 ti 35 44 61.66 fi 9 lbro 45 61.96 fi 8 whit 46 62.4 fi 7 blac, whit 47 62.78 fi 4 whit 48 63.46 fi 65 gray 49 64.72 fi 8 blac, dgra 5 64.74 fi 85 dgre, blac 51 66.13 ti 7 52 66.17 ti 5 53 66.25 fi 35 gray 54 66.49 ti 5 55 66.51 ti 8 56 69.13 fi blac, gray 57 7.3 fi 35 gray 58 7.1 fi 3 blac, gray 59 7.94 fi 4 dgra 6 71.38 ti 45 61 71.49 ti 75 62 72.36 fi 85 whit 63 75.69 fi 3 lgree, gray 64 77.76 fi 75 whit 65 78.55 fi 8 whit 66 78.58 fi 7 whit 67 78.7 fi 25 gray, blac 68 79.27 clfi 4 gray 69 79.46 fisl 5 lgra 7 79.49 fi 35 lgra 71 81.63 fi 6 \Vhit Fracture Thickness Fracture filling of filled shape fracture carb 1.5 sulf plan carb, sulf plan sulf sulf plan carb, sulf plan sulf carb, sulf sulf kaol carb.5 plan carb, mica 1 carb, sulf.5 carb, sulf sulf carb, sulf 1 carb carb, sulf plan carb, sulf plan carb carb, mica plan clay, carb, mica carb, mica CUIY mica, carb k:aol 1 Fracture hness smoo smoo smoo smoo smoo smoo - Remarks some crystals some crystals parly, filling -1 mm, undulating splitted, also fisl r--'...,..., 2 (1J "C/l r--' to Vl >- '" '" (1J [ ;:;: VI
I Fracture Start End Type Fracture Colour of number depth depth angle fracture m m CO) surface 72 84.21 ti 7 73 84.58 fi 8 dgra 74 84.72 fi 7 gray, whit 75 85.8 fi 7 lbro 76 86.13 ti 6 77 86.31 ti 7 78 87.4 fi 7 whit 79 88.44 fi 6 lgra 8 9.52 fi 4 gray 81 91.8 fi 8 lgra 82 91.22 fi 75 lgra 83 91.29 fi 75 lgra 84 92.79 ti 2 85 93.8 ti 7 86 93.72 ti 5 87 94.32 ti 55 88 95.57 fi 6 gray 89 95.77 fi 6 lbro 9 95.82 ti 75 91 95.85 fi 6 blac, whit 92 97.46 fi 8 gray, whit 93 1.82 fi 7 94 11.94 ti 45 95 12.14 fi 45 gray 96 12.53 fi 5 gray 97 13. fi 5 gray 98 13.1 ti 6 99 13.34 ti 35 1 14.6 fi 35 whit 11 15.9 ti 5 12 17.17 fi 55 lbro 13 17.7 fi 75 whit, lbro 14 17.85 fi 85 whit, lbro 15 18.94 ti 3 16 19.5 ti 75 17 19.53 fisl 6 ggra -- Fracture Thickness Fracture filling of filled shape fracture sulf sulf, carb sulf plan lite carb, sulf carb carb, sulf sulf, carb carb carb, sulf lite lite sulf plan sulf carb plan carb, sulf lite carb, sulf carb carb, sulf carb, sulf sulf carb, sulf carb, sulf klor CUI\ 1 lite plan plan lite Fracture hness smoo Remarks some crystals partly mostly splitted, r...., ::p P-l n 2..., (D V(/) r---' Id VI >- '" '" () ;:l ;;, \[) Vt
I I Fracture Start End Type Fracture Colour of number depth depth angle fracture m m CO) surface 18 111.45 ti 65 19 112.6 ti 65 11 112.42 ti 111 113.18 ti 3 112 113.86 fi 5 whit, cray 113 114.71 clfi 7 gray 114 114.88 ti 4 115 115.21 fi 4 lgra 116 116.3 ti 6 117 117.51 ti 5 118 117.66 fi 4 blac, lgra 119 118.7 fi 5 gray 12 118.72 fi 55 gray 121 119.9 fi 4 lbro 122 119.11 fi 65 gray 123 119.22 clfi 4 blac, gray 124 119.27 ti 35 125 119.29 fisl 25 blac, lgra 126 119.34 fi 6 lgra 127 119.8 ti 2 128 119.9 fi 4 1gra 129 119.97 fi 55 gray 13 12.66 fi 6 lgra 131 12.74 fi 6 b1ac 132 121.31 fi 5 dgra, gray 133 121.75 grfi 65 gray, blac 134 122.28 fi 6 dgra 135 122.36 fi 6 gray, dgra 136 123.8 fi 75 gray, blac 137 123.34 fi 65 gray 138 123.37 ti 6 139 123.46 fi 7 dgra 14 124.76 fi 75 dgra 141 125.3 fi 6 dgra 142 125.14 fi 6 dgra 143 125.32 fi 3 blac, dgra Fracture Thickness Fracture filling of filled shape fracture irrc kaol, sulf clay carb, sulf plan carb, sulf carb, sulf.5 carb, sulf.5 carb litc litc clor, carb carb.5 varb, sulf plan carb 1 carb lite 7 lite plan sulf lite sulf plan sulf sulf 1 Fracture hness smoo smoo Remarks clay with sandy material some crystals also fis1 crushed rock, not picked up t--< I-+; (') 2 1-i Y' r ;N Vo > :g ('t ;:I ;;, oc \ Vo t-...j
