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Abstract
The Real-Time Soil Moisture Monitoring Network provides integrated observation of water, energy and temperature in the soils of the Shale Hills Susquehanna Critical Zone Observatory watershed. Electric Conductivity is measured at between 4 and 5 depths at 13 sites. Electric conductivity is measured with HydraProbes manufactured by Stevens Instruments, and by 5TE probes manufactured by Decagon. At 2 sites (15 and 55) electric conductivity is measured with 2 loggers, which have different time stamps.
Subject Keywords
Coverage
Spatial
Temporal
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| End Date: |
Content
ReadMe.md
SSHCZO -- Hydropedologic Properties, Electrical Conductivity -- Shale Hills -- (2009-2013)
OVERVIEW
Description/Abstract
The Real-Time Soil Moisture Monitoring Network provides integrated observation of water, energy and temperature in the soils of the Shale Hills Susquehanna Critical Zone Observatory watershed. Electric Conductivity is measured at between 4 and 5 depths at 13 sites. Electric conductivity is measured with HydraProbes manufactured by Stevens Instruments, and by 5TE probes manufactured by Decagon. At 2 sites (15 and 55) electric conductivity is measured with 2 loggers, which have different time stamps.
Creator/Author
Lin, Henry
CZOs
Shale Hills
Contact
Dr. Henry Lin, Crop and Soil Science, The Pennsylvania State University, 444 Agricultural Sciences and Industries Building, University Park, PA. 814-865-6726 henry.lin@psu.edu
Subtitle
Level 1 - Quality Controlled Data
SUBJECTS
Disciplines
Soil Science / Pedology
Topics
Hydropedologic Properties|Electrical Conductivity
Keywords
soil|water|hydrology|hydropedology|soil science|soil temperature
Variables
Julian Day|Decimal Time of Day|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)|Electrical Conductivity (dS/m)
Variables ODM2
Electrical conductivity
TEMPORAL
Date Start
2009-01-01
Date End
2013-12-31
SPATIAL
Field Areas
Susquehanna Shale Hills Critical Zone Observatory
Location
Shale Hills
North latitude
40.6649680616
South latitude
40.6639684182
West longitude
-77.9068646529
East longitude
-77.904664515
REFERENCE
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.
Publications of this data
Lin, H.S., Kogelmann, W., Walker, C., and Bruns, M.A. (2006). Soil moisture patterns in a forested catchment: A hydropedological perspective. Geoderma 131:345-368. http://dx.doi.org/10.1016/j.geoderma.2005.03.013
Publications using this data
Graham, C., and Lin, H.S. (2011). Controls and Frequency of Preferential Flow Occurrence: A 175-event Analysis. Vadose Zone Journal 10:816-831 http://dx.doi.org/10.2136/vzj2010.0119
Jin, L., Andrews, D.M., Holmes, G.H., Lin, H., and Brantley, S.L. (2011). Opening the 'Black Box': Water Chemistry Reveals Hydrological Controls on Weathering in the Susquehanna Shale Hills Critical Zone Observatory . Vadose Zone Journal 10:928-942, http://dx.doi.org/10.2136/vzj2010.0133
Lin, H.S., and Zhou, X. (2008). Evidence of Subsurface Preferential Flow Using Soil Hydrologic Monitoring in the Shale Hills Catchment . European Journal of Soil Science 59:34–49. http://dx.doi.org/10.1111/j.1365-2389.2007.00988.x
Lin, H.S. (2006). Temporal stability of soil moisture spatial pattern and subsurface preferential flow pathways in the Shale Hills Catchment. Vadose Zone Journal 5:317-340. http://dx.doi.org/10.2136/vzj2005.0058
Takagi, K. and H.S. Lin. (2011). Temporal Dynamics of Soil Moisture Spatial Variability in the Shale Hills Critical Zone Observatory. Vadose Zone Journal 10:832-842, http://dx.doi.org/10.2136/vzj2010.0134
CZO ID
2602
COMMENTS
Comments
Probe Depths at each site, in cm:
Site A4: 5, 20, 36; Site 3: 10, 20, 30, 40, 50; Site 6: 60, 40, 30, 20, 10; Site 8: 10, 20, 30, 40, 50; Site 11: 11, 36, 66, 11, 24, 36, 51; Site 12: 10, 48, 81, 11, 27, 48, 64; Site 15: 5, 13, 20, 41, 41, 52, 73, 73; Site 55: 5, 8, 14, 14, 30
Additional Metadata
| Name | Value |
|---|---|
| czos | Shale Hills |
| czo_id | 2602 |
| 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. |
| comments | Probe Depths at each site, in cm: Site A4: 5, 20, 36; Site 3: 10, 20, 30, 40, 50; Site 6: 60, 40, 30, 20, 10; Site 8: 10, 20, 30, 40, 50; Site 11: 11, 36, 66, 11, 24, 36, 51; Site 12: 10, 48, 81, 11, 27, 48, 64; Site 15: 5, 13, 20, 41, 41, 52, 73, 73; Site 55: 5, 8, 14, 14, 30 |
| keywords | soil, water, hydrology, hydropedology, soil science, soil temperature |
| subtitle | Level 1 - Quality Controlled Data |
| variables | Julian Day, Decimal Time of Day, Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m), Electrical Conductivity (dS/m) |
| disciplines | Soil Science / Pedology |
Related Resources
| This resource is referenced by | Lin, H.S., Kogelmann, W., Walker, C., and Bruns, M.A. (2006). Soil moisture patterns in a forested catchment: A hydropedological perspective. Geoderma 131:345-368. http://dx.doi.org/10.1016/j.geoderma.2005.03.013 |
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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