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Risk Assessment of Land Subsidence in Kathmandu Valley, Nepal, Using Remote Sensing and GIS

机译:利用遥感和GIS风险评估LATHMANDU VALLEY LINAL沉降

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Land subsidence is identified as a global problem and intensive studies are being conducted worldwide to detect and monitor risk of this problem. Risk assessment of land subsidence is simply an evaluation of the probability and frequency of occurrence of land subsidence, exposure of people and property to the subsidence and consequence of that exposure. Remote sensing technology was used to extract information of land subsidence in Kathmandu Valley, Nepal. Also, Disaster Risk Index method and Analytic Hierarchy Process (AHP) along with Geographic Information System (GIS) tools were used to assess risk of land subsidence in Kathmandu Valley, Nepal. Subsidence volume for locations Central Kathmandu, Chauni, Lalitpur, Imadol, Thimi, Madhyaour Thimi, New Baneshwor, Koteshwor and Gothatar was calculated using a simple mathematical formula. The subsidence depth for these locations was found to be in a range of 1 cm to 17 cm and the maximum subsidence velocity was found to be 4.8 cm/yr. This study revealed that the location where maximum subsidence was observed (i.e. Central Kathmandu and Lalitpur) was found to be at high risk of experiencing land subsidence induced damage. Other location where subsidence was observed was found to be at medium risk and the rest of the Kathmandu valley was found to be at low risk with current data situation. This study can be considered as the first step towards other comprehensive study relating to land subsidence risk assessment. The outcome of this research provides a basic understanding of the current situation that can further assist in developing prevention and risk management techniques.
机译:土地沉降被确定为全球问题,并在全球范围内进行密集的研究,以检测和监测这个问题的风险。土地沉降风险评估只是对土地沉降,人口暴露和财产的发生概率和频率的评估,以至于该暴露的沉降和后果。遥感技术用于提取尼泊尔加德满都山谷的土地沉降信息。此外,灾害风险指数方法和分析层次处理(AHP)以及地理信息系统(GIS)工具用于评估加德满都谷,尼泊尔的土地沉降风险。使用简单的数学公式计算地点Central Centrals Central Centrands Central Centralu,Chauni,Lalitpur,Imadol,Thimi,Madhyaour和Gothatar。发现这些位置的沉降深度在1厘米至17厘米的范围内,最大沉降速度被发现为4.8cm / yr。该研究表明,发现最大沉降的位置(即中央加德满都和LALITPUR)被认为是经历土地沉降造成损伤的高风险。观察到沉降的其他位置是处于中等风险,并且剩下的加德满都谷被发现与当前数据情况有低风险。该研究可以被视为与土地沉降风险评估有关的其他综合研究的第一步。本研究的结果提供了对当前情况的基本理解,可以进一步协助开发预防和风险管理技术。

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