基于vc+sql的光谱数据库管理系统设计【论文+开题报告】

1开题报告本文源码索取，请联系QQ68661508一、研究的目的和意义水资源是人类赖以生存和发展的基本要素之一，地球上的水资源虽然总量有限，但是可以循环利用。然而水资源却极易受到污染，并且是污染物的载体，能导致污染物的扩散与蔓延。随着我国经济的稳步发展，水污染问题也变得日益严重。水质监测是水质评价与水污染防治的主要依据。随着水体污染问题的日渐严重，水质监测成为经济社会可持续发展必须解决的重大问题，尤其是内陆水体，因为其水质影响到国民生产和人们的生活用水，准确、快捷的水质监测显得尤为重要。充足、优质的水资源是21世纪可持续发展战略实施的重要保障。随着社会经济的发展，水G3324国民经济和社会发展G1025的地G1313和G1328用G17246G7481G17246G12373G1998。G3内陆水体G1025的G5760G9026物G2559量G11G54G54G726G54G88G86G83G72G81G71G72G71G3G54G72G71G76G80G72G81G87G12是重要的水质G2454G6980之一，G3G54G54G993G1177可以G1328为污染物的G12046G17406G2070，其G2559G8813量的G3822G4581G11464G6521影响水体G17891G7138G5242、G8997G8990G5242、水G14406G12573G1821G4410G5627质，也影响水生生G5589G7477G1226和G8839G2487G9035G4748G5114G1926G9144变G2282G17819G12255，G4557G17829G4748G5049G12255、G9219G2487G14334G17959G5326G16786G12573G18129G1867有重要的G5859G1053，是G1114解和G12661G10714G9035G4748G1461G5699的重要依据。G17977G5875监测内陆水体G5760G9026物G2559量是G17902G17819G11752G12362水体G2465G4568G1821G16901G10317G5461与G5760G9026物G2559量之G19400的G1863G13007，并G5326G12447G5760G9026物G2465G9448G12651G8873的基G11796上G17839G15904的。G17829G5192G7481随着G20652G1821G16901G6228G7427的发展，G16780G3822G4410G13785G17839G15904G1114G5760G9026物G1821G16901G10317G5461和利用成G1699G1821G16901G1214监测内陆水G5760G9026物G2559量的G11752G12362，并G2474得G17751大的G17839展。G3本G11752G12362的G11458的G4613是利用地物G1821G16901G1214测量水体的G1821G16901G2465G4568G10587，G6980据存G1660G1849G54G52G47G6980据G5223G1025，用G57G38G13546G12255G17731G1226G17839G15904G2010G7524，并G3324G2010G7524G1821G16901G2465G4568G10587与G2528步水体G5760G9026物G2559量G1863G13007的基G11796上，利用G13491G16757G7053G8873G5326G12447G5760G9026物G2559量的G2465G9448G12651G8873，为G4570G7481利用成G1699G1821G16901G1214G6980据G1284G12651我国内陆水体G5760G9026物G2559量提供G2454考。G3二、分析国内外现状和发展趋势早G332420世纪70G5192代初G47AG81G71G54AG87G31刚刚发G4568成功，KLG72G80AG86G12573提G1998G1114用MG54G54G17977G5875G6980据G1284G12651G10317拉华湾G11DG72LAWAG81G72G3BAYG12G54G54G2559量的G13491G16757模型。随后G16780G3822G4410G13785提G1998G1114G993G2528模型G7481模拟G54G54与G17977G5875G6980据的G1863G13007，尤其G3324利用NOAAAG57HRRG7481获G2474G54G54的G2559量G7053面G1328G1114大量的G5049G1328。但其11KG80的G2010辨G10587G4557G8839G2487G9035G4748G5114区域G7481说显得太粗糙，而TMG3G6980据30G80的G2010辨G10587G1867有G17751大的优势。黎夏推导G1998一个G13491一式，其形式包G2559G1114GORG71OG81表达式和负指G6980G1863G13007式G726G3（1）G3GORG71OG81G1863G13007式为RG38G54/G11ABG54G12，式G1025R为水面G1821G16901G2465G4568G10587G54为G2559G8813量ABG38为G13007G6980它是根据准单散G4568G17829似公式得到，G3324实际应用G1025用得G993G3822但G17751有名适用区G19400包括低G2559G8813量和G20652G2559G8813量区；G32（2）G3负指G6980G1863G13007式为RABG111G72DG54G12或LG81G11DG47G12ABG54，式G1025R为水面G1821G16901G2465G4568G10587G54为G2559G8813量G47为亮G5242值ABD为G13007G6980各常G6980项均由与水层内的G1821G4410G5627质，和G5760G9026颗粒粒径有G1863的G2454G6980构成G17751难准确表达G20652G2559G8813量区的G20652阶变G2282。