Capacitively Coupled and Direct-current Resistivity Surveys of Selected Reaches of Cozad, Thirty-Mile, Orchard-Alfalfa, Kearney, and Outlet Canals in Nebraska, 2012-13

Authors

Christopher M. Hobza, Nebraska Water Science CenterFollow
Bethany L. Burton, Nebraska Water Science Center
Jeffrey E. Lucius, Nebraska Water Science Center
Ryan E. Tompkins, Nebraska Water Science Center

Date of this Version

2014

Citation

United States Geological Survey, Open File Report 2014-1007

Comments

United States government work

Abstract

Understanding the spatial characteristics of leakage from canals is critical to effectively managing and utilizing water resources for irrigation and hydroelectric purposes. Canal leakage in some parts of Nebraska is the primary source of water for groundwater recharge and helps maintain the base flow of streams. Because surface-water supplies depend on the streamflow of the Platte River and the available water stored in upstream reservoirs, water managers seek to minimize conveyance losses, which can include canal leakage. The United States Geological Survey, in cooperation with the Central Platte Natural Resources District and Nebraska Public Power District, used capacitively coupled (CC) and direct-current (DC) resistivity techniques for continuous resistivity profiling to map near-surface lithologies near and underlying the Cozad, Thirty-Mile, Orchard-Alfalfa, Kearney, and Outlet Canals. Approximately 84 kilometers (km) of CC-resistivity data were collected along the five canals.