Dissertations / Theses on the topic 'White River (Ind. : River)'

This creative project has culminated in a design solution to a water quality problem in the City of Indianapolis, Indiana. Pogues Run is a stream that has been buried in an underground culvert for almost a century. It has a long history of water quality problems including high bacteria levels and nonpoint source pollution. In addition, it has long been a flood threat to neighboring communities.To address the issue, a master plan was created for the last 1400' of Pogues Run before it emptied into the White River. The stream was removed from the culvert, brought back up to grade, a series of wetlands were developed to slow and filter stream flow, and an urban revitalization project was developed centering on the stream. The design solution provided flood control, stormwater storage and treatment, mixed-use redevelopment of historical buildings, a recreational area, and a high-density residential community.
Department of Landscape Architecture

Thesis (M.A.)--Indiana University, 2009.
Title from screen (viewed on August 27, 2009). Department of History, Indiana University-Purdue University Indianapolis (IUPUI). Advisor(s): Philip V. Scarpino. Includes vita. Includes bibliographical references (leaves 165-173).

This is a general regional research design for the prehistoric archaeological resources of the Upper White River Drainage region of east-central Indiana. Following the example of McGinsey, Davis, and Griffin (1968), this design consists primarily of research problems, questions, and hypotheses suggested by the current state of the regional data base and the pertinent literature. These research problems are organized into three basic groups which represent the goals of the discipline of archaeology (that is, the study of culture history, extinct lifeways, and culture process). These groups are themselves expressed as a hierarchy to demonstrate the relative significance of the problems expressed in each. When used as part of a greater research design process (including more specific designs) this design has the potential to contribute to the scientific rigor as well as the efficiency of archaeological research carried out in this region.

A survey of the Upper White River Valley located 76 new sites additional information on 6 previously recorded sites. After a preliminary literature review, artifacts from the Ball State University Archaeology Laboratory were reanalyzed and local artifact collectors were contacted to obtain additional knowledge survey area. The fieldwork focused on the floodplain and the location of Woodland sites in regards to Ross soil. Surface manifestations of Woodland-affiliated sites indicated that 33% of the sites in the project area were located in the floodplain and all Woodland components were represented on or adjacent to Ross soil. Results from the fieldwork indicate a positive correlation between Woodland sites and Ross soil in the Upper White River Valley of east-central Indiana.
Department of Anthropology

Geology
M.S.
Flagstaff Rim near Casper, WY preserves the most complete late Eocene section of the White River Group with over 219 m of late Eocene age sediment compared to 35 m preserved at Toadstool Park, NE. While Flagstaff Rim does not span the Eocene-Oligocene transition, it holds the earliest clues in the White River Group of a late Eocene (37-34 Ma) climatic deterioration. In this study 8 paleosols were collected, described and analyzed based on pedogenic features, mineralogy, and geochemistry, above and below dated volcanic ash beds. The lowermost paleosol is composed of smectite- rich red mudstone, with greenish gray drab haloes, and weather into hummocks. The sediments within this part of the section are the lithologic equivalent of the Peanut Peak member of Toadstool Park, NE and reflect a moist humid environment. Overlying these sediments is the lithologic equivalent of the Big Cottonwood Creek member. These sediments are comprised of smectite poor mudstones and yellow/beige sandstones, are indurated with calcium carbonate, and reflect a more arid environment. The transitional zone between the Peanut Peak and Big Cottonwood Creek lithologies corresponds with an increase in volcanism from the Great Basin, impact events, and building of ephemeral glaciers on Antarctica. The impact events and increase in volcanism, while synchronous with the transitional zone between the Peanut Peak and Big Cottonwood Creek lithologies, cannot explain the long term climatic perturbation, which persists within the White River Group. Instead, the climatic deterioration is likely explained by the building of ephemeral Antarctic ice sheets, which was compounded by the increase in volcanism and impacts. Regional variations in ä18O isotopes within the White River Group can likely explain the suggested variations in paleoclimate across the Eocene-Oligocene transition.
Temple University--Theses

Geology
M.S.
Climate change across the terrestrial Eocene-Oligocene boundary of the Great Plains is recorded by shifts in sediments, facies, paleosols, and isotopic records, and is interpreted as a shift to overall cooler and drier conditions. As an independent test of paleoenvironmental shifts caused by climatic change, I compared microwear on M2 molars of Leptomeryx from the White River Group (WR) at Toadstool Park, Nebraska (n = 9) and Flagstaff Rim, Wyoming (n = 11). Comparisons of microwear were made through time at each section. Various measurements of microwear were quantified on original, uncoated specimens using environmental scanning electron microscopy and Microware 4.0 software, and evaluated with ANOVA and Kruskal-Wallis statistical tests. Values of the scratch:pit ratio, scratch number, feature major:minor axis ratio, feature vector length, major axis standard deviation, major:minor axis standard deviation, and feature orientation standard deviation for Leptomeryx M2 molars are significantly different (p<0.05) between Wyoming and Nebraska. Microwear patterns suggest paleoecological differences between the two locations, possibly related to differences in Leptomeryx diet or in amount or character of sediment adhering to ingested vegetation. Little fossil evidence of vegetation type is preserved at either locality, other than clay-filled root traces or occasional rhizoliths or silicified fragments. However, sediments of the WR are a mixture of volcaniclastic enriched mudstone, siltstone, and sandstone, with generally coarser overall particle sizes in Wyoming that reflect proximity to siliciclastic sources. The degree of overall volcaniclastic enrichment and number of airfall tuffs is also higher at Flagstaff Rim. Paleosols suggest a shift from closed canopy forest to progressively open conditions at each locality and, although microwear differences could result from differences in vegetation or particle sizes of adhered sediments on plants, no or very low correlations between microwear features and stratigraphic level were detected at either locality, indicating that any changes in paleoecology over time did not significantly alter the diets of Leptomeryx, although diet may have been geographically different.
Temple University--Theses

Geology
M.S.
Understanding local and regional reactions to the global Eocene-Oligocene climate transition is a continuing challenge. The White River Group in the North American midcontinent preserves dynamic fluvial, volcaniclastic and lacustrine facies that yield to aeolianites. To test whether this shift in sedimentation style was driven by climate change, 20 paleosols from 8 profiles were analyzed from the fluvial-aeolian Orella Member through the aeolian-dominated Whitney Member of the earliest Oligocene Brule Formation at Toadstool Geologic Park, NE. Paleosol morphology and geochemistry were used to assess the balance of aeolian vs. alluvial sedimentation at key stratigraphic intervals and lithologic transitions. Significant loess deposition began at least as early as the lower Orella Member but is masked in most settings by concomitant fluvial deposition. As fluvial influence on landscapes waned across the Orella-Whitney Member boundary, loess deposits predominated and became more recognizable. Paleosols follow different pedogenic pathways in direct response to depositional setting. Whereas all paleosols formed through top-down pedogenesis in alluvial settings, paleosols in aeolian-dominated settings formed though pedogenic upbuilding during aggradational phases and through top-down pedogenesis during depositional hiatuses. The disparity between each style of pedogenic development creates fundamentally different pedogenic associations that must first be understood before climatic interpretations can be drawn from macroscopic paleosol morphology alone. Microscopic analysis of loessic and alluvial paleosols indicates that pedogenic features do not greatly change across the Orella-Whitney Member boundary. Furthermore, results of climofunction calculations from five paleosol Bw and Btk horizons show mean annual temperature (ca. 9.0-10.5 °C) and precipitation (ca. 650-800 mm/y) do not significantly vary across the Orella-Whitney Member transition. Clay mineralogy and the presence of pedogenic carbonate and translocated clay corroborate paleoclimate estimates. However, geochemical paleosol profiles are uniform and do not reflect observed vertical associations of pedogenic features. Constant additions of aeolian sediment, which replenishes base losses through leaching, explain this phenomenon. Interpretations of paleovegetation from root trace morphology and paleosol taxonomy indicate that predominantly open canopy to savanna habitats were in place in the lower Orella Member and continued into the Whitney Member. Evidence for riparian partitioning exists in the lower Orella Member but disappears as fluvial deposits wane in the Whitney Member. Lacking evidence of climate change from paleosol analysis, changes in sedimentation style and vegetative biomes are most likely a reaction to increased aeolian deposition.
Temple University--Theses

