IIIIIIII

IIIiI

CKMHIU.MEMORANDUM

TO: Dr. T. D. Chatwin/SLCBeth Moore/DENBill Bluck/SLC

FROM: Grant Buma/EI-SLC

DATE: June 21, 1985 ...Li

RE: March Sampling Protocol-UNC C

PROJECT: W6 62 15. 00 >

This will confirm our telephone conversation today regardingsampling procedures and protocol followed during the Marchsampling on the above referenced project.

I Sampling protocol was explained by Phil Smith of CH2M HILL.* In general, samples were filtered in the field by pumping

water directly from the wellhead through a sample filter

I diaphram. Samples to be analyzed for cations (metals) wereimmediately acidified in the field with nitric acid ( 2ml

(. concentrated/liter). Sample containers were rinsed with

•

sample water prior to collecting sample. Sample apparatuswas decontaminated between sampling each well by rinsingfirst with deionized water, then with dilute acidic water,

_ and a third time with deionized water. Splits and dupli-• cates were taken of selected wells for QA. Duplicates were™ collected in series immediately following each other. Splits

were collected in a single vessel and then divided between

I two smaller vessels. Initially two each 1-liter sampleswere collected; one was acidified as stated above, the otherwas not, which required special analytical service (SAS).

•

Selected wells were sampled for radionuclides; this con-sisted of a 1-gallon sample which was not acidified.

In general, each well was to be pumped by pumping five casingvolumes before collecting a sample. In cases where the pro-ductive capacity is so low that it takes many hours to pumpthe well to this extent, they were to be excavated severaltimes prior to sampling. These wells are identified below.In some cases where productive capacity of certain wells waslow an alternative criteria was offered by the EPA,: i.e.,to pump the well until both pH and conductivity stabilize.It is noteworthy that, considering the construction of someof these wells, this criteria does not guarante that a freshsample of formation water is obtained. On a purely volumebasis, with 4-inch casing in a 12-inch hole, neglecting porespace, five casing volumes would barely evacuate the wellbore. This would also result in a temporarily stable pH andconductivity in the discharge from the well head.

IIIIIIIIII(,IIIIIIIII

MEMORANDUMPage 2June 21,1985W66215.00

Sampling conditions were adverse with wind gusting up to70 mph carrying dense clouds of radioactive dust off thetailings ponds which have now dried out. Sampling undersuch conditions should not have been attempted perhaps, butbudget and time constraints forced completion of sampling atthat time. Due to these adverse conditions, sampling timeson some wells were protracted and it became necessary tofilter some samples in the laboratory rather than the fieldin order to save in filtering time. Those samples are iden-tified below as well.

In each case, both before and after sampling; pH, conduc-tivity, and temperature were measured. The table below sum-marizes sampling conditions of wells where the protocol wasfollowed without deviation:

Cv

O

Well ft Date Time

41013141521222324252822A

3/28/853/28/853/29/853/28/853/28/853/26/853/26/853/28/853/27/853/27/853/28/853/26/85

11:0014:4511:009:4812:56

13:2214:3014:3017:15

pH T(°C)

6.96.66.85.66.26.96.46.36.86.47.06.5

1413111113

1312121212

Conduc-tivity

2940315027802300240012003900300023OO210035001380

SWL(ft)

2061641515710322542241414821

Volume(Gal)

190220255680810990717838

excessexcess760168

The following summarizes data from wells where less thanfive casing volumes were pumped due to the extremely lowproductive capicity of the wells. In each case, the wellwas "blown out" two or three times during the days precedingsampling. Otherwise normal sampling procedures werefollowed.

MEMORANDUMPage 3June 21,1985W66215.00

Well # Date Time pH

23576891819202627

3/29/853/29/853/27/853/27/853/28/853/29/853/29/853/29/853/29/853/29/853/27/853/27/85

15:3015:309:4115:2413:5712:4413:2713:3011:009:45

6.55.97.56.53.97.77.77,87.66.86.79.0

131413141311111312131313

Conduc-tivity

29203450320045004890152530002900260050006000

SWL(ft)

118107153226165165174

4545

Volume(Gal)

135612015020

<10<104

<101510040

c\;

The following summarizes sampling data from wells which werefiltered in the laboratory rather than the field due to timeconstraints and adverse field conditions:

Well #

11112

*504B610611621*625

Date

3/29/853/29/853/29/853/29/853/29/853/29/853/29/853/29/85

Time

16:33

pH

6.16.76.42.74.86.54.8

T(°C)

1191210

1110

Conduc- Volumetivity SWL(ft) (Gal)

2302900 2103180 152200 blow out4900 constant pumping2900 constant pumping3800 constant pumping4300 blow out

*These wells did not have pumps in them. They were routinely sampled by

evacuating the casing with air and then collecting a sample by bailing.

IIIIIIIIIIrfIIIIIIII

MEMORANDUMPage 4June 21,1985W66215.00

Well £12 is a dry hole and Well #16 could not be sampled formechanical reasons. Surface water samples were collected atfour points on the stream in Pipeline Canyon and at BorrowPit #2. These samples were filtered in the laboratory.

