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Appendix VI--Analytical Methods and Results
Nitrate
Nitrate was determined using a portable colorimeter (Hach Co., Model DR/1A, Ames, IA.) according to a cadmium reduction method modified to use gentisic acid in place of 1-naphthylamine. All necessary reagents were combined into a single stable powder pillow called NitraVer S Nitrate Reagent. The test registered both nitrate and nitrite (as N) present in a 2S ml water sample. In most cases, dilutions were not needed because the operating range 0-30 mg/l as N was used.
The samples were brought to room temperature (20° to 24°C as recommended) before analysis. Only a few samples collected from Clear Creek and well L26 required filtering prior to analysis. One reagent blank (using distilled water) and three nitrate-N standards (10, 20, and 30 mg/l as N) were tested prior to and following each group of samples or when the chemical reagent of one lot number was exhausted and that of another was started. The three standards were freshly prepared each month just before analysis from a stock 100 mg/l nitrate-N standard which was prepared every two to three months.
After each group of samples was analyzed, an averaged blank value was subtracted from each of the sample concentrations and the resulting concentrations were corrected using calibration curves of the nitrate standards. Corrected values that were less than 1 mg/l or zero were reported as <1 mg/l.
The results were converted by multiplying by 4.43 and expressed as mg/l nitrate-NO3 for this study. The results of the nitrate determinations are presented in Table A1.
Several duplicate samples were collected and analyzed for nitrate concentration in order to estimate the analytical error of the in-field testing equipment. The duplicates were analyzed by the Analytical Services Section of the Kansas Geological Survey. The reported accuracy of the automated cadmium reduction method utilized by the Section was 4 percent or less (Standard Methods, 1980). The difference in nitrate concentrations determined by the two methods ranged from 4 to 27 percent with the average difference being 16 percent. The greater percent differences were associated with longer holding times of some samples before nitrate analysis could be performed using the in-field testing equipment. Because samples analyzed using the Hach method were not preserved at the time of collection, the nitrate values reported were consistently lower than the nitrate values obtained using Standard Methods.
Table A1--Results of the nitrate, chloride, and specific conductance determinations.
Well No. |
1984 | 1985 | ||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
July 31 |
August 1-2 |
