三峡水库对长江中游水文过程和地下水循环的影响
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- 英文论文题名：Analysis on the Influence of the Three Gorges Reservoirs Operation on Hydrological Process of the Middle Reaches of the Yangtze River
- 论文作者：何沛欣 ; 唐仲华
- 英文论文作者：HE Pei-xin ; TANG Zhong-hua ; School of Environmental Studies ; China University of Geosciences
- 年：2017
- 作者机构：中国地质大学(武汉)环境学院;
- 论文关键词：趋势性分析 ; R/S分析 ; 突变性检验 ; 小波分析 ; 地下水数值模拟
- 英文论文关键词：trend analysis ; R/S method ; abrupt change test ; wavelet analysis ; groundwater numerical simulation
- 会议召开时间：2017-04-08
- 会议录名称：2017第九届河湖治理与水生态文明发展论坛论文集
- 语种：中文
- 分类号：TV697.2;TV12
- 学会代码：SLJS
- 会议名称：2017第九届河湖治理与水生态文明发展论坛
- 会议地点：中国陕西西安
- 主办单位：流域水循环模拟与调控国家重点实验室、国际水生态安全中国委员会、长江水利委员会长江科学院、南京大学常熟生态研究院
- 学会名称：中国水利技术信息中心
- 页数：9
- 文件大小：1372k
- 原文格式：O
- 会议级别：全国
摘要
基于1965～2015年长江中游4个水文站实测水文资料,利用Mann-Kendall趋势性检验法、突变性检验法、小波分析法及数值模拟法,系统分析了长江中游年径流的趋势性、突变性和周期性特征以及周边地下水循环变化特征。研究结果表明:过去51年宜昌站、监利站、螺山站和汉口站径流均呈下降趋势,未来保持下降趋势的可能性很大,并且径流序列在2001年、2006年、2003年和2005年发生突变:长江中游年径流呈现多种周期不同尺度的振荡特性,变化周舛以11~13a和24~27a最为显著。三峡水库运行后长江中游径流集中度在减小,径流量呈下降趋势,年际变异系数增加。三峡水库运行后洪湖地区长江补给地下水天数增加至200d以上,地下水排泄方式由以蒸发排泄和河流排泄为主转变为蒸发排泄和侧向排泄。
Based on the measured hydrological data from 1965 to 2015 from four hydrological stations,the Mann-Kendall test method,mutation test method and wavelet analysis method were adopted to diagnose the tendency,mutation and periodicity of annual runoff in the middle reaches of the Yangtze River.The groundwater numerical simulation method was also used for a systematic study on the variation characteristics of groundwater circulation alongshore.The results indicated that annual runoff of Yichang,Jianli,Luoshan and Hankou stations had shown a declining trend in the past 51 years through Mann-Kendall test method and would maintain the decreasing tendency in the future through R/S analysis.Annual runoff of these stations had significant changes,which respectively occurred in 2001,2006,2003 and 2005.[t was also found that the hydrologic meteorological oscillation over the middle reaches of the Yangtze River presented a variety in time scales.Annual runoff variations were mostly in time periods of 11-13 years and 24-27 years over the middle reaches.Since the Three Gorges Reservoirs(TGR) operation,the concentration degrees(RCD) and the amount of runoff have been decreasing.While,the interannual variation coefficient has increased.In addition,the period,when the Yangtze River recharged groundwater in Honghu,has increased to over 200 days.The groundwater discharge has changed from the form of evaporation and river discharge to the form of evaporation and lateral discharge.
Based on the measured hydrological data from 1965 to 2015 from four hydrological stations,the Mann-Kendall test method,mutation test method and wavelet analysis method were adopted to diagnose the tendency,mutation and periodicity of annual runoff in the middle reaches of the Yangtze River.The groundwater numerical simulation method was also used for a systematic study on the variation characteristics of groundwater circulation alongshore.The results indicated that annual runoff of Yichang,Jianli,Luoshan and Hankou stations had shown a declining trend in the past 51 years through Mann-Kendall test method and would maintain the decreasing tendency in the future through R/S analysis.Annual runoff of these stations had significant changes,which respectively occurred in 2001,2006,2003 and 2005.[t was also found that the hydrologic meteorological oscillation over the middle reaches of the Yangtze River presented a variety in time scales.Annual runoff variations were mostly in time periods of 11-13 years and 24-27 years over the middle reaches.Since the Three Gorges Reservoirs(TGR) operation,the concentration degrees(RCD) and the amount of runoff have been decreasing.While,the interannual variation coefficient has increased.In addition,the period,when the Yangtze River recharged groundwater in Honghu,has increased to over 200 days.The groundwater discharge has changed from the form of evaporation and river discharge to the form of evaporation and lateral discharge.
