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草本植物对土质路面径流水动力学特征及水沙过程的影响
引用本文:田风霞,刘 刚,郑世清,马春艳,张 琼.草本植物对土质路面径流水动力学特征及水沙过程的影响[J].农业工程学报,2009,25(10):25-29.
作者姓名:田风霞  刘 刚  郑世清  马春艳  张 琼
作者单位:1. 西北农林科技大学中国科学院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,杨凌,712100;兰州大学西部环境教育部重点实验室,兰州,730000
2. 西北农林科技大学中国科学院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,杨凌,712100;三峡大学三峡库区地质灾害教育部重点实验室,宜昌,443002
3. 西北农林科技大学中国科学院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,杨凌,712100
4. 三峡大学三峡库区地质灾害教育部重点实验室,宜昌,443002
基金项目:国家重点基础研究发展计划资助项目(2007CB407205);中国科学院西部行动计划项目(KZCX2-XB2-05)
摘    要:通过室内人工模拟降雨,研究了草本植物不同覆盖度土质路面的径流水动力学特征以及路面的产流产沙过程。结果表明,路面径流的弗劳德数和雷诺数属层流的急流范畴,并且二者与径流流速及过水断面单位能量相同,均随草本植物覆盖度的增大而减小。而Darcy-weisbach阻力系数以及曼宁糙率系数则均随覆盖度的增大而增大。在不同覆盖度土质路面上,径流量随径流时间急剧增大后趋于稳定,且二者符合移轴双曲线关系,而输沙率则经历了先增大后减小的过程。随着植被覆盖度的增大,土质道路的水分入渗率逐渐增大,而径流量、输沙率及含沙率均逐渐减小。该研究表明土质路面种植的草本植物具有较好的水土保持功能,为阐明草本植物与土壤侵蚀的关系提供了理论依据。

关 键 词:水动力学,径流,人工降雨,覆盖度,土质路面,减水减沙
收稿时间:2008/3/11 0:00:00
修稿时间:2009/7/13 0:00:00

Influence of herbaceous plants on runoff hydraulic characteristics and sediment generation on terrene roads
Tian Fengxi,Liu Gang,Zheng Shiqing,Ma Chunyan and Zhang Qiong.Influence of herbaceous plants on runoff hydraulic characteristics and sediment generation on terrene roads[J].Transactions of the Chinese Society of Agricultural Engineering,2009,25(10):25-29.
Authors:Tian Fengxi  Liu Gang  Zheng Shiqing  Ma Chunyan and Zhang Qiong
Abstract:Indoor rainfall simulation was employed to investigate the hydraulic characteristics of runoff, and runoff generation and sediment generation processes on terrene roads with different coverage degrees of herbaceous plants. The study indicated that on the roads the Froude numbers and Reynolds numbers of runoff fell into the category of supercritical flow of laminar flow. Their unit energies were consistent with the runoff velocity and water-carrying section, which were decreased with the increasing of the coverage degrees of herbaceous plants. The Manning roughness coefficients and the Darcy-weisbach friction coefficients increased as the coverage degrees increased. On the terrene roads with different coverage degrees, the amounts of runoff initially increased sharply and then stabilized with runoff-lasting time. Both the amounts of runoff and the runoff-lasting time were following an offset hyperbola, whereas the sediment yield rates initially increased and then declined. With the increasing of coverage degrees, the infiltration rates of water into the terrene roads gradually increased and the amounts of runoff, sediment yield rates and sediment concentration all gradually decreased. The study revealed that on terrene roads herbaceous plants could play a favorable role in soil and water conservation and provided a theoretical basis for understanding the relations between herbaceous plants and soil erosion.
Keywords:hydrodynamic  runoff  cloud seeding  coverage degree  terrene road  runoff and sediment reduction
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