For landscapes dominated by agriculture, land cover plays an important role in the balance between anthropogenic and natural forces. Therefore, the objective of this thesis is to describe two different methodologies that have been implemented to create high-resolution land cover classifications in a dominant agricultural landscape. First, an object-based segmentation approach will be presented, which was applied to historic, high resolution, panchromatic aerial photography. Second, a traditional per-pixel technique was applied to multi-temporal, multispectral, high resolution aerial photography, in combination with light detection and ranging (LIDAR) and independent component analysis (ICA). A critical analysis of each approach will be discussed in detail, as well as the ability of each methodology to generate landscape metrics that can accurately characterize the quality of the landscape. This will be done through the comparison of various landscape metrics derived from the different classifications approaches, with a goal of enhancing the literature concerning how these metrics vary across methodologies and across scales. This is a familiar problem encountered when analyzing land cover datasets over time, which are often at different scales or generated using different methodologies. The diversity of remotely sensed imagery, including varying spatial resolutions, landscapes, and extents, as well as the wide range of spatial metrics that can be created, has generated concern about the integrity of these metrics when used to make inferences about landscape quality. Finally, inferences will be made about land cover and land cover change dynamics for the state of Iowa based on insight gained throughout the process.

No description available.

The processes that generated the distinctive landscape of the Iowa Erosion Surface (IES) of northeastern Iowa have been debated for over a century. A number of researchers have concluded that the IES experienced a periglacial environment and was underlain by continuous permafrost during the last glacial maximum. Ubiquitous throughout the IES is a stone zone that lies 60-100cm below the surface. Several explanations for the genesis of the stone zone have been proposed, including a lag concentrate, biomantle processes, and cryogenesis. We utilized a combination of coring and trenching, ground penetrating radar and resistivity to investigate the 3D distribution of the stone zone, overlying "pedisediment" and the underlying contact with dense till across a 100m2 area on a typical IES hillslope in east-central Iowa . Our preliminary results indicate that the stone zone occurs in the basal few decimeters of pedisediment that rests uncomformably and abruptly on eroded, dense till. Ice wedge casts extend from the stone zone into the underlying till. The depth of the stone zone below the modern surface increases downslope and the stone zone dissipates and eventually is replaced by relatively thick loamy sand beneath the footslope. These relationships argue against the stone zone being of biogenic origin. The occurrence of ice wedge casts associated with the stone zone and systematic changes in the thickness and texture of the pedisediment suggest to us that stone zone on the IES was formed by a combination of cryogenic and active zone erosive processes during the full glacial period.

