日(ri)前(qian)
，蒼(cang)南(nan)縣(xian)實(shi)施(shi)完(wan)成(cheng)地(di)下(xia)水(shui)水(shui)位(wei)遠(yuan)程(cheng)自(zi)動(dong)監(jian)測(ce)
，安(an)裝(zhuang)自(zi)動(dong)化(hua)監(jian)測(ce)儀(yi)


，實(shi)現(xian)了(le)地(di)下(xia)水(shui)資(zi)源(yuan)管(guan)理(li)有(you)關(guan)信(xin)息(xi)的(de)實(shi)時(shi)收(shou)發(fa)，相(xiang)關(guan)人(ren)員(yuan)足(zu)不(bu)出(chu)戶(hu)就(jiu)可(ke)以(yi)在(zai)電(dian)腦(nao)上(shang)查(zha)看(kan)地(di)下(xia)水(shui)水(shui)量(liang)、水位的實時動態信息。 

   地(di)下(xia)水(shui)動(dong)態(tai)監(jian)測(ce)作(zuo)為(wei)地(di)質(zhi)環(huan)境(jing)監(jian)測(ce)的(de)一(yi)項(xiang)主(zhu)要(yao)內(nei)容(rong)，根(gen)據(ju)國(guo)家(jia)統(tong)一(yi)部(bu)署(shu)，自(zi)上(shang)世(shi)紀(ji)八(ba)十(shi)年(nian)代(dai)以(yi)來(lai)，蒼(cang)南(nan)縣(xian)建(jian)立(li)了(le)以(yi)江(jiang)南(nan)平(ping)原(yuan)為(wei)中(zhong)心(xin)的(de)地(di)下(xia)水(shui)動(dong)態(tai)監(jian)測(ce)網(wang)，近(jin)30年來獲取了數以十萬計的監測數據，為解決當前地下水監測方法落後、監測設備陳舊、監測成果時效性差等實際問題,縣地質環境所聯合市地質環境監測站和省地質環境監測總站，實施完成地下水水位遠程自動監測，為蒼南縣的國土整治、環境保護、地下水資源開發的研究、預防提供了大量的基礎數據。 

   cangnanxianjiangnanpingyuanshidizhizaihaidimianchenjiangzhongyifaqu。dimianchenjiangshihuanbianxingde，yidanjileidaoyidingchengdu，jiuchengweibukenizhuandepohuai。jianggeicangnanxianjiangnanpingyuanjishiwanqunzhongshenghuohejingjijianshe，dailaibukeguliang。julejie,引起地麵沉降主要原因是地下水
、天然氣、shiyoudengkaicai。ercangnanxianjiangnanpingyuangongyejiaoweifada，daliangkaicaidixiashuizaiweipingyuandiqushenghuohegongyeyongshuitigongyouxiaobaozhangdetongshi
，yezaochengdixiashuiweijijuxiajiang，tongshipohuailedimianshuiping
，dailaidimianchenjiang。kexuekaifa
、liyonghebaohudixiashuijiubixuyikaochangqidedixiashuijiance，jishizhangwodongtaibianhuaqingkuang。zhexianggongzuodekaizhanbiaozhizhecangnanxiandixiashuijiancemaishangyigexintaijie，jiangweicangnanxiandizhihuanjingguanlitigongjishizhunquedeshuju
，bingweicangnanxiandixiashuikaicai

、保護、使用提供科學依據。