G3利用TMG6980据，该式被应用于珠江G2487G54G54的G17977G5875定量G2010G7524G1025。TAG86G86AG81G4557G9035G4748G5114G54G54、叶绿素、黄G14406物质的卫星G17977G5875G1461G5699提G2474G17839G15904G1114深G1849的G11752G12362。G3国内G4557陆地水体的G17977G5875G11752G12362从单纯的水域识别发展到G4557水质G2454G6980G17839G15904G17977G5875监测、制图和预测。随着G4557物质G1821G16901G10317G5461G11752G12362的深G1849、G12651G8873的改G17839以及G17977G5875G6228G7427本身的G993断革新，G17977G5875监测水质从定G5627发展到定量，且可G17902G17819G17977G5875预测的水质G2454G6980种类逐渐增加，包括G5760G9026颗粒物、水体G17891G7138G5242、叶绿素A浓G5242以及溶解G5627有机物、水G1025G1849G4568与G1998G4568G1821的垂G11464衰减G13007G6980，和一G1135G13520G2524污染指G7643G3926G14841G1871G10378G5589指G6980G12573。G3G3G3G6980据G5223G6228G7427是G10628代G16757G12651机G6228G7427G1025的一个重要的G13464成G18108G2010G15是人们G3800G10714G6980据的有G6940的G5049G1867。G16757G12651机的应用G6228G7427也G5062从用G6155模式逐步G2533G4470G6155机/G3G7393G2165G3132G13605G13488模式发展G15G1237G1119G1006单G1313G4557于一G1135G6980据G5223资源G1861G1151、G6980据的G19610G1025G3800G10714与G2010G5079式G3800G10714要G8726G17246G7481G17246G20652G15而MG76G70ROG86OG73G87G3的G54G52G47G3G54G72RG89G72RG3G1328为一个优G12180的大型G1863G13007型G6980据G5223G12661G10714G13007G13491G11DBMG54G12G3G15G5062成为G16780G3822G6980据G5223应用G12255G5219G20330G17885的G6980据存G1660和G7828G13046的后G2500G6915持G15G2528G7114G57G76G86G88ALG38G3G3G25G30G3G1328为G2081G2500G5332发G5049G1867G15G1867有G4557G6980据G5223应用G6915持G1852面G15G16787问G17907G5242快G15G2356用资源G4581G12573优G9869G15并且G5203G8879应用于基于G6980据G5223应用G12255G5219G1025。G3G3G3G3G3G1821G16901G5223是存G1660各类地物的G6980据G5223。地面或大G8680G1821G16901G5223的G5326G12447G4557于成G1699G1821G16901G1214的应用G7481说是G2325G2010重要的，也是G2325G2010G17165G7114和G17165G2159的。一G7098G5326G12447G1114G1821G16901G5223，我们G4613能G3827从图G1699G12447G7053体G1025提G2474G1998G1821G16901G7366G13459并根据其G1821G16901G10317G5627与G1821G16901G5223G1025G7828G13046到的类似的G1821G16901G1582G2317G18209G3800G10714，G6226到G7380G6521G17829的G1821G16901，达到G1699G1815G2010类的G11458的G30G2528G7114也为地物G1821G16901重G5326及重G5326G1821G16901的G8616G17751G2010G7524提供G1114依据。G1821G16901G5223资G7021G7481G14270实G20576G4472或G10628G3342G1821G16901测量G6980据，G17837G1135G6980据应G6252G12651到G7588成G1699G1821G16901G1214的G10317定G8886G8585G11G1821G16901重G18331G7691G12。G13666国G3G56G54GG54G11国G4490地质G16855G7609G4628G12和G3G45G51G47G3G11NAG54AG12有内G4493G1028G4512的G1821G16901G5223。G8504G3818，成G1699G1821G16901G1214或地面G1821G16901G1214可以用于测量地面或大G8680G1821G16901，可以G1028G4512G8886G16901G5223。