Principles Of Soil Water Movement

Through experiments on saturated water flow through sand beds, Darcy18 found that the rate of flow, Q (L3/T), through a cross-sectional area A (L2), is directly propor-

Ten Principles Climate Change Images

Water content

Figure 7 Changes in water retention characteristics between sorption and desorption.16

Water content

Figure 7 Changes in water retention characteristics between sorption and desorption.16

0 0

Post a comment