首页|降雨对广西梧州滑坡灾害的影响分析

降雨对广西梧州滑坡灾害的影响分析

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为了研究降雨对梧州地区滑坡的影响,在收集整理梧州地区2005~2012年的滑坡资料和降雨资料的基础上,分析梧州地区滑坡发生的规模、时空分布,以及滑坡与降雨天数的相关性。采用前期有效降雨量模型研究梧州的临界雨量,并用实例加以验证。研究结果表明:梧州在降雨的作用下,易发生小型的浅层土质滑坡;梧州市的滑坡集中发生在每年6月份,暴雨频次和暴雨强度在6月份达到最大值;梧州市的滑坡地质灾害与暴雨关系非常密切;梧州市滑坡灾害基本发生在暴雨发生的当天或者暴雨发生的第二天;梧州市滑坡灾害的临界有效雨量为连续两日累计有效降雨量为300 mm,临界雨强为150 mm/d。研究成果可为梧州地区滑坡灾害的预警预报提供理论依据。
Relationship between rainfall and landslides in Wuzhou Guangxi
In order to obtain the rainfall threshold value in Wuzhou, the data of landslide and rain-fall during the year from 2005 to 2012 in Wuzhou prefecture were studied. The scale of landslide, the spatial and temporal distribution of landslide and the relativity between rainfall and landslide were also analyzed. The results show that, under the rainfall, the landslide in Wuzhou prefecture is easy to take place in the superficial layer of slope; that the landslide in Wuzhou prefecture occurs mainly in June each year, and the frequency and intensity of rainstorm reach the maximum value in June, so the relationship between landslide and rainstorm is very close; that the landslide disaster often occurs on the rainstorm day or one day after the rainstorm day; that the critical rainfall for landslide in Wuzhou prefecture is accumulative 300 mm in two consecutive days, and the critical in-tensity of rainfall is 150 mm/d. The results can be considered as a theoretical foundation of warning and forecasting of landslide in Wuzhou.

landsliderainfalleffective rainfall modelrainfall threshold value

许英姿、范皓然、陈立华、赵艳林、李岳顺

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广西大学 土木建筑工程学院,广西 南宁 530004

广西防灾减灾与工程安全重点实验室,广西 南宁 530004

滑坡 降雨 有效降雨量模型 临界雨量

国家自然科学基金资助项目广西国土厅重大科研课题广西国土厅重大科研课题

51178124GXZC2014-G3-0371-KLZB-LGXZC2015-G3-0371-KLZB-M

2015

广西大学学报(自然科学版)
广西大学

广西大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.767
ISSN:1001-7445
年,卷(期):2015.(4)
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