对柴西洼地地下水中NO_2^-、NH_4^+成因的探讨  

INQUISTION ON CAUSE OF NO_2^- AND NFL_4^+ FORMATION IN UNDER-GROUND WATER OF LOW-LYING LAND ON CHAI WEST

作　　者：陶振德 

机构地区：[1]新疆地矿局第一水文工程地质大队

出　　处：《干旱环境监测》1990年第1期37-40,20,共5页Arid Environmental Monitoring

摘　　要：本文探讨了乌鲁木齐市东南郊柴窝堡盆地西部洼地地下水中NO_2^-、NH_4^+的成因,偏高机理.作者提出水资源利用的意见.This paper discusses the cause of NO22 and NH4+ formation in under-ground water of low-lying land on chai west(Chai is on southeast of Wulumqi) and researches mechanism of the above-mentioned ion con centration on high side. A propsal of using water resources is put forward on the paper.

关 键 词：地下水 NO₂^- NH₄⁺ 形成机理 

分 类 号：X83[环境科学与工程—环境工程]