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碎石含量影响下紫色土坡面径流流速变化过程及土壤侵蚀的阶段性
引用本文:韩珍,王小燕,李馨欣.碎石含量影响下紫色土坡面径流流速变化过程及土壤侵蚀的阶段性[J].中国农业大学学报,2016,21(10):102-108.
作者姓名:韩珍  王小燕  李馨欣
作者单位:西南大学 资源环境学院/三峡库区生态环境教育部重点实验室, 重庆 400716;西南大学 资源环境学院/三峡库区生态环境教育部重点实验室, 重庆 400716;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 杨陵 712100;西南大学 资源环境学院/三峡库区生态环境教育部重点实验室, 重庆 400716
基金项目:国家自然科学基金项目(40120514);黄土高原土壤侵蚀与旱地农业国家重点实验室基金课题(K318009902-14);西南大学大学生科技创新“光炯”培育项目(20140105)
摘    要:在室内人工模拟降雨条件下,对6种不同碎石含量(0,5%,10%,20%,30%,40%)的土壤侵蚀产流产沙的过程进行模拟研究。结果表明:碎石含量对径流流速的影响不显著,随着碎石含量的增加,平均径流流速呈减小的趋势。碎石含量对坡面侵蚀径流含沙率影响显著(F=30.076,P0.05),随着碎石含量的增加,径流含沙率呈降低的趋势。累积产沙量与降雨历时具有对数相关关系,碎石含量为5%时相关性最大,碎石含量越大累积产沙量递增速率越小。土壤中碎石混合通过改变土壤的物质组成和结构,增强土壤的抗蚀性和抗冲性,随着碎石含量的增加,土壤流失量逐渐减少,土壤侵蚀速率显著降低。

关 键 词:碎石  平均流速  径流含沙率  累积产沙量  侵蚀速率
收稿时间:2015/12/31 0:00:00

Processes of runoff velocity and stages of soil erosion under the effect of rock fragment content
HAN Zhen,WANG Xiao-yan and LI Xin-xin.Processes of runoff velocity and stages of soil erosion under the effect of rock fragment content[J].Journal of China Agricultural University,2016,21(10):102-108.
Authors:HAN Zhen  WANG Xiao-yan and LI Xin-xin
Institution:College of Resources and Environment/Key Laboratory of Eco-environments in Three Gorges Region Ministry of Education, Southwest University, Chongqing 400716, China;College of Resources and Environment/Key Laboratory of Eco-environments in Three Gorges Region Ministry of Education, Southwest University, Chongqing 400716, China;Chinese Academy of Sciences and Ministry of Water Resources State Key Laboratory of Soil Erosion and Dryland Farming an Loess Plateau, Yangling 712100, China;College of Resources and Environment/Key Laboratory of Eco-environments in Three Gorges Region Ministry of Education, Southwest University, Chongqing 400716, China
Abstract:Experiments were conducted to evaluate the effect of six different rock fragment contents (0,5%,10%,20%,30%,40%) on runoff and sediment yield with simulated rainfall equipment on the purple soil hillslope.The results showed that:content of rock fragment has no significant effect on the runoff rate.The increase of rock fragment will promote the wetting front downward migration;The sediment yield rate of the slope erosion was significantly effected by rock fragment content(F=30.076,P<0.05).With the increasement of rock fragment content,the rate of sediment yield decreased significantly.There was a linear correlation between cumulative erosion sediment yield and rainfall duration,which was maximum when rock fragment content is 5%.The more of rock fragment content,the lower of the sediment yield increasing rate.By changing the composition and structure of soil,soil mixed with rock fragments improved soil anti-erodibility and anti-scouribility.With the increasement of rock fragment content,the soil loss amount decreased gradually and the rate of soil erosion decreased significantly.
Keywords:rock fragment  average flow velocity  sediment concentration  cumulative sediments  erosion rate
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