I Fracture Start End Type Fracture Colour of number depth depth angle fracture m m () surface 144 125.79 fi 55 with, blac 145 125.85 fi 8 lbro 146 125.99 fi 6 lbro 147 126.28 fi 6 ggra 148 126.62 fi 4 with, gray 149 127. fi 2 dgra 15 127.9 fisl 4 blac, gray 151 127.14 fi 2 with, lbro 152 127.29 ti 65 153 127.38 ti 8 154 127.4 ti 75 155 127.56 fi 8 dgra 156 127.6 fi 9 gray, whit 157 127.79 ti 75 158 128.3 fi 75 dgra 159 128.89 fi 6 gray 16 129.27 fi 7 gray 161 129.35 fi 4 b1ac, gray 162 129.54 ti 3 163 129.7 fi 65 1bro, whit 164 129.84 1i 8 gray 165 129.91 fi 6 dgra 166 129.94 fi 3 gray 167 129.99 fi 8 lbro 168 13.26 ti 6 169 13.43 fis1 2 blac, lbro 17 131.51 fi 5 1bro 171 131.56 fisl 5 blac 172 131.67 fi 8 gray 173 131.69 fis1 4 blac 174 132.21 fi 8 gray 175 132.29 fi 5 lbro 176 132.41 fi 35 whit 177 132.51 fi 25 whit 178 133.55 fi 7 lbro, whit 179 133.67 fi 8 lbro Fracture Thickness Fracture filling of filled shape fracture kaol, sulf plan sulf sulf lite sulf kaol, sulf carb lite clor, carb kaol, sulf lite sulf lite kaol trre su1f lite sulf lite carb, sulf litc su1f litc carb carb, sulf.5 sulf, carb.5 sulf sulf, grap sulf lite sulf lite sulf sulf lite sulf lite su1f kao1 kao1 litc sulf, kao1.5 litc su1f Fracture hness smoo smoo Remarks little covem, little covem, little covem, little covem, partl:y' little covem, partly r c... ql p;l c -I (1) "[/l r?:l U1 )> " "d (1) ::J p.. ;:;, '- U1 vj
i I Fracture Start End Type Fracture Colour of number depth depth angle fracture m m () surface 18 133.82 fi 8 lgra 181 134. ti 6 182 134.46 fi 8 gray, \Vhit 183 134.7 fi 7 dgra 184 134.88 fi 45 gray 185 135.72 fisl 35 blac 186 135.72 fisl 65 blac 187 137.5 ti 55 188 138.8 fi 65 lgra 189 14.48 ti 2 19 14.73 fi 35 gray, whit 191 141.61 fi 75 gray, lbro 192 141.88 fi 7 blac 193 142.11 fi 8 dgra 194 143.77 fisl 4 blac 195 144.99 ti 2 196 146.66 ti 6 197 146.79 fl 45 whit 198 147.39 fi 55 blac 199 147.48 grfi 6 gray, blac 2 147.62 fi 6 dgra 21 147.96 ti 6 22 148.22 fi 5 dgra 23 148.28 fi 5 dgra 24 148.33 fisl 25 blac 25 148.4 148.63 26 148.66 fisl 35 blac 27 149.47 ti 65 28 15.11 ti 35 29 157.83 ti 4 21 159.8 ti 5 Fracture Thickness Fracture filling of filled shape fracture carb, sulf sulf, kaol grap, sulf grap, sulf plan carb, sulf litc carb, sulf sulf sulf sulf sulf kaol, carb sand, clay 1 plan grap plan plan Fracture hness smoo smoo smoo smoo smoo smoo smoo smoo Remarks little covem, a little clay A section with clay and grain filled fractures. Shear zone. About 8 fractures, one clay filling about 15 nun, widest filling varies 3-5 mm. Sample not picked up. I c: ;!;.......,,... 2. (D y;, c- ::: Ul )> ' ' (D ::l ;;, 'D Ul #
Fracture Start End Type Fracture Colour of number depth depth angle fracture m m () surface 211 161.35 ti 5 212 164.41 fisl 4 blac 213 164.71 fi 45 gray, whit, lbro 214 166.27 ti 4 215 167.26 fi 5 gray, whit 216 167.34 ti 4 217 167.62 ti 45 218 167.81 ti 65 219 167.87 fi 4 whit 22 169.31 ti 65 221 169.55 fi 2 lgre, blac 222 169.72 fi 5 lbro, blac 223 169.85 fi 5 224 169.95 fisl 35 dgra 225 17.6 fi 5 with lgra 226 17.29 fisl 55 blac 227 17.44 fi 5 gray, blac 228 171.53 fi 2 whit 229 172.1 fi 35 dgra 23 173.2 ti 7 231 174.12 fisl 3 blac 232 174.19 fisl 25 blac 233 174.27 ti 6 234 174.62 fi 6 gray, lbo 235 174.91 fi 55 whit, blac 236 176.94 fi 15 blac, whit 237 177.36 ti 7 238 177.48 fi 6 lbro, blac 239 177.54 fi 15 lbro, blac 24 177.67 fi 55 dgra 241 178.41 ti 55 242 179.62 fi 6 whit 243 18.81 fi 6 whit 244 181.27 ti 6 245 181.38 ti 45 246 181.59 ti 6 Fracture Thickness Fracture filling of filled shape fracture carb, sulf kaol lite lite carb, sulf sulf carb.5 plan carb 1 litc grap plan grap lite plan carb, sulf.5 carb.5 litc plan sulf plan sulf plan kaol litc kaol plan Fracture hness smoo smoo smoo smoo smoo Remarks some crystals crystals l"' -... J n 2 VC/) l"' Id Vt )> '"d '"d ::l.. - Vt v.
