At a given height above the free-water level, the capillary water becomes irreducible .
2.
Minimal soil disturbance keeps humus levels high and maintains a network of permanent pores for draining excess water and moving capillary water around.
3.
Experiments on capillary water absorption have shown that increased amounts of lime in the mixture results in an increase in quantity and in reduced width of capillary canals, proving the material s erosion resistance.
4.
This capillary water forms the irreducible water saturation ( Swi ) with respect to effective porosity ( notwithstanding the inclusion of microporous water as V sh during the log analysis ) whereas for total porosity, the CBW and capillary water combined form the Swi .
5.
This capillary water forms the irreducible water saturation ( Swi ) with respect to effective porosity ( notwithstanding the inclusion of microporous water as V sh during the log analysis ) whereas for total porosity, the CBW and capillary water combined form the Swi .
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