Sept. 24(a) |
Oct. 24 |
Nov. 27 |
Dec. 17 |
Jan. 22-23 |
Feb. 18 |
March 18 |
April 24 |
May 8(a) |
May 20-23 |
June 17 |
July 24 |
Aug. 15 |
||
L1 | Cl | 240 | ||||||||||||||
NO3 | -- | |||||||||||||||
SpCond | 2,900 | |||||||||||||||
L2 | Cl | 68 | 39 | 33 | 31 | 31 | 30 | 32 | 36 | 35 | 47 | 53 | 82 | 33 | 35 | |
NO3 | -- | 22 | -- | 13 | 13 | 11 | 12 | 14 | 15 | 47 | 85 | 237 | 15 | 19 | ||
SpCond | 1,270 | 945 | 920 | 920 | 928 | 935 | 934 | 935 | 941 | 1,122 | 1,183 | 1,649 | 947 | 940 | ||
L3 | Cl | 130 | 84 | 69 | 55 | 59 | 88 | 57 | 72 | 71 | 38 | 65 | 94 | 56 | 65 | |
NO3 | -- | 63 | -- | 28 | 33 | 39 | 27 | 34 | 33 | 15 | 31 | 38 | 28 | 27 | ||
SpCond | 2,380 | 1,560 | 1,530 | 1,227 | 1,363 | 1,885 | 1,252 | 1,617 | 1,575 | 757 | 1,333 | 1,950 | 1,263 | 1,400 | ||
L4 | Cl | 28 | 29 | 33 | 40 | 32 | 32 | |||||||||
NO3 | 13 | 15 | 18 | 139 | 38 | 19 | ||||||||||
SpCond | 902 | 895 | 969 | 1,263 | 988 | 960 | ||||||||||
L5 | Cl | 100 | 23 | 23 | 23 | 26 | 33 | 43 | 36 | |||||||
NO3 | -- | 14 | 14 | 20 | 20 | 22 | 26 | 22 | ||||||||
SpCond | 1,298 | 837 | 830 | 837 | 865 | 900 | 980 | 934 | ||||||||
L6 | Cl | 64 | 23 | 145 | 31 | |||||||||||
NO3 | -- | 19 | 92 | 22 | ||||||||||||
SpCond | 1,120 | 885 | 1,775 | 901 | ||||||||||||
L7 | Cl | 48 | ||||||||||||||
NO3 | -- | |||||||||||||||
SpCond | 1,030 | |||||||||||||||
L8 | Cl | 243 | ||||||||||||||
NO3 | -- | |||||||||||||||
SpCond | 2,195 | |||||||||||||||
L9 | Cl | 63 | 60 | |||||||||||||
NO3 | -- | 7 | ||||||||||||||
SpCond | 1,067 | 1,060 | ||||||||||||||
L10 | Cl | 48 | 49 | 34 | 33 | 38 | 33 | 39 | 51 | 49 | 63 | 64 | 69 | 48 | 51 | |
NO3 | -- | 30 | -- | 20 | 22 | 19 | 22 | 21 | 21 | 17 | 22 | 21 | 22 | 20 | ||
SpCond | 1,046 | 940 | 909 | 915 | 974 | 942 | 949 | 1,072 | 1,052 | 1,181 | 1,192 | 1,219 | 1,017 | 1,031 | ||
L11 | Cl | 74 | ||||||||||||||
NO3 | -- | |||||||||||||||
SpCond | 1,361 | |||||||||||||||
L12 | Cl | 190 | 164 | 162 | 189 | 182 | 175 | 173 | 161 | |||||||
NO3 | -- | 37 | 42 | 39 | 48 | 43 | 42 | 36 | ||||||||
SpCond | 1,735 | 1,565 | 1,617 | 1,725 | 1,700 | 1,737 | 1,665 | 1,625 | ||||||||
L13 | Cl | 32 | ||||||||||||||
NO3 | -- | |||||||||||||||
SpCond | 934 | |||||||||||||||
L14 | Cl | 72 | 43 | 81 | 76 | |||||||||||
NO3 | -- | 13 | 62 | 34 | ||||||||||||
SpCond | 1,128 | 960 | 1,227 | 1,135 | ||||||||||||
L15 | Cl | 137 | 96 | 101 | 110 | 93 | 127 | 112 | 107 | |||||||
NO3 | -- | 56 | 47 | 41 | 51 | 36 | 55 | 57 | ||||||||
SpCond | 1,620 | 1,353 | 1,360 | 1,488 | 1,316 | 1,620 | 1,410 | 1,390 | ||||||||
L16 | Cl | 112 | 108 | 107 | 105 | 107 | 103 | 96 | 96 | 103 | 104 | 104 | 100 | 107 | 99 | |
NO3 | -- | 43 | -- | 25 | 28 | 27 | 31 | 26 | 27 | 35 | 26 | 26 | 26 | 27 | ||
