Quantity of water in steady state unsaturated flow in direction of upward movement evaluator uses Total Water Volume = (Effective Hydraulic Conductivity*Cross-Sectional Area*((Water Rise-Length of the Water Column)/Length of the Water Column))+Hydraulic Gradient to evaluate the Total Water Volume, The Quantity of water in steady state unsaturated flow in direction of upward movement defined as Steady-state unsaturated flow (Q) is proportional to the effective hydraulic conductivity (K), the cross-sectional area (A) through which the flow occurs, and gradients due to both capillary forces and gravitational forces. Total Water Volume is denoted by Vw symbol.
How to evaluate Quantity of water in steady state unsaturated flow in direction of upward movement using this online evaluator? To use this online evaluator for Quantity of water in steady state unsaturated flow in direction of upward movement, enter Effective Hydraulic Conductivity (Ke), Cross-Sectional Area (A), Water Rise (hc), Length of the Water Column (z) & Hydraulic Gradient (dhds) and hit the calculate button.