用户名: 密码: 验证码:
长江上游水库改变干流磷通量、效应与修复对策
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Dams altered Yangtze River phosphorus and restoration countermeasures
  • 作者:周建军 ; 张曼 ; 李哲
  • 英文作者:ZHOU Jianjun;ZHANG Man;LI Zhe;Department of Hydraulic Engineering,Tsinghua University;Chongqing Institute of Green and Intelligent Technology,Chinese Academy of Sciences;
  • 关键词: ; 泥沙 ; 水库 ; 生态环境 ; 长江保护
  • 英文关键词:Phosphorus;;sediment;;reservoirs;;eco-environment;;Yangtze River protection
  • 中文刊名:FLKX
  • 英文刊名:Journal of Lake Sciences
  • 机构:清华大学水利系;中国科学院重庆绿色智能技术研究院;
  • 出版日期:2018-07-06
  • 出版单位:湖泊科学
  • 年:2018
  • 期:v.30
  • 基金:国家重点研发计划(2016YFE0133700);; 国家自然科学基金项目(51509137)联合资助
  • 语种:中文;
  • 页:FLKX201804001
  • 页数:16
  • CN:04
  • ISSN:32-1331/P
  • 分类号:3-18
摘要
磷主要随河川径流循环,是水域重要营养或污染物质,是长江及河口浮游生物限制因子.在自然与人类活动作用下,磷循环规律及变化对水生态环境具有重要作用.本文根据实测资料、理论和模型系统分析了长江磷自然循环属性、水库作用及可能的环境影响.长江磷以颗粒态为主,与泥沙关系密切,受水库影响大量沉积;颗粒磷的潜在生物有效磷(BAP)较高,总量超过人类排放;自然背景下磷与淡水系统关系较小,到河口及周边海域释放BAP是这里生态系统关键的营养资源;水库拦截使在底泥沉积并在缺氧环境释放的BAP成为河流上游潜在污染源.水库拦沙也破坏了下游河流泥沙的磷缓冲机制,增加环境脆弱性,降低污染承受能力,抬高水库下泄背景溶解磷浓度和河口碳、氮的相对程度,增加干流最下游大型水库污染和水华风险.另一方面,实测资料对比研究表明,我国河流地表水环境监测规范中的磷分析方法存在问题,采用"澄清样"方法使磷大量漏测,上下游、河湖库及汛枯期间磷通量监测口径不同、标准不一,很难适应流域一体化管理要求;依此监测的评估也会严重低估水库作用,忽视其拦磷和抬高背景溶解磷等机制,误导污染源解析,影响环境管理与决策.流域水库改变泥沙、磷及循环规律是当前长江干流环境条件的实质性改变,是长江保护生态面临的主要问题和修复重点之一,建议在大型水库持续挖泥用以功能性修复河流物质通量和消除上游潜在污染内源.
        Phosphorus( P),as a limiting and vital macronutrient in global freshwaters,circulates mainly with sediment through rivers. In this paper,we analyzed and summarized the regime of P and its variations that induced by dams burgeoning in the upper Yangtze River basins in recent decades. We revealed that more than 91% of the P flux is in particulate form,among which the potential dissolvable bio-active P( BAP) can exceed the total load that discharged from the riparian basins. The P is closely correlated with sediment and we estimated that reservoirs have by more than 3 quarters of it sequestrated. Previously,the BAP was mostly absorbed by sediment and flushed by floods to the estuary,where it supported a flourishing saline bio-ecosystem at the same time,with minor residuals in the lowland freshwaters. However,this nature endowed regime was upset by the sequestration of reservoirs that reallocated reversely the background P as inner pollution for the freshwater corridors and snatched the inherent nutrient for ecosystem of the estuary. Moreover,the resultant clear-stream lost its buffering effect that sediment regulates P and the lowland freshwater becomes more vulnerable with lowered environmental capacity. Accounting for the actual eutrophic status,the pool elevated dissolvable P level may also add potential risks in stimulating harmful algal blooms and hypoxia to the Three Gorges Reservoir and others. On another hand,in order to keep a basin wide consistent monitoring and criterions in P control from water to water and we can evaluate the harmful effect of dams more objectively,we recommend urgently to correct the present P analysis regulation,which requires P extraction from water samples after 30 min settling,that can lose a significant amount of P. Finally,we proposed to restore the downstream biogenic-substance and eliminate the in-pool accumulating P contamination through successive slurry dredging from reaches in front of the dams.
引文
[1]Zhou JJ,Zhang M.On the forefront ecological and environmental problems of current Yangtze River and restoration priorities.Environmental Protection,2017,45(617):17-24.[周建军,张曼.当前长江生态环境主要问题与修复重点.环境保护,2017,45(617):17-24.]
