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Field-based monitoring of sediment runoff from natural gas well sites in Denton County,Texas, USA
Authors:H F L Williams  D L Havens  K E Banks  D J Wachal
Institution:(1) Department of Geography, University of North Texas, P.O. Box 305279, Denton, TX 76203, USA;(2) 3520-G Victorine Lane, Del Valle, TX 78617, USA;(3) Division of Environmental Quality, City of Denton, 901-A Texas Street, Denton, TX 76209, USA;(4) Institute of Applied Sciences, University of North Texas, P.O. Box 305279, Denton, TX 76203, USA
Abstract:This study evaluates sediment runoff from gas well development sites in Denton County, Texas. The magnitude of sediment runoff was investigated by intercepting sediment in traps and weirs at the periphery of each gas well site and by measuring the growth of debris lobes that formed down slope from two sites. Four debris lobes formed at one gas well site and one formed at a second site. Debris lobes ranged in size from 30 to 306 square meters. Sediment from one site entered local creek channels, either as a component of storm water runoff or, in one case, as a debris lobe that flowed into a channel. The study findings suggest that sediment movement is significantly diminished once areas disturbed by gas well construction become naturally re-vegetated. Based on estimates of debris lobe volumes, sediment loading rates of about 54 metric tonnes per hectare per year were calculated for one site. It is concluded that gas well development sites in areas similar to those studied, especially where vegetation has been removed and terrain has relatively steep slopes (greater than 6%), generate sediment runoff comparable to small construction sites and should therefore be considered for regulations requiring erosion and sediment control measures.
Keywords:Gas well  Land disturbance  Storm runoff  Erosion  Sediment
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