基于MISOHRM模型的非一致性洪水频率计算方法及应用IV:西江中游堤防防洪能力影响评价
Algorithm and Application of Inconsistent Flood Frequency Based on the MISOHRM Model (IV): Flood Control Ability Assessment in the Middle of Xijiang River
DOI: 10.12677/JWRR.2012.16073, PDF, HTML, 下载: 2,955  浏览: 6,295  国家自然科学基金支持
作者: 许 斌, 谢 平, 李析男, 刘 宇:武汉大学水资源与水电工程科学国家重点实验室
关键词: 水文堤防防洪能力西江Hydrology; Flood Returning to Main Channel; Flood Control Ability; Xijiang River
摘要: 为了抵御洪水的堤防工程被不断加高,改变了原天然河道的洪水槽蓄关系,促使洪峰流量序列发生变异,使得洪水序列失去了一致性,导致防洪堤的防洪能力一再受到挑战和质疑。本文在梧州站基于MISOHRM模型的非一致性洪水频率计算结果的基础上,对其堤防防洪能力进行了分析。结果显示:梧州站堤防的防洪能力有显著降低的趋势,在安全超高2.0~2.5 m的条件下,其右堤可以抵御的洪水标准从过去条件下的77.13~145.90年一遇,降低到现状条件下的6.20~10.93年一遇和未来条件下的3.33~4.95年一遇。左堤可以抵御的洪水标准从过去条件下的24.53~39.72年一遇,降低到现状条件下的3.13~4.25年一遇和未来条件下的1.85~2.32年一遇。
Abstract: The levees were built to control the flood, and with the higher and higher flood control standard, the flood series become inconsistent and the hydrological alteration happens in the flood peak series, the flood control ability was under challenge and suspicion, while the research of flood control ability in the changing environment was not too much. With the calculation results of inconsistent flood frequency method based on the MISOHRM model of Wuzhou station, the flood control ability was analyzed. The results show that: the decrease tendency of flood control ability is obviously at Wuzhou station, under the condition of safe super elevation from 2.0mto2.5m, the flood control ability of right levee decreased from 77.13 -145.90 yd (past condition) to 6.20 -10.93 yd (present condition) and 3.33 -4.95 yd (future condition), the left levee decreased from 24.53 -39.72 yd (past condition) to 3.13 -4.25 yd (present condition) and 1.85 -2.32 yd (future condition).
文章引用:许斌, 谢平, 李析男, 刘宇. 基于MISOHRM模型的非一致性洪水频率计算方法及应用IV:西江中游堤防防洪能力影响评价[J]. 水资源研究, 2012, 1(6): 460-464. http://dx.doi.org/10.12677/JWRR.2012.16073

参考文献

[1] 刘兴华. 流域防洪能力研究[D]. 河海大学, 2007. LIU Xinghua. Study on the flood control capability in river basin. Nanjing: Hohai University, 2007. (in Chinese)
[2] 梁在潮, 李泰来. 江河堤防防洪能力的风险分析[J]. 长江科学院院报, 2001, 18(2): 7-10. LIANG Zaichao, LI Tailai. Risk analysis and computation of flood control capacity for river levee. Journal of Yangtze River Scientific Research Institute, 2001, 18(2): 7-10. (in Chinese)
[3] 袁峥. 渭河下游干流堤防防洪能力分析[J]. 地下水, 2005, 27(5): 408-409. YUAN Zheng. Flood control ability analysis of the levee at the downstream of the Wei River. Groundwater, 2005, 27(5): 408- 409. (in Chinese)
[4] 李析男, 谢平, 许斌, 等. 基于MISOCRM模型的非一致性洪水频率计算方法及应用(II): 西江中游水文要素时空变异规律[J]. 水资源研究, 2012, 1(5): 310-314. LI Xinan, XIE Ping, XU Bin, LIU Yu, et al. Algorithm and ap-plication of inconsistent flood frequency based on the MISOHRM model (II): Hydrological elements alteration regulation at the middle stream of Xi River from the temporal and spatial scale. Journal of Water Resources Research, 2012, 1(5): 310-314. (in Chinese)
[5] 刘宇, 谢平, 李析男, 等. 基于MISOCRM模型的非一致性洪水频率计算方法及应用(III): 模型的构建与非一致性洪水频率计算[J]. 水资源研究, 2012, 1(6): in press. LIU Yu, XIE Ping, LI Xi’nan and XU Bin. Algorithm and appli-cation of inconsistent flood frequency based on the MISOHRM model (III): Hydrological frequency analysis with inconsistent flood series. Journal of Water Resources Research, 2012, 1(6): in press. (in Chinese)
[6] 珠江水利委员会. 珠江流域防洪规划[R], 2005. Water Resources Conservancy Committee of Pearl River. Flood control planning of Pearl River basin, 2005. (in Chinese)
[7] 徐海亮. 西江流域洪水灾害和水文变异分析[J]. 人民珠江, 2007, 4: 42-46. XU Hailiang. Analysis of flood disaster and hydrological alteration in Xijiang River. Pearl River, 2007, 4: 42-46. (in Chinese)