SpCond | 1,272 | 1,260 | 1,270 | 1,270 | 1,270 | 1,271 | 1,246 | 1,245 | 1,262 | 1,286 | 1,288 | 1,316 | 1,271 | 1,245 | ||
L17 | Cl | 52 | 57 | 60 | 58 | 57 | 57 | 50 | 56 | 53 | ||||||
NO3 | -- | 38 | 41 | 40 | 37 | 41 | 42 | 39 | 34 | |||||||
SpCond | 921 | 949 | 955 | 960 | 935 | 941 | 959 | 935 | 933 | |||||||
L18 | Cl | 121 | 125 | 118 | 111 | 103 | 100 | 95 | 102 | 115 | 124 | 114 | 123 | 115 | 114 | |
NO3 | -- | 38 | -- | 26 | 24 | 19 | 21 | 23 | 28 | 30 | 25 | 26 | 28 | 26 | ||
SpCond | 1,328 | 1,360 | 1,345 | 1,316 | 1,297 | 1,280 | 1,261 | 1,270 | 1,352 | 1,337 | 1,335 | 1,370 | 1,333 | 1,326 | ||
L19 | Cl | 144 | 116 | 93 | 89 | 95 | 100 | 145 | 155 | 196 | 187 | 180 | 149 | *116 | ||
NO3 | -- | 115 | 77 | 72 | 67 | 69 | 76 | 88 | 162 | 162 | 144 | 92 | 70 | |||
SpCond | 1,875 | 1,558 | 1,445 | 1,422 | 1,560 | 1,585 | 2,190 | 2,040 | 2,430 | 2,550 | 2,460 | 1,980 | 1,674 | |||
L20 | Cl | 77 | 84 | 66 | 69 | 68 | 67 | 70 | 69 | 63 | 61 | 69 | 70 | 68 | 70 | |
NO3 | -- | 90 | -- | 62 | 63 | 55 | 63 | 58 | 55 | 60 | 54 | 55 | 55 | 57 | ||
SpCond | 1,335 | 1,302 | 1,253 | 1,245 | 1,253 | 1,236 | 1,237 | 1,245 | 1,220 | 1,159 | 1,245 | 1,235 | 1,235 | 1,245 | ||
L21 | Cl | 96 | 97 | 83 | 87 | 89 | 88 | 79 | 88 | 104 | 98 | 99 | 98 | 95 | ||
NO3 | -- | 39 | -- | 23 | 24 | 20 | 22 | 24 | 28 | 27 | 27 | 26 | 28 | |||
SpCond | 1,210 | 1,181 | 1,168 | 1,160 | 1,175 | 1,145 | 1,145 | 1,152 | 1,220 | 1,220 | 1,227 | 1,210 | 1,219 | |||
L22 | Cl | 5 | 9 | 9 | 8 | 8.5 | 9 | 10 | ||||||||
NO3 | 18 | 15 | 18 | 19 | 14 | 18 | 16 | |||||||||
SpCond | 778 | 784 | 783 | 778 | 796 | 790 | 784 | |||||||||
L24 | Cl | *26 | 28 | 25 | *33 | 35 | 38 | |||||||||
NO3 | 21 | 20 | 19 | 26 | 25 | 23 | ||||||||||
SpCond | 877 | 865 | 864 | 955 | 961 | 947 | ||||||||||
L25 | Cl | 30 | 71 | 45 | 42 | 38 | ||||||||||
NO3 | 27 | 78 | 48 | 35 | 33 | |||||||||||
SpCond | 947 | 1,298 | 1,047 | 1,030 | 1,010 | |||||||||||
L26 | Cl | 23 | 23 | 63 | 27 | 73 | 78 | 44 | 61 | |||||||
NO3 | 16 | 11 | 187 | 27 | 190 | 195 | 56 | 139 | ||||||||
SpCond | 902 | 848 | 1,660 | 907 | 1,725 | 1,790 | 1,177 | 1,517 | ||||||||
L27 | Cl | 58 | 56 | 63 | 55 | |||||||||||
NO3 | 464 | 473 | 629 | 434 | ||||||||||||
SpCond | 1,885 | 1,875 | 2,265 | 1,810 | ||||||||||||
L27 | Cl | (b) 52 | (b) 52 | (b) 42 | (c) 122 | |||||||||||
NO3 | 383 | 454 | 269 | 246 | ||||||||||||
SpCond | 1,675 | 1,875 | 1,466 | 1,445 | ||||||||||||
L28 | Cl | 37 | 41 | 17 | 38 | 27 | 29 | 31 | 30 | 23 | 38 | 28 | ||||
NO3 | -- | <1 | 12 | 3 | 8 | <1 | <1 | 1 | 5 | 2 | <1 | |||||
SpCond | 920 | 961 | 365 | 947 | 621 | 704 | 800 | 807 | 740 | 790 | 674 | |||||
L29 | Cl | 114 | 107 | |||||||||||||
NO3 | 36 | 34 | ||||||||||||||
SpCond | 1,699 | 1,699 | ||||||||||||||
L30 | Cl | 173 | ||||||||||||||