G3G57G38是可G16282G2282、面G2533G4557G16949的G5332发G5049G1867，其G1867有G17935G17765G8022G5577深G2063G9177G7982，G13479构G1129然，与G58G76G81G71OWG86G13546G12255G13479G2524G13051G4506的G10317G9869。G3324G57G38，DG72LG83G75G76，G57BG1972种G5332发G5191G2500G1025G57G38是G7380G9801活，功能G7380G5390大的，也是G7380难用G3921的。G57G38G10317别适G4464G13546G1901G13007G13491G17731G1226，大型的G4557G6980据实G7114G5627和稳定G5627要G8726G20652G6523制G17731G1226。G5332G6930式G6980据G5223G17842G6521G11ODBG38G12是一个G16855用G13435G6521G2487，G57G38G12573G17902G17819ODBG38G6980据源，与G54G52G47、AG70G70G72G86G86G12573G6980据G5223G17902G1461，可G5332发用G6980据G5223存G1660各种G6980据表G7696的G12544G989G7053G6980据G5223G12661G10714G13007G13491。G54G52G47G3G54G72RG89G72RG32000是G1025型G6980据G5223，G9397足G1025G4579型G1237G1006G4557G6980据与G1461G5699的存G1660要G8726。G3三、主要研究目标，实现的途径及技术路线主要的G11752G12362G11458G7643G726G33G111G12利用G17977G5875G7053G8873G17839G15904水质监测的基G11796G5049G1328是G5326G12447G993G2528污染物G2559量水体的G10317G5461G1821G16901，并由G10317G5461G1821G16901G8616G17751推G12651G5465G11752G12362水体的污染物质G2559量。水体G1025G5760G9026物质可能G8889G8813G17839G15904模拟，所以可G17751G7053便地G4557水体G1025G5760G9026物的浓G5242G17839G15904G6523制。G3G112G12G3324实G20576G4472G7477G1226下，G4570G5465测纯水G1025加G1849G993G2528G2559量的G8889G8813，形成G993G2528G5760G9026物的浓G5242的水体，测量其G1821G16901G10317G5461，得到典型浓G5242的G1821G16901G10317G5461。G3G113G12要G8726利用G54G52G47G3G54G72RG89G72RG32000G5326G12447G1821G16901G5223，熟悉G54G52G47语言的使用，能G3827G4570G3324大量G6980据存G1849G6980据G5223G1025。G3G114G12有G1114G1821G16901G5223G6980据后，要G8726利用G57G38G5332发，后G2500用G54G52G47G3G54G72RG89G72RG32000G6980据G5223保存G1821G16901G6980据和相G1863辅助G2454G6980G7481G2010G7524G1821G16901G6980据。G3G115G12G4557未知G9026物浓G5242的水体，可由其G10317G5461G1821G16901利用G3822种G7053G8873和G7643准G1821G16901相G8616G17751，从而G2465G9448得G1998水体G5760G9026物G2559量，要G8726G18331用G57G38G13546G12255实G10628。G3G3实G10628的途径和主要G6228G7427路G13459G726G3G111G12G3G3324实G20576G4472G7477G1226下，G4570G5465测纯水G1025加G1849G993G2528G2559量的G8889G8813，形成G993G2528G5760G9026物的浓G5242的水体，测量其G1821G16901G10317G5461，得到典型浓G5242的G1821G16901G10317G5461。G3G112G12G3用G54G52G47G3G54G72RG89G72RG32000G5326G12447一个G6980据G5223，主要用G7481存G1660G993G2528G2559量G5760G9026物的浓G5242水体的相G1863G1461G5699和G993G2528G2559量G5760G9026物的浓G5242水体的G1821G16901G6980据G15以及其它的一G1135G6980据。G3G113G12G3把获得到的G5760G9026物水体的G1821G16901G10317G5461G6980据导G1849上面G5062经G5326G3921的G6980据G5223G1025，G7380G3921用G57G38G13546G12255实G10628G6980据的导G1849。G3G114G12G18331用G57G38G250G13546G12255语言G7481实G10628相G1863功能，利用ODBG38G3驱动G12255G5219G7481与G54G52G47G3G54G72RG89G72RG6980据G5223G17839G15904G17842G6521，G17839G15904G6980据的读G2474G1901G1849。