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湿地水文学研究进展

邓伟 潘响亮 栾兆擎

邓伟, 潘响亮, 栾兆擎. 湿地水文学研究进展[J]. 水科学进展, 2003, 14(4): 521-527.
引用本文: 邓伟, 潘响亮, 栾兆擎. 湿地水文学研究进展[J]. 水科学进展, 2003, 14(4): 521-527.
DENG Wei, PAN Xiang-liang, LUAN Zhao-qing. Advances in wetland hydrology[J]. Advances in Water Science, 2003, 14(4): 521-527.
Citation: DENG Wei, PAN Xiang-liang, LUAN Zhao-qing. Advances in wetland hydrology[J]. Advances in Water Science, 2003, 14(4): 521-527.

湿地水文学研究进展

基金项目: 国家自然科学基金资助项目(40171017);吉林省资助重大项目(20010401)
详细信息
    作者简介:

    邓伟(1957- ),男,辽宁沈阳人,中国科学院东北地理与农业生态研究所研究员,博士生导师,博士,主要从事水资源与生态方面的研究.E-mail:dengwei@mail.neigae.ac.cn

  • 中图分类号: S286;P333.1;G353.11

Advances in wetland hydrology

Funds: The project is supported by National Natural Science Foundation of China(No.40171017).
  • 摘要: 水文过程在湿地形成、发育、演替直至消亡全过程中起重要作用.降水截流、径流和蒸散作用是湿地 大气界面水文过程研究的热点和重点,开发的模型较多但尚需进一步检验和完善.片流和明渠流是湿地主要地表径流,其中片流受地形坡度等因素影响而难以精确计算.湿地的地下水文系统对季节性积水湿地尤为重要,但是关于泥炭沼泽的垂向水力联系尚需进一步研究.可持续的湿地水文管理必须将人类活动和气候变化这两个因素纳入湿地综合水文模型,然而目前除少数几个综合模型外,大多数的湿地水文模型并非如此.加强湿地水文观测、多手段多技术相结合和开发综合湿地水文模型应是今后湿地水文学研究的主流.
  • [1] Hollis G E,Thompson J R.Hydrological data for wetland management[J].J CIWEN,1998,(12):9-17.
    [2] Lafieur P M,McCaughey J H,Joiner D W,et al.Seasonal trends in energy,water,and carbon dioxide fluxes at a Northern boreal wetland[J].Journal of Geophysical Research,1997,102:29 009-29 020.
    [3] Pook E W,Moore P H R,Hall T,et al.Rainfall interception by trees of pinus radiata and eucalyptus viminalis in a 1300 mm rainfall area of southeastern new South Wales[J].Hydrol Process,1991,(6):127-141.
    [4] Rutter A J,Kershaw K A,Robbins P C,et al.A predictive model of rainfall interception in forests.Ⅰ.A derivative of the model from observations in a plantation of Corsican pine[J].Agric Met,1971,(9):367-384.
    [5] Rutter A J,Mortorn A J,Robbins P C.A predictive model for rainfall interception in forests.[.Generalization of the model and comparison with observations in some coniferous and hardwood stands[J].J Appl Ecol,1975,(12):367-380.
    [6] Gash J H C.An application of the Tutter model to the estimation of the interception loss from Thefford Forest[J].1979,35:385-396.
    [7] Whitehead D,Kelliher F M.A canopy water balance model for a Pinus radiata stand before and after thinning[J].Agri For Meteorol,1991,55:109-126.
    [8] Liu S.A new model for the prediction of rainfall in forest canopies[J].Ecol Model,1997,99:151-159.
    [9] Sellers P J,Randall D A,Collatz G J,et al.A revised land surface parameterization for atomospheric GCMs.Part Ⅰ Model formation[J] J Climate,1996,9:676-705.
    [10] Zeng N,Shuttleworth J W,Gash J H C.Influence of temporal variability of rainfall on interception loss.Part Ⅰ:Point ananlysis[J].J Hydrol,2000,228(3-4):228-241.
    [11] Aboal J R,Morales D,Hernandez M,et al.The measurement and modeling of the variation of stemflow in a laurel forest in Tenerife,Canary Islands[J].J Hydrol 1999,221(3-4):161-175.
    [12] Taniguchi M,Tsujimura T,Tanaka T.Significance of stemflow in groundwater recharge 1:evaluation of the stemflow contribution to recharge using a mass balance approach[J].Hydrol Process,1996,10(1):71-80.
    [13] Boyd C E.Evapotranspiration/evaporation(E/E0) ratios for aquatic plants[J].J Aquatic Plant Management,1987,25:1-3.
    [14] Campbell D,Williamson JL.Evaporation from a raised peat bog[J].J Hydrol,1997,193:142-160.
    [15] Price JS.Hydrology and microclimate of a partly restored cutover bog,Quebec[J].Hydrol Process,1996,(10):1 263-1272.
    [16] Hussey B H,Odum W E.Evapotranspiration in tidal marshes[J].Estuaries,1992,(15):59-67.
    [17] Souch C,Susan B C,Charlotte P W.Evapotranspiration rates from wetlands with different disturbance histories:Indiana Dunes National Lakeshore[J].Wetlands,1998,18:216-229.
    [18] William R B.Evapotranspiration From a Burlrush-Dominated Wetland in the Klamath Basin,Oregon[J].J Am Water Res Assoc,2000,36:1 309-1 320.