NO3 | 11 | |||||||||||||||
SpCond | 1,950 | |||||||||||||||
#31 | Cl | 27 | 21 | 26 | 20 | 21 | 19 | 20 | 31 | 21 | 34 | 37 | 22 | |||
NO3 | -- | -- | -- | -- | 33 | 29 | 34 | 28 | 31 | 29 | 28 | 26 | ||||
SpCond | 757 | 756 | 750 | 757 | 704 | 783 | 740 | 837 | 761 | 783 | 796 | 790 | ||||
(a) Chloride and nitrate concentrations represent results from standard inorganic chemistry analyses. Specific conductance values represent measurements made in field. * Well L19: this sample was collected August 19, 1985 * Well L24: these samples were collected January 25 and June 20, 1985, respectively (b) For well L27: These samples were collected minute(s) after first samples (c) For well L27: This sample was collected after 2 minutes of pumping. It was reported that approximately 1,600 gallons had been pumped from this well prior to collection of this sample. Cl - Chloride (mg/L) NO3 - Nitrate (mg/l as NO3) SpCond = Specific Conductance (µmhos/cm ) |
Chloride
Chloride concentrations were determined by using a hand-held digital titrator, a 2.256N Mercuric Nitrate Titration Cartridge, and Diphenylcarbazon Reagent Powder Pillows (Hach Co., Ames, IA.). The analysis was performed on a 100 ml sample of water.
The samples were already at room temperature prior to analysis and several had been filtered prior to the nitrate determinations. One blank (distilled water) and four standards (50, 100, 250, and 500 mg/l Cl) were titrated before and after each group of samples, or when the chemical reagents of one lot number were exhausted and those of another were started. These titrated values were used to construct a calibration curve which was then used to correct the titrated sample concentrations. The estimated analytical error for the chloride determinations was 4 percent. The results are shown in Table A1.
Specific Conductance
Measurements of specific conductance were made at the same time as the chloride analyses. A portable meter (Lectro-MHO, Model MC-1, Mark 4, Lab-Line Instrument Co., Melrose Park, Il.) was used to determine specific conductance and the results are expressed in micromhos per centimeter at 25°C (Table A1). The estimated accuracy of the conductivity meter was 2 percent.
Total Organic Carbon
Volatile (VOC) and nonvolatile organic carbon (NVOC) fractions of total organic carbon (TOC) were determined using a Dohrman/Envirotech DC-80 TOC Analyzer according to methods described by Barcelona (1984). Analyses were performed in the C.L. Burt laboratory, Learned Hall, at the University of Kansas by Dr. Stephen J. Randtke. Analytical precision was ±2% and the detection limit was approximately 0.02 mg/l of carbon. Results of the VOC and NVOC determinations are presented in Table A2.