QA & QC samples were taken as duplicates and splits of fieldsamples and blanks of different lots of sample results andfilters respectively. The following table summarizes thesesamples:

Sample Pt,

610

6101313202099

1515

Sample No's

MW51, 53MW52MW54, 610MW55, 56MW57MW58MW59, 60MW61, 62MW63MW64MW50MW15,65MW66

Designation

SplitBlank 35063032DuplicateSplitDuplicateDuplicateSplitSplitDuplicateBlank lat filtersBlank 35063042SplitDuplicate

r •

CV

C

UNC collected duplicates of all of our samples and EID col-lected duplicates of most of them. A copy of the resultsfrom UNC's sampling is enclosed. It should be noted however,that many of UNC's samples were filtered in the laboratoryrather than in the field at the well head.

A second sampling round occurred one month later during theweek of April 30, 1985. The same general procedures werefollowed as for the first round, however, weather conditionswere significantly better. A summary of sampling data forthose samples were the preferred protocol is followedwithout deviation is given below:

Well # Date Time £H T(°C)

41057

4/30/854/30/855/2/855/3/85

18:3017:0017:3010:00

~

6.75.47.26.6

15171414

Conduc-tivity

3050350031503700

SWL(ft)

207163119107

Volume(Gal)

14326496185

IIIIIIIIIIiiiiiiiii

MEMORANDUMPage 5June 21,1985W66215.00

Table (cont)

Well # Date Time T(°C)

11131415212222A2324610611621625

5/1/855/1/854/30/855/1/855/2/855/1/855/1/855/1/855/2/855/2/855/3/855/3/855/3/85

11:0011:4018:0014:0014:0016:1515:1517:5012:159:4511:0011:1511:30

6.45.85.96.37.27.27.36.86.52.54.76.25.3

16151416131514141512141412

Conduc-tivity

3750380026002800110044001800460023504800320043007500

SWL(ft)

143149571032355212441

41

Volume(Gal)

241201106830007354401691100257CPCPCPCP

Due to the low productive capacity of certain wells, therequired five casing volumes could not be produced prior tosampling. In each case however, the well was "blown out"two or three times prior to sampling as described above. Inall other aspects the protocol was followed. A summary ofsampling data for these wells follows:

Well # Date Time T(°C)

1236891218192025262728

4/30/854/30/854/30/854/30/854/30/854/30/854/30/854/30/854/30/854/30/855/2/855/2/855/2/855/2/85

14:2415:4716:3018:5016:0015:4014:2015:0016:2012:4913:0015:3015:0015:00

r- .

9.87.26.33.66.65.66.75.85.56.56.56.86.97.5

1514161214151616151314131414

Conduc-tivity

29003080289050002800400041005000335063002150470036003350

SWL(ft)

2301851181532261661611651864342454548

Volume(Gal)

>35163181023117>16

53

V,

C<v!

Cc.

IIIIIIIIII

IIIIIIII

MEMORANDUMPage 6June 21,1985W66215 .00

The following samples were filtered in the laboratory be-cause no pumping facilities were available at the samplesites:

well # Date Time T(°C)

MW16MW504BculvertculvertculvertSPltBP#2

#1#2#3

5/3/855/3/855/3/855/3/855/3/855/3/855/3/85

13101616171716

:00:30:20:00:00:20:45

5.6.8.7.8.8.8.

7826632

15132525262520

VolumeSWL(ft) (Gal)

bailedbailed(2)

Conduc-tivity

43002500

7201100670720

5300

In addition to the standard suite of samples summarizedabove, three organic samples were collected from wells 610,611, and 625. These consisted of two each 1/2-gallon amberbottles and one each 40 cc glass vial for volatile organics.These samples were packed in ice immediately and shippedovernight via Federal Express to the laboratory.

As with the first sampling round, a set of QA/QC sampleswere prepared with this set of samples. A summary keyfollows:

C

Sample Pt.

MW611

MW611MW13MW13MW20MW20MW28MW28

MW15MW15

Sample No's

MW51, 53MW52MW54,611MW55,56MW57MW58MW59, 60MW61, 62MW63MW50MW15, 65MW66MW67MW68

Designation

SplitBlank 35063032DuplicateSplitDuplicateDuplicateSplitSplitDuplicateBlank 35063052SplitDuplicateBlank 35063042Blank 35063022

It is noteworthy that the sampling protocol is not designedto obtain absolute accuracy in analytical values, but ratherrelates values for comparison. Precision and uniformity in

IIIIIIIIIIIIIIIIIII

MEMORANDUMPage 7June 21,1985W66215.00

sampling are therefore paramount. The values obtained withthese methods may yield results which could be low comparedto absolute values. It is therefore recommended that futuresampling aimed at development of baseline valuesincorporated the use of more modern equipment to obtain moreaccurate absolute values. Such equipment might includedown-hole sensors for measurement of thermodynamicconditions and down-hole thief samplers for collection ofsamples under pressure for determination of dissolved gases.

The use of such methods and equipment is both time consumingand costly; budget considerations would therefore have toreflect these additional expenditures if these new methodsare adopted.

