煤田地质与勘探
煤田地質與勘探
매전지질여감탐
COAL GEOLOGY & EXPLORATION
2014年
6期
82-86,96
,共6页
浅层地下水%铬(Ⅵ)%污染机理%迁移预测%焦作地区
淺層地下水%鉻(Ⅵ)%汙染機理%遷移預測%焦作地區
천층지하수%락(Ⅵ)%오염궤리%천이예측%초작지구
shallow groundwater%Cr(VI)%pollution mechanism%migration prediction%Jiaozuo area
通过对焦作地区浅层地下水中铬(Ⅵ)污染物分布特征进行调查,分析了研究区浅层地下水中铬(Ⅵ)的污染机理,并运用Visual MODFLOW建立地下水流模型及溶质运移模型,模拟预测了浅层地下水中铬(Ⅵ)的迁移规律。结果表明:研究区浅层地下水铬(Ⅵ)污染严重,污染源是位于老君庙西南方向的焦作某电厂堆灰场,主要原因是露天堆放的粉煤灰中的铬(Ⅵ)污染物在长期淋滤作用下下渗污染含水层。气候条件、包气带岩性、地下水化学环境以及人为因素等也间接使浅层地下水铬(Ⅵ)浓度升高;模拟结果显示在未来的五年时间内,受地形和地下水动力场的影响,浅层地下水中铬(Ⅵ)的迁移方向与地下径流方向一致,沿大沙河水流方向上扩散速度更快,污染区域面积逐渐增大。
通過對焦作地區淺層地下水中鉻(Ⅵ)汙染物分佈特徵進行調查,分析瞭研究區淺層地下水中鉻(Ⅵ)的汙染機理,併運用Visual MODFLOW建立地下水流模型及溶質運移模型,模擬預測瞭淺層地下水中鉻(Ⅵ)的遷移規律。結果錶明:研究區淺層地下水鉻(Ⅵ)汙染嚴重,汙染源是位于老君廟西南方嚮的焦作某電廠堆灰場,主要原因是露天堆放的粉煤灰中的鉻(Ⅵ)汙染物在長期淋濾作用下下滲汙染含水層。氣候條件、包氣帶巖性、地下水化學環境以及人為因素等也間接使淺層地下水鉻(Ⅵ)濃度升高;模擬結果顯示在未來的五年時間內,受地形和地下水動力場的影響,淺層地下水中鉻(Ⅵ)的遷移方嚮與地下徑流方嚮一緻,沿大沙河水流方嚮上擴散速度更快,汙染區域麵積逐漸增大。
통과대초작지구천층지하수중락(Ⅵ)오염물분포특정진행조사,분석료연구구천층지하수중락(Ⅵ)적오염궤리,병운용Visual MODFLOW건입지하수류모형급용질운이모형,모의예측료천층지하수중락(Ⅵ)적천이규률。결과표명:연구구천층지하수락(Ⅵ)오염엄중,오염원시위우로군묘서남방향적초작모전엄퇴회장,주요원인시로천퇴방적분매회중적락(Ⅵ)오염물재장기림려작용하하삼오염함수층。기후조건、포기대암성、지하수화학배경이급인위인소등야간접사천층지하수락(Ⅵ)농도승고;모의결과현시재미래적오년시간내,수지형화지하수동력장적영향,천층지하수중락(Ⅵ)적천이방향여지하경류방향일치,연대사하수류방향상확산속도경쾌,오염구역면적축점증대。
Based on the investigation of the distribution characteristics of pollutant Cr(VI) in the shallow groun-dwater of Jiaozuo area, the paper analyzed the polluting mechanism of Cr(VI). The groundwater flow model and solute transport model were established with Visual MODFLOW software and using the model simulation, migration prediction of Cr(VI) pollutants in the shallow groundwater was accomplished. The results show that in the shallow groundwater of the study area, Cr(VI) pollution is very serious. The source of the pollution is the ashery of a power plant located in the southwest of Laojunmiao in Jiaozuo. The main pollution reason is that under the long-term leaching effect, Cr(VI) pollutants of fly ash piled up in the open air infiltrated and polluted the aquifer. The climate, the lithology of aeration zone, the groundwater chemical environment and human factors are the indirect causes of the increasing concentration of Cr(VI) of the shallow groundwater in this area. Simulation results show that in the next five years, influenced by landform and groundwater dynamic field, migration directions of Cr(VI) pollutants in the shallow groundwater are consistent with groundwater flow directions. The diffusion rate along the flow direction of Dasha river is more faster ,and the pollution area increases gradually with time.