Journal of Geographical Sciences >
Spatial pattern and influencing factors of landslide casualty events
Author: Wang Ying, Professor, specialized in disaster risk assessment and post-disaster recovery research. E-mail: wy@bnu.edu.cn
Received date: 2017-06-14
Accepted date: 2017-07-20
Online published: 2018-03-10
Supported by
National Key Research and Development Program Project, No.2017YFC1502505, No.2016YFA0602403
National Natural Science Foundation of China, No.41271544
Copyright
Analysis of casualties due to landslides from 2000 to 2012 revealed that their spatial pattern was affected by terrain and other natural environmental factors, which resulted in a higher distribution of landslide casualty events in southern China than in northern China. Hotspots of landslide-generated casualties were in the western Sichuan mountainous area and Yunnan-Guizhou Plateau region, southeast hilly area, northern part of the loess hilly area, and Tianshan and Qilian Mountains. However, local distribution patterns indicated that landslide casualty events were also influenced by economic activity factors. To quantitatively analyse the influence of natural environment and human-economic activity factors, the Probability Model for Landslide Casualty Events in China (LCEC) was built based on logistic regression analysis. The results showed that relative relief, GDP growth rate, mean annual precipitation, fault zones, and population density were positively correlated with casualties caused by landslides. Notably, GDP growth rate ranked only second to relative relief as the primary factors in the probability of casualties due to landslides. The occurrence probability of a landslide casualty event increased 2.706 times with a GDP growth rate increase of 2.72%. In contrast, vegetation coverage was negatively correlated with casualties caused by landslides. The LCEC model was then applied to calculate the occurrence probability of landslide casualty events for each county in China. The results showed that there are 27 counties with high occurrence probability but zero casualty events. The 27 counties were divided into three categories: poverty-stricken counties, mineral-rich counties, and real-estate overexploited counties; these are key areas that should be emphasized in reducing landslide risk.
Key words: landslide; casualty event; spatial pattern; influencing factors; counties; China
WANG Ying , LIN Qigen , SHI Peijun . Spatial pattern and influencing factors of landslide casualty events[J]. Journal of Geographical Sciences, 2018 , 28(3) : 259 -374 . DOI: 10.1007/s11442-018-1471-3
Table 1 Data sources for the Landslides Casualty Inventory of China |
Source | Data compiler | Cases | Channel |
---|---|---|---|
China Geological Hazard Bulletin | China Institute for Geo-Environment Monitoring | 81 | CIGEM |
Reports on Geological Disaster Situation | Ministry of Land and Resources of China | 95 | MLRC |
Yesterday Disaster Report | NDRCC | 228 | NDRCC |
Web news search | News websites | 172 | Network collection and arrangement |
Figure 1 Distribution of counties in China with landslide casualties (2000-2012) |
Figure 2 Distribution of natural environment factors in landslide casualty events across China |
Figure 3 Distribution of human-economic activity factors in landslide casualty events across China |
Table 2 Variables applied in the logistic regression model |
Variables | β | S.E. | Sig. | Exp(β) |
---|---|---|---|---|
ln (Topography relief) | 1.922 | 0.117 | 0.000 | 6.834 |
ln(GDP growth rate) | 0.996 | 0.209 | 0.000 | 2.706 |
ln(Mean annual precipitation) | 0.535 | 0.178 | 0.003 | 1.707 |
ln(Vegetation coverage) | -0.333 | 0.159 | 0.037 | 0.717 |
Faults | 0.374 | 0.093 | 0.000 | 1.453 |
ln(Population density) | 0.317 | 0.063 | 0.000 | 1.373 |
Lithology a | 0.000 | |||
siliciclastic sedimentary rock | -0.649 | 0.171 | 0.000 | 0.523 |
pyroclastics | -0.448 | 0.330 | 0.174 | 0.639 |
mixed sedimentary rock | -0.173 | 0.168 | 0.302 | 0.841 |
carbonate sedimentary rock | -0.572 | 0.178 | 0.001 | 0.564 |
