院报 ›› 2021, Vol. 38 ›› Issue (10): 60-68.DOI: 10.11988/ckyyb.20210582

• 水土保持与生态修复 • 上一篇    下一篇

不同植被类型对堆积体坡面径流特性的影响

李建明1,2,3,4, 张长伟1,2, 王志刚1,2, 王一峰1,2, 许文盛1,2, 张冠华1,2, 蒲坚1,2,3,4, 刘纪根1,2   

  1. 1. 水土保持研究所,武汉 430010;
    2.水利部山洪地质灾害防治工程技术研究中心,武汉 430010;
    3.中国科学院水利部水土保持研究所 黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西 杨凌 712100;
    4.中国科学院大学,北京 100049
  • 收稿日期:2021-06-16 修回日期:2021-07-12 出版日期:2021-10-01 发布日期:2021-10-15
  • 通讯作者: 王志刚(1981-),男,湖北枣阳人,正高级工程师,博士,主要研究方向为土壤地理与土壤侵蚀。E-mail:371381624@qq.com
  • 作者简介:李建明(1989-),男,福建三明人,工程师,博士研究生,主要从事工程土壤侵蚀过程研究。E-mail:hahalijianming@126.com
  • 基金资助:
    国家自然科学基金项目(41701316,41877082,42077062); 中央级公益性科研院所基本科研业务费项目(CKSF2021447/TB,CKSF2021487/TB,CKSF2019170/TB);国家电网公司总部科技项目(52130421000L)

Impact of Different Vegetation Types on Runoff Characteristics of Spoil Heaps

LI Jian-ming1,2,3,4, ZHANG Chang-wei1,2, WANG Zhi-gang1,2, WANG Yi-feng1,2, XU Wen-sheng1,2, ZHANG Guan-hua1,2, PU Jian1,2,3,4, LIU Ji-gen1,2   

  1. 1. Soil and Water Conservation Department, Yangtze River Scientific Research Institute, Wuhan 430010, China;
    2. Research Center on Mountain Torrent & Geologic Disaster Prevention of the Ministry of Water Resources, Wuhan 430010, China;
    3. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China;
    4. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2021-06-16 Revised:2021-07-12 Online:2021-10-01 Published:2021-10-15

摘要: 针对植被防护堆积体侵蚀动力机制的问题,通过野外模拟降雨试验,分析直根系和须根系植被对堆积体径流流速、水力和水动力参数的影响。结果表明:植被削减堆积体平均侵蚀速率达88.34%~92.88%,直根系消减平均流速效益为50.51%,须根系为21.32%~35.61%;裸坡和植被堆积体径流流型均属于层流(雷诺数<40),裸坡径流在降雨强度≤1.2 mm/min时处于急流态,直根系堆积体均处于缓流态,须根系堆积体在急流态和缓流态间变化。直根系对坡面径流的阻滞作用大于须根系;植被防护下堆积体侵蚀速率、水力和水动力参数与裸坡呈显著性差异(P<0.05),径流剪切力和径流功率可用于较好地刻画坡面侵蚀动态过程,呈显著线性关系(R2为0.63~0.96)。研究成果可为生产建设项目工程堆积体水土流失量预测模型的植被因子修订提供科学依据。

关键词: 堆积体, 径流特性, 降雨试验, 流速, 侵蚀动力, 植被类型

Abstract: To obtain the erosion dynamic mechanism of spoil heaps, we examined the effects of taproot system (Artemisia gmelinii) and fibrous root system (Medicago sativa and Cynodon dactylon) vegetation on the runoff velocity, hydraulic parameters, and hydrodynamic parameters of the spoil heaps through artificial rainfall simulation experiment. Results demonstrated that vegetation reduced the average soil loss rate of spoil heaps by 88.34%-92.88%, as compared with bare spoil heaps. Average runoff velocity decreased by 50.51% under taproot system vegetation, and 21.32%-35.61% under fibrous root system vegetation. Both the runoff patterns of bare and vegetated spoil heaps were laminar (Reynolds Number <40). Runoff flow of bare spoil heaps was rapid when rainfall intensity was not greater than 1.2 mm/min; however, under the protection of taproot system vegetation, the runoff flow was slow, while under fibrous root system vegetation, the runoff flow pattern varied between rapid and slow regimes. Taproot system vegetation had a greater retardation effect on runoff resistance coefficient than fibrous root system. The flow shear stress and stream power could better describe the dynamic process of erosion on the spoil heaps under vegetation protection, showing a significant linear relationship (R2 was 0.63-0.96). Our findings offer scientific basis for revising the vegetation factors in the establishment of soil and water prediction model suitable for production and construction projects.

Key words: spoil heaps, runoff characteristics, rainfall experiment, runoff velocity, erosion dynamics, vegetation type

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