刍论矿床水文地质学研究的基本问题——兼谈霍邱铁矿开展水文地质研究的必要性
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摘要
矿床水文地质学是水文地质学的一个分支学科,是一门涉及水文地质、工程地质、环境地质、矿床学、采矿学等多门学科内容的综合性和实用性的边缘地质学科。矿床水文地质研究的主要目的就是查明矿床水文地质条件,预测矿坑涌水量;其次是科学判别矿床地下水水源,为矿床开采提供科学依据。霍邱铁矿是华东地区第一大铁矿床,它包括大型矿床9处,累计储量近20亿吨,也是我省重要的铁矿资源产地。霍邱铁矿为一个沉积变质型的特大型矿床,由于矿体埋藏深度大、水文地质条件复杂、水量较大,开采难度较大。开展霍邱铁矿床水文地质研究,不仅可以丰富沉积变质型铁矿床地下水地球化学理论,同时可以为铁矿矿井防治水实践提供技术支持,对于铁矿井下开采的疏干工程和矿山安全生产具有重要参考价值。
The deposit hydrogeology as a branch subject of hydrogeology,it's an integrative and practical interdisciplinary field,involved in hydrogeology,engineering geology,environmental geology,deposits,mining science and some other subjects.The purpose of the hydrogeological study is to ascertain the deposit hydrogeological conditions and to predict the pit inflow of water.In addition,it can scentifically identificate groundwater source and provide scientific basis for deposit mining.Huoqiu Iron Ore is the largest iron deposit in east China which consists of 9 large-scale ore deposits,the cumulate proved reserves had reached to 20×108 t,and it is also an important resource for producing iron in Anhui.Huoqiu iron ore is a super major sedimentary-metamorphic type deposit,its orebodies buried deeply.Furthermore,its hydrogeological conditions are complicated and there are a larger quantity of groundwater,so the mining is very hard.This paper researches the hydrogeology of Huoqiu iron ore deposit,which not only enriches the hydro-geochemical theory of sedimentary-metamorphic deposit,but also provides its technical support for the groundwater prevention and treatment of iron mine,which will provide the application with very important reference value for the dewatering project and safe production of mining.
The deposit hydrogeology as a branch subject of hydrogeology,it's an integrative and practical interdisciplinary field,involved in hydrogeology,engineering geology,environmental geology,deposits,mining science and some other subjects.The purpose of the hydrogeological study is to ascertain the deposit hydrogeological conditions and to predict the pit inflow of water.In addition,it can scentifically identificate groundwater source and provide scientific basis for deposit mining.Huoqiu Iron Ore is the largest iron deposit in east China which consists of 9 large-scale ore deposits,the cumulate proved reserves had reached to 20×108 t,and it is also an important resource for producing iron in Anhui.Huoqiu iron ore is a super major sedimentary-metamorphic type deposit,its orebodies buried deeply.Furthermore,its hydrogeological conditions are complicated and there are a larger quantity of groundwater,so the mining is very hard.This paper researches the hydrogeology of Huoqiu iron ore deposit,which not only enriches the hydro-geochemical theory of sedimentary-metamorphic deposit,but also provides its technical support for the groundwater prevention and treatment of iron mine,which will provide the application with very important reference value for the dewatering project and safe production of mining.
引文
[1]张人权,梁杏,靳孟贵,等.当代水文地质学发展趋势与对策[J].水文地质工程地质,2005,(1):51-56.
[2]孙枢,李晓波.我国资源与环境科学近期发展战略雏议[J].地球科学进展,2001,67(5):726-733.
[3]王大纯,张人权,史毅红,等.水文地质学基础[M].北京:地质出版社,1995.
[4]陈梦熊,马凤山.中国地下水资源与环境[M].北京:地震出版社,2002.
[5]桂和荣,陈陆望.矿区地下水水文地球化学演化与识别[M].北京:地质出版社,2007.
[6](德)B.J.Merkel,B.Planer-Friedrich.地下水地球化学模拟的原理及应用[M].朱义年,王焰新,译.武汉:中国地质大学出版社,2005.
