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SSHCZO -- Hydropedologic Properties, Soil Moisture -- Shale Hills Model Input Soil Parameters -- Shale Hills -- (2013-2013)
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Created: | Nov 19, 2019 at 4:53 a.m. | |
Last updated: | Dec 23, 2019 at 10:50 p.m. | |
Citation: | See how to cite this resource | |
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Sharing Status: | Public |
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Abstract
From detailed soil maps of the Shale Hills CZO and measurement of five soil types at different soil horizons (see USDA Soil Survey Manual, http://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/ref/?cid=nrcs142p2_054262) these parameters have been determined which can be used for watershed model input, particularly with the Penn State Intergrated Hydrologic Model (PIHM). The first table includes total porosity, saturated vertical hydraulic conductivity, and horizontal hydraulic conductivity. The second table includes van Genuchten parameters α and β.
A Flux-PIHM wiki web page has been added (http://cataract.cee.psu.edu/PIHM/index.php/Land_Surface_Scheme:_Flux-PIHM)
The Flux-PIHM code now is also available for download at a GitHub page (https://github.com/shiyuning/PIHM-MF) for the community to use.
The Flux-PIHM EnKF system code now is available for download at a GitHub page (https://github.com/shiyuning/Flux-PIHM-EnKF-2.0) for the community to use.
Subject Keywords
Coverage
Spatial
Temporal
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Additional Metadata
Name | Value |
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czos | Shale Hills |
czo_id | 3886 |
citation | The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Shale Hills Susquehanna Critical Zone Observatory. |
keywords | Soil, soil porosity, hydraulic conductivity, soil horizon, van Genuchten parameters, numerical modeling, watersheds |
subtitle | Level 3 - Interpreted Products |
variables | Soil type, soil horizon, depth, total porosity, saturated vertical hydraulic conductivity, horizontal hydraulic conductivity, van Genuchten Alpha, van Genuchten Beta |
disciplines | Hydrology, Modeling / Computational Science, Soil Science / Pedology |
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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