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黄土高原坡面水土保持措施减沙水代价分析
引用本文:严丽,侯群群,王飞,穆兴民.黄土高原坡面水土保持措施减沙水代价分析[J].水土保持通报,2013,33(2):213-217.
作者姓名:严丽  侯群群  王飞  穆兴民
作者单位:1. 西北农林科技大学资源环境学院,陕西杨凌,712100
2. 西北农林科技大学水土保持研究所,陕西杨凌712100;中国科学院水利部水土保持研究所,陕西杨凌712100
基金项目:国家自然科学基金项目"基于相同气候条件的人类活动对河流水沙影响定量评价:以黄土高原延河流域为例",中国科学院重点部署项目,黄土高原及周边沙地近代生态环境的演变与可持续性课题的子课题,中国科学院对外合作重点项目,Netherlands Organization for Scientific Research
摘    要:不同的水土保持措施在减少侵蚀泥沙的同时对径流量的影响不同.以裸坡地水土流失为对照,分析了不同水土保持措施减水减沙比(Rrs),并以其作为减沙水代价指标,根据黄土高原土壤侵蚀严重的丘陵沟壑区(西峰、绥德、天水等3个典型区)的农地径流小区多年观测资料,分析了不同耕作措施及生物措施的减沙水代价(Rrs).结果表明,不同耕作方式Rrs差异很大,变化幅度在8.5~36.4 m3/t;在耕作措施上,横向耕作的Rrs大于防冲沟和浅耕,深耕Rrs最小;生物措施方面,低秆与高秆作物间作措施Rrs大于单作低秆作物和中高秆作物轮作,牧草(草木樨、苜蓿)轮作的Rrs较农作物轮作大,且草木樨与农作物轮作的Rrs大于苜蓿与农作物轮作.随着雨量的增加和坡度的增大,耕作措施和生物措施Rrs呈减小趋势.Rrs较大的措施在减少相同的坡面侵蚀泥沙时,有利于增加土壤水分,但是不利于径流形成.

关 键 词:黄土高原  水土保持措施  减水减沙比
收稿时间:2012/3/27 0:00:00
修稿时间:2012/11/19 0:00:00

Effectiveness of Soil and Water Conservation Practices in Runoff Control on Slope Lands in Loess Plateau
YAN Li,HOU Qun-qun,WANG Fei and MU Xing-min.Effectiveness of Soil and Water Conservation Practices in Runoff Control on Slope Lands in Loess Plateau[J].Bulletin of Soil and Water Conservation,2013,33(2):213-217.
Authors:YAN Li  HOU Qun-qun  WANG Fei and MU Xing-min
Institution:College of Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China;College of Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China;Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100, China;Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China;Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100, China;Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China
Abstract:Different soil and water conservation practices often varied considerably in sediment interceptionand runoff reduction.The cost effectiveness of sediment control can be quantified by the ratio of detainedrunoff and sediment(Rrs).Perennially monitoring data were collected from three typical loess regions(Xifengand Tianshui City in Gansu Province,Suide City in Shaanxi Province)and Rrs were calculated for differenttillage and biological practices.The results showed that the Rrsvaried greatly from 8.5to 36.4m3/t.Fortillage management,contour tillage showed the highest Rrs,followed by level ditch tillage and shallow plowing,while deep plowing had the lowest.For biological managements,the Rrsof intercropping of low-stemand high-stem crops was higher than those of monoculture of low crops and rotation of middle high-stemcrops.The Rrsof pasture(sweet clover,alfalfa)rotation was significantly higher than crop rotation,andsweet clover/crop rotation system was better than alfalfa-crop rotation system in terms of erosion control.With increasing rainfall and slope gradient,Rrsvalues decreased in general.The practice with higher Rrscouldreduce more runoff discharge and increase soil moisture content with similar performance in sediment control.
Keywords:the Loess Plateau  soil and water conservation practice  ratio of detained runoff and sediment
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