首页> 外文会议>International Symposium on River Sedimentation vol.3; 20041018-21; Yichang(CN) >RECENT CHANGES IN RUNOFF AND SEDIMENT LOAD AND THEIR TENDENCY IN THE UPPER CHANGJIANG RIVER
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RECENT CHANGES IN RUNOFF AND SEDIMENT LOAD AND THEIR TENDENCY IN THE UPPER CHANGJIANG RIVER

机译:长江上游径流和泥沙负荷的近期变化及其趋势

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摘要

This paper statistically analyse the runoff and sediment load changes at the major stations in the Upper Changjiang River. Compared with the annual runoff and sediment load before 1990, there were three major changes of annual sediment load in the period of 1991-2002; the annual decrement was about 0.13 x 10~9t at Yichang Station; the annual increment was about 0.035 x 10~9t at Pingshan Station and the percentage (accounted by Yichang station) also increased from 51.8% to 71.9%; the annual decrement was about 0.0985 x 10~9t at Beibei Station and the percentage also decreased from 25.7% to 9.1%. Based on the analysis of several non-parameter statistical methods such as moving average check and Spearman order correlativity check, the paper concludes that the runoff changing tendency at Pingshan Station is not distinct, but the sediment load increasing tendency is distinct; the runoff and sediment load at Beibei Station decreased tendency aer very distinct; the runoff changing tendency at Yichang Station is not distinct, whereas the sediment load increasing tendency is distinct.
机译:本文对长江上游主要站点的径流和泥沙负荷变化进行了统计分析。与1990年之前的年径流量和泥沙量相比,1991-2002年期间的年泥沙量发生了三大变化。宜昌站年减量约0.13 x 10〜9t。坪山站的年增量约为0.035 x 10〜9t,宜昌站的占比也从51.8%增加到71.9%。北be站的年减量约为0.0985 x 10〜9t,所占百分比也从25.7%降至9.1%。通过对移动平均检验和Spearman阶数相关性检验等几种非参数统计方法的分析,得出结论:坪山站径流量变化趋势不明显,但泥沙负荷增加趋势明显。北be站径流和泥沙量减少趋势明显。宜昌站径流量变化趋势不明显,而泥沙负荷增加趋势明显。

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