The chronostratigraphic correlation of the Silurian units in Iowa is complicated by complex carbonate depositional environments and poor biostratigraphic control. In this study, we integrate conodont biostratigraphic data with carbon isotope (δ 13Ccarb) chemostratigraphic data from the Blanding, Hopkinton, Scotch Grove, and LaPorte City formations of Iowa to provide a precise chronostratigraphic framework for regional and global correlation. Conodonts from the LaPorte City Formation of eastern Iowa (East-Central Iowa Basin) in the Garrison Core indicate an early to middle Telychian age for the formation. Conodonts diagnostic of the Pterospathodus eopennatus Superzone, Pterospathodus eopennatus ssp. nov. 2 Zone, and Pterospathodus amorphognathoides angulatus Zone were recovered, allowing for the first direct comparison of the stratigraphic ranges of conodont species from the North American Midcontinent and the Baltic basin. The morphology of Pseudolonchodina fluegeli ssp. n. Männik (2007) co-occurs with Pseudolonchodina fluegeli fluegeli sensu Männik (2007a) in the LaPorte City Formation and are not stratigraphically separated in Iowa as they are in the East Baltic. Wurmiella? polinclinata polinclinata ranges much lower in the East-Central Iowa Basin (Pt. eopennatus ssp. nov. 2 Zone) than the Baltic Basin, so it cannot be used as an index fossil diagnostic of the Pt. am. amorphognathoides Zone in global correlations. Three carbon isotope excursions were recovered from the Hopkinton and Scotch Grove formations. The late Aeronian (herein renamed “Farmers Creek”) carbon isotope excursion and a heretofore unrecorded carbon isotope excursion were recorded from the Hopkinton Formation in the SS-10 Core (Jones County). The Farmers Creek Excursion can be correlated to Johnson County, where it was recorded in the Hopkinton Formation by McAdams et al. (in prep). The Valgu excursion was recovered from the uppermost Hopkinton Formation through the overlying Buck Creek Quarry Member of the Scotch Grove Formation in the Garrison Core (Benton County). This excursion can be correlated to Johnson County, where it was recorded in the same formations. The integration of conodont biostratigraphic and carbon isotope chemostratigraphic data from the Silurian of Iowa allows for the first regional chronostratigraphic correlations at a resolution finer than stage level. The oxygen and carbon isotope values from the Garrison Core and the evidence for post-diagenetic karsting and fluid movement through the units may provide further evidence that the dolomitization process of the LaPorte City Formation was halted by the influx of meteoric phreatic water. This study shows the first high-resolution chronostratigraphic correlation of Silurian units in Iowa, and highlights the utility of integrated carbon isotope chemostratigraphy as a tool for chronostratigraphic correlation in strata with poor biostratigraphic control. The conodonts recovered from the LaPorte City Formation shows the utility of the small limestone formations on the northwest flank of the East-Central Iowa Basin for refining global Silurian conodont biostratigraphic zonation.

Objective: To understand the association between dental insurance coverage and dental care utilization in Iowa children. Methods: The 2010 Iowa Child and Family Household Health Survey (IHHS) data was used to assess the association between dental insurance coverage and dental care utilization in Iowa children. Andersen’s model of health services utilization was used as a framework for determining the predictors of dental care utilization. Chi-square test was used for determining bivariate associations and Logistic regression analysis was used to determine factors associated with dental care utilization. Results: The results from the multivariable logistic regression model indicate that children with private dental insurance (p<0.001) and 4-9 years of age (p=0.005) were more likely to have a dental visit. Additionally, respondents who were always able to get dental appointments for their child (p<0.001), had a regular source of dental care for the child (p<0.001) and perceived dental need for their child (p<0.001), were more likely to report having a dental check-up for their child in the past 12 months. Conclusion: Dental insurance was significantly associated with having a dental visit in the past year in Iowa children 4-17 years of age. Some of the other predictors of dental care utilization were: having a regular source of dental care for the child, ease of getting dental appointment for the child, younger child’s age and having perceived dental need for the child.

Thesis (D. Min.)--Covenant Theological Seminary, 2007. / Includes abstract. Includes bibliographical references (leaves 227-231).

No description available.

The present study examines the relationship of emotional awareness to anticipatory psychophysiological markers and performance on the Iowa Gambling Task (IGT). The IGT is a computerized card game that simulates real-life decisions through uncertainty of reward or punishment. The participant’s goal is to make advantageous card choices. Anticipatory somatic markers of physiological arousal, like electrodermal activity and heart rate, have been proposed to bias decisions in the IGT. The central hypothesis is that a participant’s emotional awareness is related to their ability to make advantageous decisions through biasing psychophysiological responses. The Toronto Alexithymia Scale was used to assess each participant’s emotional awareness. Less emotional awareness was associated with enhanced performance on the IGT. However, anticipatory physiological arousal (electrodermal activity and heart rate) and emotional awareness yielded no significant relationships. Findings suggest a need for further research on cognitive models, such as the expectancy valence model, in relation to decision-making.

Thesis (Ph. D.)--University of North Texas, May, 2007. / Title from title page display. Includes bibliographical references.

Thesis (D.W.S.)--Institute for Worship Studies, 2007. / Abstract. Includes bibliographical references (leaves 177-181).