SLC53/08

192/t? I * 3

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KERR HC GEE AND STREA1 FICU DATA

MC GEE SP SELCU SP CUL'.' CULV 111 CULV 82 CUI.V 13 CULV »3CAFE OUT FLOU OUT FLCU HI IN OUT OUT IN OUT SP SI SP »2 iP *3

17 FEE 65 2624.85Id FEB 35 2552.531? FEB 85 2493.5228 FEB 85 2561.3121 FEB 65 2547.3322 FEB 85 2538.7623 FEB 85 2445.6124 FEB 85 2576.8625 FEB 85 2582.8? £'•' .26 FEB 35 2474.8327 FEB 85 2425.5628 FEB 85 2563.3981 MR 85 2548.4282 MR 85 2588.9483 MR 85 2472.26 r-84 MAR 85 2587.33 ^85 MR 85 2548.42 . O06 MR 85 .1374.18'8? MR 85 .M87.4388 MP 85 ;:466.968' M: 85 2466.96H MR 85 2483.2311 MR 85 2529.9412 Ml! 35 2663.8613 MR 85 2467.23H ME 85 261,.4115 MR 85 2495.7516 MR 85 254V.8517 MR 85 2577.3718 MR 85 2521.7219 MR 85 2521.8220 MR 85 232?.862- MR 85 2396.1522 MR 85 2418.9623 MR 85 2585.8824 MR 85 2435.6425 BW 85 2531.5526MR 85 2351.432? MR 85 2428. J62f MR 85 2514.682? MR 85 2455.593P MR K 2581.363! MR 85 2494.8381 APR 85 2488.9482 APR 85 2587.8783 APR 85 2325.8784 APR 85 2438.2385 APR 85 2451.4986 APR 85 2452.6207 APR 85 2456.7438 APR 85 2479.748? APR 85 2533.4218 APR 85 2455.3811 APR 35 2512.?412 APR F 2376.8313 APR 35 2W.8414 APR 6S 243?.1715 APR 8h 2447.?!)16 APR 85 2564,1117 APR 85 2419.9818 APR 85 254-:.3619 APR 35 2569.3!29 APR 85 25«*.7221 APR £5 2633.^522 APR 35 2518.N23 APR 35 2536.4-i2-5 APR 85 2651.3425^;:R S5 M3>V?326 AP5 S5 25!v.2827 API? 35 2437.322S APR 85 2-!??. 1529 APR 85 2526.2/ '••« APf; J5 2511.52

111

11•

1•

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MC GEE Sp BELQU SP CULV CULV ill CULV «2 CULV n CULV 13DATE OUT FLOU O'JT FLOU ftl IN OUT OUT IN OUT

81 MY 85 24 .'5. 9382 hAY 85 24?7.5783 MY 65 2628.2484 MY 85 26-'9.54 2655 2982 383285 MY 85 2JI9.29 2571 254186 MY 85 2564.3287 MY 85 2557.6788 MY 81) 2548.6889 MY 85 2f63.5918 MY 85 2535.38 2671 2885 3864 2746 271711 MY 35 2516.32 238112 MY 85 2511.1213 MY 95 2528.7314 MY 85 2542.2415 MY 85 2458.6516 MY 85 2531.9517 MY 85 2482.3918 MY 85 2471.4319 HAY 95 2472.422* MAY 85 2581 .8521 MY 85 2<24.4222 MY 85 2518.9723 MAY 35 2499.5924 MY 85 2479.3825 WY 35 2438.4226 MY 85 2467.8727 MY 35 2454.7628 MY 85 2f.83.5929 WY 35 L'456.7838 W 85 2488.7831 MY 35 2549.6281 iW 85 2551.7882 Jill 85 2548.6883 Oil 85 2145.1864 JUI 85 2612.9885 JIM 85 2391 .8906 ilW 85 2449.8787 JIM 85 2452.1788 JUT' 85 2<21.78 2288 225389 jUK 85 2576.8618 JIM 85 2565.6711 m 35 2725.8612 JIM 85 2496.5813 JLN 85 2545.7714 Jl)N 85 2*19.6815 JUM 85 2683.3416 JIN 85 2636.8417 JIN 85 2489.58 3841 2819 1495 1983 2635 168718 JUN 85 2571.18 3424 3516 2989 4322 1888 229818 JUN 85 2571.18 3388 3125 3315 4322 2783!•> JIM 35 2527.59

#'£ FLW 2515.69

fc

SP it! SP d2 SP «3

2459 2261 2225

2548 2584 2867

2249 2298 22893448 2598 29722686 2353 2229

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DATEMYMAYMA Iff1AYmJLNJUNJLN

HAYKAYmit-'AiJLNJIMi;lMUN

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COLLECTEDA

DATA:B

MC GEE SP BELOUOL(T FLOU OUT FLOU

85 2679,5485 2619.2985 2535.3885 2516.3285 2621.7885 2489.5885 2571.1885 2571.18

DELTA FLOW

85 2679.5435 2619.2985 2535.3885 2516.3285 2621.7835 2489.5885 2571.1885 2571.13

AVERAGE

NOBttUZED

85 2679.5485 2619.2985 2535.3885 2516.3285 2621.7835 2489.5885 2571.1885 2571.18

AVERAGE:

