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Duan Yi, Luo Bingjie, Zheng Guodong, Yang Xinghua. Chemical Properties and Geochemical Significance of Humic Acids and Kerogens in the Sediments from the Gannan Marsh[J]. Acta Sedimentologica Sinica, 1996, 14(2): 131-136.
Citation: Duan Yi, Luo Bingjie, Zheng Guodong, Yang Xinghua. Chemical Properties and Geochemical Significance of Humic Acids and Kerogens in the Sediments from the Gannan Marsh[J]. Acta Sedimentologica Sinica, 1996, 14(2): 131-136.

Chemical Properties and Geochemical Significance of Humic Acids and Kerogens in the Sediments from the Gannan Marsh

  • Rev Recd Date: 1995-06-10
  • Studied samples were collected from the Gannan marsh,southern Gansu Provice,where the climate is cold and moist,and organism consists mainly of herbs,for example,kobresia Humilis and Festuca sp. Peat distribution is wide and the mean peat thickness is about 4 m in this region. Sedimentary medium is acidic with a pH value of 5-5. 4. We here have studied chemical properties and geochemical significance of humic acids and kerogens by analyses of element and infrared spectra. Results show as follows:(1)The humic acids in the Gannan marsh sediment contain higher carbon content and lower hydro-gen and nitrogen contents as compared with those isolated from marine sediments. In-frayed spectra of humic acids in the studied samples show aromatic一rich and aliphatic一poor characteristics relative to those isolated from marine sediments. Those above indicate the features of land一marsh sedimentary enviroment. (2) With increasing depth,H/C,N/C and O/C atomic ratios and the carbohydrate content of infrared spectra for humic acids decrease,and the aromatic content of infrared spectra for humic acids increases,which shows an increase of condensation and aromaticity of humic acids with burial depth.(3) In the plot of O/C vs H/C atomic ratios,hmic acids and kerogens fall on the very im-mature region of maturation pathway of Type Ⅲ kerogen,while kerogens fall toward higher maturation than the corresponding humic acids. Infrared spectra show that kero-gens have a lower carbohydrate content and higher aromatic content relative to humic acids. Those above indicate the transformation of humic acids to kerogens,which under-ges condensation and aromaticity reactions.
  • [1] 1.Hatcher P. G.,et al,,Aliphatic structure of humic acids:a clue to their origin,Org. Geochem.1981,3 ; 43-48.

    2.Wilson M, A.,et al.,Analysis of the structure of dissolved marine humic substance and their phytoplanktonic pre-cursors by 1 H and 13 C nuclear magnetic resonance, Chem. Geoi.,1983, 10:187-201,

    3.李香兰,关山不同植被下山地普通棕壤腐殖质研究,土壤学报,1987, 24(1):27---33。

    4.Nissenbaum A.,et al,Chemical and isotopic evidence for the in situ origin of marine humic substance, Limnol.Oceanogr.,1972,17:570-582.

    5.Stuermer D. H,,et al,,Source indicators of humic substances and proto一kerogen; stable isotope ratios, elemental compositions and etection spin resonance spectra, Geochim. Cosmochim,Acta, 1978,42;989-997.

    6.王启军等,油气地球化学,武汉:中国地质大学出版社,1988, 126--142。

    7.Robin P. L.,et al.,Charactetiration of kerogens and study of their evolution by inf cared spectroscopy carbonyl and carboxyl groups, Geochim. Cosmochim.,Aeta, 1978,42;1341-1349.

    8.Pillon P.,et al.,,Qxygen一containing functional groups in land一derived humic acid- I.Changes in the cxygen distribution of humic acid during early diagenesis as revealed by derivatiaation methods,Org. Geochem.,1986, 9;
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  • Revised:  1995-06-10

Chemical Properties and Geochemical Significance of Humic Acids and Kerogens in the Sediments from the Gannan Marsh

Abstract: Studied samples were collected from the Gannan marsh,southern Gansu Provice,where the climate is cold and moist,and organism consists mainly of herbs,for example,kobresia Humilis and Festuca sp. Peat distribution is wide and the mean peat thickness is about 4 m in this region. Sedimentary medium is acidic with a pH value of 5-5. 4. We here have studied chemical properties and geochemical significance of humic acids and kerogens by analyses of element and infrared spectra. Results show as follows:(1)The humic acids in the Gannan marsh sediment contain higher carbon content and lower hydro-gen and nitrogen contents as compared with those isolated from marine sediments. In-frayed spectra of humic acids in the studied samples show aromatic一rich and aliphatic一poor characteristics relative to those isolated from marine sediments. Those above indicate the features of land一marsh sedimentary enviroment. (2) With increasing depth,H/C,N/C and O/C atomic ratios and the carbohydrate content of infrared spectra for humic acids decrease,and the aromatic content of infrared spectra for humic acids increases,which shows an increase of condensation and aromaticity of humic acids with burial depth.(3) In the plot of O/C vs H/C atomic ratios,hmic acids and kerogens fall on the very im-mature region of maturation pathway of Type Ⅲ kerogen,while kerogens fall toward higher maturation than the corresponding humic acids. Infrared spectra show that kero-gens have a lower carbohydrate content and higher aromatic content relative to humic acids. Those above indicate the transformation of humic acids to kerogens,which under-ges condensation and aromaticity reactions.

Duan Yi, Luo Bingjie, Zheng Guodong, Yang Xinghua. Chemical Properties and Geochemical Significance of Humic Acids and Kerogens in the Sediments from the Gannan Marsh[J]. Acta Sedimentologica Sinica, 1996, 14(2): 131-136.
Citation: Duan Yi, Luo Bingjie, Zheng Guodong, Yang Xinghua. Chemical Properties and Geochemical Significance of Humic Acids and Kerogens in the Sediments from the Gannan Marsh[J]. Acta Sedimentologica Sinica, 1996, 14(2): 131-136.
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