Table A2
Well No. | May 8, 1985 | August 15, 1985 | ||
---|---|---|---|---|
VOC (mg/l) |
NVOC (mg/l) |
VOC (mg/l) |
NVOC (mg/l) |
|
L2 | Nil | 1.11 | Nil | 4.47 |
L3* | Nil | 6.12 | Nil | 5.80 |
L5* | Nil | 0.74 | Nil | 1.25 |
L10 | Nil | 3.27 | Nil | 2.15 |
L16 | Nil | 1.92 | Nil | 3.05 |
L18* | Nil | 2.95 | Nil | 4.81 |
L19 | Nil | 5.63 | Nil | 4.88 |
L20 | Nil | 4.38 | Nil | 3.10 |
L21 | Nil | 1.22 | Nil | 3.05 |
L22* | -- | -- | Nil | 3.51 |
Nil = less than 0.020 mg-C/l. * well of pre-standard construction |
Analysis of the May 8th samples was performed with samples having 1-2 ml of headspace for 24 hours because equipment malfunction had caused the original analyses to be invalid (Randtke, 1985). This could have affected the detection of VOC in these samples. However, the method of sample collection for TOC probably had a greater effect on the detection of VOC.
The May 8th sample from well l3 had a trace of sediment, but the sediment was not disturbed and the sample was not filtered prior to analysis (Randtke, 1985).
Dissolved Gases
Samples collected May 8, 1985, were analyzed for dissolved methane, oxygen, and carbon dioxide using a gas chromatograph/mass spectrometer. The analyses were performed by Dr. Charles Judson of the Mass Spectrometry laboratory at the University of Kansas. Methane was determined according to methods described by McAuliffe (1971). The results of the determinations are presented in Table A3.
Table A3
Well No. | Methane (CH4) (µg/l) |
Oxygen (O2) (mg/l) |
Carbon Dioxide (CO2) (mg/l) |
---|---|---|---|
L2 | 0.7 | 1.3 | 13.3 |
L3* | 1.3 | 1.0 | 8.3 |
L5* | 0.1 | 2.7 | 3.0 |
L10 | 0.7 | 2.2 | 8.0 |
L16 | 1.9 | 0.5 | 8.1 |
L18* | 0.1 | 2.6 | 5.5 |
L19 | 1.5 | 6.5 | 40. |
L20 | 2.7 | 1.9 | 5.8 |
L21 | -- | -- | -- |
* well of pre-standard construction |
A sample collected at Well L21 was accidentally broken in the laboratory, therefore, results are not available.
Standard Inorganic Chemistry
The standard inorganic chemistry analyses were performed by the Analytical Services Section of the Kansas Geological Survey housed at Moore Hall on the West Campus of the University of Kansas in Lawrence, KS.
Analytical results for the September 24, 1984 and May 8, 1985 samplings are presented in Table A4. The ionic balances computed for these results indicate that the analyses are very good with the greatest deviation from electroneutrality (the difference between the sums of milliequivalents/l of anions and cations divided by total milliequivalents/l) equal to 2.87 percent for the September 1984 analyses and 2.37 percent for the May 1985 analyses (Hathaway, 1984 and 1985).
Table A4--Results of the standard inorganic chemistry analyses showing percent differences between the September 1984 and May 1985 samplings.
