BRWIS > People, Organizations, and Projects > Projects > Research > Hydrologic Contributions from Springs on the Logan River, Utah
Hydrologic Contributions from Springs on the Logan River, Utah
| Investigators
Michael Gooseff - Department of Aquatic, Watershed, & Earth Resources, College of Natural Resources, Utah State University
James Evans - Department of Geology, College of Science, Utah State University
Peter Kolesar - Department of Geology, College of Science, Utah State University
Thomas Lachmar - Department of Geology, College of Science, Utah State University
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| Abstract
The Utah State University Water Initiative has proposed to establish a Laboratory Watershed in the Bear River basin. The
Bear River Range is the primary recharge area for the Bear Lake and Cache Valleys, two important sub-basins.
The range exhibits snowmelt-dominated flow in the shallow soil or regolith zone, and deep
bedrock groundwater flow, controlled by karst and fracture/fault zones. Carbonate rocks (limestone and
dolostone) are abundant in the Bear River Range, and these rocks weather by dissolution, producing many
sinkholes, caves and springs. As a result, much of the water in streams entering Bear Lake and Cache
Valleys originates as springs in the Bear River Range. However, little is known about the flow paths,
chemical evolution, and partitioning of the amounts of each component of flow in the system. Further,
the locations of the recharge areas for these springs are largely unknown.
This project will be a pilot study that will consist of a time-series of isotopic and water chemistry analyses of the
Logan River above Third Dam, and at two of the largest springs that flow into the river. These springs
are associated with faults and fracture zones, and likely collect water from a large portion of the range.
These data will be used to try to deduce the proportion of hydrologic contribution for the springs and the
chemical evolution of the ground water as it flows from these recharge areas to the springs. We will use
these results as a springboard for further work to determine the rates and fluxes of water in the different
parts of the system. Such data and analyses will be critical for making management decisions regarding
the watershed, and will contribute to determining how climate changes might affect this portion of the
Bear River watershed.
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| Contact Information
Michael Gooseff
5210 Old Main Hill
Logan, UT 84322-5210
435-797-8292
michael.gooseff@usu.edu
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