摘要
煤、气、油和铀矿等多种能源矿产在沉积盆地内共存富集、成藏成矿现象普遍存在,它反映了沉积环境中有机质演化和铀等金属元素迁移、聚集成矿的地球化学过程和相互作用的结果。铀成矿与有机质的关系从化学角度看,主要有两种作用:配位作用和还原作用。煤中的腐殖酸,可以与铀通过配位作用形成配合物沉积或迁移;天然气和石油等有机烃类可以通过还原作用将高价态的铀还原成低价铀沉积成矿。在实验室条件下,我们设计了一系列的实验来模拟有机质与铀的反应。从实验模拟、测试分析和化学机理等方面进行系统的研究,可以为多种能源同盆共存的研究提供可借鉴的思想、理论和实例,具有重要的科学意义。
本文分别选取芳香有机酸来替代煤中的腐殖酸,采自鄂尔多斯盆地的天然气和石油以及不同的石油馏分为反应物,分别与铀酰离子进行成矿作用的模拟实验,证明了煤、气、油在铀成矿过程中的重要作用。
1.利用芳香有机酸来代替煤中的腐殖酸,与铀酰离子进行水热反应,模拟腐殖酸在铀成矿过程中的配位作用,得到了二十多种有机酸铀酰配合物,对它们进行了元素和红外测试分析,并对其中五种铀酰配合物进行了X-射线单晶结构的测定。
2.在低温实验条件下,将采自鄂尔多斯盆地的天然气通入到含有铀酰离子的溶液中进行还原反应,模拟天然气在铀成矿过程中所起的还原作用。将得到的产物进行了X-射线粉末衍射测试及扫描电镜分析,得到的反应产物的主要成分为UO_2。
3.在水热条件下(加入铀矿石及伴生元素,模拟鄂尔多斯盆地的实际地质环境),选取石油馏分及采自鄂尔多斯盆地不同地区的石油分别与铀酰离子进行反应,从而模拟石油在铀成矿过程中所起的还原作用,将得到的产物进行了X-射线粉末衍射测试,产物的主要成分为处于混合价态的U_3O_8、U_4O_9和U_3O_7等铀氧化物。
It is familiar that coal, natural gas, petroleum and uranium can coexist, enrich and deposit in the same sedimentary basin, which reflects the evolvement of organic matter, the geochemical evolution of uranium (e.g. transfer, enrichment and deposit) and the result of interaction in sedimentary environment. From the chemical point of view, the relationship between the uranium deposit and organic matter are coordination and reduction. The humic acids in coal could coordinate to uranium and form complexes to deposit and transfer, the high valence uranium could be reduced to the low valence uranium, which deposits to mine, by the hydrocarbons of petroleum and natural gas. In laboratory conditions, a series of experiments were designed to simulate the reaction of organic matter with uranium. Thus, investigating the reaction mechanism by experiment simulation, test analysis and chemical mechanism not only provides the useful thought, theory and example for the research on multi-energy resources minerals in one basin, but also has the important scientific significance.
Some aromatic organic acids which represent humic acids in coal, the natural gas, petroleum collected from the Ordos basin and petroleum distillate reacted with UO_2~(2+) to simulate the process of uranium mineralization. The experimentals prove the important function of coal, natural gas and petroleum in the process of uranium mineralization.
1. Some aromatic organic acids were used to represent humic acid in coal, which reacted with uranyl ion via the hydrothermal condition to simulate its coordination role. More than 20 kinds of uranyl complexes were gained and five complexes' crystal structures were determined by x-ray diffractometer.
2. In the low temperature, the natural gas reacted with uranyl solution. The main product was UO_2 which was tested by x-ray powder difrractometer.
3. The petroleum and petroleum distillate were used to react with uranyl ion. The products were tested by x-ray powder diffractometer. The main products are U_3O_8, U_4O_9 and U_3O_7 in mixed valence.
