城市地质
城市地質
성시지질
URBAN GEOLOGY
2012年
2期
27-29
,共3页
郑州北郊水源地%中深层地下水补给量%排泄量和均衡差
鄭州北郊水源地%中深層地下水補給量%排洩量和均衡差
정주북교수원지%중심층지하수보급량%배설량화균형차
Water sources in northern suburb of Zhengzhou%Balanced analysis%Medium-deep groundwater%Recharge and drainage amounts
本文在依据郑州北郊地区水文地质条件,分析了其水源地深层地下水的补给量和排泄量：中深层地下水补给量为7152m3/d,排泄量为7134m3/d,均衡差为18m3/d;开采条件下,中深层地下水的补给量为46301m3/d,排泄量为46320m3/d,均衡差为-19m3/d。
本文在依據鄭州北郊地區水文地質條件,分析瞭其水源地深層地下水的補給量和排洩量：中深層地下水補給量為7152m3/d,排洩量為7134m3/d,均衡差為18m3/d;開採條件下,中深層地下水的補給量為46301m3/d,排洩量為46320m3/d,均衡差為-19m3/d。
본문재의거정주북교지구수문지질조건,분석료기수원지심층지하수적보급량화배설량：중심층지하수보급량위7152m3/d,배설량위7134m3/d,균형차위18m3/d;개채조건하,중심층지하수적보급량위46301m3/d,배설량위46320m3/d,균형차위-19m3/d。
This paper analyzes deep groundwater recharge and drainage amounts in the northern suburb of Zhengzhou. Under the status conditions and the exploitation conditions, the hydro-geological condition analysis and balanced analysis are studied. It concludes that under the status conditions groundwater recharge amount is 7152m^3/d, drainage amount of 7134m^3/d, the balanced difference of 18 m^3/d; under the exploitation conditions, groundwater recharge amount is 46301m^3/d, drainage amount of 46320m^3/d, the balanced difference of-19m^3/d.
