Micromorphology and Stable-Isotope Geochemistry of Historical Pedogenic Siderite Formed in PAH-Contaminated Alluvial Clay Soils, Tennessee, U.S.A.

@article{Driese2010MicromorphologyAS,
  title={Micromorphology and Stable-Isotope Geochemistry of Historical Pedogenic Siderite Formed in PAH-Contaminated Alluvial Clay Soils, Tennessee, U.S.A.},
  author={S. Driese and G. Ludvigson and J. A. Roberts and D. Fowle and L. Gonz{\'a}lez and J. Smith and V. Vulava and L. Mckay},
  journal={Journal of Sedimentary Research},
  year={2010},
  volume={80},
  pages={943-954}
}
Abstract Alluvial clay soil samples from six boreholes advanced to depths of 400–450 cm (top of limestone bedrock) from the Chattanooga Coke Plant (CCP) site were examined micromorphologically and geochemically in order to determine if pedogenic siderite (FeCO3) was present and whether siderite occurrence was related to organic contaminant distribution. Samples from shallow depths were generally more heavily contaminated with polycyclic aromatic hydrocarbons (PAHs) than those at greater depth… Expand
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References

SHOWING 1-10 OF 79 REFERENCES
Paleo-roothole facilitated transport of aromatic hydrocarbons through a Holocene clay bed.
  • 16
...
1
2
3
4
5
...