technical report wrd94004 · first placing a wood/rubber seal above the mud. using the mud pump a...
TRANSCRIPT
Technical Report WRD94004
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Report No: 04/94
I MATTHEWS
HYDRO GEOLOGIST
AYERS ROCK (yuLARA)
Rl.'l" 16360
BORE COMPLETION REPORT'
WATER RESOURCES BRA."N"CH. ALICE SPRINGS
July 1994
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SYNOPSIS
A successful production bore, RN 16360 was constructed for the
Yulara water supply. The bore has a maximum recommended
pumping rate of 10 L/s. The water has a TDS of 1440 mg/L.
The water is drawn from unconsolidated Tertiary sands. Inert
casing and stainless steel screens were used due to mild
corrosion problems within the borefield.
SUBJECT
GEOLOGY
LOCATION
KEYWORDS
Community water supply
Borefield
Corrosion
Tertiary sediments
Ayers Rock
Dune Plains Borefield
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1. INTRODUCTION
2. BACKGRorJND
3 . HYDROGEOLOGY
4. DRILLING AND TESTING
5. DISCUSSION
6. CONCLUSIONS
7. RECOMMEJ)J"DATIONS
8. REFERENCES
1. WATER QUALITY DATA
1. LOCATION K~P
2. BORE LOCATION ~~P
3 . LOCAL GEOLOGY ~_~
4 . CONSTJl..J)j"T RATE DRAw"DOtVN GRAPH
5. PREDICTED DRAw"DOWN GRAPH
A. CO~..POSITE LOG - RN 16360
B. TEST REPORT - R."l 16360
C. GJl..MM!'. LOG - Rl"'J 16360
D. GAMMA LOG - RN 12452
CONTENTS
TABLES
FIGURES
APPENDICES
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bgl
EC
GWP
ID
Lis
kIn
m
mg/L
mm
R..1'J
SWL
TDS
!LS/cm
below ground level
electrical conductivity
galvanised water pipe
inside diameter
litres per second
kilometres
metres
milligrfuils per litre
millimetres
registered number
standing water level
total dissolved solids
microsiemens per centimetre
TECHNICAL SUPPORT BRANCH, ALICE SPRINGS
WATER RESOURCES LIBRARY, ALICE SPRINGS
\\lATER RESOURCES LIBRARY, DA.R.wIN
PAWA LIBRARY, DARWIN
PRINCIPp~ ENGINEER GROUNDWATER
AUTHOR
ABBREVrAT:IONS
D:ISTR:IBUT:ION
2
3
1
1
1
1
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1. INTRODUCTION
Ayers Rock Resort (Yulara) is located 440 km south-west of
Alice Springs, see Figure 1. Water is drawn from the Dune
Plains Borefield and there has been an average increase in
water consumption of between 9% and 10% per annum since 1984.
The Ayers Rock Resort Corporation believes this trend will
continue.
Following a request for further production bores sited to
exploit areas of the aquifer containing lower salinity waters,
bore RN 16360 was constructed.
2 • BACKGROUND
Since 1992 the majority of Yulara's water needs have been met
by bores RN 10490 and RN 12058, other~ise known as 'Diesel'
bores. These bores are 200 m apart and l:ave recolmnended
maxim~~ p~~ping rate of 23 L/s <L~d 7 L/s respectively.
Problems with the bores forking were experienced in 1991.
The alternative production bores, R1~ 13363 and RN 13365
('Electric' bores) are not being utilised as the water quality
is inferior to that available from the Diesel bores.
Utilisation of the poorer quality water available these from
bores would result in increased treatment costs and necessitate
expansion of the treatment facilities.
Three other production bores, RN's 12453, 12455 and 12458 -
located between the Diesel and Electric bores - were drilled
and tested in 1980/81. See Figure 2 for a bore location map.
These bores have never been used for production purposes and
were retested in 1992 with a drop in performance noted in two
of the three bores. The water quality is similar to that from
the Diesel Bores.
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When retested in 1992 all three produced rust flakes and rusty
coloured sludge. This suggested corrosion of the steel casing
which may effect the future operation of the bore.
Following a request from Technical Support Branch for two new
production bores it was originally decided to redrill near
bores RN 12458 and RN 12455.