2381

384134243388

(02-01)

-135

632853729

519

FLOU:

8.946

1.2621.3321.283

1.286

ANALYSIS

CSP CULV

81 IN2655

2671

281935163125

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-25

136

418945554

484

8.991

1.853

1.1781.3671.215

1.159

DCULV Hi

OUT2982

2885

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278

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338744

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1.186

8.84?8.6281.1311.289

1.812

ECULV »2

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3864

198343224322

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775

1.132

1.288

8.7981.6811.681

1.298

FCULV 03

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25712746

26351888

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AVERAGE NORMALIZED FLOU• 2565.521 528 469 31 765 -9J

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STATION FLOWS AS AVE. OF ALL DISCHARGE FLOUS2515.69 3844 2925 . 2547

AVE. NOW. DELTA3281 2425

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STREAMLINE FLOWTotal Station Flow

5/5

4 ,-r 6 8_ (Thousands)

_ DISTANCE DOWN STREAM (FT)5/10 A 6/17 V 6/18

10

v 6/18p

• STREAM FLOW DATA DATE &? - S ~£&~

CULVERT # 1 Discharge 1" from the end

1 s^ ~~\

1 / \ 12"

_, — „ , ?ii" 'i \~ j-+\ f /

I \ -7-7 /

V '"'- y'\^^ ^^X ?ty

Velocity & , Z fp's

flow Q= 4 92 cfs

rro B gpmI* %

1CULVERT 1 2 Discharge 61 from the end

• . "

1 / \ 30"

I ! c o - ^ !1 ,, ° / '/ f1 . ^ ^/ \

m CULVERT # 3 Inlet 6' from the end

1 -'" N\ 20%"

• 4- ' 14i . - J

1 . ' /

1 - -'"

t

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\ gpm

\

Ve1ocity\ fps

flow Q= N^ cfs

\ gpmX

• Discharge 1" from the end

1 .X '" "\

• / \1 / \ 2035"' ' 1

I . /'» •-< c1 '•

i \ " y „

Velocity fc?'£3 fps

flow Q= S".o2 cfs

-^^^^ gpm

C

DATE , TIME ^ tj '• '- 'sWlPLE POINT • / / • ,.. ' _ Stream width j'\ 1n. Number of sections

DATUM

5"

10"

20,,

SURFACE

!OTTOM

)EPTH

Of

'ELOCITY fps_

10W cfs

SECTION WIDTH

OMMENTS:

in.TOTAL AREA - . , / TOTAL FLOW: j i T T c f s , AVERAGE VELOCITY fps

DATEf? TIME '. 3 'J '- f ' ^AM'PLE POINT £u/v "I ,„[. Stream width SV3 In . Number of sections BDATUM

5"

10"

15'

20"

SURFACE

IOTTOM

)EPTH

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LOW cfs

SECTION W I D T H in.TOTAL AREA TOTAL FLOW:

OMMENTS:cfs, / '.-/:• gpm AVERAGE VELOCITY .;'. fps

| STREAM FLOW DATA DATE /7 JL< <§"<"" j*<ar~.

CULVERT* 1 Discharge 1" from the end

1 /-^ ^^

1 / \ 12"

/ 1 1. . ._ ?4"

i V MI \ — • • *^_ ^/ -.,

Velocity Tr — fp's

flow Q= /' - . • cfs

: . gpm

\CULVERT f 2 Discharge 6' from the end

1 ^ ^-^x

1 / \ 30"

1 ' rn- ' v '

-I I I- \ , - ' / \1 v s 41 CULVERT 1 3 Inlet 6' from the end

i ,-' N\ 20V

1 •' ' \m 1 yf£

1 M:" \ 1, /V /

\ ^"— -^

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flow Q= •') f':j/ cfs

?•• '•,'• gpm

tic*

Velocity ^> <f fps

flow Q= £T>£>7 cfs

% y :-,;-/ gpm

z* **-

m - - ••Discharge 1" from the end

1 /-^ ^x.

1 / \ 20V

/ 1 5?S"

I -T . -r '„. , . , . jt i ii ' - -tz<; AL.i v. -' y

Velocity <^-O fps

flow Q= 3, £18 cfs

^

76-7

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i i tin imi MIT

SAMPLE POINT " / Stream width .• : 1n. Number of sections V l

DATUM -px

5"

10"

15"

20"

URFACE

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EPTH

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LOW cfs

•y/.

SECTION WIDTH in.TOTAL AREA

OMMENTS:TOTAL FLOW: •','/ cfs. _gpm AVERAGE VELOCITY -/-. i fps

DATE TIME *~" • l/_ " SAMPLE POINT Stream width

DATUMin. Number of sections

xn

5"

SURFACE

BOTTOM

DEPTH

AREA

I Zl

VELOCITY fps_

FLOW cfs

SECTION WIDTH in.TOTAL AREA TOTAL FLOW:

COMMENTS:cfs, gpm AVERAGE VELOCITY /... -, • 'fps

DATE . . . - . -

DATUM

TIME -;- ty •'- L SAMPLE POINT Stream width 1n. Number of sections

iURFACE

iOTTOM

| >EPTH

.RE A

ELOCITY fps .

