地质通报2024,Vol.43Issue(4) :641-650.DOI:10.12097/gbc.2022.07.027

基于RUSLE模型的塔里木河流域上游土壤保持时空变化研究

Spatio-temporal variation of soil conservation in the upper reaches of the Tarim River Basin based on RUSLE model

熊茂秋 刘晓煌 张雪辉 刘玖芬 郑艺文 张子凡 赖明 付宇佳
地质通报2024,Vol.43Issue(4) :641-650.DOI:10.12097/gbc.2022.07.027

基于RUSLE模型的塔里木河流域上游土壤保持时空变化研究

Spatio-temporal variation of soil conservation in the upper reaches of the Tarim River Basin based on RUSLE model

熊茂秋 1刘晓煌 2张雪辉 3刘玖芬 2郑艺文 4张子凡 5赖明 1付宇佳6
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作者信息

  • 1. 中国地质大学(武汉)资源学院,湖北武汉 430074;自然资源要素耦合过程与效应重点实验室,北京 100055
  • 2. 自然资源要素耦合过程与效应重点实验室,北京 100055
  • 3. 廊坊市园林绿化事务中心,河北廊坊 065000
  • 4. 自然资源要素耦合过程与效应重点实验室,北京 100055;中国地质大学(武汉)地质调查研究院,湖北武汉 430074
  • 5. 自然资源要素耦合过程与效应重点实验室,北京 100055;中国地质大学(武汉)地理与信息工程学院,湖北武汉 430074
  • 6. 自然资源要素耦合过程与效应重点实验室,北京 100055;中国地质大学(武汉)地球物理与空间信息学院,湖北武汉 430074
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摘要

新疆塔里木河流域是中国重点生态保护区,流域土壤保持量的研究有利于水土保持功能区划和水土保持治理措施布局,对于区域生态修复与维护有重要作用.以塔里木河流域上游区为研究对象,基于该区域 2000-2020 年的降雨、土壤、地形等数据,采用修正通用土壤流失方程(RUSLE模型),估算 2000-2020 年流域土壤在水力侵蚀下的土壤侵蚀量和土壤保持量,分析其时空变化规律,并就土壤保持对其影响因子的敏感性展开分析.结果表明:流域以微度和轻度土壤侵蚀为主,在 2000-2020 年的土壤侵蚀面积总体呈减少趋势;土壤保持空间分布呈现中间高、四周低格局,且 2000-2020 年的土壤保持强度在一定程度上得到增强;降雨、地形和土地利用是土壤保持变化的主要驱动因子,且土壤保持能力随着降水量和植被覆盖总体呈现梯度增长趋势.评价结果揭示了研究区土壤保持时空分布特征,以及土壤保持对驱动因子的敏感性,可为流域水土侵蚀防治和生态修护提供指导依据.

Abstract

The Tarim River Basin in Xinjiang is a key ecological reserve in China,and the study of soil conservation in the basin is beneficial to the functional zoning of soil and water conservation and the layout of soil and water conservation management measures,and plays an important role in regional ecological restoration and maintenance.Based on the rainfall,soil and topography data of the upper Tarim River Basin from 2000 to 2020,the Revised Universal Soil Loss Equation(RUSLE model)is used to estimate the soil erosion and soil conservation of the watershed soils under hydraulic erosion from 2000 to 2020,analyse their spatial and temporal variation patterns,and conduct a sensitivity analysis on the soil conservation to its influencing factors.The results show that soil erosion and soil retention in the basin are characterised by micro-and micro-erosion.The results show that:soil erosion in the watershed is mainly slight and mild,and the area of soil erosion is generally decreasing from 2000 to 2020;the spatial distribution of soil conservation shows a pattern of high in the middle and low in the surroundings,and the intensity of soil conservation is enhanced to a certain extent from 2000 to 2020;rainfall,topography and land use are the main driving factors of soil conservation changes,and the soil conservation capacity is increasing with the amount of The results of the evaluation reveal that the soil conservation capacity of the study area is increasing in a gradient with the amount of precipitation and vegetation cover in general.The evaluation results reveal the spatial and temporal distribution characteristics of soil conservation in the study area,as well as the sensitivity of soil conservation to the driving factors,and the results of the study can provide guidance for the control of soil erosion and ecological conservation in the watershed.

关键词

RUSLE模型/土壤保持/驱动因子/时空格局/塔里木河流域

Key words

RUSLE rnodel/soil conservation/driving force/spatiotemporal pattern/Tarim River Basin

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基金项目

中国地质调查局项目(ZD20220144)

&&(2021xjkk140104)

出版年

2024
地质通报
中国地质调查局

地质通报

CSTPCDCSCD北大核心
影响因子:1.226
ISSN:1671-2552
被引量2
参考文献量21
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