Thesis (Ph. D.)--Public Policy, Georgia Institute of Technology, 2008. / Committee Chair: Paul J. Ferraro; Committee Member: Alex Pfaff; Committee Member: Douglas Noonan; Committee Member: Gary T. Henry; Committee Member: Gregory B. Lewis.

Thesis (M.Arch.)--University of Detroit Mercy, 2009. / "24 April 2009". Includes bibliographical references (p. 125).

Thesis (Ph. D.)--University of Missouri, 1935. / Vita. "Selected bibliography": p. 49-51.

Originally a part of the author's doctoral thesis entitled La desamortización en El Bierzo. / Includes bibliographical references (p. 131-137).

Thesis (Ph. D.)--University of Wisconsin--Madison, 1931. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 301-307).

Thesis (Ph. D.)--Washington State University, May 2010. / Title from PDF title page (viewed on Apr. 30, 2010). "Department of History." Includes bibliographical references (p. 260-272).

Inaug.-Diss.--Giessen. / Lebenslauf. Literatur-Verzeichnis: p. [91]-92.

This work is dedicated to the question of political and cultural relations of Czech lands and England in the second half of the 14th century. Attention is also paid to international relation in western Europe which led to cultural and artistic exchanges. Using historical events as a background, it analyses extant resources and works of art, by which can be the contact proven. Detailed analysis of the preserved works of art with English origin in the second half of the 14th century during the reign of English King Richard II, is followed by comparison with contemporary art production in Czech lands. The goal is to find features these two groups share and to find a way, through which the cultural ideas were transmitted. In that respect it is especially the marriage of the royal daughter Anne of Bohemia to English king Richard II Plantagenet in the year of 1382.

No description available.

One of the major issues in surface coal mine land reclamation is the impact of total dissolved solids (TDS) on water quality. To address this issue, this study assessed whether vegetation could reduce TDS nutrient ion movement from the rooting zone in early reclamation stages when TDS generation is often highest. Vegetated and un-vegetated paired plots were established across eight sites with gradients in age, spoil material, and vegetative productivity. Ion exchange resin lysimeters were used to compare nutrient ion fluxes in soil solution that contribute to TDS between paired plots. Soil and vegetation properties (used as proxies for evapotranspiration and plant uptake) were characterized at each site and correlated with log ratios of common TDS contributing ions [i.e., base cations Ca2+, Mg2+, Na+, K+ (RBC), sulfate (RSO42-), and total Ca2+, Mg2+, Na+, K+, SO42- (Rtotal)] between un-vegetated and vegetated plots. Strong Spearman correlations were found between RTotal, RBC, and RSO42- during the peak growing season, and were weakened overall during vegetative dormancy. Soil organic matter was shown to be a strong correlate through dormant periods. Correlations between TDS nutrient ions and vegetation suggest evapotranspiration in the growing season, and interception during dormant periods, exert an influence on nutrient ion fluxes. These findings indicate that aggrading forests may reduce TDS nutrient ion loading, through solute retention mechanisms driven by organic matter inputs and plant uptake. / Master of Science / Total dissolved solids (TDS) coming from surface coal mines are greatly impacting water quality in Appalachia. This study investigated whether vegetation could reduce TDS (specifically calcium, potassium, magnesium, sodium and sulfate ions) in solution draining from the soil into streams. Vegetated and un-vegetated plots were established across eight sites that differed in age, rock material, and plant communities. Ion exchange resins that capture TDS ions in soil solution were used to compare nutrient ion fluxes that contribute to TDS between paired plots. Soil and vegetation properties (used as proxies for evapotranspiration and plant uptake) were characterized at each site and correlated with log ratios of common TDS contributing ions. Strong correlations were found during the peak growing season, suggesting that the presence of vegetation reduced the amount of dissolved ions in soil solution. In addition, soil organic matter was correlated with TDS contributing nutrient ions in all seasons. These finding suggests that productive, growing forests could reduce TDS contributing nutrient ions draining from soils into streams through plant and organic matter retention.