煤田地质与勘探
煤田地質與勘探
매전지질여감탐
COAL GEOLOGY & EXPLORATION
2013年
4期
46-49
,共4页
矿井水%水质特征%重金属%沉积物
礦井水%水質特徵%重金屬%沉積物
광정수%수질특정%중금속%침적물
mine water%water quality%heavy metal%sediment
通过对山西省马兰煤矿2号煤层采掘面在开采和封闭时期的矿井水和沉积物的研究,揭示采掘面封闭前后对矿井水水质和沉积物的影响机理。研究结果表明:马兰煤矿矿井水均为 SO4-Ca型水质,矿井水均富含 SO2-4和 Fe离子;随着上部煤层的不断开采,3处矿井水呈现相同的变化规律,矿井水的pH值升高,Eh值降低,SO2-4、Fe、Mn和Zn离子浓度随之下降,其中北一暗斜井处的矿井水水质变化最显著;矿井水水质指标和流速变化能够控制其沉积物的矿物组成和结晶程度,北一暗斜井处的沉积物在两次采样中由斯沃特曼铁矿变为针铁矿,而其他两处的矿井水沉积物矿物组分没有发生变化,主要由针铁矿组成。研究结果能够提高对老空区积水水质的预测精度,并对煤矿突水水源判识具有重要意义。
通過對山西省馬蘭煤礦2號煤層採掘麵在開採和封閉時期的礦井水和沉積物的研究,揭示採掘麵封閉前後對礦井水水質和沉積物的影響機理。研究結果錶明:馬蘭煤礦礦井水均為 SO4-Ca型水質,礦井水均富含 SO2-4和 Fe離子;隨著上部煤層的不斷開採,3處礦井水呈現相同的變化規律,礦井水的pH值升高,Eh值降低,SO2-4、Fe、Mn和Zn離子濃度隨之下降,其中北一暗斜井處的礦井水水質變化最顯著;礦井水水質指標和流速變化能夠控製其沉積物的礦物組成和結晶程度,北一暗斜井處的沉積物在兩次採樣中由斯沃特曼鐵礦變為針鐵礦,而其他兩處的礦井水沉積物礦物組分沒有髮生變化,主要由針鐵礦組成。研究結果能夠提高對老空區積水水質的預測精度,併對煤礦突水水源判識具有重要意義。
통과대산서성마란매광2호매층채굴면재개채화봉폐시기적광정수화침적물적연구,게시채굴면봉폐전후대광정수수질화침적물적영향궤리。연구결과표명:마란매광광정수균위 SO4-Ca형수질,광정수균부함 SO2-4화 Fe리자;수착상부매층적불단개채,3처광정수정현상동적변화규률,광정수적pH치승고,Eh치강저,SO2-4、Fe、Mn화Zn리자농도수지하강,기중북일암사정처적광정수수질변화최현저;광정수수질지표화류속변화능구공제기침적물적광물조성화결정정도,북일암사정처적침적물재량차채양중유사옥특만철광변위침철광,이기타량처적광정수침적물광물조분몰유발생변화,주요유침철광조성。연구결과능구제고대로공구적수수질적예측정도,병대매광돌수수원판식구유중요의의。
Quality characteristics of mine water and mineral compositions of sediments at different time from the Malan coal mines, Shanxi Province, China were investigated. The results show that water quality types of all mine water samples were SO4-Ca, and mine water samples had high concentrations of sulfate and iron. With mining of the upper coal seam, pH increased and Eh value, SO2-4 , Fe, Mn and Zn ions concentrations of mine water samples decreased. Mine water samples in three sampling sites showed the same change patterns and the most significant changes of mine water quality happened in No.1 northern inclined shaft. Mineral composition and crystalline de-gree of sediments are controlled by water quality index and velocity of mine water. The minerals of sediment in No.1 northern inclined shaft have changed form schwertmannite to goethite in twice sampling. There were no changes of mineral constituents in other two sediment sampling sites, which were composed of goethite.