Effect of Contributing Area Threshold on the Evaluation of Soil Erosion

DING Lin; YU Xianju; FU Suhua; WU Sinan

doi:10.13870/j.cnki.stbcxb.2018.03.010

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Effect of Contributing Area Threshold on the Evaluation of Soil Erosion

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- Effect of Contributing Area Threshold on the Evaluation of Soil Erosion
- Vol. 32, Issue 3, Pages: 61-67(2018)
- 作者机构：
  
  1. 北京师范大学地理科学学部,北京,100875
  2. 中国科学院水利部水土保持研究所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西杨凌,712100
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2018.03.010
  CLC：
- Published：2018
- 稿件说明：
移动端阅览
DING Lin, YU Xianju, FU Suhua, et al. Effect of Contributing Area Threshold on the Evaluation of Soil Erosion[J]. 2018, 32(3): 61-67.
DOI：

DING Lin, YU Xianju, FU Suhua, et al. Effect of Contributing Area Threshold on the Evaluation of Soil Erosion[J]. 2018, 32(3): 61-67. DOI： 10.13870/j.cnki.stbcxb.2018.03.010.

摘要

土壤侵蚀预报模型是定量评价水土流失和评估水土保持措施效益的重要手段。通用土壤流失方程（Universal Soil Loss Equation，USLE）和中国土壤流失方程（Chinese Soil Loss Equation，CSLE）被广泛应用于土壤侵蚀定量评价。这些模型中坡长的计算受汇水面积阈值的影响较大。为揭示汇水面积阈值对土壤侵蚀定量评价的影响，选取北方土石山区、西北黄土高原区、东北黑土区、南方红壤丘陵区、西南紫色土区、西南山地区和西南岩溶区210个流域面积在0.2~3.0 km2的小流域，以1∶10 000地形图10 m分辨率DEM为数据源，分别计算了1 000，1 500，2 000，2 500，3 000，5 000，7 000，9 000，11 000，13 000，15 000 m2共11个汇水面积阈值下各小流域不同坡长、土壤侵蚀强度级别以及土壤侵蚀的面积比例，分析了它们对汇水面积阈值变化的敏感性。结果表明：平均坡长、土壤侵蚀面积和轻度以上各级别的侵蚀强度面积比例都随汇水面积阈值的增加先增加而后趋于稳定。微度侵蚀面积比例随汇水面积阈值的增加逐渐减小并趋于稳定。当汇水面积阈值由1 000 m2增加到15 000 m2时，北方土石山区、西北黄土高原区、东北黑土区、南方红壤丘陵区、西南紫色土区、西南山地区和西南岩溶区的平均坡长分别增至阈值为1 000 m2时的1.53，4.16，1.95，1.90，1.69，1.57，1.47倍；土壤侵蚀面积比例分别增至阈值为1 000 m2时的1.20，1.85，1.43，1.37，1.77，1.44，1.30倍。汇水面积阈值对各分区的影响程度存在差异。从平均坡长和土壤侵蚀面积来看，东北黑土区受汇水面积阈值的影响最大。研究结果不仅为精确评价土壤侵蚀提供了数据支撑，而且对水土保持综合防治措施的评价和优化具有指导意义。

Abstract

Soil erosion model is a technical tool to calculate the soil loss and assess the efficiency of soil and water conservation practice. The universal soil loss equation (USLE) and Chinese soil loss equation (CSLE) were widely used to calculate the soil loss. The slope length in these models is significantly affected by the contributing area threshold. In this study

210 small watersheds which area varied from 0.2 km2 to 3.0 km2 were selected to investigate the effect of contributing area threshold on the slope length and then the soil loss. The small watersheds are located in Northern rocky mountain area

Northwestern loess plateau

Northeastern black soil area

Southern red soil hilly area

Southwestern purple soil area

Southwestern mountainous area and Southwestern karst area. The 1:10 000 scale topographical map and 10 m×10 m DEM of the small watersheds were collected. 11 contributing area thresholds

namely

1 000

1 500

2 000

2 500

3 000

5 000

7 000

9 000

11 000

13 000

15 000 m2 were used to calculate the slope length and soil loss. The characteristics of slope length

soil erosion intensity and soil erosion area with the different contributing area thresholds were analyzed. The results showed that the average slope length and soil loss area firstly rose with the increase of contributing area threshold and then tended to keep constant. In the Northern rocky mountain area

Northwestern loess plateau

Northeastern black soil area

Southern red soil hilly area

Southwestern purple soil area

Southwestern mountainous area and Southwestern karst area

the average slope length with contributing area threshold of 15 000 m2 was 1.53

4.16

1.95

1.90

1.69

1.57

1.47 times those of contributing area threshold with 1 000 m2 and the soil loss area percentage with contributing area threshold of 15 000 m2 was 1.20

1.85

1.43

1.37

1.77

1.44

1.30 times those of contributing area threshold with 1 000 m2. The contributing area threshold had different effects in the different area. The average slope length and soil loss area in Northeastern black soil area was significantly affected by the contributing area threshold. The results will be helpful for calculating soil loss and for selecting the soil and water conservation practices.

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