中国煤炭地质
中國煤炭地質
중국매탄지질
COAL GEOLOGY OF CHINA
2013年
9期
25-29
,共5页
李灿%唐书恒%张松航%王善博%李昭
李燦%唐書恆%張鬆航%王善博%李昭
리찬%당서항%장송항%왕선박%리소
煤层气井%产出水%化学特征%动态变化%柿庄南部%沁水盆地
煤層氣井%產齣水%化學特徵%動態變化%柿莊南部%沁水盆地
매층기정%산출수%화학특정%동태변화%시장남부%심수분지
CBM well%produced water%chemical characteristics%dynamic variation%Shizhuang south area%Qinshui Basin
以沁水盆地柿庄南部煤层气井产出水的测试数据为依据,采用统计、对比方法,系统研究了3号煤和15号煤煤层气井产出水离子成分、矿化度及pH动态变化规律。结果发现,排采210d内3号煤煤层气井产出水水型基本保持不变,而15号煤煤层气井产出水类型变化较大,由Na·Mg-Cl型逐渐过渡为Na-HCO3·Cl型。通过分析3号煤和15号煤煤层气井产出水的矿化度变化规律及原因,将15号煤煤层气井产出水的矿化度划分为三个阶段,15号煤煤层气井产出水的pH受季节变化的影响较大,表现为夏季煤层气井产出水的pH值较低,说明受大气降水的影响较严重。
以沁水盆地柿莊南部煤層氣井產齣水的測試數據為依據,採用統計、對比方法,繫統研究瞭3號煤和15號煤煤層氣井產齣水離子成分、礦化度及pH動態變化規律。結果髮現,排採210d內3號煤煤層氣井產齣水水型基本保持不變,而15號煤煤層氣井產齣水類型變化較大,由Na·Mg-Cl型逐漸過渡為Na-HCO3·Cl型。通過分析3號煤和15號煤煤層氣井產齣水的礦化度變化規律及原因,將15號煤煤層氣井產齣水的礦化度劃分為三箇階段,15號煤煤層氣井產齣水的pH受季節變化的影響較大,錶現為夏季煤層氣井產齣水的pH值較低,說明受大氣降水的影響較嚴重。
이심수분지시장남부매층기정산출수적측시수거위의거,채용통계、대비방법,계통연구료3호매화15호매매층기정산출수리자성분、광화도급pH동태변화규률。결과발현,배채210d내3호매매층기정산출수수형기본보지불변,이15호매매층기정산출수류형변화교대,유Na·Mg-Cl형축점과도위Na-HCO3·Cl형。통과분석3호매화15호매매층기정산출수적광화도변화규률급원인,장15호매매층기정산출수적광화도화분위삼개계단,15호매매층기정산출수적pH수계절변화적영향교대,표현위하계매층기정산출수적pH치교저,설명수대기강수적영향교엄중。
On the basis of CBM well produced water tested data in the Shizhuang south area, Qinshui Basin, using statistics and compar-ative methods, systematically studied ion composition, total dissolved solid and pH dynamic variation pattern of CBM well produced wa-ter from coal Nos.3 and 15. The result has found that during 210 days of drainage, water type of produced water from coal No.3 is basical-ly unchanged, while from coal No.15 changed considerably, transited from Na-Mg-Cl type to Na-HCO3-Cl type gradually. Through analyses of TDS variation pattern and causation of well produced water from coal Nos.3 and 15, divided TDS of water from coal No.15 in-to three stages, while the pH value is closely related to seasonal variation, appeared as rather low in summer, thus accounted for the im-pact from atmospheric precipitation.