引文
[1]王艳君,姜彤,施雅风.长江上游流1961-2000年气候及径流变化趋势[J].冰川冻土,2005,27(5):709-714.
[2]陈国金,殷鸿福,李长安,等.长江中游荆江高洪水位形成的地质环境分析[J].长江流域资源与环境,2010,19(8):919-925.
[3]李学山,王翠平.荆江与洞庭湖水沙关系演变及对城螺河段水情影响分析[J].人民长江,1997,28(8):7-9.
[4]吴作平,杨国录,甘明辉.荆江-洞庭湖水沙关系及调整[J].武汉大学学报(工学版),2002,35(3):5-8.
[5]武旭同,李娜,王腊春.近60年来长江干流水沙特征分析[J].泥沙研究,201 6(5):40-46.
[6]郭文献,王鸿翔,徐建新,等.三峡梯级水库对长江中下游水文情势影响研究[J].中国农村水利水电,2009(12):7-10.
[7]张翼,夏军强,邓珊珊,等.上荆江典型断面河床纵横向变形过程的概化模拟[J].长江科学院院报,2016,33(7):6-11.
[8]汪曼琳,万新宇,钟平安,等.长江上游降水特征及时空演变规律[J].南水北调与水利科技,2016,14(4):65-71.
[9]潘雅婧,王仰麟,彭建,等.基于小波与R/S方法的汉江中下游流域降水量时间序列分析[J].地理研究,2012,31(5):811-820.
[10]陆志华,夏自强,于岚岚,等.松花江千流中游段径流年内分配变化规律[J].河海大学学报(自然科学版),2012,40(1):63-69.
[11]何报寅,蔡述明.三峡工程与长江中游浅层承压水动态[J].长江流域资源与环境,1999,8(1):94-99.
[12]张红,陈世俭,张光岳,等.三峡工程对洪湖地区地下水动态和土壤潜育的影响[J].农业系统科学与综合研究,2009,25(3):3 17-321.
[2]陈国金,殷鸿福,李长安,等.长江中游荆江高洪水位形成的地质环境分析[J].长江流域资源与环境,2010,19(8):919-925.
[3]李学山,王翠平.荆江与洞庭湖水沙关系演变及对城螺河段水情影响分析[J].人民长江,1997,28(8):7-9.
[4]吴作平,杨国录,甘明辉.荆江-洞庭湖水沙关系及调整[J].武汉大学学报(工学版),2002,35(3):5-8.
[5]武旭同,李娜,王腊春.近60年来长江干流水沙特征分析[J].泥沙研究,201 6(5):40-46.
[6]郭文献,王鸿翔,徐建新,等.三峡梯级水库对长江中下游水文情势影响研究[J].中国农村水利水电,2009(12):7-10.
[7]张翼,夏军强,邓珊珊,等.上荆江典型断面河床纵横向变形过程的概化模拟[J].长江科学院院报,2016,33(7):6-11.
[8]汪曼琳,万新宇,钟平安,等.长江上游降水特征及时空演变规律[J].南水北调与水利科技,2016,14(4):65-71.
[9]潘雅婧,王仰麟,彭建,等.基于小波与R/S方法的汉江中下游流域降水量时间序列分析[J].地理研究,2012,31(5):811-820.
[10]陆志华,夏自强,于岚岚,等.松花江千流中游段径流年内分配变化规律[J].河海大学学报(自然科学版),2012,40(1):63-69.
[11]何报寅,蔡述明.三峡工程与长江中游浅层承压水动态[J].长江流域资源与环境,1999,8(1):94-99.
[12]张红,陈世俭,张光岳,等.三峡工程对洪湖地区地下水动态和土壤潜育的影响[J].农业系统科学与综合研究,2009,25(3):3 17-321.
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