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SSHCZO -- Hydropedologic Properties, Matric Potential -- MPS Probes -- Shale Hills -- (2007-2014)


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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. Soil Matric Potential is measured at between 3 and 13 depths at 10 sites. Matric potential is measured with MPS1 probes manufactured by Decagon.

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Resource Level Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Susquehanna Shale Hills Critical Zone Observatory, Shale Hills
North Latitude
40.6656°
East Longitude
-77.9038°
South Latitude
40.6642°
West Longitude
-77.9057°

Temporal

Start Date:
End Date:

Content

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SSHCZO -- Hydropedologic Properties, Matric Potential -- MPS 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 3 and 13 depths at 10 sites. Matric potential is measured with MPS1 probes manufactured by Decagon.

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

MPS Probes

Keywords

soil|water|hydrology|hydropedology|soil science|matric potential

Variables

Julian Day|Decimal Time of Day|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)|MPS Matric Potential (kPa)

Variables ODM2

Water potential, Matric potential




TEMPORAL

Date Start

2007-01-01

Date End

2014-08-18




SPATIAL

Field Areas

Susquehanna Shale Hills Critical Zone Observatory

Location

Shale Hills

North latitude

40.6655931893

South latitude

40.664180911799995

West longitude

-77.9056734264

East longitude

-77.9037753202




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

2606




COMMENTS

Comments

Probe Depths at each site, in cm: Site A4: 5, 36; Site 11: 11, 36, 66; Site 12: 10, 48, 81; Site 15: 14, 20, 41, 55, 71, 91, 94; Site 51: 6, 17, 27, 40, 70, 95, 162; Site 53: 10, 22, 42, 69, 121; Site 55: 8, 14, 41, 86, 90, 111; Site 60: 14, 41; Site 61: 12, 20, 36, 67, 85, 95, 127; Site 74: 7, 12

Additional Metadata

Name Value
subtitle Level 1 - Quality Controlled Data
disciplines Soil Science / Pedology
variables Julian Day, Decimal Time of Day, MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa), MPS Matric Potential (kPa)
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, 36; Site 11: 11, 36, 66; Site 12: 10, 48, 81; Site 15: 14, 20, 41, 55, 71, 91, 94; Site 51: 6, 17, 27, 40, 70, 95, 162; Site 53: 10, 22, 42, 69, 121; Site 55: 8, 14, 41, 86, 90, 111; Site 60: 14, 41; Site 61: 12, 20, 36, 67, 85, 95, 127; Site 74: 7, 12
keywords soil, water, hydrology, hydropedology, soil science, matric potential
czos Shale Hills
czo_id 2606

References

Related Resources

The content of this resource serves as the data for: 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

Lin, H. (2019). SSHCZO -- Hydropedologic Properties, Matric Potential -- MPS Probes -- Shale Hills -- (2007-2014), HydroShare, http://beta.hydroshare.org/resource/798ce02b8b374fc8bde80ba29258b3e8

This resource is shared under the Creative Commons Attribution CC BY.

 http://creativecommons.org/licenses/by/4.0/
CC-BY

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