Grouser
Civil/Environmental
- Dec 11, 2002
- 101
I was reading another thread regarding GWL uncertainty in clay soil and it reminded me that the historic GWL can be approximated by where the clay changes color from brown to gray. This is the result of the oxidation of ferrous iron Fe+2 into ferric iron Fe+3 by oxygen above the water level, or at least that's the way I remember it. Comments are welcome. Obviously this technique works only when other chemicals don't confuse the issue. Anyway that's my tip for what it's worth.
Happy bore hole logging!
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Happy bore hole logging!
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