LOW cfs

SECTION WIDTH in.

OMMENTS:TOTAL AREA TOTAL FLOW: v •',% cfs, _gpm AVERAGE VELOCITY fps

J 17 ,1 L U 0hlHEHM J-l <)W DATA

DATE TIME : SAMPLE POINT-DATUMUM 1 Un s. - - - - - - - - . _ - - _ _ . — . » _ . _ _

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7,

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DATE

DATUM

5"

SURFACE

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IREA

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Stream width in. Number of sections

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10W cfs

SECTION WIDTH . in.TOTAL AREA ^_

OMMENTS:TOTAL FLOW: cfs, , ' - ' _ 5 : ' • gpm AVERAGE VELOCITY fps

STREAM FLOW DATA DATE

IIII

I

I

I

IIIII

CULVERT # 1 _ Sfoforry 1" from the end

CULVERT # 2 Discharge 6* from the end

CULVERT #3 Inlet 6' from the end

20V

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41"

20V

!-!-

i

Velocity

flow Q= -

fps

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Velocity

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fps

cfs

gpm

Velocity

flow Q=

fps

cfs

gpm

Velocity

flow Q=

fps

cfs

gpm

cIf.

C

IIIIII

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STREAM FLOW DATA DATE

CULVERT # 1 Discharge 1" from the end

CULVERT I 2 Discharge 6* from the end

CULVERT i 3 Inlet 6' from the end

14 ?*'

Discharge 1" from the end

Velocity

flow Q =

Velocity _

flow Q=

_fps

_cfs

.gpm

_fps

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_gpm

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/Q o o gpm

Velocity

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fps

£./:

_cfs

gpm

O

DATE

DATUM

TIME A- S'WPLE POINT Stream width /.-•/ 1n. Number of sections

:URFACE

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lEPTH

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LOW cfs

SECTION WIDTH in.TOTAL AREA

OMMENTS:TOTAL FLOW: ?.-:..fl cfs. : - '. // gpm AVERAGE VELOCITY '/,'- fps

.3

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DATUM ^ I T fi_

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OMMENTS:gpm AVERAGE VELOCITY fps

.-» i m.Mi'i r I IIM DM IM

DATE

DATUM

TIME V is L Ly SAMPLE POINT Stream width // in. Number of sections

5"

10

SURFACE

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7

SECTION WIDTH in.TOTAL AREA TOTAL FLOW:

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DATE

DATUM

TIME *-• SAMPLE POINT•••/!, /•' Stream width : In. Number of sections

5"

SURFACE

BOTTOM

DEPTH

AREA ''

VELOCITY fps_

FLOW cfs

SECTION WIDTH

COMMENTS:

in.TOTAL AREA v. TOTAL FLOW: ' '•'-. cfs. ? -v H .. gpm AVERAGE VELOCITY / fps

DATE

DATUM

TIME '*' b~ " *• ;SAMkE POINT--/. "• : - S t r e a m width In. Number of sections

SURFACE

50TTOM

)EPTH

VREA

'ELOCITY fps

LOW cfs

SECTION W I D T H in.TOTAL AREA

OMMENTS:TOTAL FLOW: .-'. -'if. cfs, .'( ''•' • . •'• gpm AVERAGE VELOCITY / fps

II

IIIIII

I

I

IIII

STREAM FLOW DATA DATE

CULVERT # 1 _ntsf_hap§e 1" from the end

CULVERT if 2 Discharge 6' from the end

CULVERT # 3 Inlet 6' from the end

Discharge 1" from the end

Velocity

flow Q=

Velocity

flow Q=

Velocity

flow Q=

Velocity

_fps

_cfs

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fps

-Cfs

gpm

fps

cfs

gpm

fps

flow Q = c f s

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**-,-•

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STREAM FLOW DATA DATE ~ IS -

IIIIIIII

1

III

I

CULVERT i 1 Discharge 1" from the end

CULVERT I 2 Discharge 6' from the end

CULVERT # 3 Inlet 6' from the end

Discharge 1" from the end

Velocity

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Velocity

flow Q=

Velocity

flow Q=

Velocity

flow 0=

_fps

cfs

/PS

_cfs

gpm

_fps

_cfs

gpm

fps

cfs

gpm

ec

L O OSTRFAM FinW DATA

DATE • TIME SAMPLE POINT / Stream width „ In. Number of sections •HATIlM

5 n . . . _ _ _ _ _ . _ .

.