[7]Ian D.Clark,Peter Fritz.水文地质学中的环境同位素[M].张慧,张新基,等,译.郑州:黄河水利出版社,2006.
[8]王立志.王窑铁矿地下水研究[D].西安:西安建筑科技大学(硕士学位论文),2009.
[9]田开铭,陈铭佑.裂隙水偏流[M]北京:学苑出版社,1989.
[10]田开铭,万力.各向异性裂隙介质渗透性的研究与评价[M].北京:学苑出版社,1989.
[11]张有天.裂隙岩体渗流数学模型研究现状[R].北京:水利水电科学研究院结构材料所,1989.
[12]Snow D T.Rock Fracture Specings,Openings,and Porosi-ties[J].Journal of thd Soil Mechanics and Foundations Di-vision,1968,94(1):73-92.
[13]庄稼.环境同位素方法在判定矿井水源中的应用[J].中国煤田地质,1997,9(2):48-49.
[14]Barth S R.Stable Isotope Geochemistry of Sedi ment-hosted Groundwater From a Late Paleozoic-early Meso-zoic in Central Europe[J].Journal of Hydrology,2000,19(7):80-81.
[15]Darling W G,Edmunds WM,Smedley PL.Isotope Evi-dence for Palaeowaters in British Isles[J].Applied Geo-chemistry,1997,12(8):813-829.
[16]孙瑞华,李状.苏家庄铁矿水文地质条件及矿山地质环境评价[J].水文地质工程地质,2004,(5):74-77.
[17]李百贵.通过水力连通试验判断工作面水源[J].江苏煤炭,2003,(1):33-34.
[18]袁文华,桂和荣.任楼煤矿地温特征及在水源判别中的利用[J].安徽理工大学学报(自然科学版),2005,25(4):9-11.
[19]吕纯.淮南谢一矿地下水化学特征及突水水源判别El-man神经网络模型[D].合肥:合肥工业大学(硕士学位论文),2009.
[20]桂和荣,陈陆望,宋晓梅.皖北矿区地下水中氢氧稳定同位素的漂移特征[J].哈尔滨工业大学学报,2005,37(1):111-114.
[21]桂和荣,陈陆望.皖北矿区主要突水水源水文地质特征研究[J].煤炭学报,2004,29(3):323-327.
[22]陈陆望,桂和荣,殷晓曦.地下水溶解碳酸盐中碳氧稳定同位素组成特征与演化规律[J].煤炭学报,2008,33(5):537-542.
[23]孙亚军,杨国勇,郑琳.基于GIS的矿井突水水源判别系统研究[J].煤田地质与勘探,2007,35(2):34-37.
[24]崔喜.基于GIS的淮南孔集矿地下水化学特征分析及突水水源判别模型[D].合肥:合肥工业大学(硕士学位论文),2007.
[25]杨梅.基于GIS的淮南老矿区地下水环境特征及突水水源判别模型[D].合肥:合肥工业大学(硕士学位论文),2008.
[26]余克林,杨永生,章臣平.模糊综合评判法在判别矿井突水水源中的应用[J].金属矿山,2007,(3):47-50.
[27]卫文学,卢新明,施龙青.矿井出水点多水源判别方法[J].煤炭学报,2010,35(5):811-815.
[28]高艳秋.多组逐步判别分析在矿井水源判别中的应用[J].北京工业职业技术学院学报,2007,6(2):10-14.
[29]赖树钦.福建马坑矿区地下水化学成分的变化特征研究[J].福建地质,2009,28(4):320-325.
[30]张文慧.福建马坑铁矿主要充水岩层地下水水位动态特征[J].有色金属,2010,62(2):39-43.
[31]王建国.邯邢地区大水铁矿田开采对地下水环境的影响及防治[J].水资源保护,2009,25(5):98-102.
[2]孙枢,李晓波.我国资源与环境科学近期发展战略雏议[J].地球科学进展,2001,67(5):726-733.
[3]王大纯,张人权,史毅红,等.水文地质学基础[M].北京:地质出版社,1995.
[4]陈梦熊,马凤山.中国地下水资源与环境[M].北京:地震出版社,2002.