    [19] Souch C,Charlotte P W,Susan B C,et al.Wetland Evaporation and Energy Partitioning:Indiana Dunes National Lakeshore[J].J Hydrol,1996,84(3-4):189-208.
    [20] Brutsaert W.Evaporation Into the Atomosphere-Theory,History,and Applications[M].D Reidel,Boston,Massachusetts,1982.
    [21] Salvador S,Miguel A,Manuel B.A simple method for estimating water loss by transpiration in wetlands[J].Hydrol Sci J,2001,46(4):537-552.
    [22] Jorge I,Angela M,Jayantha.A Wetland Simulation Module for the MODFLOW Ground Water Model[J].Ground Water,1998,30:764-770.
    [23] Devito K J,Hill A R.Sulphate dynamics in relation to groundwater-surface water interactions in headwater forested wetlands of the southern Canadian Shield[J].Hydrol Processes 1997,11(5):485-500.
    [24] Quintnn WL,Roulet NT.Spring and summer hydrology of a subarctic patterned wetland[J].Arctic and Alpine Research,1998,30:285-294.
    [25] Gafni A,Brooks K.Hydraulic characteristic of four peatlands in Minnesota[J].J of Hydrol,1990,70:239-253.
    [26] Hoag R,Price J.The effects of matrix diffusion on solute transport and retardation in undisturbved peat in laboratory columns[J].J Contaminant Hydrol,1997,28:193-205.
    [27] Siegel D.Ground water and the evolution of patterned mires.Glacial Lake Agassiz Peatlands.Minnesota[J].J Ecol,1983,71:913-921.
    [28] Siegel D,Glaser P.Groundwater flow in a bog-fen complex,Lost River Peatland,northern Minnesota[J].J Ecol,1987,71:913-921.
    [29] Devito K J,Waddington J M,Branfireun.Flow reversals in peatlands influenced by local groundwater systems[J].Hydrol Processes,1997,(11):103-110.
    [30] Chanton,Jeffrey,James Bauer,et al.Radiocarbon evidence for the substrates supporting methane formation within northern Minnesota peatlands[J].Geoehimica et Cosmochimiea Acta,1995,59:3 663-3 668.
    [31] Wise W R,Annable M D,Walser R S,et al.A wetland-aquifer interaction test[J].J Hydrol,2000,227(1-4):257-272.
    [32] Reeve A S,Siegel D I,Glaser P H.Simulating vertical flow in large peatlands[J].Journal of Hydrology,2000,227(1-4):207-217.
    [33] Burkett,Jon Kusler.Climate Change:potential impacts and interactions in wetlands of the united states,Virginia[J].J Am Water Res Associ,2000,36:313-320.
    [34] Penland S,Ramsey K.Relative Sea-level Rise in Louisiana and the Gulf of Mexico:1908-1988[J].Journal of Coastal Research,1997,(6):323-342.
    [35] Short F T,Neckles H A.The Effects of Global Climate Change on Seagrasses[J].Aquatic Botany,1999,63:169-196.
    [36] Van der Kamp G,et al.Drying out of small prairie wetlands after conversion of their catchments from cultivation to permanent brome grass[J].Hydrol Sci J,1999,44(3):387-398.
    [37] Euliss N H Jr,Mushet D M.Water-level fluctuations in wetlands as a function of landscape condition in the prairie pothole region[J].Wetlands,1996,16:587-593.
    [38] Christie H W.Soil and subsoil moisture accumulation due to dryland agriculture in southern Alberta[J].Can J Soil Sci,1985,65:805-810.
    [39] de Jong E,Kachanoski R G.The role of grasslands in hydrology[M].Canadian Aquatic Resources,1987.215,213-241.
    [40] Thompson J R,Hollis G E.Hydrological modeling and the sustainable development of the Hadejia-Nguru Wetland[J].Nigeria Hydrol Sci J,1995,40:97-116.
    [41] Sun G,Riekerk H,Nicholas B.Modeling the forest hydrology of wetland-upland ecosystems in Florida[J].J Am Water Res Assoc,1998,34:827-841.
    [42] Merritt M L.Simulation of the water-table altitude in the Biscayne Aquifer,Southern Dade County,Florida,water years 1945-1989[M].Tallahassee,Florida:USGS UNITED STATES GOVERNMENT PRINTING OFFICE,WASHINGTON,1997.
    [43] Mansell R S,Bloom S A,Sun Ge.A model for wetland hydrologx description and validation[J].Soil Science,2000,165:384-397.
    [44] Refsgaard J C,Storm B.MIKE SHE In:Computer Models of Watershed Hydrology[C].(ed by V.P.Singh),Water Resources Publications,Englewood Cliffs,New Jersey,USA.1995.809-846.
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出版历程
  • 收稿日期:  2002-04-22
  • 修回日期:  2002-07-10
  • 刊出日期:  2003-07-25

