水土保持通报   2020, Vol. 40 Issue (3): 175-179.  DOI: 10.13961/j.cnki.stbctb.2020.03.025
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引用本文 

王飞龙, 陈明, 王晓迪, 等. 汶川地震震中地区崩滑体的植被恢复与长期效应[J]. 水土保持通报, 2020, 40(3): 175-179. DOI: 10.13961/j.cnki.stbctb.2020.03.025
Wang Feilong, Chen Ming, Wang Xiaodi, et al. Vegetation Recovery of Co-seismic Landslide and Long-Term Effect at Central Area of Wenchuan Earthquake[J]. Bulletin of Soil and Water Conservation, 2020, 40(3): 175-179. DOI: 10.13961/j.cnki.stbctb.2020.03.025

资助项目

国家重点研发计划项目“强震山区特大地质灾害致灾机理与长期效应研究”(2017YFC1501004)

第一作者

王飞龙(1991-), 男(汉族), 河南省周口市人, 硕士, 助理工程师, 研究方向为环境地质灾害、遥感应用。Email:584975674@qq.com.

通讯作者

陈明(1993-), 男(汉族), 湖北省荆州市人, 博士生, 主要从事工程地质和地质灾害方向研究。Email:chenminggeo@163.com.

文章历史

收稿日期:2019-11-13
修回日期:2020-01-16
汶川地震震中地区崩滑体的植被恢复与长期效应
王飞龙1 , 陈明2 , 王晓迪2 , 丁军1 , 张皓1     
1. 中国建筑西南勘察设计研究院有限公司, 四川 成都 610052;
2. 成都理工大学 地质灾害防治与地质环境保护国家重点实验室, 四川 成都 610059
摘要:[目的] 评估汶川地震震中地区崩滑体自然植被恢复过程,旨在为该区震后地质环境恢复、灾害防治和重建提供依据。[方法] 以四川省汶川县映秀镇为研究区,以多期空间分辨率为30 m×30 m的Landsat遥感影像为数据源,分析震后崩滑体上的植被动态恢复变化,结合地形因子分析地震9 a后植被恢复的空间分布特征。[结果] 研究区震后至2011年,经历植被恢复程度较差,差等水平以下占比68%,期间暴雨泥石流活动频率高,至2013年后就达到一个较好的恢复水平,差等水平以下占比32%,之后就处于一个缓慢的恢复过程,至2017年植被恢复差等以下的崩滑体仍主要处于30°~50°的坡度区间,1 500~2 100 m高程区间、东南坡向。[结论] 四川省汶川县映秀镇总体上经过近9 a的恢复过程,植被覆盖度恢复到0.74,与震前相比差值为0.08,根据拟合模型预计2022年植被覆盖度能恢复到震前水平,但仍主要以草本和灌木为主,植被种群结构与震前差异较大。
关键词汶川地震    滑坡体    植被恢复    长期演变    
Vegetation Recovery of Co-seismic Landslide and Long-Term Effect at Central Area of Wenchuan Earthquake
Wang Feilong1 , Chen Ming2 , Wang Xiaodi2 , Ding Jun1 , Zhang Hao1     
1. China Southwest Survey and Design Research Institute of Architecture Co., Ltd., Chengdu, Sichuan 610052, China;
2. State Key Laboratory of Geo-hazard Prevention and Geo-environment Protection, Chengdu University of Technology, Chengdu, Sichuan 610059, China
Abstract: [Objective] The vegetation recovery process of the co-seismic landslide at central area of Wenchuan earthquake was assessed in order to provide the basis for the ecological environment restoration, disaster prevention, and reconstruction after the earthquake in the study area. [Methods] Yingxiu Town of Wenchuan County, Sichuan Province was taken as a study area, and the dynamic changes of vegetation at landslide sites after the earthquake were analyzed based on multi-temporal images with a resolution of 30 m. The spatial distribution characteristics of vegetation recovery in the past nine years were analyzed based on the topographic factors. [Results] The vegetation of the landslides did not recover well from 2008 to 2011 in the study area, and 68% of the sites were below the "poor" level. During this period, the frequencies of rainstorms and debris flow activity remained high. After 2013, a better recovery level was reached overall, and the number of landsides below the poor level decreased to 32%. Then, it had been in a slow recovery process. In 2017, the landslides with a poor level of vegetation recovery were mainly located in the slope range of 30°-50°, the elevation range of 1 500-2 100 m, and a southea