Increased urbanization in the United States and the rest of the world, has led to more research on the effects it has on the local ecology. Urbanization can be defined as the creation of impervious cover in areas previously covered by natural vegetation (forest, grassland or farmland) as well as the potential influence of sewage treatment plants. Small increases in impervious cover can cause noticeable changes in stream chemistry. The goal of this study is to quantify the impact of smaller industrial cities on water and sediment geochemistry in a largely agricultural watershed. The study area is in east-central Indiana along the west fork of the White River and includes the cities of Winchester, Muncie and Anderson. This area is dominated by agriculture and the impact of cities in the region on water chemistry has not been studied. To evaluate this impact, sampling sites were selected up- and downstream of the three cities to characterize White River water chemistry before and after it flows through the cities as well as sewage treatment plants. Sampling was done over the course of one year to obtain samples characteristic of high and low flow river conditions. Samples were analyzed for major cation and anion concentrations as well as total suspended solids. Metals data was also obtained in sediments, although sampled only twice throughout the study. Results show that sediment load, on average, increases on the downstream side as the river flows through urbanized areas. Chemical analyses show that major cations and anions, Na, K, SO4 and Cl, have distinct spikes in concentration on the downstream side of the cities, as well. Na and Cl are specifically linked to human and urbanized activity, and were up to four times higher downstream of urbanized cities. The concentration of other major ions, including Ca, Mg and NO3, was mostly due to agricultural land use and local bedrock geology. Trace metals characteristic of pollution from automobiles, including Cd, Cr and Zn, showed large increases downstream of urban areas as well. This indicates that even in an area that is largely dominated by agriculture, smaller cities have a quantifiable impact to White River water quality.
Department of Geology

1989, the Archaeological Resources Management Service Ball State University conducted a reconnaissance level survey of 550 acres located within and adjacent to the Wabash River Valley in Huntington and Wabash Counties, Indiana. Additional survey was conducted in 1990 and 1991 on areas of expanded right-of-way within the original project area. The field reconnaissance located 188 archaeological sites. Twenty-one of the sites located by those surveys were subjected to archaeological testing.This study examines data from the survey and testing and presents a distribution of sites and human settlement across the study area. The study also develops a site typology which is used to address settlement pattern questions for the study area.
Department of Anthropology

Several population characteristics were calculated for smallmouth bass Micropterus dolomieui and rock bass Ambloplites rupestris populations on the west fork of the White River in Randolph, Delaware, and Madison counties, Indiana and were compared to other populations. When compared to streams of similar size in Indiana that were sampled with the same methods, relative abundance (CPUE) of smallmouth bass was average (18.9-35.0 fish/hour) while rock bass were two to ten times more abundant (44.3-53.0 fish/hour). Age analysis and back calculation of length at age were only performed for smallmouth bass. These results indicated strong year classes were cyclical and smallmouth bass growth was above average for Indiana streams, but average for streams of the Midwest. Proportional stock density values were average for smallmouth bass (28-39%) and slightly below average for rock bass (17-33%). Strong weight-length models were also found for both species and relative weight values were optimal.
Department of Biology

Water quality parameters including ammonia, nitrate+nitrite, phosphate, total suspended solids, Escherichia coli, and dissolved oxygen were statistically evaluated from sampling data collected by the Bureau of Water Quality (City of Muncie, Indiana) at five sampling locations in Delaware County over a five-year period (2002-2006). These data were also compared with water quality standards/guidelines to determine how sample values compared to acceptable levels of these parameters. Friedman's non-parametric test was used to study the differences between sites and seasons. Spearman's Rank Correlation was used to study the correlations between water quality parameters at each sampling site. Significant differences were observed for individual parameters when evaluated relative to sampling location based on pooled monthly collected data as well as data evaluated on a seasonal basis. These differences indicated the fact that different sources were responsible for observed concentrations at a particular location and that seasonal phenomenon such as precipitation, discharge and temperature also affected sample concentrations at individual sampling locations. Most notable were differences in geometric mean concentrations of ammonia, nitrate+nitrite, phosphate and E. coli upstream and downstream of the wastewater treatment plant (WWTP), with highest concentrations downstream, indicating the significant impact of the WWTP on water quality in the White River. Significant correlations observed among some study parameters suggested that sample concentrations may have been affected by similar sources. In comparison to water quality standards, concentrations of ammonia, nitrate+nitrite, phosphate, and E. coli were at unacceptable levels at most sampling locations.
Department of Natural Resources and Environmental Management

Thesis (M.A.)--Indiana University, 2010.
Title from screen (viewed on July 19, 2010). Department of History, Indiana University-Purdue University Indianapolis (IUPUI). Advisor(s): Robert G. Barrows, Annie Gilbert Coleman, Xin Zhang. Includes vitae. Includes bibliographical references (leaves 115-121).

In River Thieves, the white settlers are responsible for the vanishing of the Beothuk which reflects the spiritural loss of the white settlers. The major themes of truth, regret and guilt are discussed in the novel.

This study documents the stage adjustments in the Lower White River between 1931 and 2012 at four rated gaging stations along the trunk stem of the river. The study reach extends from Calico Rock, Arkansas, to the confluence of the White River with the Mississippi River north of Arkansas City, a distance of about 509 km. The specific gage approach was used to track hydrological response in the study reach. In order to approach spatial homogeneity across the four gaging locations along the study reach, input discharges were normalized to multiples of mean daily flow (MDF). Specific gage analysis tracks water surface elevation changes for fixed discharge conditions over time. Three discharges were analyzed at each station: low flow, mean flow, and high flow. The low flow specific gage trends are emphasized to highlight degradation and aggradation due to the sensitivity of specific stages at low flows to channel bed elevation changes. An `enhanced interpolation' technique was used to fill gaps in the specific stage time series in order to avoid errors derived from extrapolation of annual rating curves. The analysis shows decreasing trends in specific stage at Clarendon and DeValls Bluff at low flows, indicating net degradation. The gages at Newport and Calico Rock show increasing trends in specific stage over time at low flows, indicating aggradation downstream of Norfork and Bull Shoals reservoirs.