Well No. |
Sample date |
Temp °C, field |
Specific conductance, µmhos/cm |
pH, field |
pH, lab |
Total dissolved solids, (calc) mg/L |
SiO2 mg/L |
Ca mg/L |
---|---|---|---|---|---|---|---|---|
L2 | 09-24-84 | 15.5 | 955 | 7.2 | 7.7 | 598 | 23 | 117 |
05-08-85 | 14.4 | 1122 | 7.15 | 7.35 | 699 | 18 | 132 | |
% change | -7 | 15 | -1 | -4 | 14 | -22 | 11 | |
L3 | 09-24-84 | 15 | 1430 | 7.15 | 7.6 | 1156 | 30 | 241 |
05-08-85 | 757 | 6.65 | 6.8 | 464 | 17 | 90 | ||
% change | -47 | -7 | -10 | -60 | -43 | -63 | ||
L10 | 09-24-84 | 14.8 | 960 | 7.15 | 7.58 | 591 | 20 | 99 |
05-08-85 | 14.7 | 1181 | 7.1 | 7.2 | 690 | 16 | 104 | |
% change | -1 | 19 | -1 | -5 | 14 | -20 | 5 | |
06-21-83 | 15 | 1540 | 6.95 | 898 | 20 | 126 | ||
% change | 1 | 38 | -3 | 34 | 0 | 21 | ||
L16 | 09-24-84 | 15 | 1270 | 7.1 | 7.5 | 759 | 26 | 134 |
05-08-85 | 14.7 | 1286 | 7.05 | 7.15 | 744 | 21 | 132 | |
% change | -2 | 1 | -1 | -5 | -2 | -19 | -1 | |
L18 | 09-24-84 | 15 | 1380 | 6.95 | 7.45 | 825 | 28 | 143 |
05-08-85 | 15 | 1337 | 7.05 | 7.15 | 767 | 21 | 130 | |
% change | 0 | -3 | 1 | -4 | -7 | -25 | -9 | |
L19 | 09-24-84 | 14.6 | 1600 | 7.1 | 7.55 | 1032 | 24 | 137 |
05-08-85 | 13.6 | 2430 | 7.05 | 7.2 | 1575 | 19 | 161 | |
% change | -7 | 34 | -1 | -5 | 34 | -21 | 15 | |
L20 | 09-24-84 | 15 | 131B | 7.05 | 7.6 | 842 | 25 | 134 |
05-08-85 | 14.4 | 1159 | 7.15 | 7.3 | 714 | 20 | 117 | |
% change | -4 | -12 | 1 | -4 | -15 | -20 | -13 | |
L21 | 09-24-84 | 14 | 1219 | 7.15 | 7.6 | 744 | 23 | 129 |
05-08-85 | 14.2 | 1220 | 7.15 | 7.2 | 713 | 18 | 125 | |
% change | 1 | 0 | 0 | -5 | -4 | -22 | -3 |
Well No. |
Mg mg/L |
Na mg/L |
K mg/L |
Sr mg/L |
NH4 mg/L |
HCO3 mg/L |
SO4 mg/L |
Cl mg/L |
---|---|---|---|---|---|---|---|---|
L2 | 45 | 27 | 2.1 | 1.8 | < 0.1 | 374 | 137 | 39 |
49 | 42 | 1.8 | 1.9 | < 0.1 | 400 | 163 | 47 | |
8 | 36 | -14 | 5 | 6 | 16 | 17 | ||
L3 | 56 | 59 | 8.1 | 4.2 | < 0.1 | 375 | 426 | 84 |
16 | 52 | 1.4 | 1.2 | < 0.1 | 267 | 102 | 38 | |
-71 | -12 | -83 | -71 | -29 | -76 | -55 | ||
L10 | 45 | 52 | 3.1 | .6 | < 0.1 | 428 | 81 | 49 |
47 | 89 | 2.5 | .6 | 0.1 | 523 | 93 | 63 | |
4 | 42 | -19 | 0 | 18 | 13 | 22 | ||
61 | 126 | 3.1 | .6 | 553 | 148 | 106 | ||
26 | 59 | 0 | 0 | 23 | 45 | 54 | ||
L16 | 58 | 57 | 3.8 | .8 | < 0.1 | 447 | 108 | 108 |
57 | 56 | 3.9 | .8 | < 0.1 | 441 | 117 | 104 | |
-2 | -2 | 2 | 0 | -1 | 8 | -4 | ||
L18 | 56 | 78 | 3 | .7 | < 0.1 | 473 | 120 | 125 |
51 | 78 | 3.5 | .6 | < 0.1 | 483 | 91 | 124 | |
-9 | 0 | 14 | -14 | 2 | -24 | -1 | ||
L19 | 68 | 126 | 3 | 1.9 | < 0.1 | 459 | 215 | 116 |
84 | 267 | 2.7 | 1 | < 0.1 | 642 | 366 | 196 | |
19 | 53 | -10 | -47 | 28 | 41 | 41 | ||
L20 | 58 | 72 | 4.5 | 1.2 | < 0.1 | 400 | 176 | 84 |