Bore R-~ 12458 taps an unconsolidated Tertiary sediment aquifer
and casing failure may lead to an influx of soft sand and clay.
For this reason, a redrill near bore RN 12458 was undertaken.
Bore RN 12455 yields water from hard Proterozoic sediments and
casing breaks would not be expected to greatly effect bore
performance. A downhole video camera ~Jas used to inspect bore
RN 12455. The casing appears to be in reasonable condition,
and it was decided not to redrill. This bore should be
equipped at the recommended rate of 4 Lis. A redrill, with a
possibly higher yield due to more efficient construction
techniques, may be necessary at some stage in the future.
3. HYDROGEOLOGY
Outcrop in the area is sparse and consists of the Cambrian Mt
Currie Conglomerate (Ayers Rock and the Olgas) and the
Proterozoic wi~~al and Inindia Beds (The Sedimentaries). See
Figure 3.
In the Dune Plains borefield area the sediments were deeply
eroded and subsequently infilled during the Tertiary period by
a thick sequence of interbedded clays and sands.
Within the borefield, aquifers were intersected in both the
Tertiary sediments and underlying Proterozoic and Cambrian
rocks. See Knott (1980) for further details.
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4. DRILLING AND TESTING
Bore RN 16360 was drilled to 59.5 m with a 280 rom tricone bit
and bentonite based mud. 192 rom ID ABS casing was set to 59.0
m with centralisers placed 1 m and 9 m above the bottom of the
casing. A cement plug was set at the bottom of the ~~S by
first placing a wood/rubber seal above the mud. Using the mud
pump a measured amount of cement slurry and water was PQ~ped
into the casing to displace the mud and set the c~~ent at the
correct level.
The mud pits were cleru~ed and biopolymer mud used to complete
the hole. A 187 ~~ bit was used to deepen the hole to 68.0 m
~~d 154 rom ID, then 0.5 rom aperture stainless steel screen
placed between 57.6 m and 66:6 m. The top of the packer is at
57. 3m with a sump between 66.6 m and 67.0 m. A left hand
thread lowering sub is welded to the base of the sump. See
Appendix A for a composite log of the bore.
The mud was displaced with clean water and the bore airlifted
approximately 10 Lis for 30 minutes from 55 m. Due to the high
airlift yield, a breakback chemical to aid mud dispersion was
not used.
A four step and 24 hour constant rate test was undertaken. The
step test was undertaken at rates of 3, 6, 9 and 12 Lis. The
final drawdown was 9.5 m. The available drawdo~n was 26.7 m.
A 12 Lis, 24 hour,' constant rate test was also carried out with
the drawdown being 14.2 m at the completion of the test. Bores
~~ 12452,12457 ~~d 12458 were monitored during the testing.
See Figures 4 and 5 for constant rate and predicted drawdown
graphs.
No variation was noted in RN 12452. This bore is equipped ,·lith
unslotted 50 ~~ GWP to 140.0 m. The GWP should be cleaned out
(if possible) when suitable equipment is next in the area.
This bore taps the deener, hardrock aquifer and monitoring
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results may help define the relationship between the upper and
lower aquifers.
5. DISCUSSION
When drilling through the aquifer zone, the great majority of
the cuttings consisted of soft yellow and white clay. Sandier
horizons were evident with some well-rounded quartz grains to
5 mm. The sandier sections appeared to be in the minority.
Once construction was completed the bore airlifted 10 Lis and
produced only small a~ounts of fine sand and clay after the
first few minutes. Considering the alnount of clay in the
aquifer zone this was unexpected. The gfu~a log for both bore
R-~ 12452 and RN 16360 (Appendix C and D) suggests that the area
screened is the main producing zone.
To minimise local drawdown effects the pumping load should be
shared as evenly as possible between the three available
pumping 'cfu"tres'; &~ 16360, RN 12455 and &~ 10490/12058. Due
to the close proximity of bores RN 10490 and RN 12058 they
should be pumped simultaneously only when necessary. It is
suggested that bore Rl~ 12455 (4 Lis) and bore R-~ 16360 (10 Lis)
be pumped continuously vlith RN 10490 or RN 12058 making up the
shortfall.
drawdowns.
