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Liu Zhili, Liu Xuexian, Li Pengfu. Mineralization Tests Made by Algae and It's Organic Matters[J]. Acta Sedimentologica Sinica, 1999, 17(1): 9-18.
Citation: Liu Zhili, Liu Xuexian, Li Pengfu. Mineralization Tests Made by Algae and It's Organic Matters[J]. Acta Sedimentologica Sinica, 1999, 17(1): 9-18.

Mineralization Tests Made by Algae and It's Organic Matters

  • Received Date: 1997-07-14
  • Rev Recd Date: 1998-08-20
  • Publish Date: 1999-03-10
  • The experimental methods of accumulation metal and mineralization by algae-bacteria are introduced as follow: I.A artificial development on large scale algal mats have been carried out in Guan-rao saltwork,Shandong Province, from 1992-1996.According to last examination on December 2,1996,the thickness of algal mats come up 2.5cm. The sediment microzones with relating redox-gradient,which are developing in the algal mats,on the test pond floors have a strong influence for the mobilization and fixation of irons and sulfide.The precipitation of inorganic calcium carbonate(CaCO3)and gypsum (CaSO4)formed in the algal mats. As a result of the decay of organic matter in the black layer,an anaerobic microenviroment appears where hydrogen sulfide(H2S) is produced by the activity of sulfate reducing bacteria. Organic matters from algal mats are divided into more than 335 compounds which could accumulate metal ions. Iron,which is bound on clay and other minerals,and which is dissolved also in the pore water,is in solution as Fe2+ underneath the black layer and precipitates as Fe3+,ferric oxide above the algal mats. In this higher productivity microenvironment of such an algal mat,the redox gradients are very high (more than 200mv Eh-difference between above and below the algal mat). Contents(‰) of some complex ions in the polysaccharide and protein from algal mats show that the Al,Ca,Fe,Mg, Sr,Zn in protein,are more than that in polysaccharide. Ⅱ.The tests of accumulating Au by algae,bacteria and fungi 1.Bacteria and Fungi Thiobacillus ferrooxiduns and Thiobacillus thiooxidans were separated from Tongling Au ore deposit.The results of culture experiment and test by X-ray-diffracterometer evidence that both generally existed in the mineral body,and from sulphate and H2SO4,changed the environment into acidity and the organic matters produced by bacteria decay could enrich the Au.The experiment made by Aspergillus niger also evidence the accumulation of Au. 2.The experimental results made by Lyngbya confercides,Spirulina platensis,Spirulina subsalsa of Cyanophyta and Chorella pyrenoidosa, Kirchneriate lunaris of Chlorophyat show that the activities of algal growth changed the blance of the ions systems CO2-HCO- 3-CO2- 3 and Ca2+-Mg2+-Na+-PO3-4-Au2+,and,resulting in the rise of pH and the drop of Eh during growth stage.The Au contents accumulated by these algae are 3.74-20.354 times of cultural liquor concentrations,after growth for three weeks. 3.Algal action on formation and deposition of phosphates. The algae used in experiment are Spirulina platensis of Cyanophyta. (1)The OD value of algal growth was determined by a Model 721 spectrophoto-meter in 560nm wavelength. (2)The pH and Eh value of algal liquor was measured by a data acquisition system connected with a Model 251 glass electrode and a saturated calomal electrode was used for comparison.The surveying system consists of a sharp PC-1500A computer with a CE-printer and a 86-4D/A convertor. (3)The determination of the PO3-4 concentration was performed with a 721 spectrophotometer connected to computerized data acquisition system. (4)The tests of accumulation of phosphorus in algal cells were made by six 2L beakers,which were divided three groups.In group (1),the K2HPO4 concentration is 0.5g/L,in group (2) it is 1.5g/L,and in group (3)it is 2.5g/L. They were cultured under the onditional illumination of 2200LX.light/dark as 16/8h. (5)Phosphorus compounds (inorganic phosphate,ATP,ADP,polyphosphate containing phosphohexose,nucleotide and phosphate ester in algal cells)were extracted (as Liu Zhi-li et al,1996). (6)Mineralogical determinations were made with a D/MAX rotating anode X-ray diffracterometer. The results show that after the algal logarthmic growth stage,the pH Value rose From 8.323 to 9.027 (average value),the Eh dropped from 0.4259V to 0.2828V.Spirulina platensis could grow in the cultural liquor that contained PO3-4 ionic concentration up to 7.25g/L.After a growth cycle of the algae,the PO3-4 concentration in the cultural liquor dropped to an absolute value,0.9g/L,and white deposits of calcium magnesium phosphate [Ca2Mg(PO4)2.2H2O] and calcium sodium carbonates[Na2Ca(CO3) 2.5H2O] were separated from bottom of the bottles.The results of simulated test of mineralization show that under the normal atmospheric temperture and presure and in the Ca2+-HPO2-4-F-HCO3 -H2O system,the polyphosphate extracted from algal cels of Spirulina subsalsa may form mineral deposits which contain mainly carbonate fluorapatite,calcite and non-crystal phosphorus. Simulated tests of algae and ist organic matters actions on formatoin and deposition of the Cu,Mn,Zn etc.also show that algae and it's organic matter have important signification in the accumulation of metal ions.
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    2 Kohring R.Biological metal accumulation in the red beds(Guetioua Member of the Bathoniac (Dogger) of Msemrir,Central High Atlas,Morocco Geologische Rundschuau,Band 81,Itern I,1992.85~90

