Anoxic microsites in upland soils dominantly controlled by clay content

Keiluweit, Marco; Gee, Kaitlyn; Denney, Amanda; Fendorf, Scott

doi:10.1016/j.soilbio.2017.12.002

Title: Anoxic microsites in upland soils dominantly controlled by clay content

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Authors:

;

; Denney, Amanda; Fendorf, Scott

Publication Date:: 2018-03-01

Sponsoring Org.:: USDOE Office of Science (SC), Basic Energy Sciences (BES); USDOE Office of Science (SC), Biological and Environmental Research (BER)

OSTI Identifier:: 1548995

Grant/Contract Number:: AC02-05CH11231; FG02-13ER65542

Resource Type:: Publisher's Accepted Manuscript

Journal Name:: Soil Biology and Biochemistry

Additional Journal Information:: Journal Name: Soil Biology and Biochemistry Journal Volume: 118 Journal Issue: C; Journal ID: ISSN 0038-0717

Publisher:: Elsevier

Country of Publication:: United Kingdom

Language:: English

Citation Formats


                    Keiluweit, Marco, Gee, Kaitlyn, Denney, Amanda, and Fendorf, Scott. Anoxic microsites in upland soils dominantly controlled by clay content.  United Kingdom: N. p., 2018. 
Web.  doi:10.1016/j.soilbio.2017.12.002.

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                    Keiluweit, Marco, Gee, Kaitlyn, Denney, Amanda, & Fendorf, Scott. Anoxic microsites in upland soils dominantly controlled by clay content.  United Kingdom.  https://doi.org/10.1016/j.soilbio.2017.12.002

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                    Keiluweit, Marco, Gee, Kaitlyn, Denney, Amanda, and Fendorf, Scott. Thu .  
"Anoxic microsites in upland soils dominantly controlled by clay content".  United Kingdom.  https://doi.org/10.1016/j.soilbio.2017.12.002.

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@article{osti_1548995,

  title        = {Anoxic microsites in upland soils dominantly controlled by clay content},

  author       = {Keiluweit, Marco and Gee, Kaitlyn and Denney, Amanda and Fendorf, Scott},

  abstractNote = {},

  doi          = {10.1016/j.soilbio.2017.12.002},

  journal      = {Soil Biology and Biochemistry},

  number       = C,

  volume       = 118,

  place        = {United Kingdom},

  year         = {2018},

  month        = {3}

}

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