I l"'ract ure Start End l'ype Fracture Colour of number depth depth angle fracture m m () surface 247 182.73 fi 7 whit 248 184.26 fi 7 whit 249 184.35 fi 6 dgra 25 184.78 ti 1 251 184.89 fi 7 gray, 1bro 252 185.86 ti 4 253 186.59 fi 8 dgra, whit 254 187.31 fi 45 gray 255 188.24 ti 2 256 188.44 ti 65 257 188.57 fi 9 whit 258 188.6 ti 7 259 188.78 fi 1 lgra, b1ac 26 188.81 ti 7 261 189.31 fi 7 dgra, 1bro 262 19.3 fi 7 lgra 263 19.16 fi 8 \:Vhit 264 19.47 ti 6 265 191.54 fi 5 blac, lbro 266 192. ti 7 267 193.2 fi 75 whit, lbro 268 196.38 fi 4 dgra 269 197.18 ti 2 27 2.7 fi 35 whit 271 2.81 fi 7 lgra 272 21.3 ti 75 273 216.98 ti 4 274 217.51 fi 4 gray, lbro, whit 275 22.73 fi 7 lbro 276 22.89 fi 7 gray 277 221.44 fisl 35 blac 278 221.55 ti 6 279 223.1 fisl 5 blac 28 223.11 fi 55 lgra 281 223.7 ti 2 282 224.91 ti 35 Fracture Thickness Fracture filling of filled shape fracture kaol kaol lite lite sulf plan kaol, sulf carb, sulf lite lite carb, kao1 lite sulf, carb carb lite sulf.5 plan kaol, sulf plan sulf lite carb, kaol, sulf carb lite lite sulf sulf sulf plan carb Fracture hness smoo smoo smoo smoo Remarks little cavern, crystals partly small crystals partly l' - c '""'i r, E '-! (i) (f, r :;:d VI ' g. - \D VI \
Fracture Start End Type Fracture Colour of number depth depth angle fracture m m () surface 283 225.28 ti 5 284 226.46 fi 2 lgra 285 227.35 fi 55 whit 286 227.54 ti 5 287 227.62 fi 4 dgra 288 227.64 fi 8 gray 289 228.39 ti 75 29 228.51 fi 5 lgre 291 228.89 ti 45 292 23.28 ti 7 293 23.95 fisl --- _]_J L_ blac - Fracture Thickness Fracture filling of filled shape fracture carb, sulf 1.5 kaol sulf irrc mica, quar 3 lite grap, sulf, carb Fracture hness smoo Remarks filling 1-2 nun, some crystals filling 1-12, r' -... ::::;< p (") 2 '""1 (!; "1:/l r' Vi Vt..._] >- ' u (!;.. ;;;: \
Fracture Start End Type Fracture number depth depth angle m m () 1 2.88 fi 7 2 3.3 ti 4 3 3.6 fi 5 4 3.1 fi 65 5 3.13 fi 6 6 3.21 fi 7 7 3.3 fi 75 8 3.34 fi 6 9 3.53 fi 5 1 3.57 fi 6 11 3.72 ti 6 12 3.76 fi 85 13 3.78 fi 9 14 4.2 fi 6 15 5.21 fi 7 16 5.24 ti 8 17 5.42 fi 65 18 5.46 ti 6 19 5.48 ti 35 2 6.1 ti 7 21 6.14 fi 8 22 6.22 clfi 8 23 6.24 ti 75 24 6.44 fi 7 25 6.59 fi 55 26 6.73 ti 1 27 6.86 fi 6 28 7.1 fi 5 29 7.27 fi 1 3 8.8 fi 7 31 8.44 fi 6 32 8.48 fi 6 33 8.77 fi 8 34 8.78 fi 9 35 8.8 fi 91 36 8.R2 ti 85 Colour of Fracture Thickness fracture filling of filled surface fracture lbro sulf lgra carb, sulf.5 whit carb, sulf \vhit, lbro carb, sulf 1 whit carb, sulf lgra carb whit, lbro carb, sulf whit, gray carb whit, lgre carb \V hit lgra \V hit carb 1 dgra dgra, whit ea rh gray clay 1 whit whit blac, lbro lbro blac, gray gray, lbro blac, lbro blac, lbro gray whit whit carb, kaol carb, kaol sulf sulf carb sulf sulf sulf Fracture shape litc lite litc plan rrre Fracture hness Remarks filling.5-2 mm, undulating,...,., :::t p.l :::: '""I r. er, r' ::... Vl t::o )> '1j '1j Cil c.. ;;:;: \.Q VI
Fracture Start End Type Fracture Colour of number depth depth angle fracture m m () surface 37 9.86 ti 7 38 1.14 fi 8 gray 39 1.63 fi 2 dgra 4 1.74 ti 7 41 1.76 ti 75 42 11.14 ti 75 43 11.56 fi 85 whit, blac 44 12.8 fi 65 gray 45 12.35 fi 65 dgra, blac 46 12.4 ti 8 47 12.48 ti 9 48 12.68 fi 7 whit 49 13.15 ti 65 5 13.2 ti 7 whit 51 13.3 ti 7 52 13.32 fi 9 \Vhit 53 13.41 fi 7 gray 54 13.48 fi 6 gray, whit 55 13.54 ti 75 56 13.84 ti 35 57 13.91 ti 6 58 14.66 ti 5 59 14.73 fi 7 whit 6 14.82 fi 6 blac 61 15.11 clfi 7 lgra 62 15.23 clfi 65 whit 63 15.25 clfi 7 whit 64 15.89 clfi 65 gray 65 15.91 clfi 7 gray 66 16.87 fi 65 lgra 67 17.16 ti 6 68 17.2 ti 45 blac, gray 69 17.3 ti 55 lgra, lbro 7 17.42 fisl 4 blac 71 17.74 ti 1 72 17.83 fi 5 gray Fracture Thickness Fracture filling of filled shape fracture plan lite lite litc litc carb 1 lite plan carb, sulf.5 litc carb.5 plan carb sulf carb 1 IITC carb 1 cl or 1 carb 1.5 1 2 carb litc carb, sulf carb, sulf litc lite carb, sulf Fracture hness smoo smoo smoo Remarks partly t r.h..., ::;> 2 (1) "'"" VVJ r-' 7;; U1 OJ > "'d "'d r. ::l \ U1 \