This type of pumping regime would minimise local
The water quality from bore RN 16360 is acceptable and similar
to the "Diesel" bores currently in use. See Table 1 for full
chemical analyses of.selected bores. Bore Rl~ 16360 has higher
sodium and chloride levels but with lower nitrate and silica
levels. The chloride concentration (423 mg/L) exceeds the
recommended guidelines for non-health related limits. The
water quality for bore RN 12455 is also similar to that from
'Diesel' bores, once again with slightly elevated chloride
levels.
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As such, the production use of bores RN 16360 and RN 12455
should have little effect on the quality of the feed supply to
the desalination plant.
6. CONCLUSIONS
A successful bore, RN 16360, was drilled at Yulara. Due to
mildly corrosive groundwater conditions ABS casing and
stainless steel screens were used to construct the bore.
The bore was test pumped and the reco~~ended yield is 10 Lis
with a pump setting of 57 m. The water is drawn from
unconsolidated Tertiary sediments. The water quality is
acceptable and expected to remain constant.
Bore fu'I 16360 should be pumped in conjuction with 'Diesel'
bores and bore RN 12455. This would spread out the effects of
abstraction ~~d mimimise local drawdowns.
7 • RECOMMENDATIONS
1. Bore ~~ 16360 should be plli~ped at a maximum rate of 10
Lis.
2. An airline and water meter should be installed on bore RN
16360.
3. The SWL and total depth should be noted each time pumping
equipment is removed from the bore.
4. A full chemical analysis should be carried out on each
production bore on a yearly basis.
5. Bore ~~ 12455 should be equipped at 4 Lis.
6. Extraction should be shared between bores fu'I 16360, RN
12455 and 'Diesel' bores.
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,
I MaIysIs to mJI~rams per lfu. - m¢ (u~.., """""" "'100) ,
i
BORE DATE SPECIFIC TOTAL MiliUM POTA5S- CALCIUJ.I MAGNES- mon TOTAL TOTAt snJCA CHLORIIl£ SULPIIATE NllllATE BleARS- fLlJOllI1l£ (CALC COWflITS REGISTERED OF CONDUCT- DISSOLVED IUM IUU (TOTAL) lIARD- AtKA- OflATE FROII NU~BER SA!Apuna ANCE SOUDS NESS UNTlY CHLORIDE)
RN uS'cm TDS pli '" K Co Mg Fe caCO. CaCo, S.(O, CI SO, NO, IICOJ F "'CI
12450 16/05/80 2830 1380 7.5 279 31 104 61 0.1 510 237 27 421 200 37 289 1.1 694 Pump losl
01/12192 2360 1410 7.1 287 30 107 56 0.3 498 222 28 431 323 39 271 0.9 710 Pump test
16360 14/04/94 2390 1440 7.2 317 28 105 56 0.1 493 221 23 423 323 21 269 0.9 697 Pump tast -
-
- ...
-- I ,
. -NHMRC GUIDELINES ..., 1500 6.5- 0.3 500
8.5 400 400 100 1.7 Matlm. except pH rang.
,
- . -
AYERS ROCK (YULARA) ,
WATER QUALITY DATA , , , , TABLlf1-
, , i
I
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Figures
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« •
~ I ~
\ , ,
•
NORTHERN
/>--.\"""'0-_ ... \ ...... ______ _
z -........ ~ Yulara ~ ___ -c...;.. . ';-'''-__
Olgas' ,.-, • '" 1t~r'$ R~;c.'( ~ L .!ill!F.!L. J NATJONAL PARK
:.: \i.l ~ (/)
"' ;;:
SOUTH
TERRITORY
Curtln Springs
Mt.Conner
134·
ALICE SPRINGS
1 ----'.
AUSTRALIA 1 I
100 I
o 100 200 300 Kms
-----
, \tictoria
,NORTHERN TERRITORY
I :;:. .. , ~
Tennant Creek e • -4'r .r1--
HWY
1 ... , ~ I '%-•
I ,
-90 I · "0' ALICE ! I . AYERSR~ SPRINGS I tYUUJtl • •
.-- . ___ .J
,
AYERS ROCK (YULARA)
LOCATION MAP
FIGURE 1
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528.
