首页> 外文会议>International Yellow River forum on ensuring water right of the river's demand and healthy river basin maintenance;Ministry of Water Resources;China Yellow River Foundation >Analysis of the Characters of Recent Dynamic Variation of Runoff and Sediment in the Middle Yellow River Coarse Sediment Source Area
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Analysis of the Characters of Recent Dynamic Variation of Runoff and Sediment in the Middle Yellow River Coarse Sediment Source Area

机译:黄河中游粗泥沙源地区近期径流与泥沙动态变化特征分析。

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The middle Yellow River coarse sediment source area is the most serious soil and water loss area of the Yellow River basin,to strengthen soil and water loss controlling of this area is one of the most direct and effective ways which reduced the sand into the Yellow River and the harm of siltation in the lower reaches.Mastering runoff and sediment of this area in time,is the premise of correctly analysing the variation of runoff and sediment,and is the basic data for formulating soil and water loss prevention measures and analyzing soil and water conservation benefit.In this study,we take the middle Yellow River coarse sediment sourrce area as object,the year of 1956 ~ 2004 is the basic period,2005 ~ 2010 is the monitoring contrast period,areal precipitation is obtained by the way of drawing the isoline map of precipitation which based on collecting observed data of existing rain-gauge station,considering the difference of geomorphic type and river basin management degree in this area,runoff and sediment discharge use zone plan for calculation,the flood change reacts according to the annual maximum peak discharge of hydrologic station in this study area,and the management degree of soil and water conservation reacts by means of changing of soit and water conservation measures.The outcomes show that comparing with the basic period,precipitation in the monitoring period increased by 3.9%,runoff decreased by48.2%,the total sediment,coarse sediment of grain-size larger than 0.05 mm and 0.1mm are less than 85.9%,90.8% and 93.0%,respectively.It is an estimation that there is no great flood in the area according to the annual maximum peak discharge of hydrologic station,precipitation shows a weak increasing trend,and runoff and sediment decrease remarkably,It relates to that in the monitoring period there is no happen to a wideextent and great-intensity rainstorm,precipitation intensity is smooth relatively although total precipitation has a little change.In ultra-infiltration flow area,it goes against producing runoff and sediment.Additionally effective management of soil and water conservation has been condffcted in recent years,especially the implementation of "return farmland to forests or grassland" and banned for harness measures,the ecological environment in this area has improved evidently,appearing a sharp reduction of observed runoff and sediment in the monitoring period.
机译:黄河中游粗沙源区是黄河流域最严重的水土流失区,加强对该区的水土流失控制是减少黄沙入黄的最直接,最有效的方法之一。及时掌握该地区的径流和泥沙,是正确分析径流和泥沙变化的前提,是制定水土流失防治措施,分析水土流失的基础数据。本研究以黄河中游粗沙源区为对象,以1956〜2004年为基期,2005〜2010年为监测对比期,采用图求出区域降水的方法。基于收集现有雨量计观测数据的降水等值线图,考虑该地区地貌类型和流域管理程度的差异,r排沙区利用区划计算,洪水变化根据该研究区水文站年最大洪峰流量而变化,水土保持管理程度通过改变水土保持措施而变化。结果表明,与基本期相比,监测期降水增加了3.9%,径流减少了48.2%,粒径大于0.05mm和0.1mm的粗泥沙总量小于85.9%,根据水文站的年最大洪峰流量,估计该地区没有大洪水,降水量呈弱势增长趋势,径流和泥沙量明显减少,这与水文站每年的最大洪峰流量有关。在监测期内,没有发生大范围强暴雨,尽管总降水量变化不大,但降水强度相对平稳。近年来,已经对水土保持进行了有效管理,特别是实施了“退耕还林还草”,禁止采取治理措施,这对生态环境造成了不利影响。监测期间,面积明显改善,观测到的径流和泥沙明显减少。

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