ETDP collection

Type of Document Master's Thesis
Author Fiaschetti, Aaron A.
Author's Email Address Aaron_Fiaschetti@hotmail.com
URN etd-03012007-100218
Title Assessment of Ground Water Exchange in Two Stream Channels and Associated Riparian Zones, Jocko Valley, Western Montana
Degree Master of Science
Department Geology
Advisory Committee
Advisor Name Title
Dr. William Woessner Committee Chair
Dr. Manny Gabet Committee Member
Dr. Scott Woods Committee Member
Keywords
  • temperature
  • ground water
  • hydrogeology
  • MT
  • Jocko Valley
  • surface water interactions
Date of Defense 2007-01-08
Availability unrestricted
Abstract
Fiaschetti, Aaron, M.S., December 2006 Geology

Assessment of Ground Exchange in Two Steam Channels and Associated Riparian

Zones, Jocko Valley, Western Montana

Chairperson: William W. Woessner

Degraded riparian habitat is a concern throughout the United States. Repairing anthropogenic damage to river channels and wetlands is becoming increasingly popular,though including design features to re-establish ground water and surface water exchange rates and timing are rarely implemented. The goal of this project is to characterize the surface water/ ground water exchange rates of two stream and riparian systems that have been altered by agriculture use. Hydrogeological and hydrological field experiments were performed to better understand the location and magnitude of ground water and surface water exchange throughout each site. These data were compiled into a water balance for

the Sque-que study site. Vertical hydraulic gradients, temperature monitoring and ground

water chemistry were key components used to identify areas of surface water/ground

water exchange.I concluded that surface water/ground water interactions are occurring on

sub-reach scales throughout the Sque-que study site. The riparian water table position

changed little throughout the year and remained within two meters of the land surface. At

the Jocko River site a net gain of ground water along the 1 km reach was not detectable.

Modeling suggests the position of current water table will rise if drainage ditches are

filled at the study sites and that recovery of wetlands is possible.

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FiaschettiAaron.pdf 12.06 Mb