[5]桂和荣,陈陆望.矿区地下水水文地球化学演化与识别[M].北京:地质出版社,2007.
[6](德)B.J.Merkel,B.Planer-Friedrich.地下水地球化学模拟的原理及应用[M].朱义年,王焰新,译.武汉:中国地质大学出版社,2005.
[7]Ian D.Clark,Peter Fritz.水文地质学中的环境同位素[M].张慧,张新基,等,译.郑州:黄河水利出版社,2006.
[8]王立志.王窑铁矿地下水研究[D].西安:西安建筑科技大学(硕士学位论文),2009.
[9]田开铭,陈铭佑.裂隙水偏流[M]北京:学苑出版社,1989.
[10]田开铭,万力.各向异性裂隙介质渗透性的研究与评价[M].北京:学苑出版社,1989.
[11]张有天.裂隙岩体渗流数学模型研究现状[R].北京:水利水电科学研究院结构材料所,1989.
[12]Snow D T.Rock Fracture Specings,Openings,and Porosi-ties[J].Journal of thd Soil Mechanics and Foundations Di-vision,1968,94(1):73-92.
[13]庄稼.环境同位素方法在判定矿井水源中的应用[J].中国煤田地质,1997,9(2):48-49.
[14]Barth S R.Stable Isotope Geochemistry of Sedi ment-hosted Groundwater From a Late Paleozoic-early Meso-zoic in Central Europe[J].Journal of Hydrology,2000,19(7):80-81.
[15]Darling W G,Edmunds WM,Smedley PL.Isotope Evi-dence for Palaeowaters in British Isles[J].Applied Geo-chemistry,1997,12(8):813-829.
[16]孙瑞华,李状.苏家庄铁矿水文地质条件及矿山地质环境评价[J].水文地质工程地质,2004,(5):74-77.
[17]李百贵.通过水力连通试验判断工作面水源[J].江苏煤炭,2003,(1):33-34.
[18]袁文华,桂和荣.任楼煤矿地温特征及在水源判别中的利用[J].安徽理工大学学报(自然科学版),2005,25(4):9-11.
[19]吕纯.淮南谢一矿地下水化学特征及突水水源判别El-man神经网络模型[D].合肥:合肥工业大学(硕士学位论文),2009.
[20]桂和荣,陈陆望,宋晓梅.皖北矿区地下水中氢氧稳定同位素的漂移特征[J].哈尔滨工业大学学报,2005,37(1):111-114.
[21]桂和荣,陈陆望.皖北矿区主要突水水源水文地质特征研究[J].煤炭学报,2004,29(3):323-327.
[22]陈陆望,桂和荣,殷晓曦.地下水溶解碳酸盐中碳氧稳定同位素组成特征与演化规律[J].煤炭学报,2008,33(5):537-542.
[23]孙亚军,杨国勇,郑琳.基于GIS的矿井突水水源判别系统研究[J].煤田地质与勘探,2007,35(2):34-37.
[24]崔喜.基于GIS的淮南孔集矿地下水化学特征分析及突水水源判别模型[D].合肥:合肥工业大学(硕士学位论文),2007.
[25]杨梅.基于GIS的淮南老矿区地下水环境特征及突水水源判别模型[D].合肥:合肥工业大学(硕士学位论文),2008.
[26]余克林,杨永生,章臣平.模糊综合评判法在判别矿井突水水源中的应用[J].金属矿山,2007,(3):47-50.
[27]卫文学,卢新明,施龙青.矿井出水点多水源判别方法[J].煤炭学报,2010,35(5):811-815.
[28]高艳秋.多组逐步判别分析在矿井水源判别中的应用[J].北京工业职业技术学院学报,2007,6(2):10-14.
[29]赖树钦.福建马坑矿区地下水化学成分的变化特征研究[J].福建地质,2009,28(4):320-325.
[30]张文慧.福建马坑铁矿主要充水岩层地下水水位动态特征[J].有色金属,2010,62(2):39-43.
[31]王建国.邯邢地区大水铁矿田开采对地下水环境的影响及防治[J].水资源保护,2009,25(5):98-102.
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