Not AvailableA methodology for determining the length of advancement of wetting front and potential groundwater recharge under variable depth of ponding is presented. The methodology employs the approximated green- ampt equation, which has been derived by Ali .et. al. The methodology provides no restrictions to infiltration time period, depth and nature of ponding and soil types. Performance of the proposed methodology has been comapared with Richards and Warrick et al models using the published laboratory and field experimental data. The quantitative statistics namely, coefficient of determination (R) , index of agreement (D) nd percent bias (PB) are utilized to assess the performance of the proposed methodology. Results show that the prop...
The first important physical process in basin recharge is the infiltration of water from the basin's...
Recharge to the aquifer through seepage from irrigation canals is often quoted as one of the main ca...
Groundwater recharge is a key factor in water balance studies, especially in semi-arid areas. In Ind...
Not AvailableDetermination of length of advancement of wetting front is prerequisite for estimation...
Estimating the quantity of water that reaches the water table following an infiltration event is vit...
Groundwater resources are limited and they are declining in quality and quantity due to contaminatio...
A mathematical model is developed for the estimation of groundwater recharge through surface drains ...
Excessive exploitation of ground water is one of the impacts of the high demand for clean water. Thi...
Infiltration is the process whereby water enters soil through the surface. This can be a naturally o...
The first important physical process in basin recharge is the infiltration of water from the basin's...
Not AvailableThe groundwater recharge has been routinely estimated as a residual of various compone...
Estimation of groundwater recharge to an unconfined aquifer is studied using analytical and numerica...
Appropriate groundwater resource management becomes a priority for the States of the semi-arid south...
<p>To assess recharge through floodwater spreading, three wells, approx. 30 m deep, were dug in a 35...
Groundwater recharge estimates are required for water resource management and the investigation of w...
The first important physical process in basin recharge is the infiltration of water from the basin's...
Recharge to the aquifer through seepage from irrigation canals is often quoted as one of the main ca...
Groundwater recharge is a key factor in water balance studies, especially in semi-arid areas. In Ind...
Not AvailableDetermination of length of advancement of wetting front is prerequisite for estimation...
Estimating the quantity of water that reaches the water table following an infiltration event is vit...
Groundwater resources are limited and they are declining in quality and quantity due to contaminatio...
A mathematical model is developed for the estimation of groundwater recharge through surface drains ...
Excessive exploitation of ground water is one of the impacts of the high demand for clean water. Thi...
Infiltration is the process whereby water enters soil through the surface. This can be a naturally o...
The first important physical process in basin recharge is the infiltration of water from the basin's...
Not AvailableThe groundwater recharge has been routinely estimated as a residual of various compone...
Estimation of groundwater recharge to an unconfined aquifer is studied using analytical and numerica...
Appropriate groundwater resource management becomes a priority for the States of the semi-arid south...
<p>To assess recharge through floodwater spreading, three wells, approx. 30 m deep, were dug in a 35...
Groundwater recharge estimates are required for water resource management and the investigation of w...
The first important physical process in basin recharge is the infiltration of water from the basin's...
Recharge to the aquifer through seepage from irrigation canals is often quoted as one of the main ca...
Groundwater recharge is a key factor in water balance studies, especially in semi-arid areas. In Ind...