Publication Date

2006

Document Type

Dissertation/Thesis

First Advisor

Carpenter, Philip J.

Degree Name

Ph.D. (Doctor of Philosophy)

Legacy Department

Department of Geology and Environmental Sciences

LCSH

Hydrology; Karst--Bear Creek (Tenn. and Ky.); Hydrology; Karst--Illinois--Kankakee County

Abstract

Identification of conduits that control groundwater flow is extremely important in understanding karstic systems. This study tests the hypothesis that seismic refraction tomography may be used to identify and map karst features that control groundwater flow, recharge and discharge. Tomography provides velocity images of the subsurface, from traveltimes of seismic waves generated at the surface. Rock properties, other geologic structures and water levels near recharge and discharge points were also investigated using refraction tomography. This study was conducted at two locations: Bear Creek Valley of the Oak Ridge Reservation, TN, and Perry Farm Park, Bourbonnais Township, Kankakee, IL. P-wave velocity refraction-tomography models at Bear Creek Valley mapped lateral variations in the velocity of subsurface rock units and thickness variations of the overburden (0 to 30 ft). Inverted velocities are consistent with the two distinct bedrock groups at this field site - the Nolichucky Shale and Maynardville Limestone. Distinct low-velocity zones have the appearance of “fracture-like” structures. They represent either sediments filling bedrock depressions, or thick zones of highly weathered bedrock along faults and joints. These zones may be watersaturated or partially water-saturated, and probably play an important role in the hydrogeology of the area. Some of these zones also lie directly beneath surface streams, suggesting fault control of these streams, including Bear Creek. In many such locations well logs report the presence of actual fractures, cavities, and water-level fluctuations that cannot be explained by seasonal variations alone. Seismic refraction tomography over thinly mantled (7 to 30 ft) karst at Perry Farm Park may be used to delineate bedrock highs and lows, probably associated with different facies in the dolomite bedrock and/or fracture zones. Conventional refraction surveys, especially with S-waves, appear to delineate fractures. Results suggest that near-vertical fractures may also act as ground water recharge, discharge, and transmission features at the Perry Farm Park site. Borings and piezometers are needed to confirm this hypothesis, however. This study demonstrates that tomographic models are able to estimate subsurface velocity changes associated with geologic structures with better spatial resolution than conventional seismic refraction methods. Tomographic models also provide standard errors and model covariance. The tomographic models, however, are strongly dependent on the choice of initial 1-D model and the nature of shot-point and geophone geometry. They also may include computational artifacts. Thus, independent borehole, geological, and geophysical data must be used to verify tomographic models.

Comments

Includes bibliographical references (pages [255]-266).

Extent

xxi, 398 pages : ilpages (some color pages), maps

Language

eng

Publisher

Northern Illinois University

Rights Statement

In Copyright

Rights Statement 2

NIU theses are protected by copyright. They may be viewed from Huskie Commons for any purpose, but reproduction or distribution in any format is prohibited without the written permission of the authors.

Media Type

Text

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