[1]赵军凯,李立现,李九发*,等.鄱阳湖水位变化趋势性对人类活动响应分析[J].江西师范大学学报(自然科学版),2019,(05):532-544.[doi:10.16357/j.cnki.issn1000-5862.2019.05.16]
　ZHAO Junkai,LI Lixian,LI Jiufa*,et al.The Analysis on the Response of the Water Level Change Trend to Human Activities in Poyang Lake[J].Journal of Jiangxi Normal University:Natural Science Edition,2019,(05):532-544.[doi:10.16357/j.cnki.issn1000-5862.2019.05.16]
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鄱阳湖水位变化趋势性对人类活动响应分析()
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《江西师范大学学报》（自然科学版）[ISSN:1006-6977/CN:61-1281/TN]

卷:
期数:
2019年05期
页码:
532-544
栏目:
出版日期:
2019-10-10

文章信息/Info

Title:
The Analysis on the Response of the Water Level Change Trend to Human Activities in Poyang Lake
文章编号:
1000-5862(2019)05-0532-13
作者:
赵军凯1; 李立现1; 李九发2*; 赵瑞哲3; 刘新圣1; 杨静草1
1.九江学院旅游与国土资源学院,九江市土地测量与3S技术应用重点实验室,江西 九江 332005; 2.华东师范大学河口海岸学国家重点实验室,上海 200062; 3.中国科学院信息工程研究所,北京 100080
Author(s):
ZHAO Junkai1; LI Lixian1; LI Jiufa2*; ZHAO Ruizhe3; LIU Xinsheng1; YANG Jingcao1
1.College of Tourism and Territorial Resources,Jiujiang Key Laboratory of Surveying and Mapping on Land and 3S Technology Application,Jiujiang University,Jiujiang Jiangxi 332005,China; 2.State Key Laboratory of Estuarine and Coastal Research,East China Normal University,Shanghai 200062,China; 3.Institute of Information Engineering,Chinese Academy of Science,Beijing 100080,China
关键词:
水位变化趋势性;  水库群调节;  采砂活动;  鄱阳湖;  长江
Keywords:
the water level change trend;  regulation of reservoir group;  sand excavating;  the Poyang Lake;  the Yangtze River
分类号:
TV 213
DOI:
10.16357/j.cnki.issn1000-5862.2019.05.16
文献标志码:
A
摘要:
进入21世纪以来,长江干流上游水库群的运行对鄱阳湖与长江之间物质和能量的交换过程产生了重要影响,鄱阳湖流域的秋旱现象逐渐严重,江湖关系加速演变.采用Mann-Kendall趋势检验法、R/S(Rescaled Range Analysis)分析法、变差系数Cv和偏态系数Cs等方法,分析了2000年以来鄱阳湖水位变化趋势性特征; 分析了长江干流上游水库群调节和湖区采砂活动对鄱阳湖水位趋势性变化的影响.结果显示:2000—2014年鄱阳湖水位分阶段降低,2006—2014年水位降至最低,比2000年前低1.08 m.2000年后,鄱阳湖全年、汛期和枯季平均水位都有减少趋势,10月份平均水位有非常显著的减少趋势; 不同季节主湖区与入江水道水位变化趋势性不一致; H值表明鄱阳湖冬季水位减少有较强的持续性.长江干流上游水库群调节对鄱阳湖水位影响存在时空差异,水库群蓄水期加剧了鄱阳湖水位下降的幅度,对湖心区影响达4%以上.采砂活动对鄱阳湖水位的影响在2006—2014年表现明显,除了10月份外其余季节的影响都大于长江干流上游水库群调节作用.合理调度长江干流上游水库群及湖区采砂活动在保护鄱阳湖生态环境中具有重要意义.
Abstract:
Since the 21st century,regulations of reservoir group of the Yangtze River upstream have some important impact on the process that the matter and energy exchange between Yangtze River and Poyang Lake.Autumn droughts in Poyang Lake drainage become more and more serious,and the relationship between the Yangtze River and Poyang Lake has evolved faster.Mann-Kendall trend test,R/S(Rescaled Range Analysis)analysis method,the variation coefficient Cv and skewness coefficient Cs etc.,are used to analyze the trend characteristics of water level change in Poyang Lake since 2000.The effects of reservoir group regulation in the upper reaches of the Yangtze River main stream and sand excavating in Poyang Lake on the water level change trend of Poyang Lake are quantitative analyzed.The results show that water level of Poyang Lake have decreased by step during 2000—2014,which fell to its lowest level in 2006—2014.It is 1.08 m lower than that before 2000.After 2000,the average water level in the whole year,flood season and dry season of Poyang Lake has a decreasing trend,and the average water level in October has a very significant decreasing.The variation trend of water level in main lake is inconsistent with water channel into Yangtze River in Poyang Lake in different seasons.The H value indicates that the decreasing of water level of Poyang Lake is more sustainable in winter.The impact of reservoir group regulation of the upper reaches of the Yangtze River main stream on the water level of Poyang Lake is different in spatial and temporal disparities.In impounding period, the reservoir group regulation aggravates the decline extent of the water level of Poyang Lake,whose impact on the central area of the lake is more than 4%.It is more obvious that the sand excavating activities influence on the water level of Poyang Lake from 2006 to 2014.Except October,its influence is greater than that of the reservoir group regulation in the upper reaches of the Yangtze River main stream in other seasons.It is of great significance to control rationally reservoir groups in the upper reaches of the Yangtze River trunk stream and sand excavation activities in Poyang Lake area in protecting the ecological environment of the lake.

