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RCCZO -- Geomorphology, Soil Biogeochemistry -- Character of Aeolian Material in Reynolds Creek -- Reynolds Creek Experimental Watershed -- (2015-2018)

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Created: Feb 25, 2020 at 7:17 p.m.
Last updated: Apr 24, 2020 at 5:23 p.m.
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Our study used mass flux, particle size distribution and geochemistry to analyze variations in aeolian deposition following the Soda Fire of August 2015 in southwest Idaho.The data presented characterizes the aeolian material deposited in dust traps at a height of 2 meters above the soil surface. Mass data were collected using a microbalance, particle size distributions were analyzed using laser diffractometry, and geochemistry was analyzed using inductively coupled plasma mass spectrometry.

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Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees


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Recommended Citation Roehner, Clayton; Pierce, Jennifer; Yager, Elowyn; Glenn, Nancy F.; and Pierson, Frederick. (2019). Data Supporting the Characterization of Aeolian Material Deposited in the Reynolds Creek Experimental Watershed [Data set]. Retrieved from
BSU ScholarWorks Link


Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
National Science Foundation Rapid Grant: An Integrated Study of Post-fire Wind and Water Erosion in Western Rangelands 1600816


People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.

Name Organization Address Phone Author Identifiers
USDA-ARS Northwest Watershed Research Center Reynolds Creek Experimental Watershed
Reynolds Creek Critical Zone Observatory
Boise State University

How to Cite

Roehner, C., J. Pierce, E. Yager, N. F. Glenn, F. Pierson (2020). RCCZO -- Geomorphology, Soil Biogeochemistry -- Character of Aeolian Material in Reynolds Creek -- Reynolds Creek Experimental Watershed -- (2015-2018), HydroShare,

This resource is shared under the Creative Commons Attribution CC BY.


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