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Title: Discharge estimates in surface-mine areas using channel-geometry techniques

Conference · · Univ. Ky., Off. Eng. Serv., (Bull.); (United States)
OSTI ID:5432474

Discharge estimates in surface-mine areas using channel-geometry require extensive hydrologic knowledge of an area. Channel-geometry measurements offer an alternative method of estimating streamflow characteristics at ungaged sites. The method uses the empirical development of simple or multiple power-function equations yielding a discharge value from channel-configuration and channel-material data. The equations have been developed by collecting geometry and sediment data at numerous gaged sites and statistically relating those data to specified discharge characteristics. The principal advantage of the channel-geometry method is that estimates of discharge can be obtained quickly and inexpensively. Often results are as reliable as 5 to 10 years of continuous streamflow records. Relatively recent changes in slow regimen, such as those caused by depletion of streamflow by ground-water withdrawals or diversion for irrigation, are detectable by channel-geometry techniques. Discharges of perennial streams in coal-mine areas can be estimated using equations developed from data of the central and western United States. Equations intended specifically for ephemeral channels in areas of strippable coal resources in arid and semiarid areas have been developed from data collected in the western half of the conterminous United States.

Research Organization:
Geological Survey, Lawrence, KS
OSTI ID:
5432474
Report Number(s):
CONF-791262-
Journal Information:
Univ. Ky., Off. Eng. Serv., (Bull.); (United States), Conference: Symposium on surface mining hydrology, sedimentology and reclamation, Lexington, KY, USA, 4 Dec 1979
Country of Publication:
United States
Language:
English