10

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2QH

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'FLOW cfs

SECTION WIDTH in.TOTAL AREA

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, , , , •• . , i->, STRFAM Fl nw DATAU ^ /.. i. J U _ _ -

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MU-1515D21SD2R1SD315041505150415D4R15D715D7RISP15PR

MU-21 2101'21D1R210221D2R210321D3R21P21PR

MU-23 2301230223032303R2304

.2304R23P23PR

MW-28 28012802280328042805280R28P

GPM

511

15212521

18

15

11

15

14

12

111521

15

11

2448

11

5

DATE

17 HAY 8517 HAY 85

17 HAY 8517 HAY 8517 HAY 8518 MY 85

18 HAY 85

11 HAY 85

18 HAY 85

18 HAY 85

18 HAY 85

21 HAY 85

19 JUN 8519 JIM 8519 JIM 85

11 JIM 85

13 JIM 85

31 HAY 8531 HAY 8531 HAY 8531 HAY 8531 HAY 85

12 JIM 85

TIME

15:4114:88

16:4117:2418:3318:34

18:28

13:28

11:23

11:45

14:17

21:38

11:2712:3113:48

21:41

13:11

15:1114:4818:1119:3121:47

12:31

METER

1113.31191.1

1344.31473.92484.43234.8

5191.5

21112.8

,

3499.2

4144.2

4915.9

24944,3

77454.878115.179175.1

84715.1

245197.8

4871.57195.17383.17947.48552.2

9814.8

DATE

17 HAY 8517 HAY 85

17 HAY 8587 HAY 8517 NAY 85IB HAY 85

19 HAY 85

14 HAY 85

18 NAY 85

18 NAY 85

19 NAY 85

23 NAY 85

19 JIM 8519 JIM 8519 JIM 85

U JIM 85

15 JIM 85

31 NAY 8531 HAY 8531 HAY 8531 HAY 8531 HAY 85

IS JIM 85

TIKE

15:5814:19

17:1218:1119:1219:59

18:59

17:19

11:35

'12:39

14:31

19:11

12:3113:4821 Ml

13:11

24:11

14:4118:1119:3121:4723:17

13:21

•

METER

1191.11382.2

1443.12441.13121.94782.8

21112.8

141491.9

4144.2

4915.9

24944.2

73931.1

78115.179175.184715.1

92321.1

311153.8

7895.87383.87947.48552.29814.8

31423.8

GALPUHP

87.8111.1

298.7787.1437.3

1548.8

14811.3

119388.1

447.8

739.7

28838.3

48985.7

458.21878.87548.8

5484.8

3S854.8

223.5288.8544.4484.4

1242.4

21489.8

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8879

78

54

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4378

412

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RATE

5.1418.18

14.2217.8921.9818.21

18.38

13.45

9.53

13.78

13.79

11.48

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14.75

18.44

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4.94

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IIIIIIIIIIIIIIIIIII

---- ptJMPING TEST L-0G

DATE i- -J

TIME

TIME

pH Conductivity

FLOW RATE <? 3 hr intervals

VOLUME / ZoQ €T,&

RATE ±T 3/«M 4.3 3/,n

WATER LEVEL @ 6 hr intervals

WELL TIME DEPTH TIME DEPTH

632 /• . )C Z^ '^-%5' 'Cj',47 7^4'^

GW2 i 4r? ' \*k J3'&£ Ao G

£-,, ^/^

crnMMFNT^ ^'

, " C-' c.

GW1 4£ ' Z " Z&.&\ 45 * 3%

28 i - ' /7' /0-"?. 10,0^ --5"_3 4

26 -M J-"~ ZO\Zl dA ? '

27 ! 4~'l ^ '' -ZO\Z£ (\L\ ~Z ,

/)

625 t/w"- ^/ z.<^> '.3 <^£> 3 ^^

628 , : ' -, ^" 2o\1.c\ ^/|<5"- :

629 1 ^(f /5~^ 26'. %£ 4' ^-^

630 ; 4/V^ 2o;si '(\' £~t631 : 4 / ' Xj' J-^'^C' <1l' "/^

624 ,...^. :•>•/<}' Z°A\ S?' S

RECORDERS 9 6 hr intervals

TIME READING TIME READING

CHOO ?<?\\qa\ /-?,^o I'f'MM /4;&l

CHOI / 5"- 28 • .^"??

CH02 ] /0.7Z / ^<? ti ,

CHOS 4, ft- &;44-?( a.±<-CH04 /^iapiof /a ^C-*

fc*

5?

/z

DO NOT let CHOO fall below a read inof -6-5 • . ..I.f_.th.1S point .is.reached turn off the pump and monitthe well recovery.

• •"""fruMPINGTgST-LOG --------

DATE

TIME Conductivity 3

FLOW RATE'.2c.; Sc )

TIME y .b r

VOLUME

RATE - r V x-. -

3 hr intervals

y. 7s. <'.-'.}/

/.5V

WATER LEVEL 9 6 hr intervals

WELL TIME DEPTH TIME DEPTH

632

GW2

GW1

28

26

27

. o/-S5

625 &?:•>? •y'C'yj

628 ;. :t? *V/V-?Y

629

630

631

624

4) 5-/I I

RECORDERS 0 6 hr intervals

TIME READING TIME READING

CH04 ij

/</7V'<

- */v

os1. iz.1

COMMENTS

4 1 i'/?

DO NOT let CHOO fall below a readinof •6-5-_- If.JthJ.S point ijreached turn off the pump and monitthe well recovery.

