以岷县十里铺标准图幅为研究区,基于Landsat-8 OLI(operational land imager)遥感影像数据分析1990—2018年的植被覆盖度多年动态变化特征以及发展趋势。将多年植被覆盖度与相近年份的地质灾害点进行空间叠加对比,分析植被覆盖度与地质...以岷县十里铺标准图幅为研究区,基于Landsat-8 OLI(operational land imager)遥感影像数据分析1990—2018年的植被覆盖度多年动态变化特征以及发展趋势。将多年植被覆盖度与相近年份的地质灾害点进行空间叠加对比,分析植被覆盖度与地质灾害发生的时空对应关系,结合植被的水文效应以及力学效应探讨植被的抑灾及致灾作用机理。结果表明:研究区内植被先后经历急剧退化-逐渐恢复-略微退化的发展趋势,历年发生的地质灾害点主要分布于裸地和低植被覆盖度区域。地质灾害点分布密度总体随植被覆盖度的增加而减少,呈近似负相关关系。植被并不是决定地质灾害发育的关键因素,植被的水文效应和力学效应具有抑灾和致灾作用。在研判地质灾害发生概率时应综合考虑植被覆盖度、大气降水强度、历时产渗流等特征。展开更多
Because of the confining compression of the Pacific, Eurasian and Indian plates, the Chinese mainland is frequently stricken with earthquakes, especially in the Qinghai Tibet Plateau and surrounding areas and along th...Because of the confining compression of the Pacific, Eurasian and Indian plates, the Chinese mainland is frequently stricken with earthquakes, especially in the Qinghai Tibet Plateau and surrounding areas and along the NS-trending tectonic zone from Yinchuan to Lanzhou, Chengdu, and finally to the Kunming tectonic belt （Fig. 1）. Historical records show that there are 14 earthquakes of 〉Ms 8 occurring in the two regions, eight of which occurred along the latter tectonic belt. The 2008 Wenchuan earthquake located on both the NS tectonic zone and the Longmenshan fault zone along the eastern margin of the Qinghai-Tibet Plateau.展开更多
文摘以岷县十里铺标准图幅为研究区,基于Landsat-8 OLI(operational land imager)遥感影像数据分析1990—2018年的植被覆盖度多年动态变化特征以及发展趋势。将多年植被覆盖度与相近年份的地质灾害点进行空间叠加对比,分析植被覆盖度与地质灾害发生的时空对应关系,结合植被的水文效应以及力学效应探讨植被的抑灾及致灾作用机理。结果表明:研究区内植被先后经历急剧退化-逐渐恢复-略微退化的发展趋势,历年发生的地质灾害点主要分布于裸地和低植被覆盖度区域。地质灾害点分布密度总体随植被覆盖度的增加而减少,呈近似负相关关系。植被并不是决定地质灾害发育的关键因素,植被的水文效应和力学效应具有抑灾和致灾作用。在研判地质灾害发生概率时应综合考虑植被覆盖度、大气降水强度、历时产渗流等特征。
文摘Because of the confining compression of the Pacific, Eurasian and Indian plates, the Chinese mainland is frequently stricken with earthquakes, especially in the Qinghai Tibet Plateau and surrounding areas and along the NS-trending tectonic zone from Yinchuan to Lanzhou, Chengdu, and finally to the Kunming tectonic belt （Fig. 1）. Historical records show that there are 14 earthquakes of 〉Ms 8 occurring in the two regions, eight of which occurred along the latter tectonic belt. The 2008 Wenchuan earthquake located on both the NS tectonic zone and the Longmenshan fault zone along the eastern margin of the Qinghai-Tibet Plateau.
