Woodland-period archaeological sites in the North Central Hills physiographic region of Mississippi appear to be highly variable in occupation size, site function, duration, and occupational intensity. To better understand the occupational history and settlement patterns of such sites, several characteristics of four Woodland-period sites located within the Tombigbee National Forest, Ackerman Unit, Mississippi, are evaluated and compared to a larger, previously investigated site, 22WI516. From the data obtained in the field and laboratory, a determination of the causes of the variability among Woodland-period sites in the study area is attempted. Physiographic constraints appear to underlie much of the variability presented by the archaeological record.

Assessment of aquatic plant selection by waterfowl has been conducted during the winters of 1997-2000 on 49 0.2-0.79 ha research ponds in north central Texas. Ponds were categorized by dominant plant species into eight habitat types. Census with waterfowl species identification were performed to investigate impacts of aquatic vegetation and water depth on waterfowl. Eighteen waterfowl species were observed. Peak migration occurred in late December/early January. Mixed native ponds and mixed native/hydrilla ponds were the most frequently selected habitat types. The study included correlation analysis between pond water levels and waterfowl use. Full ponds received greatest use followed by half full ponds, while almost empty ponds received minimal use. Time activity budgets were conducted on waterfowl utilizing mixed native and hydrilla ponds to compare waterfowl time partitioning on native aquatic vegetation versus hydrilla. Although only minor differences were found in time budgets, social status appears to be strongly related to habitat selection. Ducks on native ponds were paired (86%), conversely no ducks on hydrilla ponds were paired. Hydrilla pond although frequently utilized, were populated by lower status birds mostly single hens.

The life history of Isonychia sicca (Walsh) was elucidated from samples collected at Clear Creek from Oct. 1976-Jun. 1978, and Elm Fork of the Trinity River from Sept. 1977-Jun. 1978, Denton County, Texas. Adaptations for existence in an intermittent stream were of primary concern. Eggs are capable of diapausing through hot, dry summers and cold, wet or dry winters. Diapause is broken in the fall after rehydration and/or in the spring. I. sicca is usually bivoltine during a Sept.-Jul. wet period. Observations from Elm Fork indicate that emergence continues to Oct. if the stream remains permanent. Considerable overlap occurs between overwintering, spring, and summer populations.

Texas water resources are under pressure due to population growth expected in the coming decades, increasing industrial demands, and frequent periods of drought. With this increasing demand for limited water resources it is important to explore alternative water sources within the State. One of those resources that can be developed is the many small aquifers which have never been well-characterized but could be an alternative source of fresh and brackish water for agriculture, municipal, and industrial applications. The natural gas industry’s demand for water is growing in Texas as new drilling techniques such a hydraulic fracturing have opened new reserves previously considered economically non-viable. The development of smaller aquifers containing brackish water is a viable alternative to the gas industry’s current reliance on fresh (potable) groundwater resources. The aquifer sections containing brackish water need to be mapped and characterized so they can be developed as an alternative water resource by the gas industry. The Barnett Shale in North-central Texas is one of the first major gas plays in the United States to use the technique of hydraulic fracturing in field development. This technique requires large quantities of water to create the required hydraulic pressure down the gas well to fracture the normally low permeability shale. A typical horizontal well completion consumes approximately 3.0 to 3.5 million gallons (11,400 to 13,200 m3) of fresh water. Projections of future groundwater demand for the Barnett Shale gas play total 417,000 AF (5.1x108 m3), an annual average of 22,000 AF (2.7x107 m3) over the expected 2007-2025 development phase. This level of water demand has the gas industry and groundwater managers exploring alternative sources of water for future development of the Barnett Shale. One alternative source of water for the expanding footprint of the Barnett Shale gas play are the smaller local Paleozoic aquifers on the western edge of the play. These small aquifers are underutilized and contain waters with higher levels of TDS. These levels are, however, acceptable to the drilling industry. In order to characterize theses aquifers, TWDB databases were utilized to analyze water chemistry and well productivity. / text

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Thesis (Ed. D.)--University of Missouri-Columbia, 1997. / Typescript. Vita. Includes bibliographical references (leaves 207-215). Also available on the Internet.

Thesis (Ed. D.)--University of Missouri-Columbia, 1997. / Typescript. Vita. Includes bibliographical references (leaves 207-215). Also available on the Internet.

Thesis (Ph. D.)--University of Missouri-Columbia, 1999. / Typescript. Vita. Includes bibliographical references (leaves 128-139). Also available on the Internet.

Thesis (Ph. D.)--University of Wisconsin--Madison, 1925. / Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.