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Case Studies: South Central Indiana

                               
 

A Natural-Potential Survey Around
Lemon Lane Landfill, Bloomington, Indiana

for

Westinghouse Electric Corporation/CBS
Bloomington Project

April/May 1998

EXECUTIVE SUMMARY


A natural-potential (NP) survey was conducted around the perimeter of Lemon Lane Landfill in Bloomington, Indiana during April 1998. The survey was performed in order to map possible groundwater conduits conducting water to the Landfill site, and to locate likely pathways connecting the Landfill to Illinois Central Spring, where low level pcb's have been detected.


The NP survey around the Landfill identified at least 24 anomaly trends indicative of underlying groundwater conduits in carbonate rock. Around the east, north and west sides of the Landfill, a number of possible pathways for water were deduced from stacked NP profiles. In addition, crosslines within the west and north blocks revealed trends that roughly paralleled the landfill boundaries, suggesting a series of fractures concentric to the sink beneath the fill. Anomaly trends of the East Block coincided with existing depressions of the ground surface. Residual NP contours expressed the combined anomaly trends of primary and cross-lines of the West Block, while in the North Block the four north/south anomaly trends were discerned in the contour portrayal.


On the south side of the Landfill, between the railroad and the cemetery gardens, at least eight anomaly trends have been identified. These features trend generally southeastward, but whether or not water within the underlying structures flows in that direction within all of the trends is uncertain.


A major anomaly trend can be traced from Illinois Central Spring northwestward to the cemetery, where it appears to bifurcate. Other possible tributaries are evident in the stacked profiles. The anomaly trend coincides with deep sinkholes up-gradient from the spring and culminates in an M-shaped anomaly over the spring orifices. The main anomaly trend is clearly portrayed as a series of NP highs in the residual NP contour map of the Southeast Block.

 
                               
                               

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