G3G115G12用G57G38G13546G12255实G10628G993G2528G2559量G5760G9026物的浓G5242的G1821G16901G10317G5461G7366G13459的显G12046，显G12046其它的一G1135相G1863G1461G5699。G3G11G25G12模拟一G7477G1821G16901G10317G5461G7366G13459，用G57G38G13546G12255实G10628从G54G52G47G3G54G72RG89G72RG6980据G5223G1025G16855G1849G6980据G17839G15904G2317G18209，看是否存G3324相G1863的G6980据与之符G2524。G3G117G12利用G1821G16901G6980据和G7643准G1821G16901相G8616G17751G17839G15904G2465G9448，推G1998当G2081G1821G16901G6980据的相G1863G1821G16901G1461G5699，从而获G2474水体G5760G9026物G2559量。G3四、工作的主要阶段，进度及完成时间G12544一阶G8585（1G3G34周）G726收G19610资G7021G15G10714论G4410习G3G12544二阶G8585（5G3G37周）G726熟悉G57G38G5332发环境和G54G52G47G3G54G72RG89G72RG32000G6980据G5223G15实G20576，收G19610G1821G16901资G7021G3G12544G989阶G8585（8G310周）G726完成G17731G1226G5332发G5049G1328G3G12544四阶G8585（111G25周）G726撰G1901论文G15答辩G3I目录A1A2IA3A0A4A0A4A6A7111A5A8A9A10A11A12112A13A14A15A5A8A16A17213A18A19A20A21A22A23A24A25A26A27A28314A29A30A31A32A33A34A354A36A37A38A37A38A39A40A41A42A43A44A45A46A47A48A49A50A51A52A53A54A55A56A57A39A40A41A42A44A45A48A49A51A52A53A54521A58A59A60A61A62A63A64A65A66A67A68A69A70A71A72522A73A74A75A65A76A77A78723A60A61A79A80A65A81A82A71A837A84A85A86A85A86A87A88A89A90A91A92A93A94A95A96A97A89A90A91A92A96A97831A98A99A100A101A102832A103A104A98A99A100A105A106933A103A104A98A99A100A105A106A107A10811A109A110A111A110A111A112A113A114A115A116A117A114A115A116A1171241A118A119A120A121A122A1231242A118A119A124A125A126A127A128A129A13016A131A132A133A132A133A112A113A114A115A134A135A134A1352051A136A137A138A139A140A141A142A1432052A136A137A138A139A144A145A146A14722A148A1492661A150A151A152A1532662A150A151A154A155A156A157A1582663A150A151A154A153A15926A160A161A162A163A161A16227A164A16528I摘要本文G3324制定G1114水体G1821G16901G1461G5699G18331G19610的测量规范后，G4557水槽G1025的G993G2528浓G5242G2559G8813水体的G2465G4568G1821G16901G10317G5461G17839G15904G1114G18331G19610和G2010G7524。根据G5062G5326G12447的一个G1821G16901G6980据G5223G12661G10714G13007G13491G15G3详细探讨G1114G1821G16901G6980据G5223G13007G13491的G6980据规范、G13479构G16786G16757、功能G13464成G12573G1863键G6228G7427问题。再G4570G1821G16901G6980据存G1660到G1821G16901G6980据G5223G1025，G17839G15904G1821G16901G7366G13459的显G12046G2010G7524。G3324G1821G16901G6980据G5223的基G11796上再G17839G15904G1821G16901G6980据的G2465G9448G5049G1328，使未知浓G5242的水体跟G5062知类别G2010G7524G8616G17751从而得到正确的类别G1461G5699。