This paper is an archaeological. resources management plan for a proposed archaeological district in Henry County which encompasses four sites known to be significant: New Castle (12Hn-1), Commissary (12-Hn-2), Van Nuys (12-Hn-25), and Hesher (12Hn-298). Information is provided about previous e::cavations at each of the sites as well as details regarding the location, natural setting, and cultural history of each site. Research questions are outlined. The core of the plan relates to niiariagernent of the resources including suggestions regarding future uses and protection. Finally, completed National Register of Historic Places Registration Forms for the incorporation of the four archaeological sites into a single archaeological district are attached.
Department of Anthropology

Physical disturbance in the form of storm events has been implicated as a major determinant of community structure in streams. But there has been limited study of this effect on individual taxa within the communities. Such work is needed because of untested assumptions regarding the behavior of bioindicator species in these systems. Development of intricate indices of insect tolerances to organic pollution have become commonplace in environmental monitoring. However, research on the effects of natural disturbance on biological water quality assessment is lacking. Hydropsychid caddisflies are relatively intolerant to organic pollution and the United States Environmental Protection Agency has outlined the use of these organisms and others as an indication of clean water. If a species is recorded as absent from samples when it is present but hidden, this false negative would bias the water quality assessment. I tested hypotheses regarding the behavior of hydropsychid caddisflies facing increased discharge, and the effect of stream size on the magnitude of this phenomenon.Three sites along the West Fork of the White River, Indiana USA were studied during nine storms between 2001 and 2004. Stratified sampling from the upper 15 cm of substrate prior to and just after a storm, and again following reestablishment of normal flow, revealed alterations of hydropsychid distributions. During storms all but one species sought refuge in the hyporheic zone at depths dependent upon storm intensity. The possibility that poor water quality resulting from increased discharge caused the hydropsychid behavior was refuted by chemical analysis. Family level biotic index (FBI) data demonstrated that increased discharge results in a reduction of stream FBI values. These results indicate that high intensity storm events influence biological monitoring and should be factored into sampling protocol.
Department of Biology

The aquatic ecology of the White River basin has been studied since 1875 with researchers having reported 158 fish species belonging to 25 families. Recently, an EPA 319 grant allowed for further research in the Upper White River basin. The two-year study (2002-2004) examined three watersheds in Delaware County for biotic integrity, habitat quality, and stream water quality parameters. Twenty-two sites were selected to gain a perspective on agricultural, urban, and wooded landscape influences in order to locate and implement Best Management Practices (BMPs). Samples exceeded established state regulations and guideline criteria as follows: E. col/ (80%), ammonia-N (71%), dissolved oxygen (55%), nitrate+nitrite-N (38%), orthophosphate (33%), and total suspended solids (18%). A general linear model indicated that the effects of watershed and location within each watershed were significant (p <0.001) for both the Qualitative Habitat Evaluation Index (QHEI) and Index of Biotic hntegrity (IBI) index scores. Digitized land cover developed using Geographic Information Systems (GIS) was created to determine the effects of agricultural and wooded land cover ratios on the IBI and QHEI indices. A significant positive linear relationship between the amount of woodland land cover in a 5-m streamside riparian buffer and QHEI (p<0.001, r2 = 0.55) and with IBI (p<0.001, r-2 = 0.49) was found. A significant negative linear relationship was found with the amount of agricultural land in the created 5-m riparian buffer and IBI (p<0.001, r' 0.41), QHEI (p<0.001, r2 _- 0.36). The 30-nm streamside riparian buffer and delineated subwatershed land cover ratios were significant for the biotic integrity and habitat quality parameters, but were less predictive than the 5-m buffers. In addition, the amount of high runoff soils in the subwatersheds had significant negative effects on the IBI (p < 0.001, r' = 0.47) and QHEI (p = <0.001,r' = 0.43). Wetness accumulation and soil erosion was modeled in each watershed with the use of GIS, soils, and terrain parameters. The maps produced detailed locations where BMPs (wetlands, grassed waterways, riparian buffer strips etc.) could be targeted to reduce non-point source pollutants.
Department of Natural Resources and Environmental Management

Overall, the results of this study show that there are evident trends among the three ecoregions and delta of the White River. The forest stands of the Pine Ridge/Pierre Shale Ecoregion are the oldest along the river, as evidenced by aerial mapping going back into the 1930s and by the larger average trunk diameters of the trees. Historic aerial photographs for this ecoregion shows a relative static system from the 1930s-2010, with little destruction of existing or creation of new forests within the floodplain. Along with the older age of the forests, the stands in this ecoregion have the lowest floral diversity. The Pine Ridge/Pierre Shale forests are also unique along the river in that they are largely dominated by Acer negundo (box elder), a late-successional species that is largely absent from the forests of the other ecoregions. As the river continues downstream and enters the Badlands Ecoregion it gains size and volume, while its riparian forests decrease in patch size and tree density. Although the forests become smaller, the variety of communities and diversity of species increase. Unlike the Pine Ridge/Pierre Shale Ecoregion, the Badlands’ land cover was dynamic from the 1930s-2010, with increases in forest and declines in river channel area (-29%). Farther downstream and with a larger river channel, the River Breaks has even larger and more diverse riparian forests and the highest plant species richness and diversity among the ecoregions. The rate of land cover change was the greatest in the River Breaks, as the larger river has greater power for eroding existing communities and depositing sediment for recruitment. The area of riparian woody vegetation increased sharply from the 1930s-2010 (58%), while the area of channel declined (-20%). This ecoregion had the most perennial streamflow, with fewer zero flow days than in the upstream ecoregions. The Delta is unique as the only portion of the river where flows are affected by the Fort Randall Dam on the Missouri River. The impact of the reservoir on the area is evident, as it has the largest proportional area of forest along the river, as well as having the flora with the highest wetland affinity.

Three watersheds of Upper White River were chosen for this study. Stream samples were tested for total suspended solids and conductivity. Fourteen percent of the total suspended solids samples were above 80 mg L-1 which can cause negative effects to aquatic life. Total suspended solids results were tested with a general linear model and in linear regressions with discharge and nutrients. Conductivity results were tested with a general linear model. Concentrations of the total suspended solids were significantly related to watershed, Julian date, the interaction of watershed and Julian date, and discharge. Increasing total suspended solids concentrations were significantly related to increasing concentrations of orthophosphate, nitrate, and ammonia. Conductivity levels were significantly related to watershed, location within watershed, and Julian date. Total suspended solids, discharge, and nutrient concentrations were high in the spring, but decreased in the following seasons.
Department of Natural Resources and Environmental Management

