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Wang Dazhen. MICROBIOLOGICAL CONVERSION OF SUBSTANCES AND ENERGY IN ORGANIC SEDIMENTARY REGIONS[J]. Acta Sedimentologica Sinica, 1983, 1(1): 75-85.
Citation: Wang Dazhen. MICROBIOLOGICAL CONVERSION OF SUBSTANCES AND ENERGY IN ORGANIC SEDIMENTARY REGIONS[J]. Acta Sedimentologica Sinica, 1983, 1(1): 75-85.

MICROBIOLOGICAL CONVERSION OF SUBSTANCES AND ENERGY IN ORGANIC SEDIMENTARY REGIONS

  • Received Date: 1981-12-26
  • Publish Date: 1983-03-10
  • The problems of preservation and conversion of organic substances in sedimentary regions of present water spheres, oil pools as well as coal mines were discussed with respect to energy flows, food chains of microbial ecosystems and microbiological processes of C.N.S. cycles at the same time changes of C/N in present sediments were also described in detail. It has been pointed out that in aerobic conditions, organic substances can not be preserved because microogranisms mineralize them into CO2. In anaerobic conditions, when microorganisms consume organic substances, in addition to CO2, small molecular organic and reduced inorganic products are produced. Energy is stored in them, which results in a more complex process of substance and energy conversion than that under the former condition. But both aerobic and anaerobic are present in today's sediments. ( 1 ) The range of energy source substance available for microorganisms is reduced with the decrease of oxidative abilities of electron accepters O2, NO3, SO4 and C02, thus the range and the amount of organic substance to be consumed by microorganisms become limited. It follows that food chain ( or food net ) turns more complex, which helps preserve a large amount of organic substance. ( 2 ) Energy produced by metabolates in anaerobic microorganisms, is partially transferred to sediments so as to absorb O2 and to create reduced phase, which is favourable for the preservation of organic substance. The mechanisms as mentioned above have been dealt with in detail and some instances were taken to explain the relationships and the reaction levels between microorganisms and energy conversions. In short, the types, the enriched levels of organic substances and O2 volume are the key factors for the preservation of organic substance. In addition, some microbial genus and species in oil pools and coal mines, and their roles in substance and energy conversions as well as necessary ecological conditions have also been described.
  • [1] (1) Kelley, D.P.,1978, Microbial Ecology, In "The Oil Industry and MicrobialEcosystems",Ed. Chater, K.W.A.,et al, Hey>den and San Ltd.,.12-28.

    (2) 服部勉,1978,微生物生态入门,东京大学出版社,.105-107.

    (3) Кузпецов,С,И.,1961,微生物在湖内物质循环中的作用,宋大祥译,科学出版社,.125-235.

    (4) Richards, F.A.,1965, Anoxic Basins and Fiords, In "Chemical Oceanography",Ed. Riley, J.P.,et al, Academic Press, London,.611-645,

    (5) SфrensenspirationJ.,et al, 1979, A Comparison of Oxygen, NiTitrate and Sulphate Re- Sediments,Coastal Marine Microbial Ecology, 5.105-115.

    (6) Jфrgensen, B.B.,1980, Mineralization and the Bacterial Cycling of C, N and Sin Marine Sediments, In "Contemporary Microbial Ecology Ed. Ellood. D.C.,et al, Academic Press, London,.239-252.

    (7) 王大珍等,1979,微生物在有机质转化中的地质作用,青海湖综合考查报告,科学出版社,. 233-264.

    (8) Willia m s, J.,et al, 1972, Bacteria Have Destroyed 10% of World Crudes, worldOil, 174( 2),.28-29.

    (9) Кузнецов,С.И.,1972,Геохимическая дительность микроорганизмов в мссторождеппях полезных ископаедых, Известия А Н СССР Серия Вцотогическал, Ю З,.301-313

    (10) Karavaiko,G.I.,1978, Mlicroflora of Land Microewiroarsents and It's Role in the Turover of Substances, In "Environmental Biogeochernistr-, and Geomicrob-iology,Ed. Krumbein, W.E., :1nn :arbor Science,.397-411

    (11) Кузнецов, С.И., 1967,Роль мпкроорганизцов в пробрзовапни л Разрущсн-пп месторождений пефти Известия А Н СССР Серил Впологичесгая. Иб,803-818

    (12) Traxler,R.W.,otal,1965,Action of Microorganisms on Bitaminoes Materiais:1 , Effect of Bacteria on Asphalt Viscosity ,Appl, Microbiol.,13,838-841

    (13) Traxler ,R.W.,etal,1966,Action of Microorganisms on Bituminoes Materials:2. Composition of Low Molecular weight Asphaltic Fractions Analysis,J.aPPL, Chem.,16,266-271

    (14) Rozanova,E.P.,et al,1974, Microflora of Oil Deposits"Moscow Scientific Publication

    (15) N esterov,A.I.,1976, Microflora of C oal一bearing Deposits and It's Geochemical Activity,In “Ecology and Geochmical Activity of Microorganisme’Ed。IYa-nov, M.V.,Moscow Pusbchino Publications,.164-172.

    (16) Maskalenko, E,M.,etal,1976, Microbiological oxidation of CH4in Coal,In Ecology and Geochemicai A ctivity of Microorganisms E4. lvanov. M.V., Moscow Pushehino Pnblications., 172-177
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  • Received:  1981-12-26
  • Published:  1983-03-10

MICROBIOLOGICAL CONVERSION OF SUBSTANCES AND ENERGY IN ORGANIC SEDIMENTARY REGIONS

Abstract: The problems of preservation and conversion of organic substances in sedimentary regions of present water spheres, oil pools as well as coal mines were discussed with respect to energy flows, food chains of microbial ecosystems and microbiological processes of C.N.S. cycles at the same time changes of C/N in present sediments were also described in detail. It has been pointed out that in aerobic conditions, organic substances can not be preserved because microogranisms mineralize them into CO2. In anaerobic conditions, when microorganisms consume organic substances, in addition to CO2, small molecular organic and reduced inorganic products are produced. Energy is stored in them, which results in a more complex process of substance and energy conversion than that under the former condition. But both aerobic and anaerobic are present in today's sediments. ( 1 ) The range of energy source substance available for microorganisms is reduced with the decrease of oxidative abilities of electron accepters O2, NO3, SO4 and C02, thus the range and the amount of organic substance to be consumed by microorganisms become limited. It follows that food chain ( or food net ) turns more complex, which helps preserve a large amount of organic substance. ( 2 ) Energy produced by metabolates in anaerobic microorganisms, is partially transferred to sediments so as to absorb O2 and to create reduced phase, which is favourable for the preservation of organic substance. The mechanisms as mentioned above have been dealt with in detail and some instances were taken to explain the relationships and the reaction levels between microorganisms and energy conversions. In short, the types, the enriched levels of organic substances and O2 volume are the key factors for the preservation of organic substance. In addition, some microbial genus and species in oil pools and coal mines, and their roles in substance and energy conversions as well as necessary ecological conditions have also been described.

Wang Dazhen. MICROBIOLOGICAL CONVERSION OF SUBSTANCES AND ENERGY IN ORGANIC SEDIMENTARY REGIONS[J]. Acta Sedimentologica Sinica, 1983, 1(1): 75-85.
Citation: Wang Dazhen. MICROBIOLOGICAL CONVERSION OF SUBSTANCES AND ENERGY IN ORGANIC SEDIMENTARY REGIONS[J]. Acta Sedimentologica Sinica, 1983, 1(1): 75-85.
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