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Comparison of Selected Methods for Estimating Ground-Water Recharge In Humid Regions

Sorted by Method



Select Methods to Compare METHOD CATEGORY SPATIAL SCALE TEMPORAL SCALE TYPICAL QUANTITY ESTIMATED EASE OF USE DATA NEEDS RELATIVE COST
Chloride Tracer Point Years Recharge Easy Moderate Moderate
Chlorofluorocarbons Tracer Local Month to Years Recharge Difficult Moderate High
Darcian Unit-Gradient Unsaturated Zone Point Long-Term Average Potential Recharge Moderate Low High
Deep Percolation Model Water Budget Regional Day to Years Potential Recharge Moderate Moderate Moderate
Ground-Water Modeling Ground-Water Local to Regional Month to Years Recharge Moderate High High
HELP3 Model Water Budget Point to Regional Day to Years Potential Recharge Easy Low to Moderate Moderate
Recession-Curve Displacement Streamflow Watershed Event to Years Net Recharge Moderate Low Low
Seepage Meters Streamflow Point Event to Months Potential Recharge Moderate Low Low
Stream Base-Flow Streamflow Watershed Years Net Recharge Easy Low Low
Streamflow Gain/Loss Measurements Streamflow Local Instantaneous Potential Recharge Easy Low Low
Temperature Tracer Point Days to Years Recharge Moderate Moderate High
Tritium Tracer Point Month to Years Recharge Moderate Moderate High
Watershed Models Streamflow Watershed to Regional Days to Years Recharge Moderate High High
Water-Table Fluctuations Ground-Water Local Day to Years Recharge Easy Low Low
Zero-Flux Plane Unsaturated Zone Point Day to Years Potential Recharge Difficult High High
Zero-Tension Lysimeters Unsaturated Zone Point Day to Years Potential Recharge Difficult Low High

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Page Last Modified: Friday, 01-Aug-2008 12:14:49 EDT