Fracture Start End T'pe Fracture Colour of number depth depth angle fracture m m () surface 73 17.94 fi 6 lgra 74 17.99 grfi 35 gray 75 18.46 grfi 75 gray 76 18.89 fisl 2 blac 77 19.38 fi 7 whit 78 19.83 fi 6 \:Vhit 79 2.4 fi 6 lgra 8 2.23 clfi 8 whit 81 2.33 fi 7 lgra 82 2.43 fi 7 whit 83 2.64 fi 65 lgra 84 2.87 fi 6 lgra, lbro 85 2.92 fi 4 whit 86 21.36 ti 3 87 21.56 fi 35 dgre 88 21.59 fi 6 whit 89 21.96 fi 6 dgra 9 22.5 fi 6 gray, dgra 91 22.21 ti 6 92 22.47 fi 4 lgra 93 22.67 fi 5 lgra 94 22.81 fi 6 gray 95 23.7 clfi 6 dgra 96 23.11 clfi 7 ggre 97 23.21 clfi 7 whit 98 23.27 fi 65 whit 99 23".77 grfi 4 blac 1 23.98 fi 3 lgra 11 24.11 ti 8 12 24.37 fi 4 dgra 13 24.83 clfi 3 blac 14 25. fi 3 gray 15 25.27 grfi 4 blac 16 25.31 clfi 6 dgra carb Fracture Thickness Fracture filling of filled shape fracture plan lite 3 3 kaol, sulf kaol, sulf carb, kaol 1 kaol.5 lite carb 1 litc lite carb 1 lite carb, sulf.5 lite cab, kaol, sulf CUf\' lite lite carb 1.5 lite carb, sulf irrc carb carb 1 carb carb, sulf 2 plan.5 plan kaol.5 plan plan carb litc carb plan carb 4 litc plan plan plan Fracture hness smoo smoo smoo smoo Remarks weathered fracture with mainly grained material and a little clay rock pieces, grained rock and clay between two slickensided fracture S' soe crystals splitted, not picked up L' -,...,., :::;> (') 2 (il rface Y' f2 Vo td )> "a "a (!) ;::l c.. ;;, oc \D \
Fracture Start End Type Fracture Colour of number depth depth angle fracture m m () surface 17 25.37 fi 3 gray 18 25.83 ti 7 19 25.91 fi 8 lgra 11 26.3 ti 3 111 26.47 fi 35 gray 112 26.6 fi 6 whit 113 27.32 ti 55 114 28.45 fi 6 whit, lbro 115 28.96 fi 6 ggre 116 29.4 fi 6 ggre 117 29.94 fi 4 dgra 118 29.99 fi 55 dgra 119 31. fi 8 blac 12 34.65 fi 7 lgra 121 35.4 fi 75 122 35.5 fi 75 gray 123 39.9 fi 6 gray 124 39.77 ti 45 125 39.89 ti 1 b1ac 126 41.36 fi 3 whit 127 41.46 fi 4 whit 128 41.71 fisl 35 b1ac, gray 129 41.86 fisl blac, gray 13 42.15 fi 1 grav 131 42.18 fi 4 whit 132 42.2 fi 35 lgra 133 42.59 ti 55 whit 134 42.74 fi 6 gray 135 42.98 fi 8 1gra 136 43.35 fi 6 gray, lbro 137 43.84 fi 4 lgra 138 44.15 ti 7 whit 139 44.55 ti 7 14 44.63 fi 8 gray 141 44.66 ti 85 142 45.4 fi 4 hlac, gray, lbro Fracture Thickness Fracture filling of filled shape fracture carb plan plan carb carb.5 sulf, kaol sulf lite lite sulf carb carb 1 carb lite plan carb carb carb carb carb 1 carb 1 lite carb 1 carb lite carb, sulf carb, sulf 2 plan carb litc carb.5 litc litc carb carb, sulf Fracture hness smoo smoo smoo Remarks mostly splitted also grfi undulating, splitted partly r,...,., :::;" p n 2 '"'1 (ll Cil l" (Cl Vl tu )> " " ::l ;;:: \!:) \
63 Fracture frequency and RQD, OL-KR 15 Appendix 8. 1 Start End All fractures Natural fractures RQD Remarks m m pc/m pc/m % 4.12 41 2 1 41 42 4 3 96 42 43 2 1 1 43 44 4 2 96 44 45 7 4 94 45 46 6 1 1 46 47 4 2 9 47 48 3 2 1 48 49 4 1 1 49 5 3 4 1 5 51 3 1 51 52 4 2 1 52 53 4 1 53 54 2 1 54 55 6 4 88 55 56 5 3 98 56 57 5 5 9G 57 58 2 1 1 58 59 7 2 1 59 6 2 2 1 6 61 7 3 94 61 62 3 2 1 62 63 2 2 1 63 64 4 1 loo 64 65 4 2 98 65 66 2 1 66 67 4 5 8G 67 68 3 loo 68 69 2 1 69 7 1 1 loo 7 71 6 3 93 71 72 2 2 1 72 73 6 1 1 73 74 3 1 74 75 3 1 75 76 3 1 1 76 77 6 1 77 78 2 1 1 78 79 5 3 97 79 8 14 3 97 8 81 1 1 81 82 2 1 1 82 83 5 1 83 84 1 1 84 85 2 3 1 85 86 3 1 1 86 87 4 2 1 87 88 3 1 1 88 89 7 1 1 89 9 1 1 9 91 3 l 1
