中国环境科学
中國環境科學
중국배경과학
CHINA ENVIRONMENTAL SCIENCE
2014年
1期
170-177
,共8页
张亚丽%张依章%张远%孟伟%刘相超%万峻
張亞麗%張依章%張遠%孟偉%劉相超%萬峻
장아려%장의장%장원%맹위%류상초%만준
浑河%地表水%地下水%水化学%氮
渾河%地錶水%地下水%水化學%氮
혼하%지표수%지하수%수화학%담
Hun River%ground water%water chemistry%nitrate
通过分析浑河流域地表水、地下水中主要离子和不同形态氮含量,探讨了水体中水化学组成特点、各形态氮污染水平与分布特征,并采用综合指数法对流域浅层地下水水质进行了评价.结果表明,地表水水型从上游到下游由Ca-HCO3型转变为Ca-SO4型.NO3--N浓度由1.06mg/L增至6.13mg/L,NO2--N和NH4+-N仅在中游和下游地表水中检出,表明地表水在流域中下游地区受到的人为影响强烈;地下水沿流动方向水型由Ca-HCO3型依次演进为Ca-SO4和Ca-Cl型.NO3--N的含量(0.62~23.47mg/L)明显高于其在地表水中的含量.局地土地利用类型(林地、旱地、城镇用地、水田)对附近地表水体NO3--N浓度影响不显著,而旱地与水田地下水中NO3--N浓度存在显著差异,旱地地下水 NO3--N 浓度最高.浅层地下水质量评价结果显示流域浅层地下水总体质量一般,NO3--N 超出背景值1.4倍,中游地区 NO2--N 和NH4+-N污染严重,达到Ⅳ类水标准.地下水中ORP、DO、Cl-浓度和各形态氮组成特征表明由于反硝化作用,中下游地区地下水中NO3--N浓度逐渐降低,而NO2--N浓度上升到0.041mg/L.
通過分析渾河流域地錶水、地下水中主要離子和不同形態氮含量,探討瞭水體中水化學組成特點、各形態氮汙染水平與分佈特徵,併採用綜閤指數法對流域淺層地下水水質進行瞭評價.結果錶明,地錶水水型從上遊到下遊由Ca-HCO3型轉變為Ca-SO4型.NO3--N濃度由1.06mg/L增至6.13mg/L,NO2--N和NH4+-N僅在中遊和下遊地錶水中檢齣,錶明地錶水在流域中下遊地區受到的人為影響彊烈;地下水沿流動方嚮水型由Ca-HCO3型依次縯進為Ca-SO4和Ca-Cl型.NO3--N的含量(0.62~23.47mg/L)明顯高于其在地錶水中的含量.跼地土地利用類型(林地、旱地、城鎮用地、水田)對附近地錶水體NO3--N濃度影響不顯著,而旱地與水田地下水中NO3--N濃度存在顯著差異,旱地地下水 NO3--N 濃度最高.淺層地下水質量評價結果顯示流域淺層地下水總體質量一般,NO3--N 超齣揹景值1.4倍,中遊地區 NO2--N 和NH4+-N汙染嚴重,達到Ⅳ類水標準.地下水中ORP、DO、Cl-濃度和各形態氮組成特徵錶明由于反硝化作用,中下遊地區地下水中NO3--N濃度逐漸降低,而NO2--N濃度上升到0.041mg/L.
통과분석혼하류역지표수、지하수중주요리자화불동형태담함량,탐토료수체중수화학조성특점、각형태담오염수평여분포특정,병채용종합지수법대류역천층지하수수질진행료평개.결과표명,지표수수형종상유도하유유Ca-HCO3형전변위Ca-SO4형.NO3--N농도유1.06mg/L증지6.13mg/L,NO2--N화NH4+-N부재중유화하유지표수중검출,표명지표수재류역중하유지구수도적인위영향강렬;지하수연류동방향수형유Ca-HCO3형의차연진위Ca-SO4화Ca-Cl형.NO3--N적함량(0.62~23.47mg/L)명현고우기재지표수중적함량.국지토지이용류형(임지、한지、성진용지、수전)대부근지표수체NO3--N농도영향불현저,이한지여수전지하수중NO3--N농도존재현저차이,한지지하수 NO3--N 농도최고.천층지하수질량평개결과현시류역천층지하수총체질량일반,NO3--N 초출배경치1.4배,중유지구 NO2--N 화NH4+-N오염엄중,체도Ⅳ류수표준.지하수중ORP、DO、Cl-농도화각형태담조성특정표명유우반초화작용,중하유지구지하수중NO3--N농도축점강저,이NO2--N농도상승도0.041mg/L.
Hydrogeochemistry and nitrate pollution characteristics in surface water and groundwater of the Hun River basin were investigated by analyzing concentrations of the main ions and nitrogen. The results showed that the water types of the surface water changed from Ca-HCO3 to Ca-SO4 along the river while it varied from Ca-HCO3、Ca-SO4 to Ca-Cl in shallow groundwater. Concentrations of NO3--N in the surface water were increased to 6.13mg/L from the initial 1.06mg/L. However, the NO2--N and NH4+-N were only detected in the middle and lower Hun River. These results indicated that the surface water was significantly affected by anthropogenic activities. Concentration of NO3--N in groundwater was evidently higher than that in surface water. There were no significant differences of NO3--N content in surface water samples of the four land-use types (forest land, dry land, urban land and paddy field). However, significant difference for NO3--N levels in shallow groundwater were found between dry land and paddy field. Serious pollution of NO3--N, NO2--N and NH4+-N were found in shallow groundwater. In general, most of shallow groundwater samples showed medium water quality. The denitrification might exist in the shallow groundwater of the middle and lower areas based on variations of ORP, DO, Cl-and nitrate concentrations showing the content of NO3--N was decreased gradually and increase of NO2--N concents.