G3G1863键词G726G5760G9026G8889G8813；地物G1821G16901；G1821G16901G5223；G1821G16901G2317G18209；G1821G16901G6980据G2465G9448G3ABSTRACTTHISARTICLEWHICHHASFORMULATEDTHEWATERBODYSPECTRUMINFORMATIONGATHERINGSURVEYSTANDARD,CONTAINSTHATDIFFERENTSANDDENSITYINWATERREFLECTEDSPECTRUMCHARACTERISTICONGATHERINGANDTHEANALYSISACCORDINGTOASPECTRUMDATABASEMANAGEMENTSYSTEMWHICHHASALREADYESTABLISHED,THISARTICLEDISCUSSESTHESPECTRUMDATABASESYSTEMDATASTANDARD,THESTRUCTURALDESIGN,THEFUNCTIONCOMPOSITIONANDSOONINDETAILAFTERTHEABOVEFUNCTIONWECANSTORAGETHESPECTRUMDATAINTOTHESPECTRUMDATABASEANDCARRIESONTHESPECTRUMCURVEINTOTHEDEMONSTRATIONANALYSISBASEDONTHESPECTRUMDATABASEINVERSIONWORK,ITENABLESTHEUNKNOWNSANDDENSITYOFTHEWATERTOOBTAINTHECORRECTCATEGORYINFORMATIONWITHTHEKNOWNCATEGORYANALYSISCOMPARISONKEYWORDSSUSPENDEDSANDSPECTRALFEATURESSPECTRUMDATABASESPECTRUMMATCHSPECTRUMDATAINVERSION1第一章引言11研究背景简介水是G14270然环境G1025一个重要的因子，水的质量G11464G6521G1863G13007到人类以及G14270然环境的生存与发展。地球上的水资源总量有限，而且水资源极易受到污染，G17839一步能导致污染物的扩散与蔓延。随着我国经济的发展，水污染问题也变得日益严重，影响到G1114人类的生存和发展。G3水体G1025G5760G9026物的G2559量是重要的水质G2454G6980，尤其是G5760G9026G8889G8813的G2559量大G4579G11464G6521影响水体的G17891G7138G5242、混G8990G5242和水G14406G12573G1821G4410G5627质，也影响水体的生G5589G7477G1226和G8839G17959、G9035G4748G5114G1926G9144变G2282G17819G12255，因G8504G5760G9026G8889G8813G2559量的G16855G7609G4557G8839流、G9035G4748G5114的水质、地貌、生G5589、环境的G11752G12362以及G9035G4748G5049G12255、G9219G2487G5326G16786G12573G1867有重要的G5859G1053。常规的G16855G7609G7053G8873是用船逐G9869G18331G7691、G2010G7524，G16855G7609G17907G5242慢、周期长，且只能获得G3324G7114G19400、空G19400G2010G5079上G18129很离散的G4581量G9869的G6980据，而G8839流、G9035G4748G5114地区水流情况复杂G3822变，G5760G9026G8889G8813G2559量的G7114G19400变G2282G10587很大，G17837种G3324G7114空G2010G5079上很离散的G18331G7691G6980据，G4557G8616精G5242很差，使G11752G12362G13785难于G4557大面积水域G5760G9026G8889G8813G2559量的G2010G5079和变G2282有G17842续G5627的、G2528步的准确认识。卫星G17977G5875G6228G7427的发展使G17837一G10378况得到G1114彻底的改观。G3G17977G5875G1867有大尺G5242快G17907G2528步的G10317G9869，所获得的水体G5760G9026物影G1699，G18129是G3324G1972秒至G1972G2325秒，或更短的G7114G19400内“瞬G7114G2528步”扫描或摄制的。G17837种瞬G7114G2528步影G1699，G4557于G11752G12362水面G5760G9026G8889G8813的输移和沉降，是非常G11464观和有用的资G7021。G18331用G17977G5875定量G6228G7427能迅G17907地获得大面积水域G5760G9026物质G2559量的资G7021，瞬G19400G2528步G5627G3921，重复获G2474G6980据周期短，能有G6940地监测G5760G9026G8889G8813G2559量G2010G5079和动G5589变G2282，克G7393G1114常规G7053G8873的G993足，G1867有G2325G2010重要的G11752G12362价值。G3G17977G5875G6228G7427G1328为一种区域G5627水环境G16855G7609和监测手G8585，日益受到重G16282，北G13666和欧洲的一G1135国G4490早G5062G5332展G1114利用G14334空G17977G5875G6980据监测湖泊群内叶绿素G2010G5079的G11752G12362，为水质监测提供G1114一种有G6940的G6228G7427手G8585。水质G17977G5875监测是G17902G17819G11752G12362水体G2465G4568G1821G16901G10317G5461与水质G2454G6980浓G5242之G19400的G1863G13007，G5326G12447水质G2454G6980G2465G9448G12651G8873G17839G15904的，G1867有监测范围G5203、G17907G5242快、成本低和便于G17839G15904长期动G5589监测的优势，并且还能发G10628一G1135常规G7053G8873难以揭G12046的污染源和污染物迁移G10317G5461，与常规G7053G8873相G8616，G1867有G993可替代的优G17246G5627。