John Paul Sanborn
Above average climber
Movement of water through soil is a surface effect across particles.
Waster must move from particle to particle, and voids need to fill up in each strata before the water can move down to the next. You will frequently find stagnant water that has lost its free O2, thus becoming anaerobic.
The old idea of adding gravel to assits with drainage just makes the voids bigger, ir so I've read.
also when you have an homogenic boundary there is often compaction boundary that makes matters worse.
Waster must move from particle to particle, and voids need to fill up in each strata before the water can move down to the next. You will frequently find stagnant water that has lost its free O2, thus becoming anaerobic.
The old idea of adding gravel to assits with drainage just makes the voids bigger, ir so I've read.
also when you have an homogenic boundary there is often compaction boundary that makes matters worse.