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Effects of cultivation and reforestation on suspended sediment concentrations: a case study in a mountainous catchment in China

机译:造林和造林对悬浮沉积物浓度的影响:以中国山区流域为例

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Understanding how sediment concentrations vary with land use/cover is critical for evaluating the current and future impacts of human activities on river systems. This paper presents suspended sediment concentration (SSC) dynamics and the relationship between SSC and discharge (Q) in the 8973 km(2) Du catchment and its sub-catchment (4635 km(2)). In the Du catchment and its sub-catchment, 4235 and 3980 paired SSC-Q samples, respectively, were collected over 30 years. Under the influence of the Household Contract Responsibility System and Grain-for-Green projects in China, three periods were designated, the original period (1980s), cultivation period (1990s) and reforestation period (2000s). The results of a Mann-Kendall test showed that rainfall slightly increased during the study years; however, the annual discharge and sediment load significantly decreased. The annual suspended sediment yield of the Du catchment varied between 1.3 x 10(8) and 1.0 x 10(10) kg, and that of the sub-catchment varied between 6.3 x 10(7) and 4.3 x 10(9) kg. The SSCs in the catchment and sucatchment fluctuated between 1 and 22400 gm(-3) and between 1 and 31800 gm(-3), respectively. The mean SSC of the Du catchment was relatively stable during the three periods (+/- 83 gm(-3)). ANOVA (analysis of variance) indicated that the SSC did not significantly change under cultivation for low and moderate flows, but was significantly different under high flow during reforestation of the Du catchment. The SSC in the sub-catchment was more variable, and the mean SSC in the sub-catchment varied from 1058 +/- 2217 gm(-3) in the 1980s to 1256 +/- 2496 gm(-3) in the 1990s and 891 +/- 1558 gm(-3) in the 2000s. Reforestation significantly decreased the SSCs during low and moderate flows, whereas cultivation increased the SSCs during high flow. The sediment rating curves showed a stable relationship between the SSC and Q in the Du catchment during the three periods. However, the SSC-Q of the sub-catchment exhibited scattered relationships during the original and cultivation periods and a more linear relationship during the reforestation period.
机译:了解沉积物浓度如何随土地利用/覆盖而变化对于评估人类活动对河流系统的当前和未来影响至关重要。本文介绍了8973 km(2)Du流域及其子流域(4635 km(2))的悬浮沉积物浓度(SSC)动态以及SSC与流量(Q)之间的关系。在Du流域及其子流域,在30年中分别收集了4235个和3980个成对的SSC-Q样本。在中国家庭联产承包责任制和绿色换粮项目的影响下,确定了三个时期,即原始时期(1980年代),耕种时期(1990年代)和造林时期(2000年代)。曼恩·肯德尔(Mann-Kendall)测试的结果表明,在研究期间,降雨量略有增加;但是,年排放量和泥沙量明显减少。杜河流域的年悬浮泥沙产量在1.3 x 10(8)和1.0 x 10(10)千克之间变化,子流域的年度悬浮泥沙产量在6.3 x 10(7)和4.3 x 10(9)千克之间变化。集水区和耕地中的SSC分别在1至22400 gm(-3)和1至31800 gm(-3)之间波动。在三个时期(+/- 83 gm(-3)),Du流域的平均SSC相对稳定。方差分析(方差分析)表明,对于中低流量,SSC在耕作过程中没有明显变化,但在Du流域重新造林期间,在高流量下,SSC有显着差异。子汇水面积中的SSC更具可变性,子汇水面积中的平均SSC从1980年代的1058 +/- 2217 gm(-3)到1990年代的1256 +/- 2496 gm(-3)不等。在2000年代为891 +/- 1558 gm(-3)。在低流量和中流量时,重新造林显着降低了SSC,而在高流量时,种植增加了SSC。在这三个时期中,沉积物等级曲线显示了Du流域的SSC和Q之间稳定的关系。然而,该子流域的SSC-Q在原始和耕种期间表现出零散的关系,而在重新造林期间则表现出更线性的关系。

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