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SSHCZO -- Electrical Conductivity, Soil Temperature -- Garner Run -- (2018-2018)

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Created:	Nov 19, 2019 at 7:58 a.m. (UTC)
Last updated:	Dec 24, 2019 at 12:26 a.m. (UTC)
Citation:	See how to cite this resource
Content types:	Single File Content

Sharing Status:	Public
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Abstract

The Ground Hydrological Observation Gear (GroundHOG) sites in the Susquehanna Shale Hills Critical Zone Observatory provide integrated observation of water, energy, and temperature in the Garner Run field sites within the greater Shavers Creek watershed. Real and imaginary dielectric properties are measured at 3 depths; 10, 20, and 40 cm. Each of these measurements are made using HydraProbes from Stevens Instruments.

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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, Garner Run

North Latitude

40.6658°

East Longitude

-77.9040°

South Latitude

40.6644°

West Longitude

-77.9050°

Temporal

Start Date:
End Date:

Content

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Additional Metadata

Name	Value
czos	Shale Hills
czo_id	6942
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	Soil, water, hydrology, hydropedology, soil science, dielectric constant
subtitle	Garner Run - Soil Moisture, Electrical Conductivity, and Soil Temperature - Leading Ridge Mid-Slope (LRMS) Alternate Soil Pit (Level 0 Raw Data)
variables	[TmStamp], [RecNum], [SoilMoist_10_Avg], [SoilMoist_20_Avg], [SoilMoist_40_Avg], [SoilEC_T_10_Avg], [SoilEC_T_20_Avg], [SoilEC_T_40_Avg], [SoilT_C_10_Avg], [SoilT_C_20_Avg], [SoilT_C_40_Avg]
disciplines	Geochemistry / Mineralogy, Soil Science / Pedology

How to Cite

Eissenstat, D., Duncan, J., Tang, Q. (2019). SSHCZO -- Electrical Conductivity, Soil Temperature -- Garner Run -- (2018-2018), HydroShare, http://www.hydroshare.org/resource/f362d24430e0425b98a0792565c51bcc

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

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

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