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集中水流下土石混合崩积体坡面侵蚀水动力特征试验研究

蒋芳市 陈培济 黄炎和 林金石 詹振芝 葛宏力 季翔

水土保持学报2017,Vol.31Issue(6):8-14,99,8.
水土保持学报2017,Vol.31Issue(6):8-14,99,8.DOI:10.13870/j.cnki.stbcxb.2017.06.002

集中水流下土石混合崩积体坡面侵蚀水动力特征试验研究

Experimental Study on Erosion Hydrodynamic Characteristics of Concentrated Flow on Soil-rock Mixed Colluvial Deposit Slopes

蒋芳市 1陈培济 1黄炎和 2林金石 1詹振芝 1葛宏力 1季翔1

作者信息

  • 1. 福建农林大学资源与环境学院,福建省土壤环境健康与调控重点实验室,福州350002
  • 2. 中国科学院城市环境研究所,福建厦门361021
  • 折叠

摘要

Abstract

In order to study the hydrodynamic mechanism of soil erosion on earth-rock mixed colluvial deposit slopes,scouring tests were conducted in the laboratory.In the tests,four the gravel contents (mass content)(0,20%,40% and 60%),four flows (2,4,8 and 16 L/min) and four slope gradients (10°,20°,30° and 40°) were set.Results showed the following:(1) Soil erosion rate decreased with the increasing of gravel content when the slope gradient or flow was low,while when the flow or slope gradient increased,erosion rate first decreased and then increased with the increasing of gravel content;erosion rates of different earth rock mixtures could be expressed by power function of slope and flow.(2) Flow shear stress,stream power and unit stream power were all linearly related to erosion rate,while by comparison,shear stress and stream power were the optimal hydrodynamic parameters to simulate the erosion process on the earth-rock mixed colluvial deposit slopes.(3) Soil erodibility parameter and critical erosion force both increased with the increasing of gravel content.These results of this study could provide a reference for further understanding the erosion mechanism of colluvial deposit.

关键词

崩岗/崩积体/土石混合物/土壤侵蚀/水动力学

Key words

benggang/colluvial deposit/earth-rock mixture/soil erosion/hydrodynamic

分类

农业科技

引用本文复制引用

蒋芳市,陈培济,黄炎和,林金石,詹振芝,葛宏力,季翔..集中水流下土石混合崩积体坡面侵蚀水动力特征试验研究[J].水土保持学报,2017,31(6):8-14,99,8.

基金项目

国家科技支撑计划项目(2014BAD15B0303) (2014BAD15B0303)

国家自然科学基金项目(41571272) (41571272)

水土保持学报

OA北大核心CSCDCSTPCD

1009-2242

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