49 | 59 | 6.3 | 1 | < 0.1 | 388 | 150 | 61 | |
-16 | -18 | 28 | -17 | -3 | -15 | -27 | ||
L21 | 55 | 57 | 5.4 | .9 | < 0.1 | 398 | 141 | 97 |
50 | 60 | 2.5 | 1 | < 0.1 | 410 | 123 | 104 | |
-9 | 5 | -54 | 10 | 3 | -13 | 7 |
Well No. |
F mg/L |
NO3 mg/L |
PO4 mg/L |
B µg/L |
Total Hardness (CaCO3) mg/L |
Non-Carbonate Hardness (CaCO3) mg/L |
---|---|---|---|---|---|---|
L2 | .3 | 22 | .09 | 123 | 479 | 173 |
.3 | 47 | 80 | 533 | 205 | ||
0 | 53 | -35 | 10 | 15 | ||
L3 | .3 | 63 | .12 | 422 | 836 | 529 |
.2 | 15 | 90 | 292 | 73 | ||
-33 | -76 | -79 | -65 | -86 | ||
L10 | .2 | 30 | .25 | 54 | 433 | 82 |
.3 | 17 | 89 | 453 | 25 | ||
33 | -43 | 39 | 4 | -70 | ||
.2 | 35 | 566 | 113 | |||
0 | 14 | 23 | 27 | |||
L16 | .2 | 43 | .27 | 183 | 574 | 207 |
.2 | 35 | 105 | 565 | 203 | ||
0 | -19 | -43 | -2 | -2 | ||
L18 | .2 | 38 | .58 | 203 | 588 | 200 |
.3 | 30 | 95 | 535 | 139 | ||
33 | -21 | -53 | -9 | -30 | ||
L19 | .4 | 115 | .19 | 144 | 624 | 248 |
.4 | 162 | 163 | 748 | 222 | ||
0 | 29 | 12 | 16 | -10 | ||
L20 | .2 | 90 | .22 | 135 | 574 | 246 |
.2 | 60 | 92 | 495 | 177 | ||
0 | -33 | -32 | -14 | -28 | ||
L21 | .3 | 39 | .37 | 114 | 549 | 223 |
.3 | 28 | 63 | 519 | 183 | ||
0 | -28 | -45 | -5 | -18 |
Bacteriological Examination
Examination for fecal coliform and fecal Streptococcus bacteria was conducted by The Environmental laboratory and interpreted and reported by the Kansas Department of Health and Environment, both located at Forbes Building 740 in Topeka, KS.
The examination consisted of a search for the presence of coliform bacteria in the water samples collected December 17, 1984 and May 20 and 21, 1985. The method used was the membrane filter count according to Standard Methods for the Examination of Water and Wastewater (1980). The results are presented in Table A5.
The examination consisted of either a 10 ml or 20 ml portion of a 100 ml sample. The number of bacterial counts (colonies) was reported per 100 ml. Therefore, if no bacteria were found, results were reported as less than 10 counts per 100 ml for a 10 ml aliquot, and less than 5 counts per 100 ml for a 20 ml aliquot.
Table A5
Well No. |
December 17, 1984 | May 20-21, 1985 | ||
---|---|---|---|---|
fecal coliform |
fecal Streptococcus |
fecal coliform |
fecal Streptococcus |
|
L2 | <5 | <5 | <10 | <10 |
L3* | <5 | <5 | <10 | 30 |
L5* | -- | -- | <10 | <10 |
L10 | <5 | <5 | <10 | 10 |
L15 | <5 | <5 | <10 | <10 |
L18* | <5 | <5 | <10 | 30 |
L19 | <5 | <5 | <10 | <10 |
L20 | <5 | <5 | <10 | 10 |
L21 | <5 | 280 | <10 | <10 |
*well of pre-standard construction |
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Kansas Geological Survey, Geohydrology
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