64 fracture frequency and RQD, OL-KR15 Appendix 8. I Start End All fractures Natural fractures RQD Remarks m m pc/m pc/m % 91 92 7 3 93 92 93 1 1 1 93 94 3 2 1 94 95 5 1 loo 95 96 9 4 92 96 97 1 loo 97 98 5 1 1 98 99 1 1 99 1 2 1 1 1 I 3 1 1 11 12 2 1 1 12 13 2 2 1 13 14 4 3 9 14 15 4 1 1 15 16 2 1 1 16 17 2 1 17 18 5 3 1 18 19 2 1 1 19 11 5 2 97 11 111 3 1 1 I1 112 1 1 1 112 113 4 2 1 1I3 114 2 2 loo 114 115 3 2 1 115 116 2 1 1 116 117 1 1 1 117 118 4 2 loo 118 119 3 2 1 119 12 8 9 89 12 121 2 2 92 121 122 5 2 loo 122 123 4 2 92 123 124 7 4 88 124 125 4 1 loo 125 126 7 6 94 126 127 5 3 1 127 128 9 8 71 128 129 2 2 1 129 13 9 8 84 13 131 7 2 1 131 132 4 4 93 132 133 6 4 82 133 134 4 3 1 134 135 7 4 1 135 136 5 2 96 136 137 1 1 137 138 3 1 1 138 139 5 1 loo 139 14 2 1 14 141 2 2 1 141 142 2 2 1
65 Fracture frequency and RQD, OL-KR 15 Appendix 8.1 Start End All fractures Natural fractures RQD Remarks m m pc/m pc/m % 142 143 2 1 1 143 144 3 1 1 144 145 2 1 1 145 146 3 1 146 147 3 2 1 147 148 7 4 91 148 149 2 12 56 breaks over 2, fractures about 149 15 2 1 1 15 151 2 1 151 152 1 1 152 153 1 1 153 154 2 1 154 155 2 1 1 155 156 3 1 156 157 5 1 157 158 1 1 1 158 159 1 1 159 16 2 1 1 16 161 2 1 161 162 1 1 1 162 163 2 1 163 164 I 1 164 165 2 2 1 165 166 I 1 166 167 1 1 1 167 168 6 5 86 168 169 1 1 169 17 4 5 9 17 171 5 3 1 171 172 4 1 1 172 173 2 1 loo 173 174 3 1 1 174 175 17 5 85 175 176 2 loo 176 177 1 1 1 177 178 7 4 94 178 179 2 1 loo 179 18 3 1 1 18 181 3 1 1 181 182 2 3 1 182 183 3 1 1 183 184 3 1 184 185 5 4 92 185 186 4 I 1 186 187 I 1 1 187 188 1 1 94 188 189 6 6 loo 189 19 2 1 loo 19 191 3 3 1 191 192 2 1 loo 192 193 1 1 1
66 Fracture frequency and RQD, OL-KR 15 Appendix 8.1 Start End All tractures Natural tractures RQD Remarks l11 m pc/m pc/m % 193 194 2 1 IOO 194 195 3 1 195 I96 2 IOO 196 197 3 I IOO 197 198 4 I loo 198 199 1 IOO 199 2 3 IOO 2 21 4 2 1 21 22 1 I 1 22 23 2 loo 23 24 3 1 24 25 4 1 25 26 2 loo 26 27 3 IOO 27 28 2 1 28 29 1 1 29 21 I 1 21 211 5 1 211 212 2 loo 212 213 I 1 213 214 3 IOO 214 215 3 1 215 216 2 1 216 217 2 1 1 217 218 3 I 1 218 219 2 1 2I9 22 2 1 22 221 3 2 IOO 22I 222 3 2 1 222 223 4 1 223 224 4 3 99 224 225 4 1 1 225 226 1 I 1 226 227 4 I IOO 227 228 4 4 9 228 229 4 3 1 229 23 1 IOO 23 231 2 2 1 231 232 3 1 232 233 3 1 233 233.54 1
67 Fractur frequency and RQD, OL-KR15B Appendix 8.1 Stmt End All il-actures N atura1 fractures RQD Remarks m m pc/m pc/m % 2.38 3 1 1 3 4 1 12 59 4 5 4 1 1 5 6 12 5 91 6 7 7 8 86 7 8 6 2 loo 8 9 6 7 91 9 1 3 1 1 1 11 8 4 98 11 12 3 2 1 12 13 4 5 87 13 14 12 9 63 14 15 4 3 88 15 16 8 5 96 16 17 3 1 1 17 18 2 8 72 18 19 2 2 94 breaks over 2 19 2 2 2 1 2 21 6 7 85 21 22 7 4 93 22 23 1 5 95 23 24 6 6 8 24 25 5 3 1 25 26 6 6 85 26 27 5 3 1 27 28 5 1 1 28 29 4 2 96 29 3 5 3 91 3 31 5 1 31 32 4 1 1 32 33 5 1 33 34 2 1 34 35 8 1 1 35 36 2 2 99 36 37 1 loo 37 38 I 1 38 39 1 1 39 4 5 3 1 4 41 1 1 41 42 1 4 1 42 43 2 6 96 breaks over 2 43 44 3 2 1 44 45 3 4 89 45 45.14 1
----------------------------------------------------------- -- 69 Fractured zones, core loss, OL-KR 15 Appendix 8. 11 Start End Class ofthe Core loss Remarks m m fractured zone m 148,22 148,66 RiV
7 Fractured zones, core loss, OL-KR 15B Appendix 8.11 Start End Class ofthe Core loss Remarks m m fractured zone m 3,3 3,78 Rill I
