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模拟降雨条件下崩积体坡面产流产沙特征及其响应关系
引用本文:朱高立,肖泽干,刘晓静,黄炎和,邹伟,林金石,蒋芳市. 模拟降雨条件下崩积体坡面产流产沙特征及其响应关系[J]. 水土保持通报, 2016, 36(6): 1-7. DOI: 10.13961/j.cnki.stbctb.2016.06.001
作者姓名:朱高立  肖泽干  刘晓静  黄炎和  邹伟  林金石  蒋芳市
作者单位:1. 福建农林大学资源与环境学院,福建福州350002;南京农业大学公共管理学院,江苏南京210095;2. 南京农业大学公共管理学院,江苏南京,210095;3. 福建农林大学资源与环境学院,福建福州,350002
基金项目:国家自然科学基金项目“花岗岩崩岗土体胶结物质与抗剪强度的关系”(41571272),“组合指纹法分析花岗岩崩岗侵蚀产沙运移规律研究”(41001169);国家科技支撑计划项目(2014BAD15B0303)
摘    要:[目的]研究崩积体坡面产流产沙特征及其响应关系,为崩岗治理提供理论基础与科学依据。[方法]通过室内模拟降雨试验,探讨不同覆盖度(0%,25%,50%,75%,100%)和坡度(25°,30°,35°)组合坡面在90mm/h雨强条件下的产流产沙时空特征及其响应关系。[结果]不同覆盖度和坡度条件下,坡面产流时间的变化范围在33~292s;同一坡度条件下,坡面产流时间与覆盖度呈线性正相关关系;同一覆盖度条件下,坡面产流时间与坡度呈幂函数关系。通过双因素方差分析可知,坡度对径流量的影响达到极显著水平,覆盖度对产沙量的影响达到显著水平。当坡度为25°时,坡面产沙总量的临界覆盖度为50%;当坡度为30°时,坡面产沙总量的临界覆盖度为75%;当坡度为35°时,坡面径流量的临界覆盖度为50%。[结论]针对不同坡度崩积体坡面,可以选择合适的秸秆覆盖度以达到较好的水土保持效果。

关 键 词:崩积体  人工模拟降雨  秸秆覆盖  侵蚀
收稿时间:2016-05-11
修稿时间:2016-05-14

Processes and Responses of Runoff and Sediment Yield on Colluvial Deposits Under Simulated Rainfall
ZHU Gaoli,XIAO Zegan,LIU Xiaojing,HUANG Yanhe,ZOU Wei,LIN Jinshi and JIANG Fangshi. Processes and Responses of Runoff and Sediment Yield on Colluvial Deposits Under Simulated Rainfall[J]. Bulletin of Soil and Water Conservation, 2016, 36(6): 1-7. DOI: 10.13961/j.cnki.stbctb.2016.06.001
Authors:ZHU Gaoli  XIAO Zegan  LIU Xiaojing  HUANG Yanhe  ZOU Wei  LIN Jinshi  JIANG Fangshi
Affiliation:College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, Fujian 350002, China;College of Public Administration, Nanjing Agricultural University, Nanjing, Jiangsu 210095, China,College of Public Administration, Nanjing Agricultural University, Nanjing, Jiangsu 210095, China,College of Public Administration, Nanjing Agricultural University, Nanjing, Jiangsu 210095, China,College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, Fujian 350002, China,College of Public Administration, Nanjing Agricultural University, Nanjing, Jiangsu 210095, China,College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, Fujian 350002, China and College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou, Fujian 350002, China
Abstract:[Objective] The erosion mechanism of colluvial deposits was researched to provide a theoretical basis and scientific evidence for the treatment of collapsing hills.[Methods] An indoor rainfall simulation experiment on slopes of colluvial deposits under 90 mm/h rainfall,and with the treatments of coverages(0,25%,50%,75%,100%) and slopes(25°,30°,35°) was carried out. Runoff and sediment were measured.[Results] The initiating time of runoff under different conditions changed from 33 to 292 s. Under the same slope gradient, there was a linear positive correlation between the initiating time of runoff and the straw coverage, and the initiating time of runoff had a power function with slope as independent variable. Through two-way variance analysis, the influence of slope on runoff was very significant and the influence of coverage on sediment yield was significant. The critical straw coverage of sediment yield was 50% under 25°, the critical straw coverage of sediment yield was 75% under 30°, the critical straw coverage of runoff was 50% under 35°.[Conclusion] For different slope gradients of colluvial deposits,we can choose optimal coverage of straw to reduce sediment yield and runoff effectively.
Keywords:colluvial deposits  artificial simulation rainfall  straw mulch  erosion
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