Stream Bottom Resisitivity, Burd Run, PA

Our work in the Burd Run Watershed focused on changes in stream bottom resistivity between low-stage and high-stage flows that indicated seeps beneath the stream and the geologic heterogeneities that control them.



Nyquist, J.E., P. A. Freyer, and L. Toran (2008) Stream bottom resistivity tomography to map ground-water discharge, Ground Water, 46(4): 561-569. (July-Aug)