Characteristics and susceptibility evaluation of geohazard development in Shunping county, Hebei province

WAN Jiawei; FENG Chengjun; QI Bangshen; SUN Mingqian; YANG Xiaoxiao; WANG Huiqing; FAN Yulu; ZHANG Peng; MENG Jing; TAN Chengxuan

doi:10.12090/j.issn.1006-6616.2020.26.04.053

Volume 26 Issue 4

Aug. 2020

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Article Navigation > Journal of Geomechanics > 2020 > 26(4): 604-614

WAN Jiawei, FENG Chengjun, QI Bangshen, et al., 2020. Characteristics and susceptibility evaluation of geohazard development in Shunping county, Hebei province. Journal of Geomechanics, 26 (4): 604-614. DOI: 10.12090/j.issn.1006-6616.2020.26.04.053

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Characteristics and susceptibility evaluation of geohazard development in Shunping county, Hebei province

doi: 10.12090/j.issn.1006-6616.2020.26.04.053

WAN Jiawei^{1, 2, 3
,},
FENG Chengjun^{1, 2},
QI Bangshen⁴,
SUN Mingqian^{1, 2},
YANG Xiaoxiao^{1, 2
,
,},
WANG Huiqing^{1, 2},
FAN Yulu^{1, 2},
ZHANG Peng^{1, 2},
MENG Jing^{1, 2},
TAN Chengxuan^{1, 2}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Key Laboratory of Neotectonic Movement & Geohazard, Beijing 100081, China
3.
China University of Geosciences, Beijing 100083, China
4.
Beijing Institute of Geo-exploration Technology, Beijing 100120, China

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Received: 2020-05-15
Revised: 2020-06-25
Published: 2020-08-28

Abstract

Abstract

Shunping county of Hebei province is located at the eastern foot of the Taihang Mountains. There mainly are four kinds of geohazards, including rockfall, landslide, mud-rock flow, and earth fissures, which are widely distributed in different geomorphic units of this county. Based on the analysis of geohazard development characteristics, this paper selects six factors, namely slope angle, level difference, slope direction, engineering geological rock group, normalized differential vegetation index (NDVI), and distance to rivers, to evaluate the susceptibility of geohazards in Shunping county, by the GIS technology and Information Value method. The results show that:(1) The areas with high susceptibility, where rockfalls occur frequently and landslides and mud-rock flows occur in less often, are scattered on the medium-low mountains and hills in the northwestern Shunping with the area about 125 km², accounting for 17.5% of the total area of this county; (2) The areas with medium susceptibility, where rockfalls, landslides and mud-rock flows occur occasionally, are widely distributed on the medium-low mountains and hills in the northwestern Shunping with the area about 200 km², accounting for 28.0% of the total county area; (3) The areas with low susceptibility, where earth fissures occur occasionally and rockfalls, landslides and mud-rock flows occur rarely, are mainly distributed on the plains in the southeastern Shunping and the wide gullies between the hills in the northwest, with the area about 389 km², accounting for 54.5% of the total county area.
- the eastern foot of the Taihang Mountains,
- geohazard,
- developement characteristics,
- susceptibility,
- information value model

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Characteristics and susceptibility evaluation of geohazard development in Shunping county, Hebei province

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