    3 Gorjevsky D I.Action of the organic matter during formation of coloured and precious metal.《Abstracts of 29th IGC》1992,1(3):6

    4 陈其英,李菊英,封兰英.初论工业磷块岩生物成矿作用,见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社,1996.25~40

    5 陈其英,中国东部主要成矿时代的磷块岩组成.沉积学报,1987,5(3):135~148

    6 朱士兴,王观耕.中国开阳磷矿中的磷质叠层石,第五层国际磷块岩讨论会文集,北京:地质出版社,1984.141~161

    7 曾瑞骥.震旦纪叠层石与磷块岩,晚前寒武纪叠层石及相关矿产.西安:西北大学出版社,1982.105~117

    8 范德廉,叶杰,尹磊等.早期成岩过程中的微生物富锰作用以高燕碳酸锰矿床为例,见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社.1996.81~101

    9 叶连俊.生物成矿的类型、作用、过程和背景.见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社,1996.1~24

    10 李菊英.贵州息烽温泉磷矿生物化石类型及特征.见:叶连俊主编,生物有机质成矿作用.北京:北京:海洋出版社,1996.120~131

    11 李任传,张淑坤,陈锦石等.昆仑碳酸盐锰矿床的机质生物成矿作用地球化学证据和古环境的研究.见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社,1996.102~119

    12 刘文均,伊海生,温春齐.花垣铝锌矿的形成与古油气藏.见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社,1996.154~167

    13 李雅芹,蔡文六,麦伟等.细菌在铁帽型金矿形成中的作用.见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社,1996.

    14 卢家烂,傅家谟,庄汉平.有机质在铅锌矿元素迁移中的作用.见:叶连俊主编,有机质成矿作用.北京:海洋出版社,1996.

    15 卢家烂,傅家谟,刘金中等.有机质在层控锌矿床形成中的作用腐殖酸与铅锌的相互关系.见:叶连俊主编,生物成矿作用.北京:海洋出版社,1996.187~207.

    16 Maktygina V A,Razvohyeva E A,et al, Organic matter and trace elements in the metamorphism of metaplites at Khamar Daban,southwest Baykal region. Economic Geology,1992,87:325~369

    17 Liu Zhili,Liu Xuexian,Li Pengfu. Simulation Test of Algal Actione on Formation and Deposition of phosphates, In:Aspects of Piomineralization ye.Lianjun,ed.Beijing:Seismoiogical Press,China,1996.162~177

    18 Rossotti F J,Rossotti.H The Detettnination of Stahilion,Constants New York:McGraw-Hill Book Co,1961.23

    19 Hansley P L,Spirakis C S.Organic matte diagenesisas the key to aunllying theory for the geneais oftabular uranium-vanadinm deposits in the Morrison Formation,Colorado plateau.Econonic Geology,1992,87(2):352~365

    20 James R O,T Healy W.Adsorption of Hydorlyzable Metal lons at the Oxide-Water Interface I.Co(Ⅱ)Adsorption on SiO2 and TiO2 as Model Systems,.J Colloid Interface Sci 1972,40:42~52

    21 薛炽松,唐天福等.黔中陡沱期磷块岩中的微化石组合及磷酸盐化作用.见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社,1996.41~54

    22 Duhig J A,James R O,Leckie J O.Surface Ionizstion and Complexation at the Oxide-Water Interface Computaton of Electrical Double Layer Properties in Simple Electrolytes,J.Colllid InterfaceSci.1978,(63):480~499

    23 Hedetnquist J W.Matsuhisa Y Iyawa E,et al.Gelogy,Geochemisty,and Origin of High Sulfidation Cu-Au Mineralization in the Nansatsu District,Japan Econotnic Geology and the Bulletin of the Society of Economic Geologists 1994,89(1):2~4

    24 MacNaughton M G,James R O.Adsorption of Aqueous Mercury (Ⅱ) complexea at the Oxide/Water Inface J.Collold Inter face Sci.,1974,47:431~440

    25 Watterson J R.Preliminary Evidence for the Involvemenc of Budding Bacteria in the Orgin of Alaskan Placer.Gold Geology, 1992,20(4):315~318

    26 刘志礼、刘雪娴、李朋富.藻类参与铜矿形成的模拟试验,见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社,1996.198~206

    27 刘志礼、刘雪娴.几种藻聚金的对比试验,见:叶连俊主编,生物有机质成矿作用.北京:海洋出版社,1996.213~217

    28 Yin Leiming. Microbiotas of latest Precambrian sequences in Straitigraphy and Paleontology of the Systematic Boudaries in China. Precambrian-Cambrian Boundary 1.Nanjing: Nanjing University Publishing House,1987.415~494
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  • Received:  1997-07-14
  • Revised:  1998-08-20
  • Published:  1999-03-10

