Redox Processes and Flow Paths in Riparian Zone of a Glacial Outwash Aquifer

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Using Chemical, Hydrologic, and Age Dating Analysis to Delineate Redox Processes and Flow Paths in the Riparian Zone of a Glacial Outwash Aquifer-Stream System

By Larry J. Puckett, Timothy K. Cowdery, Peter B. McMahon, Lan H. Tornes, and Jeffrey D. Stoner

[Water Resources Research, vol. 38, no. 8, August 2002]

Figure 5. Argon and nitrogen gas concentrations in ground water and their theoretical values assuming air-saturated water equilibrium at 420-m elevation and temperatures ranging from 0 degrees to 20 degrees C. [Horizontal tic marks on the equilibrium line indicate Ar and N₂ equilibrium concentrations from 0 degrees to 20 degrees C in 2-degree increments.]

Argon and nitrogen gas concentrations in ground water
and their theoretical values assuming air-saturated water equilibrium at 420-m
elevation and temperatures ranging from 0 degrees to 20 degrees C.

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