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Subsections
GroundwaterCharacterization Parameters to be Measured
-
Static Water Level
- using beeper tape
-
Water Chemistry
-
Temperature
- by thermometer, pH meter or dissolved oxygen
meter
-
pH
- by pH meter
-
Turbidity
- by portable turbidimeter
-
Nitrate
- by spectrophotometer
(colorimeter)
-
D.O.
- by dissolved oxygen meter
-
Water Level Recovery
- monitor return of water levels to static
condition after water samples are removed. Use beeper
tape.
- measure static water level in borehole (all groups do this
together before water sampling begins), use ``beeper tape''
- collect water sample from borehole
- following bailer procedure collect 1 liter sample
- save one split in 500 ml amber glass bottle, cap the bottle
leaving no air space (for D.O. and nitrate measurement)
- Caution: after 1/2 the contents of the bailer have
been poured out, water will begin to leave the bottom end of the
bailer as well as the top
- Monitor water level recovery
- form a water level measuring group composed of one member of
each of the regular groups for the day
- this group will record water levels, beginning immediately
after the last group has extracted its sample from the borehole.
- follow the slug test procedure, using the
beeper tape.
Record data in suggested format (Fig. 6.6)
- Measure chemical state. The following tasks may be performed
in any order, if you find yourself waiting for a piece of
equipment, try to start on one of the other tasks
- temperature (by thermometer or meter)
- pH (follow pH-meter procedure)
- dissolved oxygen content, electrical conductivity, salinity,
see D.O. meter procedure
- Measure Turbidity, see turbidity procedure
- Prepare Filtered Split, see filtration procedure
- Measure Nitrate Content, colorimetry procedure
GroundwaterCharacterization Comparative Results
See Tables 6.2-6.4 for
sample data from earlier semesters, and
Fig. 6.9 for slug test results.
Table 6.2:
Class well sampling results, SE corner of Synergy Parkway and
Rutford Dr., UTD campus, Oct. 10th 1998. The instructor and TA
comprise ``Group W'', data gathered Oct. 7th. Static water depth was
10.5 ft.
|
|
Group |
Component |
Units |
A |
B |
C |
W |
Static depth to water |
ft |
10.1 |
10.1 |
10.1 |
10.5 |
Conductivity |
S |
799 |
818 |
764 |
805 |
Salinity |
ppt |
0.40 |
0.4 |
0.2 |
0.4 |
pH |
|
7.28 |
7.42 |
7.44 |
7.35 |
Turbidity |
NTU |
7.15 |
10.2 |
1.93 |
3.19 |
D.O. |
% sat |
21.2 |
7.1 |
11 |
5.5 |
D.O. |
mg/l |
|
0.6 |
1.0 |
0.5 |
Nitrate |
ppm |
1.9 |
1.8 |
1.2 |
0.6 |
Water Temp. |
|
20.9 |
20.8 |
21.9 |
21.6 |
Table 6.3:
Class well sampling results, SE corner of Synergy Parkway and
Rutford Dr., UTD campus, Sat. Feb. 16, 2000. Initial depth to water
was 8.4 ft.
|
Group |
Parameter |
GROUP A |
GROUP B |
GROUP C |
GROUP D |
|
1st liter |
2nd liter |
3rd liter |
4th liter |
Temp (C) |
20.7 |
21.7 |
21.1 |
20.0 |
pH |
7.11 |
7.13 |
7.15 |
7.24 |
Turbidity (NTU) |
1.2 |
1.4 |
2.0 |
3.3 |
DO (%) |
26.5 |
24.6 |
24.4 |
29.1 |
DO (mg/L) |
2.27 |
2.11 |
2.08 |
2.59 |
Conductivity (uS) |
814 |
825 |
818 |
813 |
Salinity (ppt) |
0.4 |
0.4 |
0.4 |
0.4 |
Total Disolved Solid (TDS) |
350 |
360 |
340 |
330 |
Nitrates (mg/L) |
0.80 |
0.8 |
0.9 |
1.0 |
Table 6.4:
Class well sampling results, SE corner of Synergy Parkway and
Rutford Dr., UTD campus, June 24, 2000. Initial depth to water was
6.1 ft.
|
Group |
Parameter |
GROUP A |
GROUP B |
|
1st liter |
2nd liter |
Temp (C) |
25.1 |
24.3 |
pH |
5.87 |
6.4 |
Turbidity (NTU) |
1.8 |
1.9 |
DO (%) |
11.4 |
16.8 |
DO (mg/L) |
0.92 |
1.37 |
Conductivity (uS) |
682 |
684 |
Salinity (ppt) |
0.3 |
0.3 |
Nitrates (mg/L) |
1.1 |
1.3 |
Include the following topics in your discussion
- analyze the withdrawal slug test data (water level recovery
vs. time) using the Hvorslev method described in p. 141-145,
Sanders (1998)
- Discuss your own group's results, including any significant
potential sources of error.
- Compare your results to those of the other groups, and (if
desired) historical data, and try to explain any differences.
- Compare your results to the stream chemistry
data we took
earlier, and discuss any differences you see.
- Compare the specific discharge to the streamflow you measured
in Lab 2. Does the stream receive a large or small percentage of
what is flowing in the aquifer?
Read the ``Lab 4 Activities'' section of the handouts. Since the UTD
borehole was destroyed several months ago, we will use previous
classes' data (see attached sheets). Break up into your groups to
discuss the results, in preparation for writing your lab report on
this data.
Figure 6.9:
UTD Borehole slug test
comparison, plotted as log fractional drawdown ( vs.
time). Depth to water table given in parenthesis.
|
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GEOS 3110 Professor's Notes, Summer 2007
Dr. T. Brikowski, U. Texas-Dallas. All rights reserved.