Search results with tag "Temperature gradients to determine stream"

Analysis of Temperature Gradients to Determine Stream ...

Analysis of Temperature Gradients to Determine Stream Exchanges with Ground Water 119 hydraulic conductivity. Stallman’s equation for the simultaneous transfer of heat and water through saturated sediments for the one-dimensional case of vertical flow (z direction) is as follows: K T z q T z T t t u u u u u u 2 2 C w C s, (1) where K t

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