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Type: | Resource | |
Storage: | The size of this resource is 75.4 MB | |
Created: | Nov 19, 2019 at 2:53 a.m. | |
Last updated: | Nov 16, 2021 at 10:28 p.m. | |
Citation: | See how to cite this resource | |
Content types: | Single File Content |
Sharing Status: | Public |
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Views: | 2022 |
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Abstract
30 minute soil moisture and temperature measured in various depth for 14 pits located in the B2 desert - lower elevation site (Santa Catalina Mountains). 7 pits are located in the granite area and 7 pits are located in the schist area. Decagon EC-5 and ECT are used to measure soil moisture and temperature, respectively.
Subject Keywords
Coverage
Spatial
Temporal
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Content
Additional Metadata
Name | Value |
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czos | Catalina-Jemez |
czo_id | 2666 |
citation | The following acknowledgment should accompany any publication or citation of these data - Logistical support and/or data were provided by the NSF-supported Jemez River Basin and Santa Catalina Mountains Critical Zone Observatory EAR-0724958 and EAR-1331408. |
comments | Data are provisional and may be subject to revision. The instrumentation is maintained and data are collected by Nate Abramson, University of Arizona, nabramso@email.arizona.edu. GCSM1: Datalogger broken on 10/14/2013 and was replaced on 2/24/2014. GDSM7: Missing 7/26/2013-10/14/2013; Using Port 4 as Temp compensation for Ports 2&3. GCSM4: Datalogger broken on 6/24/2014 and was replaced on 11/4/2014. SCSM5: Missing data from 6/24/2014-8/29/2014 and 9/3/2014-12/8/2014. |
keywords | soil water, volumetric water content, VWC, soil temperature, Santa Catalina Mountains, Arizona |
subtitle | Measured soil moisture and temperature data for the B2 Desert site |
variables | Volumetric water content, Temperature |
disciplines | Soil Science / Pedology |
Credits
Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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National Science Foundation | EAR-0724958 | |
National Science Foundation | EAR-1331408 |
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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