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Estimation of suspended sediment transport in the Kebir drainage basin, Algeria

机译:阿尔及利亚凯比尔流域悬浮泥沙输送的估算

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摘要

Sediment load and sediment concentration are highly important variables that may play a key role in environment quality assessment and help to evaluate the extent of potential adverse impacts. This paper introduces a methodology to predict sediment loads in the Kebir drainage basin (681 km~2). The methodology is developed by a conventional sediment rating curve and a multiple regression model. The former method is investigated with the mean discharge classes derived from the recorded instantaneous suspended sediment concentrations and water discharges for the Kebir basin, prior to the Mexa reservoir construction. The latter is based on rock type erodibility, mean annual runoff and basin area variables, and which is applied for the ungauged Mexa reservoir basin located upstream of the Kebir gauging station (651 km~2). The mean annual suspended sediment yield of both Kebir drainage basin and Mexa reservoir basin conducted during the 24 years (1975/1976-1998/1999) and the 9 years (1999/2000 -2007/2008) are respectively 895 T km~2 year-1 and 572 T km~2 year-1. Despite the decline in sediment load during the reservoir period due mainly to disturbance in climatic regime, the basin is suffering severe soil loss, and currently 0.42% y-1 in loss of storage in the reservoir due to sedimentation has been evaluated. The high amount of sediment produced from the study drainage basin is a function of climatic and several physical factors including the high proportion of argillaceous materials and the amount of bare soil exposed.
机译:泥沙负荷和泥沙浓度是非常重要的变量,可能在环境质量评估中发挥关键作用,并有助于评估潜在不利影响的程度。本文介绍了一种预测Kebir流域(681 km〜2)的泥沙负荷的方法。该方法是通过常规的泥沙分级曲线和多元回归模型开发的。在Mexa水库建设之前,对前一种方法进行了调查,得出的平均排放量类别来自记录的凯比尔盆地瞬时悬浮沉积物浓度和排水量。后者基于岩石类型的可蚀性,年均径流量和流域面积变量,并且适用于位于Kebir测站(651 km〜2)上游的未赋权的Mexa水库盆地。 Kebir流域和Mexa水库盆地在24年(1975 / 1976-1998 / 1999)和9年(1999/2000 -2007/2008)进行的年平均悬浮泥沙产量分别为895 T km〜2年-1和572 T km〜2 year-1。尽管在储层期间沉积物负荷下降主要是由于气候条件的干扰,但流域正在遭受严重的土壤流失,目前已经评估了由于沉积而储层中的储量损失为0.42%y-1。研究流域产生的大量沉积物是气候和一些物理因素的函数,其中包括泥质材料的比例高和裸露的土壤量高。

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  • 来源
    《Quaternary International》 |2012年第7期|p.25-31|共7页
  • 作者单位

    Department of Geology, University o/Annaba, B.P.J2, Sidi Amar, Annaba, Algeria;

    Department of Geology, University o/Annaba, B.P.J2, Sidi Amar, Annaba, Algeria;

    Department of Geography, University of Annaba, B.P.12, Sidi Amar, Annaba, Algeria;

    Department of Geography and Regional Development, University of Arizona, P.O. Box 210076 Tucson, AZ 85721, USA;

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