Considerable effort has been dedicated to restoring sturgeon habitat within dammed rivers. However, sedimentation causes long-term failure because interstitial voids provide critical habitat during early life-stages. Based on the premise that a better understanding of geomorphic processes will improve restoration design, this study characterizes flow and sediment transport dynamics through a white sturgeon spawning reach on the Nechako River, BC. An extensive dataset was collected throughout the 2015 flood. Bedload transport was sampled on 36 days with flows ranging from 44 m³/s to 656 m³/s. During a high flow of 525 m³/s, channel bathymetry and water surface elevation were surveyed and velocity profiles were collected across 9 transects. Banklines, bars and island topography were later surveyed during low flow. Sediment transport into the reach was positively related with discharge. This relation was non-linear and transport rates increased rapidly once flows exceeded 400 m³/s. The relation weakened with downstream distance and sediment transport peaked progressively later throughout the year. No relation was observed at the downstream end of the reach, where transport rates remained low and constant relative to upstream. Sediment was primarily transported through secondary channels conveying a disproportionate amount of sediment compared to flow. Within the single-thread channel, the locations conveying the greatest amount of sediment remained spatially consistent over time. Hydrodynamic modelling indicates the Burrard Ave. Bridge causes backwatering once discharge exceed 225-275 m³/s. Velocity, shear stress and transport capacity at the downstream end of the reach do not increase with discharge because of the backwatering and the expansion in channel width through the island complex. The locations of maximum shear stress and transport capacity shift upstream with increasing discharge, but shear stress does not exceed 23 N/m² for flows up to 775 m³/s. The fluvial dynamics within the spawning reach create challenges and opportunities for habitat restoration. Backwatering is problematic because it causes mid-reach deposition during high flows and limits shear stress magnitude over the downstream spawning substrate. Meanwhile, the presence of sediment transport pathways through secondary channels and within the mainstem can be used to site restoration projects in areas apt to maintain suitable habitat.
Arts, Faculty of
Geography, Department of
Graduate

Stream samples were tested at 18 sites in three subwatersheds of the Upper White River for ammonia, nitrate, orthophosphate, atrazine, and diazinon. Nutrient results were tested with a general linear model and in linear regressions with selected landuse characteristics. A critical areas index for surface runoff of pollutants was created using a geographic information system. Comparisons were made between results obtained by Ball State University and by the Muncie Bureau of Water Quality and other outside laboratories. Most mean concentrations of nutrients were likely related to combinations of agricultural and residential landuse factors. Only concentrations of ammonia and orthophosphate were significantly related (a = 0.05) to any landuse characteristics. Atrazine levels were high in the spring, but decreased in the fall. Results suggest that improved or increased best management practices should be implemented in these subwatersheds to control non-point source pollution of the streams.
Department of Natural Resources and Environmental Management

According to the U.S. Environmental Protection Agency, 174 of Indiana's 428 waterbodies were listed as impaired for Escherichia coli (E. coli) in 2002. This study determined the severity of E. coli contamination and assessed the impacts of landuse on E. coli concentrations in three subwatersheds. Samples were collected and E. coli analyzed using the Coliscan Easygel method. Geographic information system analyses were used to determine impacts of spatial parameters on E. coli concentrations. Sixty-seven percent of the 162 samples exceeded the USEPA recreational water quality standard. Escherichia coli concentrations were significantly related to the ratio of five-and thirty-meter impervious surface buffer, density of septic systems, and the presence of inadequately drained soils. Confined feeding operations and combined sewer overflows also resulted in elevated E. coli concentrations. Human activity in urban areas had substantial impacts on these concentrations, impacts that can be minimized through proper management.
Department of Natural Resources and Environmental Management

White bass Morone chrysops are native to the Mississippi River and its tributaries. This range includes the Barren River in south central Kentucky. Over the last thirty years, the population of white bass in Barren River Lake, a reservoir of the Barren River, has been in decline. During that same time, two congeners of white bass have been introduced to the lake. Hybrid striped bass Morone chrysops × Morone saxatilis were introduced in 1979 and yellow bass Morone mississippiensis were first discovered in 2000. Due to the similar life histories and spawning strategies of all three Morone species, I hypothesized that the two introduced species are interfering with reproduction of the native white bass. In the springs of 2012 and 2013 I sampled fish from within a five kilometer stretch of Barren River upstream of the lake. I collected 144 white bass, 111 yellow bass and 29 hybrid striped bass. Detection of species at spawning sites was staggered with yellow bass and hybrid striped bass arriving after white bass but leading to a period of co-occurrence. White bass on the spawning sites appeared healthy: fecundity (75,200 to 741,150 eggs per female), mean gonadosomatic indices (peaked at 10.7% and 23.7% in sequential years), mean relative weight (93.8), and length at age (above the 50th percentile). Of the yellow bass stomachs examined, 21.6% contained fish eggs or larval fish. Based on arrival times and evidence of egg and larval fish predation, it is likely that yellow bass are directly impacting white bass spawning success through reproductive interference and the consumption of white bass offspring. Schoener’s index values revealed a significant degree of dietary overlap between white bass and yellow bass in larval fish, post larval fish, and arthropods (Cxy = 0.992,0.994, and 0.804, respectively), and between white bass and hybrid striped bass in arthropods (Cxy = 0.851). Information from this study may elucidate causes of the declining white bass population and aid in its management in Barren River Lake.

Previous research regarding aquatic acidification has examined the protonation of the carbonate and does not consider calcium to be a limiting factor. This is the first study to suggest that pH may affect the uptake of calcium in crustacean gills. This project describes ion transport mechanisms present in the cell membranes of white river shrimp Litopenaeus setiferus gill epithelium, and the effects of pH on the uptake of calcium by these means. Partially purified membrane vesicles (PPMV) of shrimp gills were prepared through a homogenization process that has been used previously to define ion transport in crab and lobster gill tissues. In the current study, shrimp gill PPMV calcium uptake at 50 µM, and 250 µM was greatest at pH 7.0 (p=0.01, p=0.0001). A valinomycin/K+ induced membrane potential (PD) at pH 7.0 significantly increased (p=0.003) calcium uptake from that observed in the absence of a PD. An induced PD at pH 8.0 significantly increased (p=0.003) calcium uptake from that observed in the absence of a PD, however, was not significantly greater than uptake at pH 7.0 in the presence of a PD (p=0.05). Amiloride (2mM) treatments, and amiloride (2mM) + verapamil (100µM) cocktail treatments showed significant decrease in calcium uptake from the control (p=0.03), however, they were not different from each other. This indicates an electrogenic carrier with two driving forces: calcium concentration, and asymmetric exchange stoichiometry.

An archaeological survey documenting sites along Upper Eel River within the Indiana counties of Allen, Whitley, Kosciusko and Wabash was conducted during 199192 to collect data which was analyzed to provide a clearer understanding of the region's cultural chronology and describe the area's cultural resources. A total of 765 previously unrecorded sites were documented, 493 of which were field-checked during field reconnaissance of 10% of the project universe, with 1010.82 acres surveyed. A research project completed entirely by volunteers succeeded in locating a number of potential archaeological sites from the Historic Period.Data from the present study securely defined the cultural chronology of the Upper Eel River Valley and yielded valuable information concerning settlement patterns, ecological exploitation, and avenues of migration. Cultural sequencing revealed the presence of Early Paleo-Indians along the river valley at approximately 12,000 B.P. and chronicled the continued expansion of prehistoric populations within the area into historic times.
Department of Anthropology

Research can conflict with conservation when invasive techniques are used on protected animal species. We developed a decision framework including the research question, the choice of technique, and the recommended course of action following the evaluation of the risks and benefits. This evaluation includes biological risks and benefits and considerations linked to the perception of resource users. We applied this framework a posteriori to a case study, the use of biopsy sampling on St. Lawrence belugas. We monitored the biological risks and benefits over four field seasons using behavioural and physiological indices and reports on the work in progress. We evaluated the risks as "low" and the benefits as "medium". For benefits to outweigh risks, procedures to minimise risks, publication of the work, and formulation of recommendations for conservation are essential. Researchers should be prepared to discuss with stakeholders the potential conflicts between their projects and conservation.

