Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
| Authors: |
|
|
|---|---|---|
| Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
| Type: | Resource | |
| Storage: | The size of this resource is 164.2 KB | |
| Created: | Nov 19, 2019 at 12:06 a.m. | |
| Last updated: | Nov 26, 2019 at 7:59 p.m. | |
| Citation: | See how to cite this resource | |
| Content types: | Single File Content |
| Sharing Status: | Public |
|---|---|
| Views: | 1407 |
| Downloads: | 112 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
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. Soil Matric Potential is measured at between 4 and 5 depths at 2 sites. Some depths may appear duplicated because another sensor was placed at the same depth, possibly at a later date/time. Matric potential is measured with 253 probes manufactured by Campbell Scientific.
Subject Keywords
Coverage
Spatial
Temporal
| Start Date: | |
|---|---|
| End Date: |
Content
ReadMe.md
SSHCZO -- Hydropedologic Properties, Matric Potential -- 253 Probes -- Shale Hills -- (2007-2014)
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. Soil Matric Potential is measured at between 4 and 5 depths at 2 sites. Some depths may appear duplicated because another sensor was placed at the same depth, possibly at a later date/time. Matric potential is measured with 253 probes manufactured by Campbell Scientific.
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|Matric Potential
Subtopic
253 Probes
Keywords
soil|water|hydrology|hydropedology|soil science|matric potential
Variables
Julian Day|Decimal time of day|253MatricPotential (kPa)|253MatricPotential (kPa)|253MatricPotential (kPa)|253MatricPotential (kPa)|253MatricPotential (kPa)
Variables ODM2
Water potential, Matric potential
TEMPORAL
Date Start
2007-01-01
Date End
2014-08-17
SPATIAL
Field Areas
Susquehanna Shale Hills Critical Zone Observatory
Location
Shale Hills
North latitude
40.6650046968
South latitude
40.6649680616
West longitude
-77.904664515
East longitude
-77.9043705198
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
2601
COMMENTS
Comments
Probe Depths at each site, in cm: Site 55: 8, 13, 38, 73, 99; Site 60: 13, 38, 13, 13
Additional Metadata
| Name | Value |
|---|---|
| czos | Shale Hills |
| czo_id | 2601 |
| 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 55: 8, 13, 38, 73, 99; Site 60: 13, 38, 13, 13 |
| keywords | soil, water, hydrology, hydropedology, soil science, matric potential |
| subtitle | Level 1 - Quality Controlled Data |
| variables | Julian Day, Decimal time of day, 253MatricPotential (kPa), 253MatricPotential (kPa), 253MatricPotential (kPa), 253MatricPotential (kPa), 253MatricPotential (kPa) |
| 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/
Comments
There are currently no comments
New Comment