小流域山洪災(zāi)害成因及防治技術(shù)研究
[Abstract]:Because of the small watershed area and river storage ability, steep slope, short flood duration, large increase, high Hong Feng, mountain flood disaster has the characteristics of sudden occurrence, short forecast period, concentrated water quantity and great destructive power. It has become a weak link in flood control and disaster reduction in China. Because the situation of small watershed in mountainous area is complex, the influencing factors are many, the data is scarce, and the related research starts late, it is urgent to need the relevant technical support. Therefore, the research on the causes of mountain flood disaster and its prevention and control technology in small watershed is of great significance. In this paper, the Yao'an small watershed in Lianzhou, Qingyuan City, Guangdong Province is taken as the research object, and the main research contents are as follows: (1) the causes of mountain flood disaster in small watershed are analyzed. The causes of mountain flood disaster in Yao'an small watershed are analyzed from the aspects of rainfall condition, slope potential energy condition and solid material environment condition. The results show that rainfall is the direct external dynamic factor for the formation of mountain flood disaster. The unfavorable slope potential energy condition is an important factor for the formation of mountain flood disaster, and the loose solid material on the surface provides an important environmental condition for the formation of mountain flood disaster. (2) to study the risk assessment of mountain flood disaster in small watershed. Six factors, such as rainfall, elevation, slope, soil type, population density and land use type, were used as risk assessment indexes of mountain flood disaster in Yao'an small watershed. Based on GIS technology and analytic hierarchy process (AHP), the risk assessment model of mountain flood disaster was established. The risk zoning map, vulnerability zoning map and risk zoning map of mountain flood disaster are made, and the risk assessment of mountain flood disaster in this area is carried out, and the evaluation results can better reflect the actual situation. (3) the calculation and analysis method of critical rainfall of mountain flood disaster in small watershed is discussed. By using the regional critical rain method and the water level inversion method, the critical rain values for 1 h, 3 h, 6 h, 12 h and 24 h in Yao'an small watershed are comprehensively analyzed and determined. In addition, the relationship between the rainfall on the day of the mountain flood disaster and the effective rainfall in the previous period is considered. The critical rainfall datum line is established to provide reference for mountain flood disaster prevention and control. (4) on the basis of studying the flood forecasting problem in the area without data, the early warning and forecasting system of rainstorm mountain flood disaster in small watershed is constructed. The early warning and forecasting system includes critical rainfall forecast and mountain flood process forecast, in which the simulation and forecast of mountain flood process adopts Xin'an River model and empirical prediction scheme. In view of the lack of measured runoff data in this area, the simulation results of Xin'anjiang model are compared with the comprehensive unit line method of Guangdong Province, and the calibration and test of model parameters can solve the problem of flood forecasting accuracy in areas without data. (5) the prevention and control engineering measures of mountain flood disaster in small watershed are put forward. The prevention and control engineering measures of mountain flood disaster in Yao'an small watershed mainly include flood control project management, river regulation, soil and water conservation project construction and biological engineering control, etc., with emphasis on Changhe Water and Yao'an Township, which are seriously affected. Small boiling water and belt water are treated locally. The engineering measures provide a strong guarantee for improving the ability to resist mountain torrents and ensuring the safety of people's lives and property in mountain areas.
【學(xué)位授予單位】:華南理工大學(xué)
【學(xué)位級別】:碩士
【學(xué)位授予年份】:2014
【分類號】:TV87
【參考文獻】
相關(guān)期刊論文 前10條
1 張劍明;章新平;黎祖賢;張健;;湖南省46年來降水的氣候特征[J];熱帶氣象學(xué)報;2008年05期
2 陳桂亞;袁雅鳴;;山洪災(zāi)害臨界雨量分析計算方法研究[J];人民長江;2005年12期
3 張李蓀;;基于WebGIS的山洪災(zāi)害預(yù)警信息系統(tǒng)設(shè)計[J];人民長江;2009年17期
4 周金星,王禮先,謝寶元,饒良懿;山洪泥石流災(zāi)害預(yù)報預(yù)警技術(shù)述評[J];山地學(xué)報;2001年06期
5 李景保,毛德華,許樹輝;湖南省山洪災(zāi)害特征與成因分析[J];山地學(xué)報;2002年03期
6 倪化勇;李宗亮;巴仁基;蘇鵬程;宋志;;貢嘎山東坡磨西河流域泥石流暴發(fā)的臨界雨量值初探[J];山地學(xué)報;2007年06期
7 李長江;麻土華;孫樂玲;朱興盛;;降雨型滑坡預(yù)報中計算前期有效降雨量的一種新方法[J];山地學(xué)報;2011年01期
8 李娜;王靜;;山洪災(zāi)害特點分析及風(fēng)險圖制作方法探討[J];水利水電技術(shù);2011年02期
9 李娜,向立云,程曉陶;國外洪水風(fēng)險圖制作比較及對我國洪水風(fēng)險圖制作的建議[J];水利發(fā)展研究;2005年06期
10 張行南,羅健,陳雷,李紅;中國洪水災(zāi)害危險程度區(qū)劃[J];水利學(xué)報;2000年03期
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