Thesis (M.A.)--Miami University, Dept. of Geography, 2005.
Title from first page of PDF document. Document formatted into pages; contains [1], iv, 49, [6] p. : ill., maps. Includes bibliographical references (p. 44-49).

Thesis (MScAgric) -- University of Stellenbosch, 2002.
ENGLISH ABSTRACT: The table grape industry is a major contributor to the South African economy, directly through foreign earnings from this predominantly export-based industry, as well as indirectly through the employment of thousands of people. It is a growing industry and consists of several production areas. The fastest growing table grape production area in South Africa is the Lower Orange River area, which produces some of the earliest grapes in the Southern Hemisphere. The biggest river in South Africa irrigates this area and it has an extreme climate characteristic of semi-desert areas. This area is considered to be optimal for the production of high quality, early, white seedless grapes. Previously, this area was predominantly planted to Sultanina vines for the purpose of raisin production. When seedless table grapes became a consumer preference, the producers very successfully converted their production practices to yield export quality seedless grapes from the established Sultanina vineyards. Extensive new plantings as well as re-plantings occurred in this area, also including newer cultivars from local and overseas breeding programmes. Being a viticultural and economical hot-spot, the Lower Orange River area is attracting much attention as a table grape production area and it also formed the backdrop to this study. The cultivar profile is changing in the area and it is projected that Sultana-, Regal-, Prime Seedless and Sugraone will be the four major early, white seedless cultivars in 2005. Based on this knowledge and prompted by a lack of information regarding production costs and general profitability of the new cultivars, this study was initiated in the form of a comparative analysis between the four mentioned cultivars spanning the early, middle and late regions of the Lower Orange River area. The approach used extracted information regarding cultural input costs (specifically labour as man-hours and the consequent costs) per manipulation performed in the vineyards. This approach is different from the more general method of obtaining input costs for a specific area based on combined mean values, often not distinguishing between cultivars. The specific aims of the study included a comparative analysis of input costs for production cultural practices per main manipulation action, as well as a comparative analysis taking into account productivity, value and extraordinary costs related to each of the four cultivars. To this end, 22 experimental plots were identified for use in the study. Collaboration of the production managers of each of the experimental plots were procured and information regarding production costs per manipulation and productivity of each cultivar and experimental plot were extracted from their own record keeping systems or from documents provided to the production managers. The value (price achieved) of the various cultivars for the 2001/2002 table grape season were put into perspective by using data from a survey which included information regarding payments for the various cultivars during the season in the Lower Orange River area. Information regarding fruit and vine royalties was obtained from the various plant breeders' rights holders of the various cultivars, where applicable. Primary descriptions of each experimental plot concerning general cultivation practices and information regarding the specific season were used to qualify results obtained from the various blocks. Several complicating factors impacted on the study and specifically the subsequent analyses of the results. Some of the factors were already identified as complicating factors in the planning stage of the study and were mostly linked to the recent introduction of two of the cultivars to the Orange River area. From the data gathered and the analyses performed it became clear that it would be difficult to discern significant differences (where significant is defined as PS0.10), but clear trends were observed and indications obtained. Based on the input cost analyses of this study it is proposed that mature Prime Seedless will have the highest labour input and cultural production cost of the four cultivars, followed by Sugraone. The labour input and the cost for the production cultural practices studied for young Prime Seedless vines were very high in comparison to the mature Sultana Seedless and Sugraone vines, especially for the canopy management and bunch manipulation actions. Prime Seedless was especially prone to the set of small and uneven berries, which lead to very high labour input requirements and subsequent cost for bunch manipulations. Sugraone is also known for the set of small and uneven berries in the Lower Orange River area, especially in difficult climatic seasons, also requiring high labour input for bunch manipulations. The initial indication is that mature Sultana- and Regal Seedless will require similar labour inputs for cultural production practices. The fact that Regal Seedless does not require expensive gibberellic acid (GA) applications, or girdling for thinning and berry enlargement purposes, is a tremendous advantage from a production cost point of view. Accordingly, initial indications are that Regal Seedless will have the lowest cultural production cost of the four cultivars. Regal Seedless was prone to the set of uneven berries during the year of study and accordingly it is suspected that this factor will ultimately determine the labour requirements and cultural production input cost, especially in difficult climatic seasons. The labour input and ultimately the cultural production cost for Sultana Seedless will be determined by the correct timing and concentration of the GA applications for thinning and berry sizing. Sultana Seedless and Sugraone produced high yields during the 2001/2002 table grape season in the Lower Orange River area. Yield information from the various experimental plots confirmed that there is little to choose between the two cultivars in terms of yield when cultivation conditions and practices are optimal. Large variation was observed in the yield results from the Regal- and Prime Seedless experimental plots. This is largely due to the recent introduction of the cultivars to the area and the consequent scarcity of blocks of these cultivars that are in full production. It was impossible to identify clear trends in terms of the future productivity of mature Regal- and Prime Seedless, but some indications of labour inputs could be extracted and qualified. Early maturing Prime Seedless and Sugraone performed very well in terms of price, especially in the harvest period prior to week 50. This advantage of high prices early in the season is, however, not always applicable to early cultivars in the later maturing regions of the Lower Orange River area. Later during the season, after week 50, when the supply of table grapes to the overseas markets has increased sharply, Sultana Seedless is usually the best performer in terms of price of the four cultivars. The ultimate price obtained by a cultivar is to a large extent determined by supply and demand, quality and acceptance of the specific cultivar. This study and its outcomes have a strong regional (Lower Orange River) and local (South Africa) impact and the specific results will undoubtedly be valuable to the producers, exporters and other role-players with vested interest in the cultivars studied or in table grape production per se. The methodology adopted in this study, however, is of broader interest and dearly shows the advantage of having detailed and qualified information regarding cultivation practices and bringing it in relation to the labour and consequent costs required per action. This should lead to more business intelligence and realistic planning on the producer side when decisions regarding the choice of a cultivar for a specific production area with a particular marketing scope have to be made. This study has also paved the way for similar studies, specifically with regard to the detailed description of the methodology that was established. Knowledge of the problems experienced in this study provides a useful reference for the planning and execution of similar studies.
