黑龍江肇州旱灌區(qū)強(qiáng)開(kāi)放邊界含水層地下水動(dòng)態(tài)監(jiān)測(cè)與分析.pdf

1、分類號(hào)UDC一密級(jí)公開(kāi)暑哦≯產(chǎn)篝碩士研究生學(xué)位論文黑龍江肇州旱灌區(qū)強(qiáng)開(kāi)放邊界含水層地下水動(dòng)態(tài)監(jiān)測(cè)與分析申請(qǐng)人：齊鵬學(xué)號(hào)：2131405培養(yǎng)單位：水利電力學(xué)院學(xué)科專業(yè)：水利工程研究方向：水文學(xué)及水資源指導(dǎo)教師：戴長(zhǎng)雷副教授李芳花教授級(jí)高工完成日期：2015年5月5日黑龍江大學(xué)碩士學(xué)位論文AbstractGroundwatermonitoringisakindofworkwhichisequippedwithbothbasicandpubl

2、icwelfareThedynamicchangeofgroundwatercanbeobservedthroughthemonitoringofgroundwaterlevelandwaterqualityandotherhydrobgicalelementsWiththerapiddevelopmentofthewholesocietydependeneeofgroundwaterexploitationisgraduallystr

3、engtheningForthesustainabledevelopmentofthesocietythegroundwatershouldbeexpb沁dreasonablyAccordingtothemeasureddepthofgroundwaterelevationofwellhead，coordinatesofwellhead，andtheoriginallyaccumulatedrmterials，andSOforththe

4、groundwaterlevelandnetinZhaozhoucountyisdynamicallyanalyzed，whichbaseontheaspectswhichcontainsdynamicchangcofsinglewellbothinoneyearandseveralyears，anddynamicchangeofwellnetbothinoneyearandseveralyearsCombinedwiththeorig

5、inaldataofHydrobgicalBt脫auofZhaozhouCOtgltythebcalaquiferisdiscussedandanab叼edFromwhathasbeendiscussedabove，thebcalaquiferhavethecharacteristicwithstrongexchangeofmaterhlandenergycycleThus，itisdefinedasslrongopenbordersa

6、quiferNetwo呔ofgroundwatermonitoringisthebasicfacilities，itslevelistheregionalone，whichcanbereplacedbycivilianwellsandproductionwellsFinallyItcanbeincludedthatperiodicchangeofundergroundwaterispresentedinZhaozhoucountyamo

7、ngyears，whichcycleisslightlydelayed，showingmorphobgyofsinglepeakandvalleyDynamictypesofgroundwaterbebn昏toinfiltrate—evaporatemodelItcanbeconcludedfromthechangesofspatialdynamicsofgroundwaterlevelbetweenayearandseveralyea

8、rs，Groundwaterexpbitationwhichincludesproductionlife，irrigationisthewainfactorsofgraduallydecreasedgroundwaterlevelinZhaozhouCoumyyearbyyearAstheeconomydevelopdramaticallythelocalgroundwaterlevelisdecliningyearbyyeareffe