Mineralization Tests Made by Algae and It's Organic Matters

Abstract: The experimental methods of accumulation metal and mineralization by algae-bacteria are introduced as follow: I.A artificial development on large scale algal mats have been carried out in Guan-rao saltwork,Shandong Province, from 1992-1996.According to last examination on December 2,1996,the thickness of algal mats come up 2.5cm. The sediment microzones with relating redox-gradient,which are developing in the algal mats,on the test pond floors have a strong influence for the mobilization and fixation of irons and sulfide.The precipitation of inorganic calcium carbonate(CaCO3)and gypsum (CaSO4)formed in the algal mats. As a result of the decay of organic matter in the black layer,an anaerobic microenviroment appears where hydrogen sulfide(H2S) is produced by the activity of sulfate reducing bacteria. Organic matters from algal mats are divided into more than 335 compounds which could accumulate metal ions. Iron,which is bound on clay and other minerals,and which is dissolved also in the pore water,is in solution as Fe2+ underneath the black layer and precipitates as Fe3+,ferric oxide above the algal mats. In this higher productivity microenvironment of such an algal mat,the redox gradients are very high (more than 200mv Eh-difference between above and below the algal mat). Contents(‰) of some complex ions in the polysaccharide and protein from algal mats show that the Al,Ca,Fe,Mg, Sr,Zn in protein,are more than that in polysaccharide. Ⅱ.The tests of accumulating Au by algae,bacteria and fungi 1.Bacteria and Fungi Thiobacillus ferrooxiduns and Thiobacillus thiooxidans were separated from Tongling Au ore deposit.The results of culture experiment and test by X-ray-diffracterometer evidence that both generally existed in the mineral body,and from sulphate and H2SO4,changed the environment into acidity and the organic matters produced by bacteria decay could enrich the Au.The experiment made by Aspergillus niger also evidence the accumulation of Au. 2.The experimental results made by Lyngbya confercides,Spirulina platensis,Spirulina subsalsa of Cyanophyta and Chorella pyrenoidosa, Kirchneriate lunaris of Chlorophyat show that the activities of algal growth changed the blance of the ions systems CO2-HCO- 3-CO2- 3 and Ca2+-Mg2+-Na+-PO3-4-Au2+,and,resulting in the rise of pH and the drop of Eh during growth stage.The Au contents accumulated by these algae are 3.74-20.354 times of cultural liquor concentrations,after growth for three weeks. 3.Algal action on formation and deposition of phosphates. The algae used in experiment are Spirulina platensis of Cyanophyta. (1)The OD value of algal growth was determined by a Model 721 spectrophoto-meter in 560nm wavelength. (2)The pH and Eh value of algal liquor was measured by a data acquisition system connected with a Model 251 glass electrode and a saturated calomal electrode was used for comparison.The surveying system consists of a sharp PC-1500A computer with a CE-printer and a 86-4D/A convertor. (3)The determination of the PO3-4 concentration was performed with a 721 spectrophotometer connected to computerized data acquisition system. (4)The tests of accumulation of phosphorus in algal cells were made by six 2L beakers,which were divided three groups.In group (1),the K2HPO4 concentration is 0.5g/L,in group (2) it is 1.5g/L,and in group (3)it is 2.5g/L. They were cultured under the onditional illumination of 2200LX.light/dark as 16/8h. (5)Phosphorus compounds (inorganic phosphate,ATP,ADP,polyphosphate containing phosphohexose,nucleotide and phosphate ester in algal cells)were extracted (as Liu Zhi-li et al,1996). (6)Mineralogical determinations were made with a D/MAX rotating anode X-ray diffracterometer. The results show that after the algal logarthmic growth stage,the pH Value rose From 8.323 to 9.027 (average value),the Eh dropped from 0.4259V to 0.2828V.Spirulina platensis could grow in the cultural liquor that contained PO3-4 ionic concentration up to 7.25g/L.After a growth cycle of the algae,the PO3-4 concentration in the cultural liquor dropped to an absolute value,0.9g/L,and white deposits of calcium magnesium phosphate [Ca2Mg(PO4)2.2H2O] and calcium sodium carbonates[Na2Ca(CO3) 2.5H2O] were separated from bottom of the bottles.The results of simulated test of mineralization show that under the normal atmospheric temperture and presure and in the Ca2+-HPO2-4-F-HCO3 -H2O system,the polyphosphate extracted from algal cels of Spirulina subsalsa may form mineral deposits which contain mainly carbonate fluorapatite,calcite and non-crystal phosphorus. Simulated tests of algae and ist organic matters actions on formatoin and deposition of the Cu,Mn,Zn etc.also show that algae and it's organic matter have important signification in the accumulation of metal ions.

Liu Zhili, Liu Xuexian, Li Pengfu. Mineralization Tests Made by Algae and It's Organic Matters[J]. Acta Sedimentologica Sinica, 1999, 17(1): 9-18.
Citation: Liu Zhili, Liu Xuexian, Li Pengfu. Mineralization Tests Made by Algae and It's Organic Matters[J]. Acta Sedimentologica Sinica, 1999, 17(1): 9-18.
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