acid volcanic | -1.574 | 0.408 | 0.000 | 0.207 |
intermediate volcanics | -0.866 | 0.475 | 0.069 | 0.421 |
basic volcanics | -19.936 | 9093 | 0.998 | 0.000 |
acid plutonics | -0.204 | 0.184 | 0.268 | 0.815 |
intermediate plutonics | -20.172 | 12480 | 0.999 | 0.000 |
basic plutonics | -19.612 | 40190 | 1 | 0.000 |
metamorphics | 0.238 | 0.309 | 0.442 | 1.268 |
water bodies | -17.337 | 27290 | 0.999 | 0.000 |
Soil type a | 0.000 | |||
semi-alfisols | -0.396 | 0.241 | 0.1 | 0.673 |
pedocal | 0.567 | 0.31 | 0.068 | 1.762 |
aridisols | 1.183 | 0.477 | 0.013 | 3.263 |
desert soils | 2.083 | 0.532 | 0.000 | 8.026 |
amorphic soil | 0.447 | 0.169 | 0.008 | 1.564 |
semi-aqueous soil | 0.857 | 0.468 | 0.067 | 2.357 |
alkali-saline soil | -17.918 | 12030 | 0.999 | 0 |
anthrosols | 0.893 | 0.284 | 0.002 | 2.443 |
alpine soil | 0.467 | 0.3 | 0.119 | 1.595 |
ferrallisols | 0.524 | 0.157 | 0.001 | 1.69 |
Industry type a | 0.000 | |||
primary industry median county | 0.536 | 0.126 | 0.000 | 1.71 |
primary industry disadvantaged county | 0.352 | 0.145 | 0.015 | 1.422 |
Constant | -11.913 | 1.344 | 0.000 | 0.000 |
a. The reference categories of lithology, soil type and industry type are unconsolidated sediment, alfisols and primary industry advantaged county respectively |
Table 3 Confusion matrix for the LCEC model |
Observed | Predicted | ||
---|---|---|---|
Casualty | Percentage correct (%) | ||
0 | 1 | ||
0 | 1416 | 472 | 75.0 |
1 | 328 | 980 | 74.9 |
Overall percentage | 75.0 |
Figure 4 ROC curve for LCEC model and validation of models produced from 10 samples of 70% training data |
Figure 5 Distribution of landslide casualty event probabilities across China |
Table 4 Counties, stressing geological disaster risk prevention |
Category | County |
---|---|
Poverty-stricken counties | Jinyang County, Yongshan County, Qianjiang District, Luding County, Mao County, Mianning County, Zhenkang County, Shizhu County, Xichang City, Huili County, Ludian County, Mojiang County, Pingbian County, Hekou County, Yuanyang County |
Mineral-rich counties | Feng County, Jingxi County, Miyi County, Emeishan city, Hongya County, Hongya County, Huidong County, Shui Fu County, Shangluo municipal district |
Real-estate overexploited counties | Lishui municipal district, Zhoushan municipal district, Qingtian County, Wuyishan City |
The authors have declared that no competing interests exist.
[1] |
|
[2] |
|
[3] |
|
[4] |
|
[5] |
|
[6] |
|
[7] |
|
[8] |
|
[9] |
|
[10] |
China Institute for Geo-Environment Monitoring (CIGEM), 2007a. Rockfall and Landslide Disaster Map of China. Beijing: SinoMaps Press. (in Chinese)
|
[11] |
China Institute for Geo-Environment Monitoring (CIGEM), 2007b. Debris Flow Disaster Map of China. Beijing: SinoMaps Press. (in Chinese)
|
[12] |
China Institute for Geo-Environment Monitoring (CIGEM), 2013. China Geological Hazard Bulletin (2004-2012). China Geological Environmental Monitoring Institute Web. . Accessed on 20 June 2014.
|
[13] |
|
[14] |
Computer Network Information Center of CAS, 2015. Geospatial Data Cloud. . Accessed on August, 2015. (in Chinese)
|
[15] |
|
[16] |
|
[17] |
|
[18] |
|
[19] |
|
[20] |
|
[21] |
|
[22] |
|
[23] |
|
[24] |
Institute of Geographic Sciences and Natural Resources Research of CAS, 2015. Data Sharing Network of Earth System Science. . Accessed on June, 2015. (in Chinese)
|
[25] |
|
[26] |
|
[27] |
|
[28] |
|
[29] |
|
[30] |
|
[31] |
Ministry of Land and Resources of China (MLRC), 2013. Report on Geological Disaster Situation. Ministry of Land and Resources of China Web. . Accessed on 20 May 2014. (in Chinese)
|
[32] |
National Disaster Reduction Center of China (NDRCC), 2013. Yesterday's Disaster 2004-2012. Ministry of Civil Affairs National Disaster Reduction Center. (in Chinese)
|
[33] |
|
[34] |
|
[35] |
|
[36] |
|
[37] |
|
[38] |
|
[39] |
|
[40] |
|
[41] |
|
[42] |
|
[43] |
|
[44] |
The State Council, 2004. Geological Disaster Prevention Regulations. . Accessed on 15 May 2014. (in Chinese)
|
[45] |
|
[46] |
|
[47] |
|
[48] |
|
/
〈 |
|
〉 |