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Estimation Of A Water Budget For Agnes Marsh, Grand Forks County, North Dakota, Allen E. Comeskey

Theses and Dissertations

Agnes Marsh is a semipermanent wetland in the Red River Valley of northeastern North Dakota. The marsh overlies and is in direct hydraulic connection with the unconfined Elk Valley aquifer. Recent irrigation development nearby raised concerns about the hydrological impact to the marsh by a declining water table in the aquifer. The purpose of this study was to determine how Agnes Marsh interacts with the underlying Elk Valley aquifer and how sensitive the marsh is to declining water levels in the aquifer.

Three methods were used to assess how the marsh interacts with the aquifer. First, stratigraphic analysis revealed the …

Depositional And Diagenetic Controls On Porosity Evolution In The "C" Zone, Red River Formation (Upper Ordovician), Divide County, North Dakota, John S. Fox

Theses and Dissertations

Carbonates and evaporites in the "C" zone c: the Red River Formation (Upper Ordovician) in the subsurface of Divide County, North Dakota, were studied in order to determine the geologic framework of porosity evolution in this important hydrocarbon-producing formation. Examination of 28 cores, petrographic analysis, geochemical analysis, and mapping based on 120 geophysical log suites allowed the characterization of "C" zone lithologies and diagenetic features and suggests that the entire "C" zone was deposited subtidally in an increasingly restricted basin, rather than in a subtidal to supratidal regressive sequence as interpreted by others in different parts of the basin.

The …

Petrography And Inorganic Geochemistry Of The Rosebud Coal Seam At The Absaloka, Big Sky And Rosebud Mines, Powder River Basin, Montana, Lingbu Kong

Theses and Dissertations

Quantitative maceral and microlithotype analyses, huminite reflectance measurements and inorganic constituent analyses of the samples of the Rosebud subbituminous coal seam from the Absaloka, Big Sky and Rosebud Mines were used in the interpretation of the depositional environment of the seam and for prediction of ash formation during combustion. The mean huminite reflectance varies from 0.31% at the Rosebud Mine to 0.34% at the Absaloka Mine and 0.39% at the Big Sky Mine, indicating that the coal rank is transitional from lignite to subbituminous C. Despite the variation in huminite reflectance, samples from the three mines are similar in mean …