参考文献/References:

[1] Pachauri R K,Meyer R A.Climate change 2014:synthesis report.contribution of working groups I,II and III to the fifth assessment report of the intergovernmental panel on climate change[J].Journal of Romance Studies,2014,4(2):85-88.
[2] Ye Xuchun,Xu Chongyu,Li Yunliang,et al.Change of annual extreme water levels and correlation with river discharges in the middle-lower Yangtze River:characteristics and possible affecting factors[J].Chinese Geographical Science,2017,27(2):325-336.
[3] Zhang Xiaolin,Zhang Qi,Werner A D,et al.Characteristics and causal factors of hysteresis in the hydrodynamics of alarge floodplain system:Poyang Lake(China)[J].Journal of Hydrology,2017,553:574-583.
[4] Hu Qi,Feng Song,Guo Hua,et al.Interactions of the Yangtze River flow and hydrologic processes of the Poyang Lake,China[J].Journal of Hydrology,2007,347(1/2):90-100.
[5] 郭华,Hu Qi,张奇.近50年来长江与鄱阳湖水文相互作用的变化[J].地理学报,2011,66(5):609-618.
[6] Li Yunliang,Zhang Qi,Werner A D,et al.The influence of river-to-lake backflow on the hydrodynamics of a large floodplain lake system(Poyang Lake,China)[J].Hydrological Processes,2017,31(1):117-132.
[7] Yang Guishan,Zhang Qi,Wan Rongrong,et al.Lake hydrology,water quality and ecology impacts of altered river-lake interactions:advances in research on the middle Yangtze River[J].Hydrology Research,2016,47(S1):1-7.
[8] Zhang Qi,Ye Xuchun,Werner A D,et al.An investigation of enhanced recessions in Poyang Lake:comparison of Yangtze River and local catchment impacts[J].Journal of Hydrology,2014,517:425-434.
[9] 赵军凯,李九发,蒋陈娟,等.长江中下游河湖水量交换过程[J].水科学进展,2013,24(6):759-770.
[10] Yao Jing,Zhang Qi,Li Yunliang,et al.Hydrological evidence and causes of seasonal low water levels in a large river-lake system:Poyang Lake,China[J].Hydrology Research,2016,47(S1):24-39.
[11] Guo Hua,Hu Qi,Zhang Qi,et al.Effects of the Three Gorges Dam on Yangtze River flow and river interaction with Poyang Lake,China:2003—2008[J].Journal of Hydrology,2012,416/417:19-27.
[12] Lai Xijun,Jiang Jiahu,Liang Qiuhua,et al.Large-scale hydrodynamic modeling of the middle Yangtze River Basin with complex river-lake interactions[J].Journal of Hydrology,2013,492:228-243.
[13] 吴桂平,刘元波,范兴旺.近30 年来鄱阳湖湖盆地形演变特征与原因探析[J].湖泊科学,2015,27(6):1168-1176.
[14] 戴雪,万荣荣,杨桂山,等.鄱阳湖水文节律变化及其与江湖水量交换的关系[J].地理科学,2014,34(12):1488-1496.
[15] 戴志军,李九发,赵军凯,等.特枯2006年长江中下游径流特征及江湖库径流调节过程[J].地理科学,2010,30(4):577-581.
[16] 朱玲玲,陈剑池,袁晶,等.洞庭湖和鄱阳湖泥沙冲淤特征及三峡水库对其影响[J].水科学进展,2014,25(3):348-357.
