4.5 Article

Organic matter sequestered in potential energy fields predicted by 3-D clay microstructure model Direct observations of organo-clay micro- and nanofabric

期刊

MARINE GEOLOGY
卷 315, 期 -, 页码 108-114

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.margeo.2012.04.009

关键词

nanofabric; microfabric; organic matter; modeling; potential energy fields; carbon sequestering; clay microstructure; clay domains

资金

  1. National Science Foundation [SGER-0438079]
  2. NSF [OCE-0824569, OCE-0930879, OCE-0824566, OCE-0930685]
  3. Directorate For Geosciences [0824566, 0930685] Funding Source: National Science Foundation
  4. Directorate For Geosciences
  5. Division Of Ocean Sciences [0930879] Funding Source: National Science Foundation
  6. Division Of Ocean Sciences [0930685, 0824566] Funding Source: National Science Foundation

向作者/读者索取更多资源

Transmission Electron Microscopy (TEM) observations confirm theoretical predictions of the location of organic matter (OM) sequestered in fine-grained sediment. Organo-clay micro- and nanoscale fabric images validate for the first time the protective adsorption model of OM preservation. Preservation of OM against enzymatic digestion is demonstrated predominately at locations consistent with our model of the potential energy field that is developed through interactions of clay minerals, the OM, and pore water chemistry. Pores observed in 2-D fabric TEM images of clay muds commonly appear to be totally encapsulated. However, the great majority of these pores are clearly demonstrated to be open in one or more directions when observed in rotated 3-D images. Despite the scarcity of completely closed pores, OM is preserved against enzymatic attack in those locations where the predicted 3-D potential energy of interaction between clay domains and OM is attractive. (C) 2012 Elsevier B.V. All rights reserved.

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