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Type: | Resource | |
Storage: | The size of this resource is 174.7 MB | |
Created: | Jan 13, 2020 at 6:37 p.m. | |
Last updated: | Dec 18, 2020 at 6:47 p.m. (Metadata update) | |
Published date: | Dec 18, 2020 at 6:47 p.m. | |
DOI: | 10.4211/hs.5ecff343a4334ecbaac2825a46dc581a | |
Citation: | See how to cite this resource | |
Content types: | File Set Content |
Sharing Status: | Published |
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Views: | 1362 |
Downloads: | 18 |
+1 Votes: | Be the first one to this. |
Comments: | 1 comment |
Abstract
Porous media are ubiquitous, a key component of the water cycle and locus of many biogeochemical transformations. Mapping media architecture and interstitial flows have been challenging because of the inherent difficulty of seeing through solids. Previous works used particle image velocimetry (PIV) coupled with refractive index-matching (RIM) to quantify interstitial flows, but they were limited to specialized and often toxic fluids that precluded investigating biological processes. To address this limitation, we present a low-cost and scalable method based on RIM coupled PIV (RIM-PIV) and planar laser induced fluorescence (RIM-PLIF) to simultaneously map both media architecture and interstitial velocities. Here, we store and report the data used in "A biologically friendly, low-cost and scalable method to map permeable media architecture and interstitial flow" by Hilliard et al., 2020, in Geophysical Review Letters, DOI: 10.1029/2020GL090462
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Paper DOI | 10.1029/2020GL090462 |
Plane Identifiers | Each plane is identified by it's location in centimeters (cm), as in 12.80cm, 12.82cm, 12.84cm, etc. |
Credits
Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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Idaho Water Resources Research Institute | USGS 104b Program | |
National Science Foundation | The role of in-channel aquatic vegetation on hyporheic exchange | EAR1559348 |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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