    [2]Qian N,Zhang R,Zhou ZD eds.Fluvial processes.Beijing:Science Press,1987.[钱宁,张仁,周志德.河床演变学.北京:科学出版社,1987.]
    [3]Han QW,He MM,Xu JL eds.Supplementary computation of deposition of the 175 scheme TGP.Publication on research of the key problems in sediment and navigation of the Three Gorges Project.Wuhan:Wuhan Polytech Univ Press,1992:539-550.[韩其为,何明民,徐俭立.三峡水库175方案补充计算结果.长江三峡工程泥沙与航运关键技术研究——专题研究报告集.武汉:武汉工业大学出版社,1992:539-550.]
    [4]Changjiang Water Resource Commission ed.Studies on sediment problems of the Three Gorges Project.Wuhan:Hubei Science and Techology Press,1997.[长江水利委员会.三峡工程泥沙研究.武汉:湖北科学技术出版社,1997.]
    [5]Conley DJ,Paerl HW,Howarth RW et al.Controlling eutrophication:Nitrogen and phosphorus.Science,2009,323:1014-1015.
    [6]Nixon SW.Replacing the Nile:Are anthropogenic nutrients providing the fertility once brought to the Mediterranean by a great river?Royal Swedish Academy of Sciences,2003,32(1):30-39.
    [7]Pan G,Krom MD,Herut B et al.Adsorption-desorption of phosphate on Airborne dust and riverborme particulates in East Mediterranean seawater.Environ Sci Technol,2002,36:3519-3524.
    [8]Edmond JM,Spivack A,Grant BC et al.Chemical dynamics of the Changjiang estuary.Cont Shelf Res,1985,4(1/2):17-36.
    [9]Zhang J,Zhang ZF,Liu SM et al.Human impacts on the large world rivers:would the Changjiang(Yangtze River)be an illustration?Global Biogeochem Cycl,1999,3(4):1099-1105.
    [10]Liu SM,Zhang J,Chen HT et al.Nutrients in the Changjiang and its tributaries.Biogeochemistry,2003,62:1-18.
    [11]Shen ZL.Phosphorus and silicate fluxes in the Yangtze River.Acta Geographica Sinica,2006,61(7):741-751.[沈志良.长江磷和硅的输送通量.地理学报,2006,61(7):741-751.]
    [12]Zeng H,Song L,Yu ZG et al.Post-impoundment biomass and composition of phytoplankton in the Yangtze River.Int Rev Hydrobiol,2007,92(3):267-280.
    [13]Duan SW,Liang T,Zhang S et al.Seasonal changes in nitrogen and phosphorus transport in the lower Changjiang River before the construction of the Three Gorges Dam.Estuarine,Coastal and Shelf Science,2008,79:239-250.
    [14]Shen ZL,Liu Q.Nutrients in the Changjiang River.Environ Monit Assess,2009,153:27-44.
    [15]Wei JF,Chen HT,Liu PX et al.Phosphorus forms in suspended particulate matter of the Yangtze River.Advances in Water Science,2010,21(1):107-112.[魏俊风,陈洪涛,刘鹏霞等.长江悬浮颗粒物中磷的赋存形态.水科学进展,2010,21(1):107-112.]
    [16]Müller B,Berg M,Pernet-Coudrier P et al.The geochemistry of the Yangtze River:Seasonality of concentrations and temporal trends of chemical loads.Global Biogeochem Cycles,2012,26:GB2028.DOI:10.1029/2011GB004273.
    [17]Zhou J,Zhang M,Lu P.The effect of dams on phosphorus in the middle and lower Yangtze river.Water Resources Research,2013,49(6):3659-3669.
    [18]Zhou J,Zhang M,Lin B et al.Lowland fluvial phosphorus altered by dams.Water Resources Research,2015,51(4):2211-2226.
    [19]Müller B,Finger D,Sturm M et al.Present and past bio-available phosphorus budget in the ultra-oligotrophic Lake Brienz.Aquat Sci,2007,69:227-239.
    [20]Zhou J,Lin B.One-dimensional mathematical model for suspended sediment by lateral integration.J Hydraulic Eng,1998,124:712-717.
    [21]Zhou J,Lin B.Verification of mathematical model for sediment transport by unsteady flow in the lower Yellow River.Int J Sediment Res,2004,19:278-291.
    [22]Smil V.Phosphorus in the environment:Natural flows and human interferences.Annual Rev Energy Environ,2000,25:53-88.
    [23]Wang R,Balkanski Y,Boucher O et al.Significant contribution of combustion-related emissions to the atmospheric phosphorus budget.Nat Geosci,2015,8:48-54.
