Classifying the water table at regional to continental scales
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Abstract
Water tables at regional to continental scales can be classified into two distinct types: recharge-controlled water tables that are largely disconnected from topography and topography-controlled water tables that are closely tied to topography. We use geomatic synthesis of hydrologic, geologic and topographic data sets to quantify and map water-table type over the contiguous United States using a dimensionless criterion introduced by Haitjema and Mitchell-Bruker (2005), called the water-table ratio, which differentiates water-table type. Our analysis indicates that specific regions of the United States have broadly contiguous and characteristic water-table types. Water-table ratio relates to water-table depth and the potential for regional groundwater flow. In regions with recharge-controlled water tables, for example the Southwest or Rocky Mountains, USA, water-tables depths are generally greater and more variable and regional groundwater flow is generally more important as a percentage of the watershed budget. Water-table depths are generally shallow and less variable, and regional groundwater flow is limited in areas with topography-controlled water tables such as the Northeast USA. The water-table ratio is a simple but powerful criterion for evaluating regional groundwater systems over broad areas.
Study Area
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | Classifying the water table at regional to continental scales |
Series title | Geophysical Research Letters |
DOI | 10.1029/2010GL046427 |
Volume | 38 |
Issue | 5 |
Year Published | 2011 |
Language | English |
Publisher | American Geophysical Union |
Publisher location | Washington, D.C. |
Contributing office(s) | Central Mineral and Environmental Resources Science Center |
Description | L05401; 6 p. |
Country | United States |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |