Project SWIFT (Shale-Water Interaction Forensic Tools) Water Chemistry Database
| Authors: | Laura Lautz |
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| Owners: |
Laura Lautz
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| Resource type: | Composite Resource |
| Storage: | The size of this resource is 201.7 KB |
| Created: | Mar 23, 2018 at 2:17 p.m. |
| Last updated: | Mar 23, 2018 at 2:54 p.m.
by
Laura Lautz
|
| Citation: | See how to cite this resource |
| Content types: | Single File Content |
| Sharing Status: | Discoverable |
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| Views: | 128 |
| Downloads: | 0 |
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Abstract
The data set includes the following types of information for domestic wells sampled in southern New York State: geographic location (latitude and longitude), year of sample collection, concentrations of a variety of analytes, distances to various features (e.g. faults, gas wells, flow lines), topographic position, water type, well depth and type, and completion geology. Definitions of fields are provided in a worksheet within the Excel data file. When no data are available for a given field, the value is given as -9999. When concentrations are below a given detection limit, the value is given as -5555. The detection limits for chemical data in each year are given within a worksheet within the Excel data file.
Subject Keywords
Resource Level Coverage
Spatial
Temporal
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Content
References
Related Resources
| The content of this resource serves as the data for: | Christian, K, LK Lautz, GD Hoke, DI Siegel, Z Lu, J Kessler. 2016. Methane occurrence is associated with sodium-rich valley waters in domestic wells overlying the Marcellus Shale in New York State. Water Resources Research, 52(1):206-226. doi: 10.1002/2015WR017805 |
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| National Science Foundation | RAPID: Developing sensitive tests for detecting water chemistry changes associated with shale bed methane production in the Appalachian Basin | EAR 1313522 |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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