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| Type: | Resource | |
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| Created: | Nov 19, 2019 at 6:48 a.m. (UTC) | |
| Last updated: | Nov 21, 2019 at 8:07 p.m. (UTC) | |
| Citation: | See how to cite this resource | |
| Content types: | Single File Content |
| Sharing Status: | Public |
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| Views: | 3611 |
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Abstract
Hydroinnova Cosmic-Ray Soil Moisture/Snow Sensing System (COSMOS), Model CRS-1000/B, non-invasively measures moderated neutron count among an averaged area (around 700 meters in diameter (Franz et al., 2013)), which can indirectly represent soil moisture in the top 50 cm of soil. This file includes level 1 data measured directly from COSMOS. The neutron count can be affected various elements in surroundings, where hydrogen is often the dominant one (Zreda et al., 2012). The neutron rate counted by the MOD column of COSMOS therefore can be used to determine soil moisture after a standard correction and point calibration, the results of which are COSMOS Level 2 and Level 3 data. Data collected using Hydroinnova Cosmic-Ray Soil Moisture/Snow Sensing System. Prepared to be corrected and be used to determine soil moisture.
Calibration
SM a0 a1 a2 N N0
0.1771 0.0808 0.372 0.115 1963.23 3026.79
Pressure correction parameter
L = 133
PO = 956
Date Range Comments: Data to be updated quarterly.
Subject Keywords
Coverage
Spatial
Temporal
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| End Date: |
Content
Additional Metadata
| Name | Value |
|---|---|
| czos | Shale Hills |
| czo_id | 5300 |
| citation | The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Susquehanna Shale Hills Critical Zone Observatory. |
| keywords | COSMOS, Soil Moisture |
| variables | TmStamp, RecordNum, P1_mb, T1_C, RH1, Vbat, N1Cts_MOD, N2Cts_BARE, N1ET_sec, N2ET_sec, N1T_C, N1RH, N2T_C, N2RH, MOD, N1Cts(MOD), Probe, PRESS, SCALE, SANPE, INTEN, OTHER, CORR, SM |
| disciplines | Soil Science / Pedology |
| date_range_comments | Data to be updated quarterly. |
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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