IIIIIIIIIIIIIIIIIII

PUMPING TEST'liOG

DATE-S .,1.*;

TIME Q^f '. i # PH Conductivity

FLOW RATE

TIME S>\ <• Z

VOLUME.

RATE

3 hr intervals

. >-^cy t?w

44' 7

WATER LEVEL P 6 hr intervals

WELL TIME DEPTH TIME DEPTH

632

GW2

GW1

28

26

27

625 oft'.38

628 <£>S.34 41

629 oQ'.fc 4/'

630 oS

631

624

COMMENTS co

..\5".g3

4|'S V

27

RECORDERS @ 6 hr intervals

TIME READING TIME READING

CHOO o?.J9

CHOI

CH02 ,71

DO NOT let CHOO fall below a readlnof -fi-5- If_thisL point ll..__reached tjrn off the pump and monitthe well recovery.

4.

CH04 . 47

1111111111111111111

PUMPING TEST LOG

DATE- < TV//T/ 5?^-

TIME J{/'Jf JJH ',• (f- Conductivity j' '/c C

FLOW RATE 9 3 hr intervals

TIME .IC--3L J,'3.*0 ,".-./..<; 0; 'ft,'-

VOLUME /-/Jco xcYj ' / ,S/L^'n Xt?/?

RATE V. 9,2 .r.(-' 5V.' Y.?/ ^

WATER LEVEL @ 6 hr intervals ^

WELL TIME DEPTH TIME DEPTH rnMucurc "

632 ^;/<?^ ^24 •T'/ ±>; 'V*7 7£j">V C.'/

GW2 .xK'.y.? v^-1'/'^ o / ' -5 -3 : -..t'-'^'"

GWl ,^/V? ^5- S^ ^ C ; :. 6 'V.5'v^

28 Zc-17 &]W CL^U ^^'f

26 JC::W <;</'• ? .£..^3. *r<r'*-s S i - Y ? -*'''i?J ^ . < Z7 *-*<•*

27 <%) : yf 4y '3 3? ; .-. ;.-j **<-&• -* » W *** '* '% " "<- * '.•'•*.*. -v -

625 ^/;OJ V£: yJe'os.c.v vvV*" %Z?"~'Z'~*l,.f_f

628 .fo-'5<ri s ' / ^ v ' r ?-'••;•!>' * ; / ( • ' -

629 ^:^V •V / t f . 4 "62 :S£ , ^ / &£' '

630 j^6"-57 V/ '.5 £•"/••)! : S ? <ji'f:'3f'

631 ^ A' o <x V/ / f '' o i . ," / v/ V V-, - / . ^ _ . > . - .

624 c// •'/•?' O/ X ? *> I" './. ' • ' • • 7 : - - V ' '•"w'" " '- '---V T-i*,^./?.) e.;.r« ;..-....t. .

RECORDERS @ 6 hr intervals Je45 "^"T'A"'-0 ^cc^r^. >X-0

TIME READING TIME READING •'•'-.^ ""^'t*' ''"-« «-" /* i ,-

CH00^^2?» /(f-.r, 7 -'- ox. . '/ T;- DO NOT let CHOO fall helow a rearffpof -6tb-_._I_f_th.tl. Ppint is_

CHOI ! _. 5" 5 / .,.,.$! .tr , reached turn off "the pump and morH>/ / the wel 1 recovery.

CH02 1 /C. 7t \ /O. 71

CH03 I V 5^ 1 Y f 5

CH04Y/^7 /.. . /' J ,-...i'j / : . . : •••

*

IIIIIIIIIIIIII1IIII

&Sf LOG ---

DATE

TIME OS.' (4- PH _ < £ ? . Conductivity

FLOW RATE 0 3 hr Intervals

TIME <:>g:ar io\\\ MIVOLUME_

RATE

•(

4 • S"g-Jl

WELL

632

GW2

GW1

28

26

27

625

628

629

630

631

624

WATER LEVEL <? 6 hr intervals

TIME DEPTH TIME DEPTH COMMENTSC

C.

Z-

,f

41 '

41 7

RECORDERS @ 6 hr intervals

TIME READING TIME READING

CHOO

CHOI

CH02

CH03

CH04

gj.gg

. 7f

DO NOT let CHOO fall below a readtnof ~6 • 5.-_ . If .th1 s po i n t isreached turn off the pump and monitthe well recovery.

/4lce) 4 . ST

IIIIIIIIII

IIIIIIII

PUMPING TEST LOG

DATE "V V.5

TIME PH (••''• 3 Conductivity y c •':

FLOW RATE @ 3 hr intervals

TIME

RATE •V. 9gWATER LEVEL <? 6 hr intervals

WELL TIME DEPTH TIME DEPTH

632

COMMENTS

GW2 J^-'jj <VL>''.J% A -OX 40 'Jk"

cc:

26

27

625

628

629

630

631

624

Jc : 5.5 - • y.5

VS?

RECORDERS @ 6 hr intervals

TIME READING TIME READING

CHOO

CHOI

CH02

CH03

CH04

/0.7V

V. 5V

DO NOT let CHOO fall below a readinof -6 •5 •.. I.f._th1 s|_ poi nt i $reached turn off the pump and monitthe well recovery.

io.

