Arid Land Geography ›› 2025, Vol. 48 ›› Issue (4): 599-611.doi: 10.12118/j.issn.1000-6060.2024.520
• The Third Xinjiang Scientific Expedition • Previous Articles Next Articles
CHEN Shilong1,2(), MENG Qingkai1(
), DAI Yong1,3, YANG Liqiang4, WU Han1
Received:
2024-09-02
Revised:
2024-09-23
Online:
2025-04-25
Published:
2025-04-18
Contact:
MENG Qingkai
E-mail:slslug@163.com;mengqingkai@imde.ac.cn
CHEN Shilong, MENG Qingkai, DAI Yong, YANG Liqiang, WU Han. Geological disaster hazard assessment and prediction in the Ili River Basin based on CMIP6 future scenarios[J].Arid Land Geography, 2025, 48(4): 599-611.
Tab. 1
Data sources of hazard evaluation indicators"
数据内容 | 评价指标 | 数据来源 |
---|---|---|
数字高程模型数据 | 坡度 | https://www.gscloud.cn |
坡向 | https://www.gscloud.cn | |
高程 | https://www.gscloud.cn | |
曲率 | https://www.gscloud.cn | |
距河流距离 | https://www.gscloud.cn | |
土地利用类型数据 | 土地利用类型 | http://www.globallandcover.com |
工程地质岩组数据 | 工程地质岩组 | http://www.ngac.org.cn/ddzt/index1.html |
断层数据 | 距断层距离 | http://www.ngac.org.cn/ddzt/index1.html |
地震峰值加速度数据 | PGA | https://zenodo.org |
气候数据 | 降水量 | https://worldclim.org |
气温 | https://worldclim.org |
Tab. 2
Information amount of assessment factors"
评价因子 | 分区 | 崩滑信息量 | 泥石流信息量 | 评价因子 | 分区 | 崩滑信息量 | 泥石流信息量 |
---|---|---|---|---|---|---|---|
坡度/(°) | <5 | -1.523 | -1.511 | 距断层距离/m | <1000 | 0.685 | -0.887 |
5~15 | 0.008 | -0.924 | 1000~2000 | 0.102 | -0.751 | ||
15~25 | 0.887 | 0.067 | 2000~5000 | -0.068 | 0.035 | ||
25~40 | 0.285 | 0.670 | 5000~10000 | 0.158 | 0.338 | ||
>40 | -0.687 | 1.363 | >10000 | -1.271 | 0.089 | ||
坡向/(°) | 北 | 0.013 | -0.661 | 工程地质岩组 | 坚硬中-厚层状碳酸盐岩组 | -0.945 | 0.591 |
东北 | 0.425 | 0.600 | |||||
东 | 0.327 | 0.357 | 坚硬块状花岗岩岩组 | -0.316 | 0.765 | ||
东南 | -0.249 | 0.252 | |||||
南 | -0.907 | -0.009 | 第四系冲洪积、风积、 冰积黄土 | 0.867 | -1.987 | ||
西南 | -0.267 | -0.256 | |||||
西 | 0.325 | 0.036 | |||||
西北 | 0.037 | -0.292 | 互层状较软砂岩、砾岩为主的 碎屑岩岩组 | 0.584 | 0.159 | ||
高程/m | <1000 | -3.569 | -5.539 | ||||
1000~1500 | 0.422 | -1.637 | |||||
1500~2000 | 0.873 | -1.527 | 坚硬、较坚硬砂岩为主的 碎屑岩岩组 | 0.756 | -1.208 | ||
2000~3000 | -0.463 | 0.238 | |||||
>3000 | -0.526 | 1.289 | |||||
曲率 | <-1.00 | -0.157 | 0.372 | PGA/g | <0.2 | -1.420 | -0.644 |
-1.00~-0.35 | -0.274 | -0.612 | 0.2~0.25 | 0.010 | 0.319 | ||
-0.35~0.35 | -0.671 | -0.737 | 0.25~0.3 | 0.446 | -0.552 | ||
0.35~1.00 | 0.803 | 0.558 | 0.3~0.4 | -0.300 | 0.104 | ||
>1.00 | 0.054 | 0.211 | >0.4 | 0.000 | 0.000 | ||
土地利用类型 | 裸地 | -0.482 | 0.988 | 气温/℃ | <-4 | -0.443 | 1.281 |
农作物 | -2.359 | -6.898 | -4~0 | -0.553 | -0.531 | ||
建筑用地 | -3.305 | 0.000 | 0~4 | 0.822 | -1.615 | ||
灌木林地 | 0.347 | -0.097 | 4~8 | -0.132 | -2.003 | ||
其他 | -1.424 | 0.762 | >8 | -6.175 | -5.112 | ||
距河流距离/m | <200 | 0.020 | 1.044 | 降水量/mm | <250 | -0.043 | -3.174 |
200~500 | 0.392 | 1.281 | 250~350 | 0.227 | -0.956 | ||
500~1000 | 0.481 | -0.086 | 350~450 | -0.359 | 0.987 | ||
1000~2000 | -0.011 | -1.597 | 450~550 | -1.053 | 1.197 | ||
>2000 | -0.790 | -3.225 | >550 | -0.465 | 0.502 |
Tab. 3
Proportion of hazard zones under different scenarios in the Ili River Basin /%"
崩滑危险区等级 | 2000—2020年 | 2021—2040年 | |||
---|---|---|---|---|---|
SSP126 | SSP245 | SSP370 | SSP585 | ||
极低危险区 | 15.12 | 7.74 | 10.01 | 8.64 | 5.79 |
低危险区 | 17.63 | 8.26 | 11.69 | 10.24 | 10.08 |
中危险区 | 27.19 | 35.21 | 35.15 | 28.49 | 26.76 |
高危险区 | 24.84 | 28.65 | 27.32 | 31.25 | 32.61 |
极高危险区 | 15.22 | 20.14 | 15.83 | 21.38 | 24.76 |
泥石流危险区等级 | 2000—2020年 | 2021—2040年 | |||
SSP126 | SSP245 | SSP370 | SSP585 | ||
极低危险区 | 8.71 | 3.21 | 3.11 | 3.02 | 3.28 |
低危险区 | 19.71 | 16.86 | 17.47 | 14.64 | 14.94 |
中危险区 | 27.47 | 32.58 | 34.86 | 32.71 | 28.90 |
高危险区 | 27.83 | 29.12 | 27.79 | 30.06 | 31.34 |
极高危险区 | 16.28 | 18.23 | 16.77 | 19.57 | 21.54 |
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Abstract 60
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