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1 - paducah environmental information center

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Paducah Site<br />

B.1.2 DESCRiPtiON OF DATA SET<br />

The data set used for this plume map<br />

revision contains groundwater data from two<br />

types of sample locations: monitoring wells<br />

whose· screen mid-point is between elevations<br />

76.2 m (250 ft) and 97.5 m (320 ft) above mean<br />

sea level, and temporary borings in which a<br />

groundwater sample was collected from<br />

between the same two elevations. Only those<br />

wells and borings for which location coordinates,<br />

surface elevations, and screen or sample depths<br />

were available were included in the data set. As<br />

a result data from the following projects are not<br />

included in this interpretation:<br />

• monitoring wells belonging to the<br />

Tennessee Valley Authority's Shawnee<br />

Steam Plant,<br />

• residential water wells within the study<br />

area,<br />

• temporary borings from the WAG 22 RI,<br />

• temporary borings from the Northeast<br />

Plume Interim Remedial Action, and<br />

• temporary borings from the WAG 3 RI.<br />

This <strong>information</strong> is currently being<br />

gathered and will be included in the next revision<br />

as appropriate.<br />

B.1.3 SELECTION OF DATA POINTS<br />

To identify those wells and borings<br />

which fit the depth criteria, the OREIS database<br />

was queried for all water samples analyzed for<br />

TCE, 99Tc, or beta activity. The sample interval<br />

for each collected sample was converted to<br />

elevation and filtered to exclude those samples<br />

outside the elevations used to define the RGA.<br />

For monitoring wells, the elevation of the midpoint<br />

of the well screen was used as the sample<br />

depth. The samples were then segregated into<br />

lower, middle, and upper RGA intervals, defined<br />

as elevations 76.2 to 89.9 m (250 to 295 ft), 89.9<br />

to 93.0 m (295 to 305 ft), and 93.0 to 97.5 m (305<br />

to 320 ft) above mean sea level, respectively.<br />

The interval for the lower RGA is larger than the<br />

upper or middle so that data from "channels"<br />

identified in various portions of the plant would<br />

be included in the interpretation. Once the<br />

sample points were assigned to one of the three<br />

intervals, base maps for each interval that<br />

showed only those wells and borings that<br />

collected a sample from that interval were<br />

printed.<br />

B.1.4 SELECTION OF GROUNDWATER<br />

DATA<br />

The groundwater data set consists of<br />

TCE concentrations, 99Tc activities, or beta<br />

activities for those data points defined as RGA in<br />

this report. The data were selected from all<br />

groundwater data collected on or before<br />

December 31, 1999, and entered in OREIS by<br />

March 1, 2000. For monitoring well data, time<br />

versus concentration plots were created and<br />

trend lines developed. To normalize the data,<br />

these trend lines were used to determine the<br />

probable concentration of the well as of June 30,<br />

1999. This value was then plotted on the base<br />

maps. For temporary borings, the actual<br />

analytical value was used. For borings with<br />

multiple samples within one interval, the highest<br />

concentration within the interval waS selected<br />

and plotted on the base maps. Data from CY<br />

1999 were given the highest priority, while data<br />

from earlier years were used in trending and<br />

identifying approximate boundaries with the<br />

oldest data being of least value in the<br />

interpretation.<br />

B.1.5 MAPPING OF DATA.<br />

After all data were plotted on the base<br />

maps, the data were hand-contoured. Separate<br />

maps were made for both TCE and 99Tc in the<br />

upper, middle and lower RGA intervals. The<br />

contour intervals for TCE and 99Tc were as<br />

follows:<br />

0-10<br />

Appendix 0

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