引文
[1]刘池洋,谭成仟,孙卫等,盆地多种能源矿产共存富集成藏(矿)研究进展,科学出版社,2005,1-16。
[2]仉宝聚,铀矿大型集矿区与成矿作用,铀矿地质,2001,17(1),5-17。
[3]张仁里,铀-煤共生矿的成因及矿石加工类型划分的探讨,地质论评,1984,30(1),73-76。
[4]左家和,王志明,李森,511铀矿床区域水文地质综合评价中的同位素技术研究,铀矿地质,2002,18(2),104-109。
[5]李怀渊,张守鹏,李海明,铀-油相伴性探讨,地质论评,2000,46(1),355-361。
[6]肖新建,李子颖,郭华等,俄罗斯砂岩型铀矿的新近研究进展,铀矿地质,2003,19(1),35-42。
[7]李珍媛(译),陈祖伊(校),美国过去,现在和将来的铀地浸采铀业,国外铀金地质,2000,7(4),299-306。
[8]王正邦,国外地浸砂岩型铀矿地质现状与展望,铀矿地质,2002,18(1),9-21。
[9]谈成龙,铀矿-2000,国外铀金地质,2001,18(4),187-189。
[10]张金带,徐高中,陈安平,我国可地浸砂岩型铀矿成矿模式初步探讨,铀矿地质,2005,21(3),139-145。
[11]OECD(NEA)/IAEA,Uranium 2003:Resources,Production and Demand,OECD,Paris,2004.
[12]李胜祥,陈戴生,蔡煜琦,砂岩型铀矿床分类探讨,铀矿地质,2001,17(1),285-288。
[13]Landais P.,Organic geochemistry of sedimentary uranium ore deposits,Ore Geology Views,1996,11(1),33-51.
[14]陈戴生,王瑞英,李胜祥,伊犁盆地层间氧化带砂岩型铀矿成矿模式,铀矿地质,1997,13(6),327-335。
[15]吴宏海,胡勇有,黎淑平,有机酸与矿物间界面作用研究评述,岩石矿物学杂志,2001,20(4),399-404。
[16]黄文辉,唐修义,中国煤中的铀,钍和放射性核素,中国煤田地质,2002, 14(增刊),55-63。
[17]Jackson K.S.,Johnasson I.R.,Skippen G.B.,The nature of metals-sediment-water interaction in fresh-water bodies,with emphasis on the role of organic matter,Earth-Sci.Rev.,1978,14,97-146.
[18]Baranova N.N.,Varshal G.M.,Velyukhanova T.K.,Complexing properties of natural organic compounds and their role in the origin of gold deposits,(In Russian).Geokhimiya,1991,12,1799-1804.
[19]Giordano T.H.,Kharaka Y.K.,Organic ligand distribution and speciation in sedimentary basin brines,diagenetic fluids and related ore solutions,Geol.Soc.Spec.Publ.,1994,78,175-202.
[20]Tipping E.,Hurley M.A.,A unifying model of cation binding by humic substances Geochim.Cosmochim.Acta.,1992,56(10),3627-3641.
[21]Hennet R.J.C.,Crerar D.A.,Schwartz J.,Organic complexes in hydrothermal systems.Econ.Geolo.,1988,83(4),742-764.
[22]Nayak D.C.,Varadachari C.,Ghosh K.,Influence of organic acidic functional groups of humic substances in complexation with clay minerals,Soil Sci.,1990,149,268-271.
[23]Rashid M.A.,King L.H.,Major oxygen-containing functional groups present in humic and fulvic acid fractions isolated from contrasting marine environments Geochim.Cosmochim.Acta.,1970,34(2),193-201.
[24]Szalay,匈牙利煤的研究测定铀的含量,腐殖酸化学文摘,北京:科学出版社,1982,78-86。
[25]Shanbhag P.M.,Binding of uranyl by humic acid,J.Inorg.Nucl.Chem.,1981,43(1),41-54.
[26]Moutney A.W.,Computer simulation of metal ion-humiand fulvic acid interaction,J.Soil.Sci.,1992,43,679-688.
