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SSHCZO -- Hydropedologic Properties, Soil Temperature -- Shale Hills -- (2007-2014)

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Created:	Nov 18, 2019 at 11:41 p.m.
Last updated:	Nov 26, 2019 at 7:59 p.m.
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Content types:	Single File Content

Sharing Status:	Public
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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 Temperature is measured at between 4 and 5 depths at 13 sites. Soil Temperature is measured with 229 probes manufactured by Campbell Scientific, and by 5TE probes manufactured by Decagon. At 2 sites (15 and 51) soil temperature is measured with 2 loggers, which have different time stamps.

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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

40.6640°

West Longitude

-77.9069°

Temporal

Start Date:
End Date:

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Additional Metadata

Name	Value
czos	Shale Hills
czo_id	2587
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.
keywords	soil, water, hydrology, hydropedology, soil science, soil temperature
subtitle	Level 1 - Quality Controlled Data
variables	Julian Day, Decimal Time of Day, Temperature (degrees C)
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

Lin, H. (2019). SSHCZO -- Hydropedologic Properties, Soil Temperature -- Shale Hills -- (2007-2014), HydroShare, http://www.hydroshare.org/resource/4939e8fe6af54a28948230774bdf055f

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

http://creativecommons.org/licenses/by/4.0/

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