Spelling suggestions: "subject:"eology"" "subject:"atheology""
291 |
Documenting the History of Inca Precious Metal Production using Geochemical Techniques from Lake Sediments in the Andahuaylas Region of PeruKane, Molly Mae 03 June 2011 (has links)
The process of studying heavy metal concentrations in lake sediments in order to reconstruct pollution history has been used in a variety of environments and locations. Laguna Pacucha is one in a series of metal pollution studies from Peru and Bolivia, an area with a rich history of metallurgy. Laguna Pacucha lies in the Andahuaylas region of Peru, 145 km west of Cuzco, the Inca capital, and 20 km west of Curamba, a presumed ancient smelting site. The sediment record of Laguna Pacucha reveals a metal record that dates beyond 1225 AD. A major density change ~1225 AD, concurrent with a known period of drought, inhibits the possibility of a reliable age model below this point. Increases in Zn, As, and Cu after ~1225 AD could be indicative of local copper smelting, which supports separate evidence of the Curamba archeological site (near Laguna Pacucha) as a potential copper smelting site. These concentrations drop around the time of the Spanish conquest, and then the concentrations of a number of different metals increase after ~1600 and decrease by ~1850 AD, which could indicate smelting, but more likely indicates a change in land use. Our results provide a complex record of a changing Andean environment, and indicate a need for further study in the Andahuaylas region.
|
292 |
Fluorescence Characterization of Karst Aquifers in East TennesseeBrown, Teresa L. 01 August 2009 (has links)
Karst and fractured rock aquifers are primary sources of drinking water in the Appalachian region, even though most are inherently susceptible to surface-derived contamination. Many of the obstacles to water supply protection in such systems could be alleviated through the use of tracer testing to delineate recharge areas and surface-to-groundwater connections. Tracer testing is currently under-utilized, however, due to public safety concerns and ambivalence on the part of regulatory agencies. This study aimed to address this issue through a characterization of the fluorescent properties of typical carbonate aquifers for the purpose of refining the timing and design of low-concentration dye tracer tests.The subjects of this study were community water supply wells and springs in the Valley and Ridge Province of East Tennessee. Although each source exhibited a different degree of contamination potential, background fluorescence could primarily be attributed to natural dissolved organic matter (DOM) rather than manmade fluorophores. Seasonal data were collected for 23 groundwater sources during a multi-year drought (2006-2007). Untreated water samples were analyzed via fluorescence spectroscopy to identify spatial and temporal variations in the fluorescent properties of high-risk and low-risk water supply sources. Fluorescence exhibited seasonal patterns and fluctuations in DOM quality relative to rain events. Fulvic acid-like spectra were detected most consistently in all sources and exhibited maximum fluorescent intensity in the winter months. Humic acid-type fluorescence appeared in springs and high-risk wells only after major rainfall. For all sources, DOM spectra gradually shifted towards lower molecular weight fluorophores, which was interpreted as a reflection of diminishing humification and increasing generation of proteins with warmer weather and drier conditions. Variations in fluorophore composition and concentration were generally more pronounced in springs and moderate- to high-risk wells than in low-risk wells, although all sources exhibited some unique characteristics.The results indicate that extended background fluorescence characterization could enhance the design of tracer tests and sampling strategies for waterborne contaminants such as cyanotoxins, VOCs, and microbial pathogens. This study also highlights the potential benefits of monitoring DOM fluorescence as a natural tracer for source water and wellhead protection.
|
293 |
Geology of part of the Santa Monica MountainsPeterson, R. A. January 1931 (has links)
Thesis (Bachelors)--California institute of Technology, 1931. / Title from home page. Viewed 02/12/10. Includes bibliographical references.
|
294 |
Geology of the Placerita Canyon areaBattle, John A. January 1939 (has links)
Thesis (Bachelors)--California institute of Technology, 1939. / Advisor names found in the Acknowledgments pages of the thesis. Title from home page (viewed 03/16/2010). Includes bibliographical references.
|
295 |
Geology of a portion of the south side of the Santa Clara Valley near Newhall, CaliforniaHagen, Robert C. January 1939 (has links)
Thesis (Bachelors)--California institute of Technology, 1939. / Title from home page (viewed 03/16/2010). Includes bibliographical references.
|
296 |
Geology of a portion of the Ravenna quadrangle, Los Angeles CountyCowie, Roger H. January 1938 (has links)
Thesis (Bachelors)--California Institute of Technology, 1938. / Title from home page (viewed 03/16/2010). Includes bibliographical references.
|
297 |
The geology of a portion of Humphrey's quadrangleScott, David Holcomb, January 1939 (has links)
Thesis (Bachelors)--California Institute of Technology, 1939. / Title from home page (viewed 03/16/2010). Includes bibliographical references.
|
298 |
Geology of the Whittier Hills, Whittier, CaliforniaQuarles, Miller. January 1940 (has links)
Thesis (Bachelors)--California Institute of Technology, 1940. / Title from home page (viewed 03/16/2010). Includes bibliographical references.
|
299 |
Geology of the southern part of the Red Mountain quadrangle, CaliforniaAhlroth, Carl W. January 1938 (has links)
Thesis (Bachelors)--California Institute of Technology, 1938. / Title from home page (viewed 03/16/2010). Includes bibliographical references.
|
300 |
Geology of a southwest portion of San Gabriel MountainsCogen, William M. January 1931 (has links)
Thesis (Bachelors)--California institute of Technology, 1931. / Title from home page (viewed 03/16/2010). Includes bibliographical references.
|
Page generated in 0.0641 seconds