[27]Charles S.,The roles of organic matter in the formation of uranium deposits in sedimentary rock,Ore Geology Review,1996,11(1),54-55.
[28]向伟东,陈肇博,陈祖伊等,试论有机质与后生砂岩型铀矿成矿作用:以 吐哈盆地十红滩地区为例,铀矿地质,2000,16(2),65-73。
[29]杨殿忠,陈祖伊,吐哈盆地黄腐酸与铀矿形成关系研究,铀矿地质,2002,17(2),82-86。
[30]Munier L.C.,Driam A.P.,Berthelin J.,Comparison of binding abilities of fulvic and humic acids extracted from recent marine sediments with UO_2~(2+),Ore Geochem,1986,9,285-292.
[31]涂光炽,中国层控矿床地球化学(第三卷),北京,科学出版社,1988,1-36。
[32]杨永强,翟裕生,侯玉树,沉积岩型铅锌矿床的成矿系统研究,地学前缘,2006,13(3),200-205。
[33]张复新,砂岩型铀矿与浅成低温热液矿床,刘池洋主编,盆地多种能源矿产共存富集成藏(矿)研究进展,北京:科学出版社,2005,164-171。
[34]涂光炽,高振敏,程景平,低温地球化学,北京,科学出版社,1998,1-5。
[35]王国荣,层间渗入铀成矿中有机质的氧化迁移,新疆地质,2002,20(2),134-136。
[36]刘建明,叶杰,刘家军等,盆地流体中有机组分的成矿效应,矿物岩石地球化学通报,2000,19(3),141-147。
[37]王驹,杜乐天,论铀成矿过程中的气还原作用,铀矿地质,1995,11(1),19-24。
[38]赵瑞全,秦明宽,王正邦,微生物和有机质在512层间氧化带砂岩型铀矿成矿中的作用,铀矿地质,1998,14(6),338-343。
[39]庄汉平,卢家灿,温汉捷等,热液流体中的有机物质,地质地球化学,1997,1(1),85-91。
[40]程汝楠,郭起凤,陈功等,低温低压下沥青铀矿合成试验研究,沉积学报,1983,1(3),69-77。
[41]沈才卿,赵凤民,17-115℃沥青铀矿的合成及其形成速度的实验研究,铀矿地质,1985,1(3),1-10。
[42]赵凤民,沈才卿,黄铁矿与沥青铀矿的共生条件及在沥青铀矿形成过程中所起作用的实验研究,铀矿地质,1986,2(4),193-198。
[43]胡凯,张祖还,有机质在产子坪层控型铀矿形成过程中的作用,中科院地 球化学研究所有机地球化学开放实验室年报,1987,161-168。
[44]Andreyev,Reduction of uranium by natural organic Substances,Geokhimya,1964,1(1),12-22.
[45]Andreas H.V.,Kerr P.F.,Uranium organic matter association at La Bajada,New Mexico,New Mexico Econ,1972,47(1),41-54.
[46]Nakashjma S.,Experimental study of mechanisms of fixation and reduction of uranium by sedimentary organic matter under diagentic hydrothermal conditions,Ceochim cosmochim,1984,48(4),2321-2329.
[47]Meunier,Experimental evidence of uraninite form diagensis of uranium-rich organic matter,Geochim.Cosmochim.,1981,43,41-54.
[48]杨殿忠,于漫,吐哈盆地粘土矿物特征及其与铀成矿关系,地质找矿论丛,2001,16(4),262-266。
[49]Borovec Z.,Kribek B.,Tolar V.,Sorption of uranyl by humic acids,Chemical Geology,1979,27(1),39-46.
