Third-order White Clay Creek and Boulton Run - Climate, Stable Isotopes, Stream Water Chemistry (2011-2012)

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Resource type:	Composite Resource
Storage:	The size of this resource is 22.0 KB
Created:	Jan 21, 2018 at 8:09 p.m.
Last updated:	Jan 21, 2018 at 8:24 p.m.
DOI:	10.4211/hs.ff7435cd22d94914ad3a674c40b229e9
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Content types:	Single File Content

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Abstract

Deuterium and Oxygen-18 measured on stream water samples collected during baseflow and stormflow conditions.

Variables: oxygen-18 (d18O), deuterium (dD)

Date Range: (2011-2012)

Dataset Creators/Authors: Diana L. Karwan

Contact: Diana L. Karwan, Department of Forest Resources, University of Minnesota, St. Paul, MN 55108

Field Area: White Clay Creek @ SWRC

Copied from: Diana L. Karwan (2012). "CZO Dataset: Third-order White Clay Creek and Boulton Run - Climate, Stable Isotopes, Stream Water Chemistry (2011-2012)." Retrieved 21 Jan 2018, from http://criticalzone.org/christina/data/dataset/3365/

For guidance on how to parse these CZODisplayFiles, see example Jupyter Notebooks in Python at https://github.com/aufdenkampe/EnviroDataScripts/tree/master/CZODisplayParsePlot.

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Resource Level Coverage

Spatial

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

Place/Area Name:

White Clay Creek Pump House, Lab and Boulton Run

North Latitude

39.8641°

East Longitude

-75.7839°

South Latitude

39.8607°

West Longitude

-75.7858°

Temporal

Start Date:
End Date:

Content

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Credits

Funding Agencies

This resource was created using funding from the following sources:

Agency Name	Award Title	Award Number
National Science Foundation		0724971
National Science Foundation		1331856

How to Cite

Karwan, D., O. Lazareva, A. Aufdenkampe (2018). Third-order White Clay Creek and Boulton Run - Climate, Stable Isotopes, Stream Water Chemistry (2011-2012), HydroShare, https://doi.org/10.4211/hs.ff7435cd22d94914ad3a674c40b229e9

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

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

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