    [24]Xu Kaiqin,Hayashi Seiji,Murakami Shogo et al.Characteristics of water quality in the Changjiang River:Observations conducted in 1998 and 1999.Acta Geographica Sinica,2004,59(1):118-124.[徐开钦,林诚二,牧秀明等.长江干流主要营养盐含量的变化特征——1998 1999年日中合作调研结果分析.地理学报,2004,59(1):118-124.]
    [25]Müller B,M Berg,Yao ZP et al.How polluted is the Yangtze river?Water quality downstream from the Three Gorges Dam.Science of the Total Environment,2008,402:232-247.
    [26]Meybeck M.Carbon,nitrogen,and phosphorus transport by world rivers.Am J Sci,1982,282:401-450.
    [27]Russell MA,Walling DE,Webb BW et al.The composition of nutrient fluxes from contrasting UK river basins.Hydrological Process,1998,12:1461-1482.
    [28]Milliman JD,Meade RH.World-wide delivery of river sediment to the oceans.Journal of Geology,1983,91(1):1-21.
    [29]Meybeck M,Ragu A.GEMS-GLORI world river discharge database.Laboratoire de Géologie Appliquée,UniversitéPierre et Marie Curie,Paris,France,2012.DOI:10.1594/PANGAEA.804574.
    [30]Forsberg BR,Devol AH,Richey JE et al.Factors controlling nutrient concentrations in Amazon floodplain lakes.Limnology and Oceanography,1988,33(1):41-56.
    [31]Ramesh R,Purvaja GR,Subramanian V.Carbon and phosphorus transport by the major Indian rivers.Journal of Biogeography,1995,22(2/3):409-415.
    [32]Duan SW,Zhang S.The variations of nitrogen and phosphorus concentrations in the monitoring stations of three major rivers in China.Science Geographica Sinica,1999,19(5):411-416.[段水旺,章申.中国主要河流控制站氮、磷含量变化规律初探.地理科学,1999,19(5):411-416.]
    [33]SaundersⅢJF,Lewis JR WM.Transport of phosphorus,nitrogen,and carbon by Apure River,Veneuela.Biogeochemistry,1988,5:323-342.
    [34]USGS.Annual nutrient flux and concurrent stream flow to the Gulf of Mexico for the period of 1996-2005.http:∥toxics.usgs.gov/pubs/of-2007-1080/delivery/gulf_annual_loads.html.
    [35]Sutula M,Bianchi TS,Mckee BA.Effect of seasonal sediment storage in the lower Mississippi River on the flux of reactive particulate phosphorus to the Gulf of Mexico.Limnology and Oceanography,2004,49(6):2223-2235.
    [36]Goolsby DA,Battaglin WA,Lawrence GB et al.Flux and sources of nutrients in the Mississippi-Atchafalaya river basin,Topic 3 Report,National Science and Technology Council Committee on Environment and Natural Resources Hypoxia Work Group,1999.
    [37]Meybeck M.Fluvial export in biogeochemistry of inland waters.In:Ligens ed.Elsevier:Academic Press,2009:118-129.
    [38]Teodoru C,Wehrli B.Retention of sediments and nutrients in the Iron Gate I Reservoir on the Danube River.Biogeochemistry,2005,76:539-565.
    [39]International Research and Training Center on Erosion and Sedimentation(IRTCES).River sediment bulletin of China2000,Beijing,http:∥www.irtces.org/database.asp.
    [40]Delmas M,Cerdan O,Cheviron B et al.Sediment export from French rivers to the sea.Earth Surf Process Landforms,2010,37:754-762.
    [41]Ignatieva NV.Nutrient exchange across the sediment-water interface in the eastern Gulf of Finland.Boreal Environment Research,1999,4:295-305.
    [42]Horowitz AJ,Elrick KA,Smith JJ.Annual suspended sediment and trace element fluxes in the Mississippi,Columbia,Colorado and Rio Grande drainage basin.Hydrological Processes,2001,15:1169-1207.
    [43]Stanford JA,Ward JV.Limnology of Lake Powell and the chemistry of the Colorado River.Colorado River Ecology and Dam Management:Proceedings of a Symposium May 24-25,1990,Santa Fe,New Mexico.
    [44]Guo LD,Zhang JZ,Gueguen C.Speciation and fluxes of nutrients(N,P,Si)from the upper Yukon River.Global Biogeochemical,2004,18:GB1038.
    [45]Barlow JP,Glase MS.Partitioning of phosphorus between particles and water in a river outflow.Hydrobiologia,1982,91:253-260.
    [46]Cai YH,Guo LD,Douglas TA et al.Seasonal variations in nutrient concentrations and speciation in Chena River,Alaska.Journal of Geophysical Res,2008,113:G03035.
    [47]Nilsson N,Reidy CA,Dynesius M et al.Fragmentation and flow regulation of the world’s large river systems.Science,2005,308:405-408.
