AmeriFlux US-CLF Cole Farm

Davis, Kenneth J.

doi:10.17190/AMF/1987601

Title: AmeriFlux US-CLF Cole Farm

Dataset
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Abstract

This is the AmeriFlux version of the carbon flux data for the site US-CLF Cole Farm. Site Description - The Cole Farm catchment (0.65km2) is located ~ 4 km southwest of the Shale Hills site, draining orthogonally to a syncline axis of the Wills Creek Formation, a calcareous shale containing interbedded siltstone, sandstone, shaly limestone, and dolomite. Even though the farm adopted no-till practices in the 1970s, the axial channel of Cole Farm flows over a thick (>2.5 m) package of sediment in the valley floor. Soils range in texture from silty clay at the ridge top to sandy loam in the valley floor. Data was collected and funded by the Critical Zone Observatory Network.

Authors:

Davis, Kenneth J.

Department of Meteorology, Earth and Environmental Systems Institute, the Pennsylvania University

Publication Date:: Thu Jun 29 04:00:00 UTC 2023

DOE Contract Number:: AC02-05CH11231

Research Org.:: Department of Meteorology, Earth and Environmental Systems Institute, the Pennsylvania University

Sponsoring Org.:: USDOE; NSF

OSTI Identifier:: 1987601

DOI:: https://doi.org/10.17190/AMF/1987601

Citation Formats


                    Davis, Kenneth J. AmeriFlux US-CLF Cole Farm.  United States: N. p., 2023. 
        Web.  doi:10.17190/AMF/1987601.

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                    Davis, Kenneth J. AmeriFlux US-CLF Cole Farm.  United States.  doi:https://doi.org/10.17190/AMF/1987601

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                    Davis, Kenneth J. 2023.  
"AmeriFlux US-CLF Cole Farm".  United States.  doi:https://doi.org/10.17190/AMF/1987601.  https://www.osti.gov/servlets/purl/1987601. Pub date:Thu Jun 29 04:00:00 UTC 2023

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@article{osti_1987601,

  title        = {AmeriFlux US-CLF Cole Farm},

  author       = {Davis, Kenneth J.},

  abstractNote = {This is the AmeriFlux version of the carbon flux data for the site US-CLF Cole Farm. Site Description - The Cole Farm catchment (0.65km2) is located ~ 4 km southwest of the Shale Hills site, draining orthogonally to a syncline axis of the Wills Creek Formation, a calcareous shale containing interbedded siltstone, sandstone, shaly limestone, and dolomite. Even though the farm adopted no-till practices in the 1970s, the axial channel of Cole Farm flows over a thick (>2.5 m) package of sediment in the valley floor. Soils range in texture from silty clay at the ridge top to sandy loam in the valley floor. Data was collected and funded by the Critical Zone Observatory Network.},

  doi          = {10.17190/AMF/1987601},

  journal      = {},

  number       = ,

  volume       = ,

  place        = {United States},

  year         = {Thu Jun 29 04:00:00 UTC 2023},

  month        = {Thu Jun 29 04:00:00 UTC 2023}

}

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DOI: https://doi.org/10.17190/AMF/1987601

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