细沟形成对坡面产流产沙过程的影响

和继军; 宫辉力; 李小娟; 蔡强国

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细沟形成对坡面产流产沙过程的影响

和继军, 宫辉力, 李小娟, 蔡强国

文章导航 > 水科学进展 > 2014 > 25(1): 90-97

和继军, 宫辉力, 李小娟, 蔡强国. 细沟形成对坡面产流产沙过程的影响[J]. 水科学进展, 2014, 25(1): 90-97.

引用本文:

和继军, 宫辉力, 李小娟, 蔡强国. 细沟形成对坡面产流产沙过程的影响[J]. 水科学进展, 2014, 25(1): 90-97.

HE Jijun, GONG Huili, LI Xiaojuan, CAI Qiangguo. Effects of rill development on runoff and sediment yielding processes[J]. Advances in Water Science, 2014, 25(1): 90-97.

Citation:

HE Jijun, GONG Huili, LI Xiaojuan, CAI Qiangguo. Effects of rill development on runoff and sediment yielding processes[J]. Advances in Water Science, 2014, 25(1): 90-97.

细沟形成对坡面产流产沙过程的影响

1.
首都师范大学城市环境过程与数字模拟国家重点实验室培育基地, 北京 100048;
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;
3.
中国科学院地理科学与资源研究所陆地水循环与地表过程重点实验室, 北京 100101

基金项目: 国家自然科学基金资助项目（41130744；41271304）

详细信息

作者简介:
和继军（1979-），男，河北邢台人，副教授，博士，主要从事土壤侵蚀、水土保持等研究。E-mail：hejiun_200018@163.com

通讯作者:
蔡强国，E-mail：caiqg@igsnrr.ac.cn

中图分类号: S157.1

Effects of rill development on runoff and sediment yielding processes

1.
Base of the State Laboratory of Urban Environmental Processes and Digital Modeling, Capital Normal University, Beijing 100048, China;
2.
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Water and Soil Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China;
3.
Key Laboratory of Water Cycle & Related Land Surface Processes, Institute of Geographical Sciences and Natural Resources Research, CAS, Beijing 100101, China

Funds: The study is financially supported by the National Natural Science Foundation of China (No.41130744; No.41271304).

摘要: 为探明细沟形成条件下不同土壤坡面水沙变化特性，利用室内模拟降雨试验，分析了塿土和黄绵土在细沟发育及已有细沟条件下的水沙过程变化规律。结果表明，塿土产流快，易形成细沟，细沟发育有明显的规律性，在坡面上呈平行状分布，细沟密度与坡度密切相关，细沟存在会延长产流时间；黄绵土产流慢，较难形成细沟，细沟发育随机性大。细沟发育对产流过程没有明显影响，土壤入渗快慢是两种土壤产流过程存在差异的主要原因。细沟发育程度加剧，会使塿土含沙量的增加速度加快，达到稳定含沙量的时间提前，坡面已有细沟只对稳定含沙量有明显影响，细沟密度增加会使稳定含沙量提高；黄绵土含沙量的变化主要取决于细沟发育过程中的随机性，当细沟侵蚀以崩塌作用为主时，含沙量会出现急剧增加，即使雨强较小，也会产生严重的土壤侵蚀。
- 土壤侵蚀 /
- 模拟降雨 /
- 坡面径流 /
- 含沙量
Abstract: In order to understand the runoff-sediment yielding processes of rill erosion for different soils, the characteristics of runoff and sediment yield in rill development for Lou soil (silty clay loam) and loess soil were studied under different slope gradients and simulated rainfall conditions. Results show that the runoff generation occurred earlier and rills formed more easily within Lou soil than within loess soil. The rill formation exhibited a regular parallel distribution. The degree of rill development increased as the gradient increased, which could prolong the time of runoff generation. For loess soil, however, it was hard to generate runoff and induce rill formation. The rills that did form exhibited a random orientation. The processes of rill development did not have a significant effect on runoff yield; the soil infiltration rate was the major factor causing the difference in the runoff generation processes in the two soils. For Lou soil, the rate of sediment production increased with an increase in the degree of rill development. Sediment production stabilized early, and sediment concentration increased as rill density increased. For loess soil, the sediment concentration process largely depended upon the randomness in the rill development process. When the rill erosion was based on collapse, a sharp increase was noted in sediment concentration, where even low rainfall intensities could cause significant soil erosion.
- soil erosion /
- artificial rainfall /
- hillslope runoff /
- sediment concentration