I

II

II P U M P I N G TEST LOG

I DATE 5~ Ji*4 gfeT

TIME <3 g'. £ 7 pH <£? .^- Conductivi ty

• FLOW RATE 0 3 hr intervals

TIME <?#'.z > i : 4 o• VOLUME,

RATE

| WATER LEVEL 0 6 hr Intervals^ 'i<Zc? r

WELL TIME DEPTH TIME, DEPTH COMMENTS C

I 632 e&'Al Zt» <~'k IQ\ 32> Zt* &/& ^

GW2 a8.'4fe 4o'

GW1

I26

I625

28

• 628 C^jlg. jjf

629630

| 631 ^'.tfe 41' Z" IS'.^f 4T i '

I

I

RECORDERS @ 6 hr Intervals

TIME READING TIME READING

CHOO g^ioo -<p.qo /4!/^f / 7 .g<^ DO NOT let CHOO fall below a read Inm of -6.5. J_f .this; point is . _I CH01 I 5^26^ | $• 'B reached turn off the pump and mbnlt* the well recovery.

CH02 V /Q.75" ' io, 1& „ ±m C^°v -^'^ — ° - 7.2

CH03

CH04

IIIIIIIIIIIIIIIIIII

-W4MWNG TES-T--LOG-

DATE 6 'ft 5

TIME

TIME

PH Conductivi ty

FLOW RATE 0 3 hr intervals

VOLUME_

RATE

WATER LEVEL @ 6 hr intervals

WELL TIME DEPTH TIME DEPTH

632 Jo-.ff ?(„'(,%.'

GW2

; (a (a

GW1 2Q'.U>

28 2Q-.33

26 1D:</J>

27

625

628 2DL £132 Hi

629 JQ-.5&

630

631

624

J:3<?

37'/ 37't l'

RECORDERS @ 6 hr intervals

TIME READING TIME READING

CHOOdtoo}

CHOI

CH02

CH03

CH04

3: On /t-63

5.1

/a. So

5^55

' . • / / /d?.fa/

s?

COMMENTS

C

DO NOT let CHOO fall below a readfnof '6-5.•._..!£_ this, point isreached turn off the pump and monitthe well recovery.

IIIIIIIIIIIIIII/<£": •

I; a 0

1

PUMPING TEST LOG

DATE

TIME

TIME

PH Conductivity

FLOW RATE 0 3 hr intervals

VOLUME_

RATE

"&' 7"

*>$\

ff'i V44 ' '

WATER LEVEL @ 6 hr intervals

WELL TIME DEPTH TIME DEPTH

632

GW2

GW1

28

26

27

625

628

629

630

631

624

COMMENTS

>' 7

Ccv

cc

'«»

7149

41 '

t" 4/

RECORDERS <? 6 hr Intervals

TIME READING TIME READING

CHOO

CHOI

CH02

CH03

CH04 &

//;oo

. -79

DO NOT let CHOO fall below a readlnof -6.5. I_f .this, point .1jreached turn off the pump and monitthe well recovery.

4,64,

IIIIIIIIIIIIIIIIIII

PUMPING TEST LOG

DATE 7 -A-n

TIME Conductivity

FLOW RATE 9 3 hr intervals

TIME

VOLUME_

RATE

WATER LEVEL <? 6 hr intervals

WELL TIME DEPTH TIME DEPTHf \ts 'f f

GW2 68'M? 40 4 f e /a-&

GW1

28

26

27

4s48' I JB" I8\

44' &.*>& tt

4'

625 pB'tb C\Q' &/%

628

629

630

631

624

fa'

l' i

RECORDERS 0 6 hr Intervals

TIME READING TIME READING

CHOO &) \oo

CHOI

CH02

/.<?.

COMMENTS

S'

c>

c.

DO NOT let CHOO fall below a readinof -6• 5._ __I_f_this_ppint.Isreached turn off the pump and mbnTtthe well recovery.

CH03 cO:

CH04 c£l

IIII

III

PUMPING TEST LOG

DATE tS -Su>A $<'

TIME pH Conductivity

FLOW RATE 0 3 hr intervals

TIME

VOLUME

RATE

WELL TIME DEPTH TIME DEPTH COMMENTS

| WATER LEVEL 9 6 hr Intervals

I

I

630

632 frBlZl j?£ &»% . c^ a ~

GW2 C&\tl 4o' I To

GW1 O&'&'Z

28

26

27

625 6&.ZI fa' *$ %

628

629

631624

RECORDERS 9 6 hr Intervals

TIME READING TIME READING

CHOO ^QC A9.gr DO NOT let CHOO fall below a readlnof .rAilL.. JJLthiS_pp1nt_1ls

CHOI _-___jEi^£L_ reached turn off the pump and monltthe well recovery.

CH02 A^<?P

I CH03 j-v.oc.

_ CH04

I

o r- '•

n o "••

21utll

6 V /o n

-w o> <o o

0 0

r» n

r\ p '. " "

I&*/£

2,88

6*3 7 Z. 73

' , 73

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C

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