AFRIKAANSE OPSOMMING: Die tafeldruifindustrie dra grootskaals by tot die Suid- Afrikaanse ekonomie: regstreeks deur middel van buitelandse valuta vanaf hierdie hoofsaaklik uitvoer-gebaseerde industrie, asook indirek deur werkverskaffing aan duisende mense. Dit is 'n vinnig groeiende industrie en bestaan uit verskeie produksie-areas waarvan die Benede-Oranjerivierarea, waar van die vroegste druiwe in die suidelike halfrond geproduseer word, tans die meeste groei toon. Die grootste rivier in Suid-Afrika vloei deur hierdie gebied wat deur uiterste klimaatstoestande, soortgelyk aan die van semi-woestyngebiede, gekenmerk word. Hierdie gebied is baie gunstig vir die produksie van hoë-gehalte, vroeë, wit pitlose druiwe. In die verlede is hoofsaaklik Sultanina vir die produksie van rosyne in hierdie gebied verbou. Namate pitlose tafeldruiwe voorkeur begin geniet het onder verbruikers wêreldwyd, het produseerders in die area hul verbouingspraktyke suksesvol aangepas vir die produksie van uitvoergehalte tafeldruiwe vanaf die grootskaalse, reeds gevestigde Sultanina-wingerde. Uitgebreide aanplantings en heraanplantings, wat nuwe cultivars van plaaslike en oorsese teelprogramme ingesluit het, is in hierdie gebied gedoen. Die vinnige groei in tafeldruifaanplantings en -uitvoere, asook die ekonomiese impak van die industrie in die Benede-Oranjeriviergebied, het die afgelope aantal jaar sterk op die voorgrond getree en het gevolglik gedien as agtergrond vir hierdie studie. Die cultivarprofiel in dié area is besig om te verander en volgens vooruitskattings gaan Sultana, Regal, Prime Seedless en Sugraone die vier prominente vroeë, wit, pitlose tafeldruifcultivars in 2005 wees. Gebaseer op hierdie feit en na aanleiding van 'n behoefte aan meer inligting met betrekking tot produksiekostes en algemene winsgewendheid van die nuwe cultivars, is 'n vergelykende studie aangaande die vier genoemde cultivars in die Benede-Oranjeriviergebied geloods. Die benadering wat gedurende die studie gevolg is, het inligting aangaande produksie-insetkoste (spesifiek arbeid in man-ure en gevolglike koste) per manipulasie onttrek. Hierdie benadering verskil van die meer algemene metodiek om insetkoste-inligting van 'n spesifieke area van gekombineerde gemiddelde waardes te verkry. Met so 'n benadering word gewoonlik geen onderskeid tussen cultivars getref nie. Die spesifieke doelwitte van hierdie studie het 'n vergelykende analise aangaande die insetkoste van die produksiepraktyke per hoofmanipulasie/aksie ingesluit, asook 'n analise waar produktiwiteit, waarde en buitengewone koste van die vier cultivars in ag geneem is. In totaal is 22 eksperimentele persele gebruik in die studie. Samewerking van die produksiebestuurders van die onderskeie esperimentele persele is verkry ten opsigte van die verskaffing van inligting oor produksiekoste per manipulasie, en die produktiwiteit per cultivar en eksperimentele perseel. Die produksiebestuurders het die nodige dokumente ontvang om die inligting te onttrek, of kon die inligting verskaf soos dit in hul rekordhoudingsisteem voorgekom het. Die waarde (prys behaal) van die onderskeie cultivars vir die 2001/2002-seisoen is in perspektief gestel deur gebruik te maak van 'n opname wat in die Benede Oranjeriviergebied plaasgevind het. Hierdie opname het inligting oor die uitbetalings van die onderskeie cultivars in die area vir die 2001/2002- seisoen ingesluit. Inligting rakende die stok- en vrugproduksie-tantieme is vanaf die onderskeie plantttelersregtehouers van die cultivars verkry. Primêre beskywings van die algemene verbouingspraktyke van elke eksperimentele blok en inligting oor die spesifieke seisoen is gebruik om die data wat vanaf die esperimentele persele verkry is, in perskektief te stel. Verskeie kompliserende faktore het die studie en die ontleding van data beïnvloed. Verskeie van hierdie faktore is reeds geidentifiseer met die beplanning van die studie en was meestal gekoppel aan die onlangse bekendstelling van Regal en Prime Seedless aan die Benede-Oranjeriviergebied. Na aanleiding van die data wat ingesamel en ontleed is, was dit duidelik dat dit moeilik sou wees om betekenisvolle verskille (waar "betekenisvol" as PS0.10 gedifinieer is) tussen die cultivars uit te lig, maar dat dit egter wel moontlik sou wees om aanvanklike indikasies en tendense te kry. Gebaseer op die insetkoste-ontleding van die studie blyk dit dat volwasse Prime Seedless die hoogste arbeidsinsetle en produksiekoste van die vier cultivars gaan hê, gevolg deur Sugraone. Die arbeidsinsetle en koste van die produksie-aksies wat van jong Prime Seedless bestudeer is, was baie hoog in vergelyking met volwasse Sultana Seedless- en Sugraone-stokke, veral ten opsigte van lowerbestuur en trosmanipulasies. Prime Seedless was veral geneig tot die set van klein, oneweredige korrels, wat tot baie hoë arbeidsinsetle en gevolglik koste vir trosmanipulasies gelei het. Sugraone is ook daarvoor bekend dat dit geneig is tot die set van klein, oneweredige korrels in die Benede-Oranjeriviergebied (veral in moeilike klimaatseisoene), wat gevolglik tot hoë arbeidsinstle vir trosmanipulasie lei. Die aanvanklike aanduiding is dat volwasse Sultana en Regal Seedless min of meer die dieselfde arbeidsinsetle vir verbouing sal vereis. Die feit dat Regal Seedless nie duur gibberelliensuur (GS)-behandelings vir blomtrosuitdunning of korrelvergroting benodig nie, is 'n enorme voordeel in terme van produksiekoste. Gevolglik is die aanvanklike aanduiding dat Regal Seedless die laagste produksieskoste van die vier cultivars sal hê. In die studiejaar was Regal Seedless egter geneig tot die set van onweredige korrels en gevolglik word verwag dat hierdie faktor uiteindelik die arbeidsinsetle en produsiekoste van die cultivar sal bepaal, veral in moeilike klimaatseisoene. Die arbiedsinsetle en produksiekoste van Sultana Seedless sal bepaal word deur die korrekte tydsberekening en konsentrasie van die GS-behandelings vir uitdunning en korrelvergroting. Sultana Seedless en Sugraone het gedurende die 2001/2002-seisoen hoë opbrengste in die Benede-Oranjeriviergebied geproduseer. Oesdata inligting van die onderskeie esperimentele persele het bevestig dat daar min te kies is tussen die twee cultivars in terme van produktiwiteit wanneer verbouingstoestande en -praktyke optimaal is. Groot variasie is egter waargeneem in die opbrengsresultate van die Regal en Prime Seedless. Dit is hoofsaaklik as gevolg van die onlangse bekendstelling van die twee cultivars in die area en dus ook die beperkte aantal blokke van die cultivars wat reeds in vol produksie was. Dit was dus onmoontlik om duidelike tendense in terme van die toekomstige produksie van volwasse Regal en Prime Seedless te identifiseer. Indikasies van arbeidsinsette en produksiekoste kon egter wel verkry word. Vroeg rypwordende Prime Seedless en Sugraone vaar baie goed in terme van die prys wat dit behaal, veral in die oesperiode voor week 50. Hierdie voordeel van hoë pryse behaal vroeg in die seisoen is egter nie altyd van toepassing op vroeë cultivars in die later rypwordende areas van die Benede-Oranjeriviergebied nie. Later in die seisoen (na week 50), wanneer die aanbod van tafeldruiwe op oorsese markte skerp toegeneem het, is Sultana Seedless gewoonlik die beste presteerder in terme van prys van die vier cultivars. Die uiteindelike prys wat deur cultivars behaal word, word tot 'n groot mate bepaal deur vraag en aanbod, kwaliteit en aanvaarding van die cultivar deur die verbruiker. Die studie en die uitkomste daarvan het 'n sterk streeks (Benede-Oranjerivier) en plaaslike (Suid-Afrika) impak, en die spesifieke resultate salongetwyfeld van waarde wees vir produseerders, uitvoerders en ander rolspelers met bestaande belange in die cultivars of vir tafeldruifproduksie as sulks. Die metodiek wat in hierdie studie gebruik is, is egter van breêr belang en wys duidelik die voordele daarvan om gedetailleerde en gekwalifiseerde inligting aangaande produksiepraktyke te hê, wat dit ook in verband bring met arbeid en gevolglike koste per aksie. Dit behoort te lei tot meer besigheidsintelligensie en realistiese beplanning deur die produseerder met betrekking tot cultivarkeuse vir 'n spesifieke produksiearea met 'n spesifieke bemarkings geleentheid. Hierdie studie het ook die weg gebaan vir soortgelyke studies, spesifiek ten opsigte van die gedetailleerde beskrywing van die metodiek wat gevestig is. Kennis van die probleme wat in hierdie studie ondervind is, kan dien as nuttige verwysing vir die beplanning en uitvoer van soortgelyke studies.

