赣江河流悬移质泥沙与水土流失的耦合关系动态分析
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Dynamic Analysis of Couping Relation Retween Suspended Load and Soil and Water Loss of Ganjiang River in Jiangxi Province
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    摘要:

    通过对赣江河流泥沙变化量的观测与分析,跟踪寻找出水土流失严重的河流为桃江、贡水、章水、平江、乌江、遂川江。11个观测站点多年观测结果表明,赣江多年平均输沙模数上游最大,上游各河均>140 t/km2。赣江干流多年平均输沙模数自赣州市至南昌市,由上而下逐次变小,万安站144 t/km2,吉安站136 t/km2,峡江站131 t/km2,樟树站112 t/km2,外洲站114 t/km2。赣江河流泥沙颗粒多年平均值,各河大都在0.04~0.066 mm之间。赣江流域输沙量年内分布规律表现为与降水量、径流量年内分配-致;此外,对水土流失状况、原因、发展态势进行了分析并提出了防治对策。

    Abstract:

    By analyzing the data of sediment observed in 11 hydrological stations in Ganjiang River, severe soil and water loss is found in Taojiang, Ganshui, Zhangshui, Pingjiang, Wujiang and Suichuanjiang, etc.The average volume of sediment in the upper reaches of Ganjiang River is larger than that in the lower reaches.Transported sediment mod ule is 144/km2 in Wan’ an statjon, 136/km 2 in Ji’an station, 131/km2 in Xiajiang station, 112/km2 in Zhangshu station, and 114/ km 2 i n Wuzhou station.The average diameter of sediment particles is 0.04 0.066 mm, and the change in sediment content is consistent with the changes of bot h the seasons of a year and rainfall or runoff.Lastly, suspended load and soil and water loss are studied, and the countermeasures are presented so as to be the basis for the further technical application in the future.

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欧阳球林,程洪,龚向民.赣江河流悬移质泥沙与水土流失的耦合关系动态分析[J].水土保持通报,2007,(6):134-159

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  • 收稿日期:2007-01-25
  • 最后修改日期:2007-05-08
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  • 在线发布日期: 2014-12-16
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