[17] 白丽,张奇,李相虎.湖泊水量变化关键影响因子研究综述[J].水电能源科学,2010,28(3):30-35.
[18] 闵骞,占腊生.1952—2011年鄱阳湖枯水变化分析[J].湖泊科学,2012,24(5):675-678.
[19] 姜加虎,黄群.三峡工程对鄱阳湖水位影响研究[J].自然资源学报,1997,12(3):24-29.
[20] 邬年华,罗优,刘同宦,等.三峡工程运行对鄱阳湖水位影响试验[J].湖泊科学,2014,26(4):522-528.
[21] 周云凯,白秀玲,宁立新.1970—2015年鄱阳湖水位变化特征及其突变分析[J].河南大学学报:自然科学版,2018,48(2):151-159.
[22] 欧阳千林,刘卫林.近50年鄱阳湖水位变化特征研究[J].长江流域资源与环境,2014,23(11):1545-1550.
[23] 张范平,方少文,周祖昊,等.鄱阳湖水位多时间尺度动态变化特性分析[J].长江流域资源与环境,2017,26(1):126-133.
[24] 邓志民,张翔,肖洋,等.鄱阳湖水位演变及其影响因子分析[J].武汉大学学报:工学版,2015,48(5):615-621.
[25] 王鹏,赖格英,黄小兰.鄱阳湖水利枢纽工程对湖泊水位变化影响的模拟[J].湖泊科学,2014,26(1):29-36.
[26] 张楠楠,王文,王胤.鄱阳湖面积的卫星遥感估计及其与水位关系分析[J].遥感技术与应用,2012,27(6):947-953.
[27] Yao Jing,Zhang Qi,Ye Xuchun,et al.Quantifying the impact of bathymetric changes on the hydrological regimes in a large floodplain lake:Poyang Lake[J].Journal of Hydrology,2018,561:711-723.
[28] 席海燕,王圣瑞,郑丙辉,等.流域人类活动对鄱阳湖生态安全演变的驱动[J].环境科学研究,2014,27(4):398-405.
[29] 水利部长江水利委员会.长江泥沙公报2016[M].武汉:长江出版社,2016.
[30] 符淙斌,王强.气候突变的定义和检测方法[J].大气科学,1992,16(4):482-493.
[31] 白红英,侯钦磊,马新萍,等.50年来秦岭金钱河流域水文特征及其对降水变化的响应[J].地理科学,2012,32(10):1229-1235.
[32] 管华.水文学[M].2版.北京:科学出版社,2015.
[33] 邴建平,邓鹏鑫,吕孙云,等.鄱阳湖与长江干流水量交换效应及驱动因素分析[J].中国科学:技术科学,2017,47(8):856-870.
[34] 姚静,李云良,李梦凡,等.地形变化对鄱阳湖枯水的影响[J].湖泊科学,2017,29(4):955-964.
[35] 胡振鹏,傅静.长江与鄱阳湖水文关系及其演变的定量分析[J].水利学报,2018,49(5):570-579.
[36] 赖格英,张志勇,王鹏,等.拟建鄱阳湖水利枢纽工程对长江干流流量影响的模拟[J].湖泊科学,2017,29(3):521-533.
[37] 江丰,齐述华,廖富强,等.2001—2010年鄱阳湖采砂规模及其水文泥沙效应[J].地理学报,2015,70(5):837-845.
[38] 刘昌明,李艳忠,刘小莽,等.黄河中游植被变化对水量转化的影响分析[J].人民黄河,2016,38(10):7-12.
[39] Li Xianghu,Zhang Qi.Variation of floods characteristics and their responses to climate and human activities in Poyang Lake,China[J].Chinese Geographical Science,2015,25(1):13-25.
[40] 刘志刚,倪兆奎.鄱阳湖发展演变及江湖关系变化影响[J].环境科学学报,2015,35(5):1265-1273.
[41] 江西省统计局.江西统计年鉴(2000—2015)[M].北京:中国统计出版社,2016.
[42] Feng Lian,Han X X,Hu C M,et al.Four decades of wetland changes of the largest freshwater lake in China:possible linkage to the Three Gorges Dam?[J].Remote Sensing of Environment,2016,176:43-55.
[43] 罗蔚,张翔,邓志民,等.1956—2008年鄱阳湖流域水沙输移趋势及成因分析[J].水科学进展,2014,25(5):658-667.
[44] 孙鹏,张强,陈晓宏,等.鄱阳湖流域水沙时空演变特征及其机理[J].地理学报,2010,65(7):828-840.

备注/Memo

备注/Memo:
收稿日期:2019-01-20基金项目:国家自然科学基金(41361003,41561011)和江西省教育厅科技课题(GJJ180903)资助项目.作者简介:赵军凯(1973-),男,河南新郑人,副教授,博士,主要从事自然地理和水文与水资源方面的研究.E-mail:junkaizhao@163.com通信作者:李九发(1949-),男,江西南丰人,教授,博士生导师,主要从事自然地理和水文与水资源方面的研究.E-mail:jfli@re.ecnu.edu.cn
更新日期/Last Update: 2019-10-10