12453 •
. , \ "',
ores .NewBo~
u .>
-ROCK I MT Q~,,>-\>
. . 5.27
.-'-
(.- (A '.
>-
Scale 1 100000
AYERS ROCK (YULARA)
BORE LOCATIONS FIGURE 2
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Oa Os
Pzc
Euw
Alluvium Aeolian sand
Ii (
'--1----::.
Conglomerate, arkose
Scale 1 :250 000
- Mt Currie Conglomerate
FIne grained sandstone and - Winnall Beds brown siltstone
PlC:~
"
}
AYERS ROCK (YULARA) LOCAL GEOLOGY
(after Fonnan at ai, 1963)
/~ ~ I , '
Cainozoic
Cambrian
ProterozoIc
FIGURE 3
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,..., r/) Q) ... .... Q)
E ..... % ;: 0 Cl
~ a: Cl
"Tl -Ci) C ::0 m .f>.
o
5
10
15
20
25
30
35
r- ............
'" -I~-+-H-r-----t--- 1'1'-
1'-1'
, ~ -.~~~~~ , , '" ~~
f------+---f--+-+-I-+1-H------r-~--j--~I-~i_rT_----~--~,~~~~~~----_+--_r_4_4_+~ x......., ~~~ 1
I--------t----.-JI----+--I-H-+-I~---- __ ---+-__ -- -~. '" 1
~f'-.... . I------f---+-f--I--+-+-I-~ - - - -I-I--t-t-t------t---I-++-I--If-+-++-----+--+~.....,_I_++ .. ,~
1 .... 1'- . I------t---I--+-I---I--++++-------+---I-+-+- - - ~
1-------1--1--+-+-- .. --~ .----- .. -- .. - ---.- --- -. - -I----+--t--+-+--i-t-
~- ----.. -. ----. - - --f----f----t--t----H_t_ Q = 12.11 Us
L\'s :: 7.75m f----- --I--f- - - - -- .--- - -- -I----t--t-t-I-I----t---t-t----H_t_
r T :: 24m2/day - - --- - -
1
SWL 29.42m 1---+-11-+++-1-----1--1·-- f---I-+- -.-.-
14/04/94_f--___ _ ___ ---f---i--H-I-t-hf------t-+-+--+-+-+_
10 100
TIME (minutes)
1000
AYERS ROCK (YULARA) RN 16360
CONSTANT RATE DRAWDOWN GRAPH FIGURE 4
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....... I/)
o
2
4
6
•
I---r-... Q = 2 LIs
~ -r-t-_ I"-... r--
""- r----..... -<l> 8 .... """ I'-i' r- ---- -- ---.... Q = 4 LI s
"I"--I'-... ............ .......... ----- ____ -Q)
E 10 ..... 'r-. ................. ....r-. ~ ..... . z ~. 1
C 3: 1 ct a: C 1 C W f- 1 U -Cl W 2 n: 11.
"T1
G> C :0 m 01
2
2
2
2
, I'- -::-: . t---.. ...... , ~ = 6 LIs ---....~ -
~I'-............. --- -I . --.. --I-----l---lHI-H"'H--k::----+---cI--H--HH--H 1"--" ............... .......... ----- ____
I -1-++++11--·1--\---1-·-· r- ..... ....... - ...... --- -r-.
I _.. ~ Q = 8 LI s ·1- - -.I-tt+~---=:~::I---t--t-+t+H+--+--+-++++++1 ~ ....... ~
I·· . -1--I-+--t-HI+t·I- .. -_........... -- -II---tr------t"'-ll:-+++H--+-+++-I-H+J ........... , n: .....
, -!--!--+-++++I-- --1--1- -1-++-++1----.... - " . - .. -.. lii H-j+J-....... ~::--II--++H--l+-H >, i: r-. >--......... ...............
I---+--I--+-.H+J.++-<t:.~.---...... _ ... _ Z. ~.. ~ __ ~ :-... Cl 0 "-....Z ...........
