长江科学院院报 ›› 2024, Vol. 41 ›› Issue (12): 57-65.DOI: 10.11988/ckyyb.20230814

• 水土保持与生态修复 • 上一篇    下一篇

地形因子尺度效应及其对水力侵蚀估算的影响研究进展

卢刚1(), 王兴连1, 艾克拜尔·热合木吐拉1, 马惟杨2, 王一峰3, 孙宝洋3, 李力3()   

  1. 1 新疆维吾尔自治区水土保持生态环境监测总站,乌鲁木齐 830011
    2 华中师范大学 城市与环境科学学院,武汉 430079
    3 长江科学院 水土保持研究所,武汉 430010
  • 收稿日期:2023-07-26 修回日期:2023-09-25 出版日期:2024-12-01 发布日期:2024-12-01
  • 通信作者:
    李 力(1988-),男,湖北麻城人,高级工程师,博士,主要从事土壤侵蚀和水土保持研究。E-mail:
  • 作者简介:

    卢 刚(1978-),男,甘肃民勤人,高级工程师,硕士,主要从事水土保持监测和管理工作。E-mail:

  • 基金资助:
    新疆水利科技项目专项经费项目(XSKJ-2023-14); 国家重点研发计划项目(2022YFF1302901); 国家自然科学基金项目(42107353); 长江科学院基本科研业务费项目(CKSF2023340/TB)

Scaling Effects of Topographic Factors and Its Influence on Soil Water Erosion Estimation: A Review

LU Gang1(), WANG Xing-lian1, AIKEBAIER·Rehetumula1, MA Wei-yang2, WANG Yi-feng3, SUN Bao-yang3, LI Li3()   

  1. 1 Soil and Water Conservation Ecological Environment Monitoring Station of Xinjiang Uygur Autonomous Region,Urumqi 830011,China
    2 School of Urban and Environmental Sciences, Central China Normal University, Wuhan 430079,China
    3 Soil and Water Conservation Department,Changjiang River Scientific ResearchInstitute, Wuhan 430010,China
  • Received:2023-07-26 Revised:2023-09-25 Published:2024-12-01 Online:2024-12-01

摘要:

地形是影响水土流失的重要因素,地形因子是水力侵蚀估算模型的关键参数。区域土壤侵蚀研究中地形因子多基于中低分辨率数字高程模型(DEM)提取,但提取的坡度发生衰减、坡长发生扩张,显著影响水力侵蚀估算。通过总结坡度、坡长尺度效应及其对水力侵蚀估算的影响等方面的研究进展,结果显示,地形因子尺度效应广泛存在于不同侵蚀类型区,但坡度衰减、坡长扩张规律迥异;地形因子尺度效应与区域地形复杂程度相关,并受地形信息空间频率组成、地形因子计算方式和截断方式等因素的共同影响;不同区域坡度、坡长因子对DEM分辨率敏感度不同,其尺度效应对水力侵蚀估算的影响程度也不同。目前在坡度衰减、坡长扩张基本规律方面已有较为丰硕的研究成果,但坡度衰减和坡长扩张机制、坡度和坡长因子尺度效应耦合机理、人为活动引起坡面地形突变对地形因子尺度效应的影响机制、地形因子转换方法的区域适用性和地貌学原理及转换结果的不确定性评价等方面需加强后续研究。

关键词: 地形因子, DEM, 尺度效应, 水力侵蚀估算, 研究综述

Abstract:

Topography significantly affects soil erosion, and topographic factors are key parameters in water erosion models. Topographic factors in existing modelling of regional soil erosion are mostly extracted from medium and low resolution DEMs,resulting in under-estimated slope gradient and over-estimated slope length,significantly affecting water erosion estimations. This study reviews the research progresses in the scaling effects of topographic factors and the associated effects on water erosion estimations. Results showed that the scaling effect of topographic factors widely exists in different terrain type areas,but the laws of slope attenuation and slope length expansion are quite different. These scaling effects are influenced by terrain complexity,spatial frequency of terrain information,calculation methods,and truncation techniques. The sensitivity of slope gradient and slope length factors to digital elevation model(DEM) resolution varies by region,leading to differential impacts on water erosion estimations. While scientists have made considerable achievements in elucidating the fundamental laws of slope gradient attenuation and slope length expansion,several critical areas need to be further explored,including the mechanisms underlying slope gradient attenuation and slope length expansion,the coupling mechanisms of slope gradient and slope length factor scaling effects,the impact of topographic alterations caused by human activities on scaling effects,the regional applicability,geomorphological principles,and the uncertainty analysis of topographic factor transformation models.

Key words: topographic factors, DEM, scaling effects, water erosion estimation, literature review

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