G3G8616G17751而言，早期的人G5049水质监测未能克G7393本身的缺G9869，而G1867有G17751大的应用G4628限G5627。G17977G5875监测水质的G7053G8873能从G1028G4512的地面、G14334空和G14334天G17977G5875G6980G1025获G2474大面积、长期和迅G17907的水质G1461G5699，成为监测内陆湖泊、水G5223G12573水体质量的有G6940和重要手G8585。G3由于G993G2528的地物G1867有G993G2528的G1821G16901G10317G5461，G17837G5062成为利用G20652G1821G16901G17977G5875G6980据认识和识别地物、提G2474地表G1461G5699的主要思想和手G8585。G1821G16901G6980据G5223是由G20652G1821G16901成G1699G1821G16901G1214或野G3818G1821G16901G1214G3324一定G7477G1226下测得的各类地物G2465G4568G1821G16901G6980据的G19610G2524G15G4557准确地解译G17977G5875图G1699G1461G5699、快G17907地实G10628未知地物的G2317G18209、提G20652G17977G5875G2010类识别水G5191起着至G1863重要的G1328用。2因G8504G15G5326G12447地物G1821G16901G6980据G5223，运用先G17839的G16757G12651机G6228G7427G7481保存、G12661G10714和G2010G7524G17837G1135G1461G5699，是提G20652G17977G5875G1461G5699的G2010G7524G3800G10714水G5191并使其得到G20652G6940、G2524G10714应用的途径，并给人们认识、识别及G2317G18209地物提供G1114基G11796。为G1114G5326G12447一个G20652G6940实用的G20652G1821G16901G17977G5875G6980据G5223G13007G13491，G17837里我们详细探讨G1114G1821G16901G6980据G5223G13007G13491的G6980据规范、G13479构G16786G16757、功能G13464成G12573G1863键G6228G7427问题。G312国内外研究现状121G3822G1821G16901G17977G5875卫星的发展和G10628G10378G3G142701972G5192G13666国发G4568的G12544一颗地球资源卫星G11G47AG81G71G54AG871G12投G1849使用后，G17977G5875G3324G4557地观测G1025的G1328用G17246G7481G17246显著，G17977G5875实G10628G1114从单G8886G8585、单极G2282走G2533G3822G8886G8585、G3822极G2282、G3822G7114相、G3822模式发展。G3随着G8886G16901G2010辨G10587与地面G2010辨G10587的G993断提G20652，G17977G5875G3324各个领域得到G1114G5203G8879的应用。早G3324G47AG81G71G54AG871刚刚发G4568成功，G58G72G76G86BLAG87G87G3EA和YARGG72RG3HG47G12573G4613提G1998G1114用G47AG81G71G54AG871G3MG54G54G17977G5875G6980据定量G16757G12651水体G5760G9026G8889G8813G2559量的G13491G16757模型，G17837无疑是G7380早G18331用陆地卫星影G1699G17839G15904的G17977G5875定量G5049G1328之一，G8504后很G3822G4410G13785G3324G17837G7053面G17839G15904G1114很G3822实G20576，G18331用的G17977G5875G1268G5875G3132有MG54G54、TM、AG57HRR和G38G61G38G54G12573，G18331用的G7053G8873有相G1863G2010G7524、G3250G5414G2010G7524G12573G7053G8873。KLG72G80AG86G12573人提G1998G1114用MG54G54G17977G5875G6980据G1284G12651G10317拉华湾G11DG72LAWAG81G72G3BAYG12G54G54G2559量的G13491G16757模型。随后G16780G3822G4410G13785提G1998G1114G993G2528模型G7481模拟G54G54与G17977G5875G6980据的G1863G13007，尤其G3324利用NOAA/AG57HRRG7481获G2474G54G54的G2559量G7053面G1328G1114大量的G5049G1328。但其11KG80的G2010辨G10587G4557G8839G2487G9035G4748G5114区域G7481说显得太粗糙，而TMG3G6980据30G80的G2010辨G10587G1867有G17751大的优势。