. r- ~. _ +-~ ......... __ ~ .. _. .~ ... + __ . ~ 0 -H-I+t----+--+-+--I--t+++1 o Z ~,
<-;;---_.. . ... _____ •...... .._ .. _., __ ._ .. _ ... 0 _. _, _____ _LL-'-::.-. _-'-_'----'---L--L.JLLLJ
10 2 10 3 0 7
SWL 29.42m 14/04/94
10
TIME (minutes) 10
AYERS ROCK (YULARA) RN 16360
PREDICTED DRAWDOWN GRAPH FIGURE 5
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Appendices
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POWER ~ -AND-~~ WATER ~ WATER RESOURCES AUTHORITY
COMPOSITE LOG OF BORE DEPTII BORE GRAPHIC (m) CONSTRUCTION LOG STRATA DESCRIPTION
0 +---~--~--~~m C>
5 - " .- '" "0 "'", 0_ ~
10 - - '" :1; ... -0 <n-0"0
15 -'" Ec: Eo>
..... E 20 -0>
<? "
25 -
/!
'" <= <0
· ...... Il-3 Ught brown SAND & clay with minor calcrete ··:·:·X·X 3-9 Firm, brown/grey, fine to medium grained, pooriy ::::'.:: sorted, subrounded SANDSTONE with minor .. .•.. ironstone · .... '9-16 Firm, brown, fine to medium grained clayey
~:~: :~: :~: SANDSTONE with minor ironstone & chert
...... 16-18 Soft, redlbrown vel)' clayey, fine grained SANDSTONE. Minor ironstone.
· . 18-21 Red CLAY & ironstone • . 21·26 Firm redlbrown & grey sandy CLAYSTONE
AQUIFERS (Water Struck)
'" o
'" .0
26-33 Interbedded grey & red CLAY with minor grey"Y SWL 26.1m
30 -
35 -
40 - ~ "0
'" '" "'~ " " '" 45 "' E a; '" '" '-' ~ E
50 - ., '" 2 x _ '" E " ~ '" 55 - "OJ .: ci ~ Q) lD "J:--f1:j 00. 1 t:'
60 - E ~:g IX E E E """'0 '" .~ 65 _ ..- 0_
< o E E o C> -
70 - Lowering sub Oeft hand thread)
2 31S' IF -
-
-
-
E '" r-'"
· · · ·
· ·
· . · · · · · ·
. · · · · .
· ·
& red claystone 12/04/94
33-45 interbedded, whfte, grey & yellow CLAY with minor claystone
45·48 Red sandy CLAY with minor grey clay
48-54 Soft while sandy CLAY wtth minor red clay
54-68 Interbedded bright yellow sandy CLAY with yellow line grained subrounded, poorly sorted clayey sandstone & well rounded, sub angular quartz sand
. "" 10 Lis
-
-
l-
c-
l-
c-
, AYERS ROCK (YULARA) RN 16360 APPENDIX A
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WATER RESOURCES DIVISION
TEST REPORT - BORE RN. 16360
l30re Location. Yulara
c~ient. Water Operations
rntandad ~se. Domestic
Nap. ".yers Rock
Grid Reference. 695421 7204342 ********************************************************************************* RECOMMENDATIONS
PumpiIlg Rate: 10 LIs Pump SettiIlg. 55 m below Ground Level.
General recommendations are given on the reverse side~ The aquifer and bore can sustain higher pumping rates with deeper pump settings or for short periods. Further advice can be obtained from:
Water Resources Branch I Nth Stuart Highway, ALICE SPRINGS, NT.I 0870
{In all correspondence please refer to borets RN number) ************************************************************.******************** COMPLETION DETAILS
Finished depth: 67.4 m Comoletion Date: 12-04-94 Standing Water Level: 29.1 m on 12-04-94
BORE CONSTRUCTION
Interval (m)
0.0 - 5.6 0.0 - 59.0
57.3 57.6 57.6 - 66.6 66.6 - 67.0
TESTING DETAILS
Test Date: 14-04-94 Test Rates: Up to 12 Lis Test Duration: 25 hrs
Description
314 mm 1D steel casing 190 rom 1D ASS casing 152 mm 1D stainless steel packer 152 rom ID SSS, 0.5 rom aperture 152 mm 1D stainless steel sump
WARNJ:NG: MiIlimum interna~ bore diameter is 152 mm.
