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CJCZO -- Soil Redox Potential -- Bigelow Site -- (2015-2020)

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Type:	Resource
Storage:	The size of this resource is 20.6 MB
Created:	Nov 19, 2019 at 6:42 a.m.
Last updated:	Nov 19, 2021 at 9:55 p.m.
Citation:	See how to cite this resource
Content types:	Single File Content

Sharing Status:	Public
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Abstract

Reduction (redox) potential are being measured continuously using vertical redox probes with 4 platinum sensors produced by Paleo Terra at 5, 10, 30 and 60 cm depths in instrumented pedons located in the Bigelow Zero Order Basin. Continuous data are measured at 15 minute intervals and stored in Campbell CR1000 datalogers.

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Coverage

Spatial

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

Place/Area Name:

Bigelow Site (High-Elevation)

North Latitude

32.4155°

East Longitude

-110.7243°

South Latitude

32.4151°

West Longitude

-110.7249°

Temporal

Start Date:
End Date:

Content

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Additional Metadata

Name	Value
czos	Catalina-Jemez
czo_id	5198
citation	The following acknowledgment should accompany any publication or citation of these data - Logistical support and/or data were provided by the NSF-supported Jemez River Basin and Santa Catalina Mountains Critical Zone Observatory EAR-1331408.
comments	Data are provisional and may be subject to revision. Sensor data stored to Campbell CR1000 datalogger.
keywords	Reduction potential, Redox potential, Mount Bigelow, Santa Catalina Mountains, Arizona
subtitle	Bigelow ZOB Redox Potential
variables	Reduction potential
disciplines	Soil Science / Pedology, Geochemistry / Mineralogy

Credits

Funding Agencies

This resource was created using funding from the following sources:

Agency Name	Award Title	Award Number
National Science Foundation		EAR-1331408

How to Cite

Chorover, J., G. Barron-Gafford, N. Abramson (2021). CJCZO -- Soil Redox Potential -- Bigelow Site -- (2015-2020), HydroShare, http://www.hydroshare.org/resource/ed8a2be3883b4f72b73636ae5d9ed087

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

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

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