[50]夏德长,铀矿及含铀共生矿的加工近况及展望,铀矿冶,2000,19(4),266-272。
[51]刘敏,有机质在矿床形成中的作用,河北地质学院学报,1994,17(4),367-372。
[52]王剑峰,铀地球化学教程,北京:原子能出版社,1986,380-381。
[53]张祖还,铀地球化学,北京:原子能出版社,1984,17-39。
[54]史维浚,铀水文地球化学原理,华东地质学院学报,1989,12(2),79-86。
[55]Brim H.,Mofarlan S.C.,James K.F.,Engineering deinococcus radiodurans for metal remediation in radioactive mixed waste environments,Nature,2000,18(1),85-90.
[56]Suzuki Y.,Geomicrobiology of uranium,Review in Mineralogy,1999,38(1),393-432.
[57]Min M.Z.,Luo X.Z.,Mao S.L.,et al,An excellent fossil wood cell texture with primary uranium minerals at a sandstone-hosted roll-type uranium deposit,NW China,Ore Geology Reviews,2001,17(2),233-239.
[58]Panak P.J.,Raff J.,Selenska S.P.,et al,Complex formation of U(Ⅵ)with Bacillus-isolates from a uranium mining waste pile,Radiochim Acta,2000,88(1),71-85。
[59]Tucker M.D.,Barton L.L.,Thomson M.B.,Removal of U and Mo from water by immobilized desulfovibrio desulfuficans in column reactors,Biotechnology and Engineering,1998,60,88-95。
[60]闵茂中,王汝成,边立曾等,层间氧化带砂岩型铀矿中的生物成矿作用,自然科学进展,2003,13(2),164-168。
[61]黄民生,朱锦良,微生物对水中铀的富集与还原,核技术,2002,25(2),123-131。
[62]闵茂中,彭新建,铀的微生物成矿作用研究进展,铀矿地质,2003,19(5),257-263。
[63]Liu A.,Gonzalez D.,Modeling Adsorption of Copper(Ⅱ),Cadmium(Ⅱ)and Lead(Ⅱ)on Puried Humic Acid,Langmuir,2000,16,3902-3909.
[64]Lubal P.,Fetsch D.,Iroky D.S.,Potentio-Metric and Spectroscopic Study of Uranyl Complexation with Humic Acids,Talanta,2000,51,977-991.
[65]刘正义,戚大能,512矿床可地浸砂岩铀成矿环境模拟实验,铀矿地质,2000,16(6),362-375。
[66]Kubatko K.A.,Helean K.B.,Navrotsky A.,et al,Thermodynamics of uranyl minerals:Enthalpies of formation of rutherfordine,UO_2CO_3,andersonite,Na_2CaUO_2(CO_3)_3(H_2O)_5,and grimselite,K_3NaUO_2(CO_3)_3H_2O,American Mineralogist,2005,90,1284-1290.
[67]Kubatko K.A.,Helean K.B.,Navrotsky A.,Bums P.C.,Thermodynamics of uranyl minerals:Enthalpies of formation of uranyl oxide hydrates,American Mineralogist,2006,91(4),658-666.
[68]Bums P.C.,U~(6+)Minerals and Inorganic Compounds:In sights into an Expanded Structural Hierarchy of Crystal Structures,The Canadian Mineralogist,2005,43(2),1839-1894.
[69]Kubatko K.A.H.,Helean K.B.,Navrotsky A.,et al,Stability of Peroxide-Containing Uranyl Minerals,Science,2003,302(5648),1191-1193.
[70]Matiash E.B.,碳的氢化物作为还原剂在成矿中的应用,国外铀金地质,1984,1(1),27-29。
[71]Dahlkamp F.J.,Adams S.,Geology and recognition criteria for vein-like uranium deposits of the Lower and Middle Proterozoic unconformity and stratabound type,U.S.Dept.Energy.,1981,GJBX-S(81).
[1]卜贻孙,陈明智,煤中铀与煤矿环境,1996,10(4),34-37。
[2]黄文辉,唐修义,中国煤中的铀、钍和放射性核素,中国煤田地质,2002,14(增刊),55-63。
[3]Landais P.,Organic geochemistry of sedimentary uranium ore deposits,Ore Geology Views,1996,11(1),33-51.