r-------------------- 71 Flush \Vater samples Appendix 8. 12 Boreholc OL-KR15 Date Time Depth Flov'vmeter reading Quantity Batch Electric Label litres conduc- tivity concentration m before after litres no ms/m g I 1 23.1. 16:15 4. 3 625 3 628 3 1 498 23.1. 18:3 41.45 3 628 3 631 3 2 496 24.1. 19:5 53.2 2 5 3 3 498 25.1. 11: 58.97 5 8 3 4 14. 481 25.1. 16:25 63.8 8 11 3 5 15.7 51 25.1. 19:5 7.77 11 14 3 6 15. 488 26.1. 1:25 78.5 14 17 3 7 15.6 489 26.1. 17:3 85.62 17 2 3 8 15.8 511 27.1. 7:45 94.53 2 23 3 9 15.6 512 27.1. 15:25 1.46 23 26 3 1 15.5 55 27.1. 22:55 111.15 26 29 3 11 15.7 494 28.1. 7:15 115.45 29 32 3 12 15.8 488 28.1. 11:3 124.11 32 35 3 13 15.8 451 28.1. 18: 128.56 35 38 3 14 15.6 52 28.1. 22:35 135.96 38 41 3 15 15.6 519 29.1. 2:35 141.79 41 44 3 16 15.6 487 29.1. 9:3 144.75 44 47 3 17 15.7 482 29.1. 13:5 15.67 47 5 3 18 15.8 53 29.1. 19: 156.61 5 53 5 35 19 15.5 469 29.1. 22:3 159.58 53 5 56 2995 2 15.4 449 3.1. 4:3 168.48 56 59 3 21 15.8 493 3.1. 173. 59 62 3 22 15.9 513 3.1. 14:55 178. 62 65 3 23 15.7 511 3.1. 18:45 183.43 65 68 3 24 15.7 482 31.1. 3:3 189.35 68 71 3 25 15.4 55 31.1. 8: 195.19 71 74 3 26 15.8 511 31.1. 14: 21.13 74 77 3 27 16. 51 31.1. 17:4 24.11 77 8 3 28 15.9 487 1.11. 2: 21.7 8 83 3 29 15.3 55 1.11. 3:4 214.3 83 86 3 3 15.4 481 1.11. 15:3 219.28 86 89 3 31 14.7 51 1.11. 2:2 224.37 89 92 3 32 14.4 59 2.11. 2:2 227.51 92 95 3 33 15.9 538 2.11. 6:15 233.3 95 98 3 34 16.2 57 2.11. 11:3 233.3 98 1 l 3 35 15.5 458 3.11. 2:15 233.57 11 14 3 36 16.1 58
72 Flush water samples Appendix 8.12 Borehole OL-KR15B Date Time Depth Flo\'vmeter reading Quantity Batch Electric Label conduc- concentration litres tivity m before after litres no ms/m )lg I I 4.11. 9:45 5.16 14 17 3 37 14.7 5 6.11. 14:5 11.9 17 11 3 38 15.2 518 6.11. 2:1 24.55 11 113 3 39 16.2 491 7.11. 5: 32.53 113 116 3 4 15.4 513 7.11. 15:3 39.4 116 119 3 41 15.6 7.11. 2: 119 122 3 42 15.7 448
73 Returing water samples Appendix 8.13 Boreho1c OL-KR15 Date Time Depth Sample Flushing water Label batch concentration m no no JJ.g I 1 25.1. 1:45 52.1 1 ".) 423 26.1. 7:35 67.82 2 5 435 27.1. 7:4 85.62 ".) 7 282 28.1. 7:25 112.24 4 1 152 29.1. 7:25 138.91 5 15 333 3.1. 7:2 165.55 6 21 14 31.1. 7:4 189.35 7 24 17 1.11. 12:5 213.3 8 29 2 2.11. 8:1 227.51 9 33 36 Borchole OL-KR15B Date Time Depth Sample Flushing water Label batch concentration m no 11 JJ.g 11 6.11. 16:2 5.45 1 37 217 7.11. 9:3 27.14 11 39 438
75 EZ-SHOT DEVIATION SURVEY Appendix 8.14 Borehole Initial azimuth Initial dip Magnetic declination OLKILUOTO, OL-KR15 321 degrees 89.4 degrees 4. 5 degrees Start X= 92 439.91 y = 25 84.14 z = 8.42 POINT DEPHT X y z AZIM. DIP 1, 92439,91 2584,14 8,42 321, 89,4 2 3, 92439,94 2584,12 5,42 32,84 89,14 3 6, 92439,98 2584,8 2,42 32,88 88,88 4 9, 9244,3 2584,4 -,58 321,22 88,63 5 12, 9244,9 25839,99-3,58 32,97 88,38 6 15, 9244,16 25839,93-6,58 32,93 88,11 7 18, 9244,25 25839,87-9,57 32,94 87,85 8 21, 9244,34 25839,79-12,57 32,98 87,6 9 24, 9244,44 25839,71-15,57 321,12 87,34 1 27, 9244,56 25839,62-18,57 32,96 87,7 11 3, 9244,68 25839,52-21,56 32,96 86,81 12 33, 9244,81 25839,41-24,56 321,9 86,56 13 36, 9244,96 25839,29-27,55 32,99 86,31 14 39, 92441,11 25839,16-3,54 32,97 86,4 15 42, 92441,28 25839,3-33,54 321,32 85,83 16 45, 92441,46 25838,89-36,53 322,8 85,72 17 48, 92441,63 25838,75-39,52 322,49 85,7 18 51, 92441,81 25838,62-42,51 322,14 85,7 19 54, 92441,99 25838,48-45,5 321,38 85,68 2 57, 92442,17 25838,34-48,49 32,79 85,65 21 6, 92442,34 25838,19-51,49 32,83 85,61 22 63, 92442,52 25838,5-54,48 32,95 85,63 23 66, 92442,7 25837,9-57,47 321,2 85,68 24 69, 92442,87 25837,76-6,46 321,72 85,66 25 72, 92443,5 25837,62-63,45 322,41 85,6 26 75, 92443,24 25837,48-66,44 322,34 85,56 27 78, 92443,42 25837,34-69,43 322,19 85,57 28 81, 92443,6 25837,2-72,42 322,26 85,61 29 84, 92443,78 25837,6-75,42 321,83 85,62 3 87, 92443,96 25836,91-78,41 321,4 85,57 31 9, 92444,15 25836,77-81,4 321,1 85,55 32 93, 92444,33 25836,62-84,39 32,48 85,61 33 96, 92444,5 25836,48-87,38 32,61 85,65 34 99, 92444,68 25836,33-9,37 32,74 85,61 35 12, 92444,86 25836,18-93,36 32,24 85,56
