Study on the Simulation of Debris Flow for a Watershed with High Landslide Rate – a Case Study of Xinkai Village in Southern Taiwan

碩士 === 華梵大學 === 環境與防災設計學系碩士班 === 100 === Due to large landslides occurred in the upstream of watersheds to result debris-flow disasters from the attack of Typhoon Morakot in the Shinkai area in the southern Taiwan, in the paper, three watershed areas- Hongshuixian, Neighborhood 23 and Dafo are selec...

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Main Authors: Chuang, Mengru, 莊孟儒
Other Authors: Chen, Jinnchyi
Format: Others
Language:zh-TW
Published: 2012
Online Access:http://ndltd.ncl.edu.tw/handle/92884464468001119679
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spelling ndltd-TW-100HCHT06330012015-10-13T21:12:10Z http://ndltd.ncl.edu.tw/handle/92884464468001119679 Study on the Simulation of Debris Flow for a Watershed with High Landslide Rate – a Case Study of Xinkai Village in Southern Taiwan 高崩塌率下誘發土石流之模擬研究-以莫拉莫拉克風災在南台灣新開地區為例 Chuang, Mengru 莊孟儒 碩士 華梵大學 環境與防災設計學系碩士班 100 Due to large landslides occurred in the upstream of watersheds to result debris-flow disasters from the attack of Typhoon Morakot in the Shinkai area in the southern Taiwan, in the paper, three watershed areas- Hongshuixian, Neighborhood 23 and Dafo are selected as our case study, and the FLO-2D model are used to work on the studies for debris-flow simulation. Firstly, basic data collections of the watershed areas, as well as the rheological property experiments on debris flows are conducted. Secondly, to study the inflow hydrographs that will trigger debris flows under the condition of high landslide rate for the watershed areas. The paper uses the rainfall thresholds to determine the inflow hydrographs. When the cumulative rainfall (R) is greater than 200mm within 24 hours, it is seen as flooding, the given volumetric sediment concentration cv=0.1; when the rainfall intensity (I) is greater than 40mm/h, as well as the cumulative rainfall (R) is greater than 200mm, it is seen as landslide, and the given cv=0.65~0.8; from the occurrence of debris flow to the end of debris flow, the given cv=0.48~0.55. Finally, to make investigation of the influences of different inflow hydrographs, Manning’s n roughness coefficients, and sediment concentration on the flow depth and the inundation area of debris flow. Moreover, to further make comparison between the data simulated results and on-site survey data, in order to determine the conditions, such as the inflow hydrograph and resistance parameters for the three watershed areas. The simulation approaches proposed in the case study, including the simulation process, inflow hydrographs and resistant parameters, are able to work as reference for later debris-flow simulation or debris flow hazards mitigation. Chen, Jinnchyi 陳晉琪 2012 學位論文 ; thesis 109 zh-TW
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description 碩士 === 華梵大學 === 環境與防災設計學系碩士班 === 100 === Due to large landslides occurred in the upstream of watersheds to result debris-flow disasters from the attack of Typhoon Morakot in the Shinkai area in the southern Taiwan, in the paper, three watershed areas- Hongshuixian, Neighborhood 23 and Dafo are selected as our case study, and the FLO-2D model are used to work on the studies for debris-flow simulation. Firstly, basic data collections of the watershed areas, as well as the rheological property experiments on debris flows are conducted. Secondly, to study the inflow hydrographs that will trigger debris flows under the condition of high landslide rate for the watershed areas. The paper uses the rainfall thresholds to determine the inflow hydrographs. When the cumulative rainfall (R) is greater than 200mm within 24 hours, it is seen as flooding, the given volumetric sediment concentration cv=0.1; when the rainfall intensity (I) is greater than 40mm/h, as well as the cumulative rainfall (R) is greater than 200mm, it is seen as landslide, and the given cv=0.65~0.8; from the occurrence of debris flow to the end of debris flow, the given cv=0.48~0.55. Finally, to make investigation of the influences of different inflow hydrographs, Manning’s n roughness coefficients, and sediment concentration on the flow depth and the inundation area of debris flow. Moreover, to further make comparison between the data simulated results and on-site survey data, in order to determine the conditions, such as the inflow hydrograph and resistance parameters for the three watershed areas. The simulation approaches proposed in the case study, including the simulation process, inflow hydrographs and resistant parameters, are able to work as reference for later debris-flow simulation or debris flow hazards mitigation.
author2 Chen, Jinnchyi
author_facet Chen, Jinnchyi
Chuang, Mengru
莊孟儒
author Chuang, Mengru
莊孟儒
spellingShingle Chuang, Mengru
莊孟儒
Study on the Simulation of Debris Flow for a Watershed with High Landslide Rate – a Case Study of Xinkai Village in Southern Taiwan
author_sort Chuang, Mengru
title Study on the Simulation of Debris Flow for a Watershed with High Landslide Rate – a Case Study of Xinkai Village in Southern Taiwan
title_short Study on the Simulation of Debris Flow for a Watershed with High Landslide Rate – a Case Study of Xinkai Village in Southern Taiwan
title_full Study on the Simulation of Debris Flow for a Watershed with High Landslide Rate – a Case Study of Xinkai Village in Southern Taiwan
title_fullStr Study on the Simulation of Debris Flow for a Watershed with High Landslide Rate – a Case Study of Xinkai Village in Southern Taiwan
title_full_unstemmed Study on the Simulation of Debris Flow for a Watershed with High Landslide Rate – a Case Study of Xinkai Village in Southern Taiwan
title_sort study on the simulation of debris flow for a watershed with high landslide rate – a case study of xinkai village in southern taiwan
publishDate 2012
url http://ndltd.ncl.edu.tw/handle/92884464468001119679
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