湿地水文学研究进展

    基金项目:  国家自然科学基金资助项目(40171017);吉林省资助重大项目(20010401)
    作者简介:

    邓伟(1957- ),男,辽宁沈阳人,中国科学院东北地理与农业生态研究所研究员,博士生导师,博士,主要从事水资源与生态方面的研究.E-mail:dengwei@mail.neigae.ac.cn

  • 中图分类号: S286;P333.1;G353.11

摘要: 水文过程在湿地形成、发育、演替直至消亡全过程中起重要作用.降水截流、径流和蒸散作用是湿地 大气界面水文过程研究的热点和重点,开发的模型较多但尚需进一步检验和完善.片流和明渠流是湿地主要地表径流,其中片流受地形坡度等因素影响而难以精确计算.湿地的地下水文系统对季节性积水湿地尤为重要,但是关于泥炭沼泽的垂向水力联系尚需进一步研究.可持续的湿地水文管理必须将人类活动和气候变化这两个因素纳入湿地综合水文模型,然而目前除少数几个综合模型外,大多数的湿地水文模型并非如此.加强湿地水文观测、多手段多技术相结合和开发综合湿地水文模型应是今后湿地水文学研究的主流.

English Abstract

邓伟, 潘响亮, 栾兆擎. 湿地水文学研究进展[J]. 水科学进展, 2003, 14(4): 521-527.
引用本文: 邓伟, 潘响亮, 栾兆擎. 湿地水文学研究进展[J]. 水科学进展, 2003, 14(4): 521-527.
DENG Wei, PAN Xiang-liang, LUAN Zhao-qing. Advances in wetland hydrology[J]. Advances in Water Science, 2003, 14(4): 521-527.
Citation: DENG Wei, PAN Xiang-liang, LUAN Zhao-qing. Advances in wetland hydrology[J]. Advances in Water Science, 2003, 14(4): 521-527.
参考文献 (44)

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