Notes: 1. Top of casing as constructed was 0.5 m above ground level. 2. All depths are measured from natural ground level. 3. Test rates are hot necessarily indicative of sustainable long term
pumping rates ~
*********************************************************************************
COMMENTS
The above recommendations are based on a 25 hour constant rate test and assumes hydrological conditions remain constant.
&~ airline and water meter should be fitted to ~~e bore.
The total depth and SWL should be noted each time pumping equipment is ra~oved from the bore.
Bore diameter is 190 mm to 57.6 m, then reduces to 154 rom to 67.0 m.
*********************************************************************************
WATER QUALITY
See ar~lysis number /93/94
Prepared by: I Matthews
bore data APPENDIX B
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RECOMMENDATIONS FOR FJ:NJ:SI!ING, OPERATING AND PROTECTING GROUNDWATER BOllES
Atte.~tion the following points will ensure a long and safe life for the bore supply and help prevent pollution of the grou.~dwater resource.
1. Construct a concrete apron around the bore head to prevent surface flow, seepage and waste from entering the bore.
2. Seal the space betwee.~ the casing and pump equipment to preve.~t e.~try of vermini dirt and pollutants.
3.. Maintain pumping equipment in good order to prevent pollution. Prevent spillage of fuel and oil on the ground around the bore. Store fertiliser and other cha~cals at least 50 m away.
4. Keep stock away from the bore head. Discourage domestic activity at the bore. The first tap on the pipeline should not be less than 5 m from the bore head.
5. Pu."IlPing the bore a higher than recommended rates may fork the bore leading to instability or pump maintena.TJ.ce problems.. Seek the professional advice of an hydrogeologist or groundwater engineer.
6. If the bore is no longer required, the casing is to be removed or securely capped and the bore backfilled with clayey material. A cement plug may be required in some instances.
IN ADDITION, please ensure that the BORE IDENTIFICATION TAG is retained securely at all times. The registered bore number is Water Resources Division's only refere-'I'lce to the scientific a..l1.d engineering data on this bore, and hence .L"11P6rtant t-o i-iRDf s further advice t.o bore o~ners.
BORE LOCATION MAP
boredata
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GAMMA.LOG SCALE: 1 TO 300
without DEPTH CORRECTION
RN 16360 --------------------------------------------------------------------------------------------------------------------------------------------------------
GAM>IA
-4.00 cps
WG STARTS AT
I
~:iiili;i I !,I"'"-:;:~i ;;;; .. =t
i -ii----ti --rl; -il---tl--ir-------T[-i[-ij
I, l! I ! I; Ii! '. . l j 1, • i ,:' I i ~ i I I ! 1 !
\ : ' I: ,
i~ , i ,
i i 'i i i ~ l
iii !;;~~, ~~~i~~~~~~;~~~:::li===tl ==J;===i:.===i, ==jl I--tl--:'--~-=:::::~~~i:~ i. ; , . i ' iii ; Ii! iii' j 1 :
I, ,,' '~' i" I"
~i.d=-! ---+-' -----'-----+-----'--+--+--.;--+---i'--'---'---------!
i I i~:.' : ! i i 1 1 i : j t : ! I i
~~. ---i;~--4;---+----!:_---'---_+i __ ~J'_ __ ~' ___ .,-__ -'-' __ -:;
i~ i I!: I
i
I I
! I i j
r--Tl--+I--~,~~~ , l i ! , , , , II
+-__ ~I---~;---~;-:-.~;==~~:'~--~,---.,_---L---1j---1----L---";--_~' ___ ~' __ ~, __ ~, I.i!~.jii i,. :! li.1 : i ,I, I I,!.:, ',I !
! , • • I I I:
I~, I-"'=-' I i
i~,' :~ ,
i i
iii : J 1 j ! L---L-~-~--L--L--L-~--'---~-~-~~-~--LnO~G'FENm'D~S~AT~·
1. 34m.
15.00m.
30.DDm.
45.0Dm.
60.00m.
67.7lm,
APPENDIX C
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GAMMA LOG
RN 12452 Top of casing
r--r-r-V
V k:>
j
s. :.. ."
~
(
'.
\
t>
~ '--
!>
I~
metres
10
20
30
40
50
60
70
80
83
APPENDIX D