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Hydrology and water resources of Capitol Reef National Park, Utah : with emphasis on the middle Fremont River area

机译:犹他州国会礁国家公园的水文和水资源:重点在弗里蒙特河中游地区

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摘要

The water resources of the Capitol Reef National Park area include the middle Fremont River, other perennial and ephemeral watercourses, isolated springs, tinajas, and lakes fed by precipitation on surrounding plateaus, as well as ground water in alluvial, basalt, and sedimentary aquifers fed by recharge from precipitation and stream channel losses. The difference between streamflows at Bicknell (79.2 million m³/yr) and Caineville (67.8 million m³/yr) can be attributed to evapotranspiration by riparian vegetation and cultivated crops and ground-water recharge, which exceeds 1.5 million m³/yr. Regional ground-water movement is eastward from Thousand Lake Mountain and southward along the Waterpocket Fold. Ground-water quality is generally brackish while surface water is fresh, both degrading east of the Waterpocket Fold due to agricultural uses, evapotranspiration and long aquifer residence times. Along the middle Fremont River agricultural use causes a mean salt load increase of 16,100 metric tons/year, turbidity increases three-fold, and fecal coliforms generally increase.
机译:国会礁国家公园地区的水资源包括中部弗里蒙特河,其他多年生和短暂的河道,偏远的泉水,蒂纳哈斯河和周围高原降水带来的湖泊,以及冲积,玄武岩和沉积含水层中的地下水通过降水和河道损失补给。 Bicknell(7920万立方米/年)和Caineville(6780万立方米/年)之间的流量差异可归因于河岸植被和耕作作物的蒸散和地下水补给,每年超过150万立方米。区域地下水运动从千湖山向东,沿着水袋褶皱向南。地下水水质新鲜时,地下水水质通常微咸,由于农业用途,蒸散作用和较长的含水层停留时间,在水袋褶皱以东地区都会退化。在中部弗里蒙特河沿岸,农业使用造成的平均盐负荷增加了16,100公吨/年,浊度增加了三倍,粪便大肠菌群总体上增加了。

著录项

  • 作者

    Christiana David.;

  • 作者单位
  • 年度 1991
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  • 原文格式 PDF
  • 正文语种 en
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