    [48]Garnier J,Nemery J,Billen G et al.Nutrient dynamics and control of eutrophication in the Marne River system:modelling the role of exchangeable phosphorus.Journal of Hydrology,2005,304:397-412.
    [49]Duan SW,Zhang S,Chen XB et al.Concentration of nitrogen and phosphorus and nutrient transport to estuary of the Yangtze River.Environmental Science,2000,21(1):53-56.[段水旺,章申,陈喜保等.长江下游氮、磷含量变化及其输送量的估计.环境科学,2000,21(1):53-56.]
    [50]Howarth R,Jensen H,Marino R et al.Transport to and processing of P in near-shore and oceanic waters.SCOPE,1995,54:323-345.
    [51]Howarth RW,Billen G,Swaney D et al.Regional nitrogen budgets and riverine N&P fluxes for the drainages to the North Atlantic Ocean:Natural and human influences.Biogeochemistry,1996,35(1):75-139.
    [52]Chongqing Academy of Environmental Sciences.Total phosphorus prevention and control countermeasures in Yangtze river watershed of Chongqing section,Research Report,2017.[重庆市环境科学研究院.重庆长江流域总磷防控对策研究.研究报告,2017.]
    [53]Hubei Academy of Environmental Sciences.Total phosphorus prevention and control countermeasures in Yangtze river watershed of Hubei section,Research Report,2017.[湖北环境科学研究院.湖北省长江流域总磷防控对策研究.研究报告,2017.]
    [54]Blomqvist S,Gunnars A,Elmgren R.Why the limiting nutrient differs between temperate coastal seas and freshwater lakes:A matter of salt.Limnology and Oceanography,2004,49(6):2236-2241.
    [55]Zhang JZ,Huang XL.Effect of temperature and salinity on phosphate sorption on marine sediments.Environ Sci Technol,2011,45:6831-6837.
    [56]Zhou JJ,Zhang M.On the restoration strategies of alluvial rivers downstream of dams.Journal of Yangtze River Scientific Research Institute,2014,31(6):113-122.[周建军,张曼.大坝下游冲积河流修复与保护对策研究.长江科学院院报,2014,31(6):113-122.]
    [57]Ministry of Enrivonmental protection of the People’s Republic of China.Environmental quality standards for surface water.GB 2828-2002.[环境保护部.地表水环境质量标准,GB 3838 2002.]
    [58]Sonzogni WC,Chapra SC,Armstrong DE et al.Bioavailability of phosphorus inputs to lakes.Journal of Environmental Quality,1982,11(4):555-563.
    [59]Bostr9m B,Andersen JM,Fleischer S.Exchange of phosphorus across the sediment-water interface.Hydrobiologia,1988,170:229-244.
    [60]Nünberg GK.The prediction of internal phosphorus load in lakes with anoxic hypolimnia.Limnology and Oceanography,1984,29:111-129.
    [61]Hupfer M,Lewandowski J.Oxygen controls the phosphorus release from lake sediments—A long-lasting paradigm in limnology.International Review of Hydrobiology,2008,(4/5):415-432.
    [62]Conley DJ.Save the Baltic Sea.Nature,2012,486:463-464.
    [63]Redfield AC.The biological control of chemical factors in the environment.American Scientist,1958,46:205-222.
    [64]Tyrrell T.The relative influenced of nitrogen and phosphorus on oceanic primary production.Nature,2005,400:525-531.
    [65]Klausmeier CA,Litchman E,Daufresne T et al.Optimal nitrogen-to-phosphorus stoichiometry of phytoplankton.Nature,2004,429:171-174.
    [66]Yu LH,Li DJ,Fang T et al.Distribution of DSi,DIN and changes of Si:N ratio on the summer in Changjiang estuary before and after storage of Three Gorges Reservoir.Acta Ecologica Sinica,2006,26(9):2817-2826.[余立华,李道季,方涛等.三峡水库蓄水前后长江口水域夏季硅酸盐,溶解无机氮分布及硅氮比值的变化.生态学报,2006,26(9):2817-2826.]
    [67]Humborg C,Ittekkot V,Cociasu A et al.Effect of Danube river dams on Black Sea biogeochemistry and ecosystem structure.Nature,1997,386(27):385-388.
    [68]Zhang J,Fischer C,Ortner P.Potential availability of sedimentary phosphorus to sediment resuspension in Florida Bay.Global Biogeochem Cycles,2004,18:GB4008.
    [69]Wildman RA,Hering JG.Potential for release of sediment phosphorus to Lake Powell(Utah and Arizona)due to sediment resuspension during low water level.Lake Reservoir Manage,2011,27:365-375.
    [70]Zhang J,Huang X.Relative importance of solid-phase phosphorus and iron on the sorption behavior of sediments.Environ Sci Technol,2007,41(8):2789-2795.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700