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细沟形成对坡面产流产沙过程的影响

1. 首都师范大学城市环境过程与数字模拟国家重点实验室培育基地, 北京 100048;

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;

3. 中国科学院地理科学与资源研究所陆地水循环与地表过程重点实验室, 北京 100101

基金项目: 国家自然科学基金资助项目（41130744；41271304）

作者简介:
和继军（1979-），男，河北邢台人，副教授，博士，主要从事土壤侵蚀、水土保持等研究。E-mail：hejiun_200018@163.com

通讯作者: 蔡强国，E-mail：caiqg@igsnrr.ac.cn

收稿日期: 2013-04-27
刊出日期: 2014-01-25

中图分类号: S157.1

关键词:

摘要: 为探明细沟形成条件下不同土壤坡面水沙变化特性，利用室内模拟降雨试验，分析了塿土和黄绵土在细沟发育及已有细沟条件下的水沙过程变化规律。结果表明，塿土产流快，易形成细沟，细沟发育有明显的规律性，在坡面上呈平行状分布，细沟密度与坡度密切相关，细沟存在会延长产流时间；黄绵土产流慢，较难形成细沟，细沟发育随机性大。细沟发育对产流过程没有明显影响，土壤入渗快慢是两种土壤产流过程存在差异的主要原因。细沟发育程度加剧，会使塿土含沙量的增加速度加快，达到稳定含沙量的时间提前，坡面已有细沟只对稳定含沙量有明显影响，细沟密度增加会使稳定含沙量提高；黄绵土含沙量的变化主要取决于细沟发育过程中的随机性，当细沟侵蚀以崩塌作用为主时，含沙量会出现急剧增加，即使雨强较小，也会产生严重的土壤侵蚀。

English Abstract

Effects of rill development on runoff and sediment yielding processes

1. Base of the State Laboratory of Urban Environmental Processes and Digital Modeling, Capital Normal University, Beijing 100048, China;

2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Water and Soil Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China;

3. Key Laboratory of Water Cycle & Related Land Surface Processes, Institute of Geographical Sciences and Natural Resources Research, CAS, Beijing 100101, China

Funds: The study is financially supported by the National Natural Science Foundation of China (No.41130744; No.41271304).

Received Date: 2013-04-27
Publish Date: 2014-01-25

Keywords:

Abstract: In order to understand the runoff-sediment yielding processes of rill erosion for different soils, the characteristics of runoff and sediment yield in rill development for Lou soil (silty clay loam) and loess soil were studied under different slope gradients and simulated rainfall conditions. Results show that the runoff generation occurred earlier and rills formed more easily within Lou soil than within loess soil. The rill formation exhibited a regular parallel distribution. The degree of rill development increased as the gradient increased, which could prolong the time of runoff generation. For loess soil, however, it was hard to generate runoff and induce rill formation. The rills that did form exhibited a random orientation. The processes of rill development did not have a significant effect on runoff yield; the soil infiltration rate was the major factor causing the difference in the runoff generation processes in the two soils. For Lou soil, the rate of sediment production increased with an increase in the degree of rill development. Sediment production stabilized early, and sediment concentration increased as rill density increased. For loess soil, the sediment concentration process largely depended upon the randomness in the rill development process. When the rill erosion was based on collapse, a sharp increase was noted in sediment concentration, where even low rainfall intensities could cause significant soil erosion.

和继军, 宫辉力, 李小娟, 蔡强国. 细沟形成对坡面产流产沙过程的影响[J]. 水科学进展, 2014, 25(1): 90-97.

引用本文:

和继军, 宫辉力, 李小娟, 蔡强国. 细沟形成对坡面产流产沙过程的影响[J]. 水科学进展, 2014, 25(1): 90-97.

HE Jijun, GONG Huili, LI Xiaojuan, CAI Qiangguo. Effects of rill development on runoff and sediment yielding processes[J]. Advances in Water Science, 2014, 25(1): 90-97.

Citation:

HE Jijun, GONG Huili, LI Xiaojuan, CAI Qiangguo. Effects of rill development on runoff and sediment yielding processes[J]. Advances in Water Science, 2014, 25(1): 90-97.