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Water Table Fluctuations: The Correlation Between Distance and Groundwater Depth

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Type:	Resource
Storage:	The size of this resource is 424.4 MB
Created:	Apr 16, 2023 at 8:52 a.m.
Last updated:	Apr 25, 2023 at 10:56 p.m.
Citation:	See how to cite this resource
Content types:	Geographic Feature Content

Sharing Status:	Public
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Abstract

Understanding the subsurface water depth fluctuations is highly required for any further groundwater studies. In this project, the historical water level of the groundwater was studied for Cache Valley, Utah. Data of wells were called from USGS using Python, through the web service ‘NWIS’ function. Only the six wells that have enough observations were selected and then located spatially on a map. The data were plotted and statistically analyzed using different tools. Also, the data of some wells showed an abrupt change in the threshold conditions of the time series after 1987. The water table depth correlation of every two wells was visually related to the distance between the wells as they fitted the exponential correlation curve more than the linear one. Quantitatively, the Pearson test proved that the correlation between wells is correlated to the distance between them.

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Coverage

Spatial

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

North Latitude

41.7655°

East Longitude

-111.8014°

South Latitude

41.5922°

West Longitude

-111.9985°

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How to Cite

Othman, J. (2023). Water Table Fluctuations: The Correlation Between Distance and Groundwater Depth, HydroShare, http://www.hydroshare.org/resource/7f1e640e8f61447da3dec4b6ed79dd2d

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

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

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