[4]Szalay A.,Cation exchange properties of humic acids and their importance in the geochemical enrichment of UO_2~(2+)and other cations,Geochim.Cosmochim.Acta.,1964,28(10-11),1605-1614.
[5]张仁里,铀-煤共生矿的成因及矿石加工类型划分的探讨,地质论评,1984,30(1),73-76。
[6]朱培之,高晋生,煤化学,上海,上海科学技术出版社,1984,129-133。
[7]刘德汉,盛国英,傅家谟,煤成烃的某些地球化学特征,见:中国石炭-二叠纪地层及地质学术委员会论文集,北京,科学出版社,1987,350-357。
[8]Van Krevelen D.W.,Coal(3rd ed),Amsterdam:Elsevier Publishers B.V,1993,788-792。
[9]Shinn J.H.,From Coal to Single-stage and Two-stage Products:a Reactive Model of Coal Structure,Fuel,1984,63(99),1187-1196。
[10]Wood S.A.,The role of humic substances in the transport and fixation of metals of economic interest(Au,Pt,Pd,U,V),Ore Geology Reviews,1996,11(1),1-31。
[11]Templeton G.D.,Chasteen N.D.,Vanadium-Fulvic Acid Chemistry:Conformatio- nal and Binding Studies by Electron Spin Probe Techniques,Geochim.Cosmochim.Acta.,1980,44,741-752。
[12]Wilson D.E.,Kinney P.,Effects of Polymeric Charge Variations on the Proton-metal Ion Equilibria of Humic Materials,Limnol Oceanogr,1977,22,281-289。
[13]傅家漠,贾蓉芳,刘德汉,碳酸盐有机地球化学,北京,科学出版社,1989,1-2。
[14]Geisy J.P.,Geiger R.A.,Kevem N.R.,UO_2(2+)-Humate Interactions in Soft,Acid,Humate-rich Waters,J.Environ Radioact.,1986,4(1),39-64.
[15]Lauren A.,Borkowski C.,Cahill L.,Topological Evolution in Uranyl Dicarboxylates,Synthesis and Structures of One-Dimensional UO_2(C_6H_8O_4)(H_2O)_2 and Three-Dimensional UO_2(C_6H_8O_4),Inorganic Chemistry,2003,42(22),7041-7045.
[1]秦鹏,孟志强,李彦恒等,国外多种能源矿产同盆共存富集规律初探,河北建筑科技学院学报,2005,22(3),76-78。
[2]李怀渊,张守鹏,李海明,铀-油相伴性探讨,地质论评,2000,46(1),355-361。
[3]Saxby J.D.,The sginifciance of organci matter in ore genesis,In:Wofl,K.H.(Ed),Handbook of Strata-bound and Straitform.Ore Depostis 2,Geochemcial Sutdeis,Eslevei Amsetrdam,1976:111-133。
[4]刘埃平,钟子川,铀的地球化学特征及其在油气勘探中的应用,石油学报,1999,20(6),32-371。
[5]陈荣书,石油及天然气地质学,武汉,中国地质大学出版社,1994,105-106。
[6]王驹,杜乐天,论铀成矿过程中的气还原作用,铀矿地质,1995,11(1),19-24。
[7]余达淦,还原体(体系)与富铀矿的形成,铀矿地质,1989,5(6),343-349。
[8]张景廉,试论石油与铀矿床的相互关系,华东地质学院学报,1994,17(1),42-45。
[9]沈才卿,赵凤民,17-115℃沥青铀矿的合成及其形成速度的实验研究,铀矿地质,1985,1(3),1-10。
[10]赵凤民,沈才卿,黄铁矿与沥青铀矿的共生条件及在沥青铀矿形成过程中所起作用的实验研究,铀矿地质,1986,2(4),193-198。
[11]胡凯,张祖还,有机质在产子坪层控型铀矿形成过程中的作用,中科院地 球化学研究所有机地球化学开放实验室年报,1987,161-168。
[12]Andreyev,Reduction of uranium by natural organic Substances,Geokhimya,1964,1(1),12-22.