Thesis: S.M. in Management Research, Massachusetts Institute of Technology, Sloan School of Management, May, 2020
Cataloged from the official PDF of thesis.
Includes bibliographical references (pages 32-35).
In the United States, black college students are less likely to graduate than white students, which has lead many to argue that the "climate" at colleges and universities is not conducive to black students' success. However, another factor may also be important: an insufficient pipeline of college-ready black high school graduates. The process through which students select colleges can lead this insufficient pipeline to be reflected as a black-white completion gap within a given college even if all black and white admitted students are equally likely to complete college. Highly college ready black high school graduates are likely to receive more offers of admission than white peers and are less likely to attend any given college, leading black matriculents at a given college to be less college ready on average than white classmates. With data on the full set of admits and matriculants at a US college, we observe a black-white completion gap with matriculants but estimate that no such gap would occur if every admitted student chose to matriculate. This implies that a completion gap could be generated solely through black and white students' matriculation decisions and ensuing differences in college readiness.
by Ethan J. Poskanzer.
S.M. in Management Research
S.M.inManagementResearch Massachusetts Institute of Technology, Sloan School of Management

This study determines opinions of two Indiana communities concerning the proposed Patoka River National Wildlife Refuge. Surveys were mailed to residents of Pike County and Noblesville, Indiana. The response rate was 38%. Differences in attitudes were measured between residents of the two areas regarding ten issues of concern. The issues respondents were most concerned with were those focusing on the loss of county tax base, road closings and access, and a possible increase in the mosquito population. Surprisingly, the issues concerning avian diseases and land acquisition/ condemnation were not major concerns. It was originally thought that these issues of employment and property would have been of primary concern to respondents. Residents of Pike County in the affected refuge area were more aware of the refuge and the issues of concern. However, of the respondents who were aware of the refuge in both Pike county and Noblesville, few differences in their perceptions of the issues were noted.
Department of Natural Resources and Environmental Management

Functional morphology and morphometric studies on various mammalian groups have shown marked differences in crania and mandible shape based on dietary preferences and feeding habits. In this study I used three-dimensional geometric morphometric methods to measure the shape of crania and mandibles of herbivorous and omnivorous mammals from three formations in northwestern Nebraska to explore the structure and disparity of ecosystems through time: The White River Group (Chadronian/Orellan/Whitneyan), the Arikaree Group (Arikareean), and the Ogallala Group (Hemingfordian/Barstovian/Clarendonian). Throughout the time period compromising these formations the climatic conditions were becoming more arid, grasslands were expanding and the large mammalian faunal compositions were shifting from browser dominated to grazer dominated. Relative warps analysis show a visible separation of faunas between the three formations that cannot be attributed to phylogeny in plots based on either the crania or the mandibles. Phylogenetic effects were taken into account using generalized least squares. These results indicate that it may be possible to differentiate fossil taxa from different formations and environments based on the shape of cranial and mandibular elements as well as to infer the environment or diet of a fossil if other unequivocal data are not available.

In 1987, the Archaeological Resources Management Service (AXM6) at Ball State University conducted a sampling survey of a seven mile section of the Maumee River Valley in Allen County, Indiana. In addition to the primary survey, the project conducted an experiment in resurveying previously surveyed sample units, interviewed local collectors, and analyzed and tabulated data from a local collection with site level provenience. The project also reevaluated data previously collected from an adjacent section of the river valley and tested four sites in the latter study area.This study summarizes the data from the Maumee Grant Project and presents a general chronology of prehistoric habitation in the study area based upon that data. More specifically, this study has formulated provisional settlement models for the:PaleoIndian and Early Archaic habitation of the Upper Maumee River Valley, circa-10,000 to 6,000 B.C.The data indicate that the earliest peoples to inhabit the study area were Paleo-Indian bands with a preference for floodplain habitation and a subsistence strategy that emphasized hunting. As the post-glacial climate of the region ameliorated, the Early Archaic peoples that followed adapted a more diverse subsistence strategy, thus drawing upon a wider variety of terrace and floodplain resources. In contrast to their PaleoIndian forerunners, Early Archaic groups in the Upper Maumee Valley generally exhibited a preference for terrace habitation. In addition to the general Early Archaic occupation of the valley, three specific lithic traditions, the Kirk, the Bifurcate, and the Thebes, were identified and their settlement practices compared. While the origins of the earliest PaleoIndian bands in the region remained unclear, subsequent groups seem to have extended from and/or been influenced by Late Pleistocene and Early Holocene populations to the north, west, southwest, south, and east. By contributing to the regional data base and formulating provisional settlement models, this report provides a foundational basis for future research in the region.
Department of Anthropology

Thesis (Ph. D.)--University of North Carolina at Chapel Hill, 2009.
Title from electronic title page (viewed Oct. 5, 2009). "... in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Marine Sciences." Discipline: Marine Sciences; Department/School: Marine Sciences.

