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Remote Sensing for Natural Resources    2022, Vol. 34 Issue (4) : 254-261     DOI: 10.6046/zrzyyg.2021313
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Remote sensing monitoring of the dynamic changes in geologic hazards in the Huangshui River basin of Qinghai Province
XIN Rongfang1,2,3,4(), LI Zongren1,2,3,4(), ZHANG Kun1,2,3,4, ZHANG Xing1,2,3,4, HUANG Li1,2,3,4, LIU Baoshan1,2,3,4
1. Institute of Geological Survey of Qinghai Province, Xining 810012, China
2. Qinghai Remote Sensing Big Data Engineering Technology Research Center, Xining 810012, China
3. Qinghai Satellite Application Technology Center for Natural Resources, Xining 810012, China
4. The Northern Qinghai-Tibet Plateau Geological Processes and Mineral Resources Laboratory, Xining 810012, China
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Abstract  

This study investigated the causes of the frequent occurrence of geologic hazards in the Huangshui River basin of Qinghai Province in recent years mainly using the GF-1 and GF-2 satellite remote sensing data. Based on the comparative monitoring of multi-source, multi-temporal, and multi-period remote sensing images and the support of geoscience knowledge, this study built a detailed and reliable spatial distribution database of geological hazards through the sorting, analysis, and screening of existent geologic hazard data of the study area, the laboratory interpretation of remote sensing images, and field investigation and verification. Then, it conducted a statistical analysis using the spatial analysis module of GIS and the parameters of geologic hazards. Finally, this study explored the relationships between the occurrence of geologic hazards and geological environment, natural factors, and human activities. The results are as follows. In 2017, 3 188 sites of geologic hazards such as collapse and landslide were discovered in the study area. A total of 233 geologic hazard sites have changed since 2009. Among the formation conditions of geologic hazards, the geological environment conditions have changed slowly, while human engineering activities and rainfall have been the most active factors, which jointly induced geologic hazards.
Keywords geological disasters      Huangshui River basin      dynamic change      remote sensing monitoring      change analysis     
ZTFLH:  TP79  
Issue Date: 27 December 2022
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Rongfang XIN
Zongren LI
Kun ZHANG
Xing ZHANG
Li HUANG
Baoshan LIU
Cite this article:   
Rongfang XIN,Zongren LI,Kun ZHANG, et al. Remote sensing monitoring of the dynamic changes in geologic hazards in the Huangshui River basin of Qinghai Province[J]. Remote Sensing for Natural Resources, 2022, 34(4): 254-261.
URL:  
https://www.gtzyyg.com/EN/10.6046/zrzyyg.2021313     OR     https://www.gtzyyg.com/EN/Y2022/V34/I4/254
Fig.1  Geomorphic feature of the study area
Fig.2  Technical flow chart
Fig.3  Domestic high-resolutions remote sensing data distribution for this study
序号 数据类型 覆盖地区 年份 分辨率/m
1 IKONOS 西宁市辖区 2014年 1
2 TH-1 大通回族土族自治县、湟中县、湟源县、平安区、互助县 2014年 5
3 ZY-3 乐都区、民和回族土族自治县、海晏县 2014年 2.1
4 Resurs-P1 西宁市辖区 2013年 5
5 ZY-3 大通回族土族自治县、湟中县、湟源县、乐都区、平安区、民和县、互助县、海晏县 2013年 2.1
6 GeoEye 西宁市辖区 2012年 0.41
7 TH-1 大通回族土族自治县、湟中县、湟源县、乐都区、平安区、互助县、海晏县 2012年 5
8 ZY-3 民和回族土族自治县 2012年 2.1
9 GeoEye 西宁市辖区 2011年 0.41
10 ZY-3 大通回族土族自治县、湟中县、湟源县、乐都区、平安区、民和回族土族自治县、互助县、海晏县 2011年 2.1
11 WorldView-2 西宁市辖区 2010年 0.46
12 Cartosat-1 大通回族土族自治县、湟中县、湟源县、乐都区、平安区、民和回族土族自治县、互助县、海晏县 2010年 5
13 WorldView-2 西宁市辖区 2009年 0.46
14 RAPIDEYE 大通回族土族自治县、湟中县、湟源县、乐都区、平安区、民和回族土族自治县、互助县、海晏县 2009年 5
Tab.1  List of monitoring and comparison data collection
Fig.4  Remote sensing interpretation indicators of typical geological disasters
灾害发育
地质单元		 崩塌/
处		 滑坡/
处		 不稳定
斜坡/处		 合计/
处		 所占比
例/%
松散堆积物(Q2) 9 10 87 106 3.32
黄土(Q1) 105 1 172 1 152 2 429 76.20
碎屑岩(N) 46 119 45 210 6.60
碎屑岩(E) 13 125 42 180 5.64
碎屑岩(Mz) 5 35 39 79 2.48
碎屑岩(Pz) 2 1 21 24 0.75
变质岩(Pt) 20 9 87 116 3.63
花岗岩 6 2 36 44 1.38
合计 206 1 473 1 509 3 188 100
Tab.2  Statistic of remote sensing interpretation of geological disasters in the study area
Fig.5  Geological disasters slope rose diagram
划分依据 名称 基本指标 数量 所占比例/%
灾害类型 崩塌 — 7 3.00
滑坡 — 66 28.33
泥石流 — 111 47.64
不稳定斜坡 — 49 21.03
变化原因 自然因素 降雨等自然因素引起灾害发生变化 19 8.15
交通建设 铁路、公路建设工程中对灾害形成影响 21 9.01
矿业活动 矿山开采中对灾害形成影响 32 13.73
房屋建设 城市或乡村发展中,向周边扩展,开挖坡脚或在泥石流沟建设工厂、房屋等 49 21.03
农业活动 开荒建田过程中对灾害形成影响 6 2.58
工程治理 对灾害进行工程治理 29 12.45
搬迁治理 受威胁居民进行搬迁 77 33.05
变化结果 新发生 新发生的滑坡、崩塌等灾害点 19 8.15
微变形 滑坡、崩塌、斜坡发生微小滑动或出现裂隙,泥石流沟内松散堆积物发生变化 51 21.89
威胁增加 灾害威胁区域内新建工厂、房屋和道路等,使其变为隐患点 55 23.61
实施治理 已实施工程治理或搬迁治理 108 46.35
Tab.3  Classified statistic of geological disasters changes in the study area
Fig.6  Image comparison of Wangjiazhuang landslide before and after occurrence in Chengdong,Xining
Fig.7  Image comparison of Dazhuang landslide in Chengguan,Datong
Fig.8  Image comparison of Linjiaya landslide before and after treatment in Xining
Fig.9  Comparison before and after landslide in Hanzhuang,Chengxi,Xining
Fig.10  Remote sensing interpretation of Zhangjiawan landslide in Chengxi,Xining
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