[13]Andreas H.V.,Kerr P.F.,Uranium organic matter association at La Bajada,New Mexico,New Mexico Econ.,1972,47(1),41-54.
[14]Nakashjma S.,Experimental study of mechanisms of fixation and reduction of uranium by sedimentary organic matter under diagentic hydrothermal conditions,Ceochim Cosmochim,1984,48(4),2321-2329.
[15]谈成龙,层间氧化砂岩型铀矿中铼的地球化学行为及找矿意义探讨,铀矿地质,2004,20(5),299-305。
[16]朱养西,汪云亮,王志畅等,东胜砂岩型铀矿微量元素地球化学特征初探,地质地球化学,2003,31(2),39-45。
[17]丁万烈,绿色蚀变带的地球化学性质及其找矿意义探讨,铀矿地质,2003,19(5),277-282。
[1]Galloway W.E.,Hobday D.K.,Terrigenous clastic depositional system:Application to petroleum,coal and uranium exploration,New York: Springer-Verlag,1989.
[2]刘埃平,钟子川,铀的地球化学特征及其在油气勘探中的应用,石油学报,1999,20(6),32-37。
[3]惠宽洋,鄂尔多斯盆地煤成气与油型气成因类型鉴别模式研究,矿物岩石,2000,20(2),43-48。
[4]黄文辉,唐修义,中国煤中的铀、钍和放射性核素,中国煤田地质,2002,14(增刊),55-63。
[5]张如良,鄂尔多斯深盆气与铀矿化关系初探,铀矿地质,2004,20(4),213-218。
[6]魏永佩,王毅,鄂尔多斯盆地多种能源矿产富集规律的比较,石油与天然气地质,2004,25(4),385-392。
[7]张景廉,试论石油与铀矿床的相互关系,华东地质学院学报,1994,17(1),42-45。
[8]白玉宝,魏远江,孙冬胜,羌塘盆地查郎拉地区中新生界沉积相研究,西安石油学院学报,2000,15(1),1-5。
[9]白玉宝,孙冬胜,羌塘盆地查郎拉地区中新生代构造特征,西安工程学院学报,1999,21,8-11。
[10]李亮,王永康,张建晔,在油气藏周围寻找砂岩型铀矿,西安石油学院学报,2001,16(5),7-10。
[11]欧光习,纪玉峰,纪敏等,石油-热卤水与砂岩型铀矿化流体的关系,中国地球物理学会第22届年会论文集,2006,442-443。
[12]王永和,焦养泉,吴立群,从铀成矿条件分析西北地区砂岩型铀矿找矿,西北地质,2007,40(1),72-81。
[13]赵军龙,谭成仟,刘池阳等,鄂尔多斯盆地油、气、煤、铀富集特征分析,石油学报,2006,27(2),58-63。
[14]李胜祥,陈戴生,蔡煜琦,砂岩型铀矿床分类探讨,铀矿地质,2001,17(5),285-288。
[15]张如良,丁万烈,努和延式铀矿床地质特征及其油田水与铀成矿作用探讨,铀矿地质,1994,10(5),257-265。
[16]李怀渊,张守鹏,李海明,铀-油相伴性探讨,地质评论,2000,46(4),355-361。
[17]赵凤民,沈才卿,黄铁矿与沥青铀矿的共生条件及在沥青铀矿形成过程中所起作用的实验研究,铀矿地质,1986,2(2),193-195。
[18]Min M.Z.,Xu H.F.,Barton L.L.,The experimental research of anaerobe Shewcenella putrefaeiens deoxidizing U(Ⅵ):applying in Chinese interlayer oxidation zone sandstone-type uranium deposit,Science in china,ser D,2004,34(2),125-129.
[19]Merkel B.,Reactive transport modeling of uranium in groundwater,Earth Science-Journal of China University of Geoseiences,2000,20(5),451-455.