Free of O2, dissolved iron at Fe2+, lowest valence
does not contain particulate
Movement of grdw depends on P, Gravity & Porosity
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2
Q
Well depth
A
need to calculate the column of water sitting in the well
calculated as volume
remove the stagnant water from the well to ensure we collect a representative sample for specific gravity, pH, EC
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3
Q
Darcy’s Law
A
Q/A = -k (Δh/ΔL) state: the amount of water flowing across the sectional area is equal to the negative hydraulic EC * change in height over change in distance