降水对洞庭湖湿地水文补给效应
收稿日期: 2008-10-06
修回日期: 2008-12-30
网络出版日期: 2009-03-25
基金资助
"洪泛湿地水文生态过程的防洪效应研究"国家自然科学基金(40701172),北京市科技计划项目(D08040600580801),国际科技合作计划项目:(2007DFA20640),对发展中国家科技援助项目和地理信息科学江苏省重点实验室开放基金资助项目联合资助。
Hydrological recharge effect of precipitation on Dongting Lake wetland
Received date: 2008-10-06
Revised date: 2008-12-30
Online published: 2009-03-25
Supported by
"洪泛湿地水文生态过程的防洪效应研究"国家自然科学基金(40701172),北京市科技计划项目(D08040600580801),国际科技合作计划项目:(2007DFA20640),对发展中国家科技援助项目和地理信息科学江苏省重点实验室开放基金资助项目联合资助。
通过综合运用气象数据、遥感数据和典型下垫面特征资料,采用GIS技术和SCS模型,分析了降水对洞庭湖湿地水文的补给效应。在分析洞庭湖流域降水时空变化特征以及模拟地表径流的基础上,计算面积补给系数和体积补给系数。结果表明,面积补给系数较好地显示出监测时刻湖泊水域面积与流域面积之间的关系,不仅反映了某一时刻湿地水文对补给水的依赖,也定量表明降水形成地表径流后的水文补给效应及其对水域面积的影响;体积补给系数则通过注入湿地中的实际水量反映出降水对湿地水文的补给作用及其对水文循环的贡献,也可通过累加反映一段时间内的补给效应。两者的综合应用可以更好地说明大气降水对洞庭湖湿地水文的补给作用。
侯 鹏, 蒋卫国, 陈自力, 罗爱民 . 降水对洞庭湖湿地水文补给效应[J]. 地理研究, 2009 , 28(2) : 371 -378 . DOI: 10.11821/yj2009020011
Wetlands exist in a transition zone between aquatic and terrestrial environments which can be altered by subtle changes in hydrology. Hydrological process determines the formation, development and succession of wetlands. Taking the Dongting Lake as a study area, this paper studies the hydrological recharge effect of the atmosphere precipitation. According to the meteorological data, remote sensing image and typical underlay feature data, the recharge effectivity of the rainfall on the Dongting Lake wetland is analyzed supported by GIS (geographical information system) technology and SCS (Soil Conservation Service) model. Based on the analysis of spatio-temporal feature of rainfall and modeling of the runoff of precipitation, we obtained ARC (area recharge coefficient) and VRC (volume recharge coefficient). Thus, ARC well explains the acreage relationship of watershed and that of the water area in the lake sometime. It presents not only the wetland hydrology feature depending on the recharge water, but also the recharge effect of the runoff coming from rainfall and its influence on the water area. However, it is difficult to illustrate water fluid in wetland resulting from precipitation recharge in a period. Considering the relationship between flux of rainfall-runoff and volume of lake, VRC is calculated to make up for the shortcoming of ARC. According to the model, the recharge effectivity of rainfall can be computed in a certain period. ARC, together with VRC, can better explain runoff coming from rainfall as well as how it affects Dongting Lake's hydrological process and how it recharges water to the wetland, including the water area and water cycle. Thus it is significant to realize the importance of rainfall to the wetland and to protect and manage Dongting Lake wetland.
Key words: precipitation; wetlands; hydrological recharge; Dongting Lake
[1] 邓伟,潘响亮,栾兆擎.湿地水文学研究进展.水科学进展, 2003,14(4):521~527.
[2] 陆键健,何文珊,童春富,等.湿地生态学.北京:高等教育出版社, 2006.
[3] Andrew J. Baird, Robert L. Wilby.生态水文学.赵文智,王根绪 译.北京:海洋出版社, 2002.91~92.
[4] Mitsch W J, Gosselink J G.Wetlands(third edition).New York:John Wiley & Sons, Inc. ,2000.123~124.
[5] 刘春兰,谢高地,肖玉.气候变化对白洋淀湿地的影响.长江流域资源与环境, 2007,16(2):245~250.
[6] 安娜,高乃云,刘长娥.中国湿地的退化原因、评价及保护.生态学杂志, 2008, 27(5): 821~828.
[7] 罗磊.青藏高原湿地退化的气候背景分析.湿地科学, 2005,3(3):190~199.
[8] Virginia Burkett, Jon Kusler. Climate change: Potential impacts and interactions in wetlands of the United States. Journal of the American Water Resources Association,2000,36(2):313~320.
[9] 赵学敏.恢复扩大中国湿地.森林与人类, 2006,(5):5~7.
[10] 来红州,莫多闻,苏成.洞庭湖演变趋势探讨.地理研究, 2004,23(1): 78~86.
[11] 黄进良.洞庭湖湿地的面积变化与演替.地理研究, 1999,18(3): 297~304.
[12] 吴炳方,黄进良,沈良标.湿地的防洪功能分析评价——以洞庭湖为例.地理研究, 2000,19(2): 189~193.
[13] 姜加虎,黄群.洞庭湖区生态环境退化状况及其原因分析.生态环境, 2004, 13(2): 277~280.
[14] 袁作新.流域水文模型.北京:水利电力出版社,1990.
[15] 史培军,袁艺,陈晋.深圳市土地利用变化对流域径流的影响.生态学报, 2001,21(2):1041~1150.
[16] 彭定志,游进军.改进的SCS模型在流域径流模拟中的应用.水资源与水工程学报, 2006, 17(1): 20~24.
[17] 国家质量技术监督局,国家建设部.国家标准《水文基本术语和符号标准》(GB/T50095-98).1999.
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