76 EZ-SHOT DEVIATION SURVEY \ppendix 8.14 POINT DEPHT X y z AZIM. DIP 36 15, 92445,3 25836,3-96,35 319,99 85,57 37 18, 92445,21 25835,89-99,34 32,27 85,59 38 Ill, 92445,39 25835,74-12,34 32,18 85,58 39 114, 92445,57 25835,59-15,33 319,94 85,53 4 117, 92445,75 25835,44-18,32 319,96 85,47 41 12, 92445,93 25835,29 -Ill,31 32,4 85,46 42 123, 92446,11 25835,13-114,3 319,84 85,43 43 126, 92446,29 25834,98-117,29 319,28 85,38 44 129, 92446,48 25834,82-12,28 318,66 85,34 45 132, 92446,66 25834,66-123,27 318,32 85,33 46 135, 92446,84 25834,49-126,26 318,9 85,36 47 138, 92447,2 25834,33-129,25 317,85 85,37 48 141, 92447,2 25834,17-132,24 317,65 85,32 49 144, 92447,38 25834, -135,23 317,19 85,23 5 147, 92447,57 25833,83-138,22 316,68 85,15 51 15, 92447,75 25833,65-141,21 316,66 85,11 52 153, 92447,94 25833,48-144,2 317,12 85,7 53 156, 92448,13 25833,3-147,19 317,7 84,98 54 159, 92448,33 25833,13-15,17 317,81 84,9 55 162, 92448,53 25832,94-153,16 317,33 84,85 56 165, 92448,72 25832,76-156,15 317,8 84,79 57 168, 92448,92 25832,57-159,14 316,99 84,73 58 171, 92449,13 25832,38-162,12 316,9 84,71 59 174, 92449,33 25832,2-165,11 316,97 84,7 6 177, 92449,53 25832,1-168,1 317,12 84,7 61 18, 92449,73 25831,82-171,9 317,12 84,69 62 183, 92449,94 25831,63-174,7 316,8 84,62 63 186, 9245,14 25831,43-177,6 316,85 84,55 64 189, 9245,35 25831,24-18,5 317,75 84,51 65 192, 9245,57 25831,5-183,3 318,1 84,5 66 195, 9245,78 2583,85-186,2 317,39 84,49 67 198, 9245,99 2583,66-189, 316,88 84,44 68 21, 92451,21 2583,46-191,99 317,21 84,38 69 24, 92451,42 2583,26-194,98 318,15 84,34 7 27, 92451,65 2583,6-197,96 318,62 84,33 71 21, 92451,87 25829,87-2,95 318,27 84,31 72 213, 92452,9 25829,67-23,93 318,2 84,22 73 216, 92452,32 25829,46-26,92 317,79 84,16 74 219, 92452,54 25829,26-29,9 317,8 84,18 75 222, 92452,77 25829,5-212,88 318,1 84,2 76 225, 92452,99 25828,85-215,87 317,41 84,2 77 228, 92453,22 25828,64-218,85 316,14 84,2 78 231, 92453,43 25828,43-221,84 314,87 84,2
------------------------- - 77 EZ-SHOT DEVIATION SURVEY Appendix 8.14 Borehole Initial azimuth Initial dip Magnetic declination OLKILUOTO, OL-KR15B. degrees 9 degrees 4.5 degrees Start X= 92 442.21 y = 25 838.44 z = 8.35 POINT DEPHT X y z AZIM. DIP 1, 92442,21 25838,44 8,35, 9, 2 3, 92442,21 25838,44 5,35, 89,9 3 6, 92442,21 25838,45 2,35 92,49 89,78 4 9, 92442,21 25838,47 -,65 91,68 89,68 5 12, 92442,21 25838,49-3,65 91,33 89,59 6 15, 92442,21 25838,51-6,65 92,25 89,51 7 18, 92442,21 25838,54-9,65 93,1 89,46 8 21, 92442,2 25838,57-12,65 94,84 89,43 9 24, 92442,2 25838,6-15,65 94,1 89,45 1 27, 92442,2 25838,62-18,65 92,91 89,44 11 3, 92442,2 25838,65-21,65 93,52 89,38 12 33, 92442,2 25838,69-24,65 93,32 89,34 13 36, 92442,19 25838,72-27,65 91,66 89,34 14 39, 92442,19 25838,76-3,65 91,66 89,36 15 42, 92442,19 25838,79-33,65 91,66 89,34 16 45, 92442,19 25838,83-36,65 91,66 89,31
79 EZ-SHOT deviation survey Appendix 8.15 OL-KR15 Olkiluoto OL-KR15 Horizontal proct1on OT tha dv1ot1on 1n N<orth)-E(ost) coordinates N E Vrt1C1 proact1n Or thg CQV1t1on I l EZ-SHOT-borhol In1tol o:z:1muth In1t1ol dip I Total 1 liiangth dv1ot1on survy == 321. asrs 9. d.agrliiiuiiis 234. m SMOY 3-12-21