G3我国一G1135G11752G12362G13785从20世纪G1855G2325G5192代初期G5332G3999G3324G8851G9035地区G17839G15904G5760G9026G8889G8813G17977G5875定量G11752G12362，基于G1461G5699源及G11752G12362手G8585的限制，G13489大G18108G2010利用陆地卫星G11MG54G54，G3TM，G54G51OTG12和G8680G16949卫星G11NOAAG12G3822G7114相G17977G5875图G1699，根据G10317定区域的G10628G3342实测资G7021G11与卫星G2528步或准G2528步G12G5326G12447G13491G16757相G1863G1863G13007，提G1998G1114G2559G8813水体G2465G4568G10587或G2465G4568G2001G6980G73G11RG12G8022G5577。G17902G17819G10714论G16757G12651、G2559G8813水体G1821G16901发G4568G10587实G20576测G16809及G10628G3342G2528步测量G6980据G20576G16789相G13479G2524的G7053G8873，G2010别获G2474G1114二种G993G2528G1461G5699源的G5760G9026G8889G8813G17977G5875定量模式。198G251990G5192“G983G1128”国G4490G12197G6228G6927G1863期G19400，国G4490G9035G8927G4628G12544一G9035G8927G11752G12362所以长江G2487及黄G8839G2487G2559G8813水体为G11752G12362G4557G16949，以G9035G8927G1821G4410G10714论为基G11796，以实G20576G4472和G10628G3342测量为手G8585，着重讨论G2559G8813水体的G3278有G1821G4410G5627质、G2465G4568G10587G8886G16901G10317G5461和G7380G1351G17977G5875G8886G8585，G3324G8504基G11796上提G1998适G2524于我国G8839G2487G20652浓G5242G2559G8813水体G17977G5875定量模式和基本G12651G8873。G3G3G3G3G11458G2081，我国内陆水体水质监测G2010为G11464G6521和G19400G6521G1016种G7053G8873。G11464G6521G8873G4613是G4557要监测的湖泊G18331G19610水G7691，然后G3324实G20576G4472G17839G15904水质G2010G7524。根据G2010G7524G6980据，G18331用单一G2454G6980评价指G6980G8873或G3822G2454G6980的G13520G2524评价G8873G17839G15904评价。该G7053G8873虽然能G4557G1259G3822的水质指G7643G1582G1998精确的G2010G7524和评价，但是G17165G7114G17165G2159，G993经济；而且水G7691G18331G19610和G2010G7524的G6980量很有限，G4557于3G6984个水体而言，G17837G1135测G9869G6980据只G1867有G4628G18108和典型的代表G5859G1053。G19400G6521G8873常G16277的是利用G17977G5875的G6228G7427和G7053G8873G7481监测水体水质，G2375水质G17977G5875监测G7053G8873。G11458G2081常用的内陆水体水质G17977G5875监测是基于经G20576、G13491G16757G2010G7524或水质G2454G6980G1821G16901G10317G5461G17885G6333G17977G5875G8886G8585G6980据与地面实测水质G2454G6980G6980据G17839G15904G13491G16757G2010G7524，G5326G12447水质G2454G6980G2465G9448G12651G8873实G10628的。G3总之，国内G3818G4557G17977G5875G2465G9448G8889G8813G2559量G5062经G1582G1114很G3822的G11752G12362G5049G1328，但是G3926G1321G5326G12447一种G17902用模式，G3926G1321G17839一步提G20652模式的精G5242，G2029是很G3822G17977G5875G5049G1328G13785G1185G3324G9520G5527G11752G12362的问题。G11458G2081大G18108G2010G11752G12362是基于G4557卫星图G1699的G9796G5242值和准G2528步的G5760G9026G8889G8813之G19400G17839G15904G3250G5414G2010G7524G5326G12447定量G1863G13007，该G7053G8873还存G3324一G1135G993足；一、图G1699的G9796G5242值并G993能G11507实的代表水体G1461G5699，G8821有考G15397大G8680G12573因素G4557图G1699的影响；二，图G1699与G5760G9026G8889G8813资G7021G993G2528步，大大降低G1114模型的可G19764G5627。要有G6940的利用卫星G17977G5875提G2474G5760G9026G8889G8813的有G1863G1461G5699，G4613必须G4557G993G2528G8889G8813浓G5242水体的G1821G16901G17839G15904深G1849的G1114解，G11752G12362代表水体G1461G5699的G17977G5875G2465G4568G10587与G5760G9026G8