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Characteristics and influencing factors of rainfall-induced landslide and debris flow hazards in Shaanxi Province, China

机译:陕西省降雨诱发的滑坡和泥石流灾害的特征及影响因素

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Shaanxi Province, located in northwest China and spanning multiplehydroclimatic and geological zones, has many areas largely suffering fromrainfall-induced landslide and debris flow. The objectives of this study areto reveal the spatiotemporal characteristics of the two hazards and identifytheir major controlling factors in this region based on a region-wide,comprehensive ground-survey-based hazard inventory dataset from?2009 to 2012.We investigated the spatiotemporal characteristics of the two hazards andquantified the relationships between the occurrence rates of the two hazardsand their influencing factors, including antecedent rainfall amount, rainfallduration, rainfall intensity, terrain slope, land cover type and soil type.The results show that landslide has a higher occurrence rate and moreextensive distribution than debris flow in this region, while the two hazardsare both concentrated in the south with ample rainfall and steep terrains.Both of the hazards show clear seasonalities: July–September for landslideand July for debris flow. Rainfall characteristics (amount, duration andintensity) and slope are the dominant factors controlling slope stabilityacross this region. Debris flow is more sensitive to these rainfall metricson the high-value ranges than landslide in this region. Land cover is anotherinfluencing factor but soil type does not appear to impose consistent impactson the occurrence of the two hazards. This study not only providesimportant inventory data for studying the landslide and debris flow hazardsbut also adds valuable information for modeling and predicting the twohazards to enhance resilience to these hazards in this region.
机译:陕西省位于中国西北部,横跨多个水文气候和地质地区,许多地区主要遭受降雨诱发的滑坡和泥石流的影响。本研究的目的是揭示这两种灾害的时空特征,并基于2009年至2012年整个地区基于地面调查的综合灾害清单数据,确定该区域的主要控制因素。两种滑坡灾害的发生率及其影响因素之间的关系进行了定量化分析,结果表明滑坡发生率较高,范围更广,其影响因素包括降雨前期,降雨持续时间,降雨强度,地形坡度,土地覆盖类型和土壤类型。该区域的分布比泥石流大,而这两个灾害都集中在南部,降雨充沛,地势陡峭。这两个灾害都表现出明显的季节性:滑坡发生在7月至9月,泥石流发生在7月。降雨特征(数量,持续时间和强度)和坡度是控制该地区斜坡稳定性的主要因素。在该高值范围内,泥石流对这些降雨指标的敏感性高于该地区的滑坡。土地覆盖是另一个影响因素,但土壤类型似乎并未对这两种危害的发生产生一致的影响。这项研究不仅为研究滑坡和泥石流灾害提供了重要的清单数据,而且还为建模和预测这两种灾害提供了有价值的信息,以增强该地区对这些灾害的抵御能力。

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