Master's Theses

Department

Geosciences

Degree Name

Master of Science (MS)

Abstract

Three contour maps of groundwater elevation levels below Hays, Kansas generated in 2016 show that the phreatic surface in eight monitoring wells declined 3.6 inches to 1 foot 9.6 inches over a three-month period of July, August, and September. They also indicate that groundwater flows in curvilinear directions toward Big Creek. Analyses of ten north-south oriented structural cross sections of the alluvial fill beneath the central region of Hays provide evidence of buried low-sinuosity and meandering streams, floodplains, and possibly adjoining tributaries and abandoned channels. Correlation of the more porous and permeable sand and gravel facies along a northwest to southeast flow direction suggests a possible subsurface paleochannel within the Big Creek alluvium. This information is useful in determining hydraulic connectivity within the alluvium, mobility of various contaminants, and future watershed analyses.

Advisor

Dr. Kenneth Neuhauser

Date of Award

Spring 2017

Document Type

Thesis

Rights

© 2017 Krisopher John Neuhauser

Comments

For questions contact ScholarsRepository@fhsu.edu


Included in

Geology Commons

Share

COinS