This study describes the geology and late Quaternary history of the inner shelf just north of the Buffels River off Namaqualand. In this area the inner· shelf is only 2km to 3.5km wide. An "inner-shelf platform" slopes gently (1°) out to -40m. An "inner-shelf slope11 then grades relatively more steeply (2-3°) down from -40m to -75m where it is buried by a wedge of terrigenous sediment which lies at the foot of the inner-shelf slope. Precambrian bedrock is exposed over 70% of the inner shelf. Bedrock morphology, compiled from high-resolution seismic profiles, shows erosional features in the bedrock surface which indicate potentially diamondiferous areas. Gently sloping (1°) wave-abraded terraces occur at -14m to -lam, -22m to -28m, -33m to' -40m and -44m to -53m. Palaeo-channels of the Kwaganap and Kamma Rivers extend across the inner-shelf platform. Sonographs show that rugged bedrock with NNE-SSW- and NNW-SSE-trending strike-gullies (Acoustic Facies 1) occurs mostly at >30m depth and also around reefs at Stompneus Shoal and Penguin Rock. Low micro-relief bedrock with sediment-filled strike-gullies, also trending NNE-SSW and NNW-SSE (Acoustic Facies 2) , delineates the areal extent of -14m and -22m terraces. A deposit of boulders and cobbles interspersed with patches of gravelly sand (Acoustic Facies 3) occurs on the protected, landward side of Stompneus Shoal and Penguin Rock. This deposit may be associated with a lobate basal unit (shown in the seismic profiles) marking a -30m sea-level palaeo-beach within the deposit of sand north of Penguin Rock. Fine sand (Acoustic Facies 4), up to 7m thick, blankets the inner-shelf slope between Stompneus Bay and Twee Pad and extends onto the inner-shelf platform at Rob Eiland and Deurloop Bay. The sand thins progressively northwards and seismic profiles show that it extends seaward beneath the Holocene mud deposit (Acoustic Facies 5) which buries the inner-shelf slope below -75m. Evidence from this study implies that the 25m-30m thick wedge of sediment at the base of the inner-shelf slope consists. of seaward-thinning lenses of sand overlain by a thin (8-lOm) deposit of Holocene mud. The origin of the fine sand is attributed to wave-erosion of a late Pleistocene palaeo-dunefield immediately north of the Buffels River during the Flandrian transgression. In much of the study area (>70%) this reworking removed the overburden of dune sand originally covering the bedrock and the diamondiferous gravels. The upper 4m of the mudbelt shows two texturally different units and below this depth, gas-charged sediment (Acoustic Blanking Layer) masks the remaining internal structure. Fields of two-dimensional megaripples of fine sand (Acoustic Facies 6) show that the modern inner-shelf sand is actively affected by storms.

This study has presented a comprehensive study on the growth, change, and architectural character of an Ohio River town between 1816 and 1996 using New Albany, Indiana as a case study. The evidence suggest that the majority of New Albany's physical growth occurred between 1838 and 1859, and also between 1953 and 1977. The economy of New Albany transformed several times through the course of its existence. New Albany was first supported by the ship building industry. Many boat manufacturers established ship yards along the banks of the Ohio River in New Albany. The ship building industry in New Albany became non-existent in the early 1970s. The glassmaking industry that replaced the ship building industry was also located along the banks , of the Ohio River.The early twentieth century and the closure of the glass-making industry began a transformation of the location of industries in New Albany. When hardwood companies established plants in New Albany, several were attracted to the undeveloped, flat land in the northeastern fringe of the city. This process of development in the north and northeastern section of the city still continues today.The architectural character that was established in New Albany in the late 1800s remained until the early 1960s and urban renewal. Many historic structures in New Albany were demolished in the 1960s and early 1970s. Much of New Albany's architectural character today was constructed during that period. However, New Albany still retains several historic buildings, and increased preservation efforts has lead to the rehabilitation of many of them.
Department of Architecture

An investigation was undertaken to better understand the hydrogeologic framework of the Rio Cobre and Rio Minho-Milk river basins, Jamaica, West Indies. A quasi three-dimensional finite-difference groundwater flow model was used to conceptualize flow conditions and establish a hydrogeologic budget of the region.

The Rio Cobre and Rio Minho-Milk river basins lie on the Clarendon Block, an area with a complex geologic history. The geologic history includes: 1) the intrusion of calc-alkaline granites, 2) morphotectonic sedimentation, 3) three episodes of deformation by transpressional and transcurrent tectonics, 4) the deposition of a highly permeable, Tertiary carbonate platform, and 5) the development of near surface karst oriented with the major NNW-SSE fault trend in the basins. Since deposition, compression, faulting, and solution have modified the distribution and thickness of carbonate rocks impacting the ground-water flow of the region. The most notable features are the older NNW-SSE trend dip-slip faults and the younger E-W trend strike-slip faults, notably the South Coast Fault (SCF) formed during the Laramide Orogeny. The White Limestone aquifer is the principal aquifer of the Rio Cobre and Rio Minho-Milk river basins in the parishes of St. Catherine, Clarendon, and partly in Manchester. It is characterized by intercalated sequences of permeable rubbly and micritic carbonate rocks. The age of the rocks range from Late Cretaceous (Maastrichtian) to Recent.

The permeability of the South Coast fault and the high hydraulic conductivity value associated with the Tertiary carbonate platform (480 m/d) in the Lower Rio Minho-Milk River basin control the gradient of the potentiometric surface and ground water flow in that region The agreement between the measured and the simulated hydraulic heads obtained for this steady-state model suggests that the values assigned to the hydraulic properties that characterize the ground-water flow of the White Limestone aquifer are reasonable. Recharge to the area occurs as net recharge in addition to upland subsurface inflow across the general head boundary in the northern part of the study area. Comparisons of calculated and observed values of head indicate that simulated groundwater flow field generally agree with field conditions. /

Several simplifying assumptions were made for the conceptualization and simulation of flow in the basins: 1) during the 1998 water year, ground-water in the basins was considered at steady-state, 2) pumping does not significantly affect the level of hydraulic heads; therefore pumping wells are not simulated, 3) Net recharge from precipitation varies spatially, 4) karstification and aquifer heterogeneity impact on the distribution of hydraulic conductivity, 5) Darcy's law is applicable to flow through the fractures and solutions openings in a karst region, 6) flow in the White Limestone aquifer occurs in the uppermost 650 m and vertical flow is assumed to be controlled by intervening units, 7) evaporation was not explicitly simulated in the model. Recharge rates were considered as "net recharge," and 8) submarine discharge occurs from the aquifer along the coast where aquifers are hydraulically connected to the sea.

Ground-water flow in the basins was conceptualized as a quasi three-dimensional flow system in which two model layers were used. The model boundaries selected to represent natural hydrologic boundaries include (1) a no-flow along the western and eastern boundaries, (2) a constant head boundary along the freshwater/saltwater interface; (3) a general head boundary along the northern boundary; and (4) a horizontal-flow barrier boundary along the South Coast Fault; and (5) river leakage boundaries along major rivers draining the coastal basins. The simulated region is an area of 2,550 square kilometers, two-thirds of which is hilly and the remainder, irrigated plains with small swamps draining the area. The model consists of over 337,500 cells and employed a regular grid spacing of 200m x 160m. The model was designed and calibrated to steady-state conditions from data observed/estimated during water year 1998. The Water Resources Authority of Jamaica (WRAJ) will use the results of the modeling study as a predictive tool for long-term management and monitoring of water resources in the region.

The model was calibrated using a manual trial-and-error adjustment of parameters. Hydraulic conductivity values in both model layers, hydraulic conductivity at the general-head boundary, and streambed conductance were adjusted during successive simulations until computed head values approximated field conditions. The computed potentiometric surface is an adequate or reasonable match on a regional scale, with the general horizontal hydraulic gradient oriented with the main fault trend NNW-SSE in both basins.

Sensitivity tests of the calibrated model were conducted on net recharge, hydraulic conductivity, hydraulic conductivity assigned along the general-head boundary, and streambed vertical conductance to determine if differences between simulated and observed values were similar to the range of uncertainty in the values of input data and boundary conditions. Based on the results obtained from the sensitivity analysis, it is apparent that the model is extremely sensitive to changes in horizontal hydraulic conductivity and recharge in the form of precipitation. The model is least sensitive to streambed vertical hydraulic conductivity.

Master of Science