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国土资源遥感  2019, Vol. 31 Issue (4): 174-181    DOI: 10.6046/gtzyyg.2019.04.23
  技术应用 本期目录 | 过刊浏览 | 高级检索 |
基于高分辨率遥感影像的滑坡活动特征及稳定性分析——以东苗家滑坡为例
贾伟洁1,2, 王治华1
1. 中国科学院地理科学与资源研究所,北京 100101
2. 中国自然资源航空物探遥感中心,北京 100083
Landslide activity characteristics and stability analysis based on high-resolution remote sensing image: A case study of Dongmiaojia landslide
Weijie JIA1,2, Zhihua WANG1
1. Institute of Geographic Sciences and Natural Resources Research, China Academy of Sciences, Beijing 100101, China
2. China Aero Geophysical Survey and Remote Sensing Center for Natural Resources, Beijing 100083, China
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摘要 

基于综合校正后的2002—2016年间9景高分辨率影像、加密的ASTER GDEM高程数据产品和1:20万洛阳市幅区域地质图,采用数字滑坡技术解译了洛阳市东苗家滑坡地形地貌,分析了滑坡形成条件和活动特征,并推测了滑坡稳定性现状。结果显示,东苗家滑坡过程可以分为首次滑坡活动、随后牵引活动、前部滑坡活动和后续滑坡活动4个阶段; 形成7个平台和前部陡坡的四级台地地形; 东苗家滑坡的总方量约为425.4万m 3; 整体和各局部无明显变形位移现象,状态稳定。

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贾伟洁
王治华
关键词 东苗家滑坡数字滑坡技术解译基础活动特征四级台地    
Abstract

Based on the digital landslide technology, the authors employed revised 10 high-resolution remote sensing images between 2002 and 2016 as remote sensing image information source, densified ASTER DEM data as landslide elevation information source, and 1:200 000 Luoyang City regional geological maps as the geological environment source and, in combination with Dongmiaojia landslide, analyzed the creation conditions and active characteristics of the landslide, and predicted the present stability situation of landslide. The result shows that the active process of Dongmiaojia landslide can be divided into four stages, i.e., the first landslide activity, the subsequent traction activity, the front landslide activity and the follow-up activity, which formed topography of four level terraces with seven platforms and the front steep slope. The estimation of the total size of the Dongmiaojia landslide is 425.4×10 4 m 3. The comparison of ten high-resolution images indicates that there has been no obvious deformation and displacement in the Dongmiaojia landslide in recent years.

Key wordsDongmiaojia landslide    digital landslide technology    interpretation basis    activity characteristics    four level terraces
收稿日期: 2018-11-12      出版日期: 2019-12-03
:  TP79  
基金资助:高分辨率对地观测系统重大专项(编号: GFZX0404130302)及国家重点研发计划项目“基于国产遥感卫星的典型要素提取技术”共同资助(2016YFB0501404)
作者简介: 贾伟洁(1985-),在职博士研究生,主要从事地质矿产及环境遥感解译与研究。Email: weijie_agrs@qq.com。
引用本文:   
贾伟洁, 王治华. 基于高分辨率遥感影像的滑坡活动特征及稳定性分析——以东苗家滑坡为例[J]. 国土资源遥感, 2019, 31(4): 174-181.
Weijie JIA, Zhihua WANG. Landslide activity characteristics and stability analysis based on high-resolution remote sensing image: A case study of Dongmiaojia landslide. Remote Sensing for Land & Resources, 2019, 31(4): 174-181.
链接本文:  
https://www.gtzyyg.com/CN/10.6046/gtzyyg.2019.04.23      或      https://www.gtzyyg.com/CN/Y2019/V31/I4/174
Fig.1  东苗家滑坡位置和区域环境
序号 接收日期 影像特征
1 2002-09-08 初秋,清晰显示滑坡各部分特征
2 2012-06-22 初夏,植被覆盖,部分滑坡细节不清晰
3 2012-12-27 初冬,基本清楚显示滑坡各部分特征
4 2013-03-08 初春,基本清楚显示滑坡各部分特征
5 2014-11-13 秋末,清楚显示滑坡各部分特征
6 2015-03-13 春,雾重,影像不清晰
7 2015-07-01 夏,植被覆盖,部分滑坡细节不清晰
8 2015-12-14 初冬,基本清楚显示滑坡各部分特征
9 2016-09-29 深秋,植被覆盖,部分滑坡细节不清晰
Tab.1  遥感信息源
Fig.2  东苗家滑坡影像与地形叠加图
(影像获取日期为2014年11月13日,图中黄线表示滑坡边界,白线表示等高线)
Fig.3  东苗家滑坡地形平面和剖面图
Fig.4  东苗家滑坡坡度图
Fig.5  东苗家滑坡遥感解译
编号 平均高程/m 面积/ m2
T1 215 1 315
T2 217 7 224
T3 219 2 196
T4 233 2 641
T5 242 1 745
T6 248 3 080
T7 263 3 398
Tab.2  滑坡体上平台的平均高程与面积
Fig.6  东苗家滑坡主剖面图
(结合参考文献[1,2],经遥感解译改编)
Fig.7  2002—2016年9个时相东苗家滑坡变化情况
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