degree -8. l -6. + -4. + om N I I 1--'- Vl>-j.. s. a s ::;l en s:: '-<: -2. 75 3 m (T). +-----------d==----=-------------------------------+------ 2. 4. 6. EZ-SHOT-borehole devlatlon survey Olklluoto OL-KR15 Oevlatlon angle projected on the plane wlth the lnltlal borehole dlp 1: 15 SMOY 3-12-21 i 6. ;;: -Vl
m I -16. t -12. t -8....L. om rn 1 I Vl...,... a.. (!) < a s ::s rj) s:: "'1 < (!) '-< -4.... o.or-----------+-------------+-------------+-------------+----- 75 15 225 3 m <Th) 4. 8. 12. 16. EZ-SHOT-borehole dev1at1on survey Olklluoto OL-KR15 Horizontal projection 1: 15 SMOY 3-12-21 "C) (!) 5.... Vl
m -16. -12. + -8. + -4. -+. Ot'r1 N 1 I '""""' Ul.. ('D... < e... ::,:3 VJ c::. L-------------------=======+=------------- 4. 75 15 225 3 m (T) N 8. 12. EZ-SHOT-borehole deviation survey Olkiluoto OL-KR15 Projection on the plane with the initial borehole dlp 1: 15 SMOY 3-12-21 '"d ('D 8. '""""' Ul
m I / -16. t / -12. t / -8. + / om N I I o Vl.. (!)... < a... ::s rjj (!) <...<: -4. 3 m (T) o.or-----------+-------------+-------------+-------------+----- w 4. 8. 12. 16. EZ-SHOT-borehole deviation survey Olklluoto OL-KR15 Vertical projection: Axis T has the lnltlal dip of the borehole 1: 15 SMOY 3-12-21 " (!) 8. $<' Vl
degree -8-6 -4-2 Otn N 1 I --o Vl,_,.. (!) < - s Vl '-< 225 3 m (T) f---------------+---------------+---------------r--------------------.+;.. 2 4 6 8 EZ-SHOT-borehole dev1at1on survey Olklluoto OL-KR15 D1p angle projected on the vertlcal plane 1: 15 SMOY 3-12-21 "d (!) [ ;;< _. Vl
85 EZ-SHOT deviation survey Appendix 8.15 OL-KR15B Olkiluoto OL-KR15B Hor1zontcl proct1on o th dgv1ct1on 1n N<orth)-E<cst) coord1natea N Vrt1cal progct1on tha dqv1ct1n I EZ-SHOT-borgholg In1tcl caz1muth In1t1cl dip I Totcal lgnsth dv1ct1on survy 91.3 dsrqs 9. dgreiciis SMOY 45. m 3-12-21
degree -8. -6. -4. om N.._ I 'C/'l ::t Vl O'o.. a c:r ::t Ul '-< -2. 13 25 38 5 m (T). T--------------------------------------------r---------------+------ \ 2. 4. 6. EZ-SHOT-borehole dev1at1on survey Olklluoto OL-KR158 Devlatlon angle projected on the plane wlth the lnltlal borehole dlp 1: 25 SMOY 3-12-21 '"d 5. ;;:< -Vl
E EZ-SHOT deviation survey OL-KR15B I (...-f I (\J..-f. I. I 87 E Lfl (T) Lfl N (T)...-f... Appendi 8.15 >-.. QJ > L :J (/) c r-1 +) r-1 c > QJ r-1 TI m +) Lfl u QJ...-f QJ...-f...-i ::: J D :::s:::.c I L N QJ...J ()_ I L N,.....-I. I I +l +l (T) I- c :J I...-i N Lf) U1 r-1 T""' N >- I L N...-i :::::E w I...-f (f).. N (Q...-f...-i
m -16. -12. -8. -4. Ot'Il rn I I t--- V.. tljo.. (D... < a... ::::s C/:J '< 13 25 38 5 m (T). --------------+---------------+---------------------------------- 4. 8. 12. EZ-SHqT-borehole deviation survey Olklluoto OL-KR15B Projection on the plane wlth the initlal borehole dlp 1: 25 SMOY 3-12-21 "'C) (D [ <" '""""" V..
m 1-16. -12. t -8. + OtiJ LiN I I... o VI-) t:dp. (D < a en s:: 1-t (6...::: -4. 13 25 38 5 m <T). ------------------=================+=========---------- \ 4. 8. 12. 16. EZ-SHOT-borehole dev1at1on survey Olklluoto OL-KR158 Vertical projection: Ax1s T has the initial dip of the borehole 1: 25 SMOY 3-12-21 " (tl [... VI
EZ-SHOT deviation survey OL-KR15B 9 Appendix 8.15 E Lf1 aj c...-i... Lf1 (T).--4 >-.. aj > L :J en c..-t +->... a > OJ D CD Lf1 aj....-i ::: ::::s:::..c. I aj _j L D. I +> I- :J I.-I c.n... I N.-I w...-i u..-t +-> L aj > aj..c. +-> c D OJ +> u... aj D -, D (\J L I... (\J... OJ I.-I m c (T) Lf1 (\J >- o_..-t.. L.--4 c.n ru------------+------------------+------1-------+------;-------+----- ru L m QJ D I CD I I C\J I C\J
91
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