吉林农业大学学报
吉林農業大學學報
길임농업대학학보
JOURNAL OF JILIN AGRICUL TURAL UNIVERSITY
2014年
6期
690-696
,共7页
王瑞%卞建民%张真真%胡婧敏%李文睿
王瑞%卞建民%張真真%鬍婧敏%李文睿
왕서%변건민%장진진%호청민%리문예
地下水%水化学特征%三氮%污染%松嫩平原%哈尔滨
地下水%水化學特徵%三氮%汙染%鬆嫩平原%哈爾濱
지하수%수화학특정%삼담%오염%송눈평원%합이빈
groundwater%water chemical characteristic%3N ( NH+4,NO-3 and NO-2 )%pollution%Songnen plain%Harbin
针对松嫩平原地下水环境日益恶化,制约该区社会经济发展和生态平衡的现状,选择松嫩平原的第一大城市和松花江流经的重要城市———哈尔滨市区及其周边地区作为研究区,依据区内数年第四系潜水、第四系承压水的水样检测数据,综合运用描述性统计分析、离子比例系数法、Piper三线图示法及Kriging差值法,系统分析了该区地下水的水化学特征和农业污染现状。结果表明:研究区地下水以入渗溶滤水为主, HCO3-和Ca2+分别是地下水中较稳定的主要阴、阳离子,HCO3-Ca是主要的水化学类型;部分地区由于总硬度和Cl-、SO42-的明显升高影响地下水水质;地下水系统中离子反应主要来自于碳酸盐和硫酸盐类的风化溶解,且发生着离子交换作用;“三氮”污染超标严重且分布面积广。
針對鬆嫩平原地下水環境日益噁化,製約該區社會經濟髮展和生態平衡的現狀,選擇鬆嫩平原的第一大城市和鬆花江流經的重要城市———哈爾濱市區及其週邊地區作為研究區,依據區內數年第四繫潛水、第四繫承壓水的水樣檢測數據,綜閤運用描述性統計分析、離子比例繫數法、Piper三線圖示法及Kriging差值法,繫統分析瞭該區地下水的水化學特徵和農業汙染現狀。結果錶明:研究區地下水以入滲溶濾水為主, HCO3-和Ca2+分彆是地下水中較穩定的主要陰、暘離子,HCO3-Ca是主要的水化學類型;部分地區由于總硬度和Cl-、SO42-的明顯升高影響地下水水質;地下水繫統中離子反應主要來自于碳痠鹽和硫痠鹽類的風化溶解,且髮生著離子交換作用;“三氮”汙染超標嚴重且分佈麵積廣。
침대송눈평원지하수배경일익악화,제약해구사회경제발전화생태평형적현상,선택송눈평원적제일대성시화송화강류경적중요성시———합이빈시구급기주변지구작위연구구,의거구내수년제사계잠수、제사계승압수적수양검측수거,종합운용묘술성통계분석、리자비례계수법、Piper삼선도시법급Kriging차치법,계통분석료해구지하수적수화학특정화농업오염현상。결과표명:연구구지하수이입삼용려수위주, HCO3-화Ca2+분별시지하수중교은정적주요음、양리자,HCO3-Ca시주요적수화학류형;부분지구유우총경도화Cl-、SO42-적명현승고영향지하수수질;지하수계통중리자반응주요래자우탄산염화류산염류적풍화용해,차발생착리자교환작용;“삼담”오염초표엄중차분포면적엄。
The Songnen plain′s groundwater environment is deteriorating, and it becomes an impor?tant factor of restricting social economic development and ecological balance. The important city in Songnen plain?Harbin and its peripheral regions were selected to be the study area. Years of water testing data in Quaternary unconfined water, and Quaternary confined water were chosen, and de?scriptive statistics analysis, ion ratio coefficient of main ions, piper diagram and universal Krige were used to analyze chemical characteristics and pollution situation of groundwater. The results show that groundwater in the study area is mainly formed by lixiviation, Ca2+and HCO3-are respectively the major cation and anion, the main hydrochemical type is HCO3-Ca,and the high levels of total hardness and Cl- and SO4 2- are affecting groundwater quality. Ion reactions in the groundwater sys?tem mainly come from the weathering and dissolving of carbonate and sulphate, the ion exchange re?actions are also of common occurrence;the“3?nitrogen” pollution is serious and distributes widely.