降雨与植被对大别山林改园区水土流失影响试验研究
DOI:
作者:
作者单位:

中国地质调查局长沙自然资源综合调查中心

作者简介:

通讯作者:

中图分类号:

基金项目:

中国地质调查局项目“大别山区东段生态修复综合调查”(DD20242416)和中国地质调查局项目“东部平原湖区南部湖泊调查”(DD20230506)联合资助。


Experimental Study on the Impact of Rainfall and Vegetation on Soil Erosion in the Dabie Mountain Forest Reform Area
Author:
Affiliation:

Changsha General Survey of Natural Resources Center,China Geological Survey

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
    摘要:

    [目的]水土流失是制约生态环境与社会经济可持续发展的重要影响因素。大别山区作为国家级水土流失重点防治区域,近年来由于林地向园地转化的现象愈发普遍,进一步加剧了水土流失问题,造成该区域同时面临着生态脆弱化与经济可持续发展受阻的双重挑战。为深入探究大别山区水土流失的影响机制,从而为该地区生态环境治理提供因地制宜的科学支撑。[方法]本研究选取大别山区一处种植油茶的斜坡作为研究对象,自主设计原位降雨试验系统,设置了小雨、中雨、大雨以及久旱后大雨等四种降雨工况,并在 20%、40% 和 60% 三种不同植被覆盖度条件下开展降雨试验,旨在分析土壤含水率、径流量和产沙量等关键要素的变化特征及其响应关系。[结果]降雨强度是驱动大别山区林改园斜坡水土流失的主导因子。当次降雨量超42 mm且降雨强度达到 26 mm/h时,可突破植被缓冲阈值,削弱其保护作用;研究区植被覆盖度对水土流失的影响可能存在边际效益。不同降雨条件下,植被覆盖度从20%提升至40%时,平均径流削减31.33%,平均产沙削减70.5%。植被覆盖度提升至60%时,平均径流削减38.80%,平均产沙削减79.9%;研究区土壤初始含水率的变化对水土流失总量具有显著影响。当次降雨量超42mm且降雨强度达到 26 mm/h时,研究区土壤初始含水率降低5%~10%,可使径流量和产沙量平均减少26%和19%。[结论]该研究可为大别山区水土流失防控提供量化依据。

    Abstract:

    [Objective] Soil erosion is a critical factor constraining the sustainable development of both ecological environments and socio-economic systems. As a nationally designated key area for soil erosion control, the Dabie Mountains region has witnessed increasingly widespread conversion of forested land to orchards in recent years. This trend has further exacerbated soil erosion, leaving the region facing dual challenges of ecological fragility and impeded economic sustainability. To investigate the impact mechanisms of soil erosion in the Dabie Mountains and provide locally tailored scientific support for ecological management, [Methods] this study selected a tea oil plantation slope in the Dabie Mountains as the research site. An in-situ rainfall testing system was independently designed, simulating four rainfall scenarios: light rain, moderate rain, heavy rain, and heavy rain following prolonged drought. Tests were conducted under three vegetation coverage levels (20%, 40%, and 60%) to analyze changes in key parameters—soil moisture content, runoff volume, and sediment yield—and their interrelationships. [Results] Rainfall intensity emerged as the dominant driver of soil erosion on reforested slopes in the Dabie Mountains. When cumulative rainfall exceeded 42 mm and intensity reached 26 mm/h, vegetation"s protective threshold was breached, diminishing its buffering effect. The impact of vegetation coverage on erosion in the study area may exhibit diminishing returns. Under different rainfall conditions, increasing vegetation cover from 20% to 40% reduced average runoff by 31.33% and average sediment yield by 70.5%. When vegetation cover reached 60%, average runoff decreased by 38.80% and average sediment yield by 79.9%. Changes in the study area"s initial soil moisture content significantly influenced total soil erosion. When rainfall exceeded 42 mm and intensity reached 26 mm/h, a 5%–10% reduction in initial soil moisture content resulted in average decreases of 26% and 19% in runoff and sediment yield, respectively. [Conclusion] This study provides quantitative evidence for soil erosion prevention and control in the Dabie Mountains region.

    参考文献
    相似文献
    引证文献
引用本文
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2025-09-09
  • 最后修改日期:2025-09-19
  • 录用日期:2025-09-19
  • 在线发布日期:
  • 出版日期: