OSU Navigation Bar

The Ohio State University University Libraries Knowledge Bank

Geochemical Analysis of Waters in a Tropical Glacial Valley, Cordillera Blanca, Peru

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/45619

Show simple item record

Files Size Format View
Patrick_Burns_Honors_Thesis.pdf 1.796Mb PDF View/Open

dc.contributor.advisor Lyons, Berry
dc.contributor.advisor Mark, Bryan
dc.creator Burns, Patrick
dc.date.accessioned 2010-06-07T19:52:51Z
dc.date.available 2010-06-07T19:52:51Z
dc.date.issued 2010-06
dc.identifier.uri http://hdl.handle.net/1811/45619
dc.description.abstract The Cordillera Blanca, located in the central Andes of Peru, is the most glacierized mountain range in the tropics. Most of the Peruvian population lives in the arid Pacific plains which are heavily dependent on glacial melt and runoff from these mountains, especially during the dry season. Thus understanding the current physical and chemical hydrology of the region is imperative for making future predictions about climate impacts. The objective of this study is to examine a variety of geochemical parameters in a glacial valley and to determine how and why these parameters vary with elevation and between groups (surface water vs. groundwater). During the dry season of July 2009, surface water and groundwater samples were collected from the proglacial zone of Quilcayhuanca valley, a basin that is 20% glacierized and drains an area of 90 km2. The water samples from the valley (n=25) were analyzed for major cations (Ca, Mg, Na, K, Fe(II)), major anions (F, Cl, SO4), nutrients (total N, total P, and Si), and stable isotopes of water (δ18O, δ 2H). Field measurements like pH, conductivity, and temperature were also collected. The valley’s acidic waters (pH 3-4) are dominated by the major ions Ca2+, Mg2+, and SO42-, the last of which is a remnant of pyrite oxidation. Total P and total N show no trend with elevation while Si generally increases with decreasing elevation. Groundwater samples are differentiated from surface water samples by lower pH, specific conductance, and total P and higher Na+, K+, HCO3-, Si, and δ18O. Using a simple, two end-member mixing model the surface waters leaving the valley at the last site in the drainage basin were calculated to be a mixture of approximately two-thirds surface water (mostly glacial melt) and one-third groundwater. en_US
dc.description.sponsorship The Climate Water and Carbon Program at Ohio State en_US
dc.description.sponsorship Ohio State University Arts and Sciences Undergraduate Research Scholarship en_US
dc.description.sponsorship Goldthwait Scholarship in Earth Sciences en_US
dc.description.sponsorship Rector Scholarship in Earth Sciences en_US
dc.description.sponsorship Ohio Environmental Science and Engineering Scholarship en_US
dc.description.sponsorship Ohio State University College of Mathematical and Physical Sciences Alumni Scholarship en_US
dc.language.iso en_US en_US
dc.publisher The Ohio State University en_US
dc.relation.ispartofseries The Ohio State University. School of Earth Sciences Honors Theses; 2010 en_US
dc.subject tropical glaciers en_US
dc.subject meltwater and groundwater en_US
dc.subject geochemistry en_US
dc.subject nutrients en_US
dc.subject major ions en_US
dc.subject stable isotopes of water en_US
dc.subject Cordillera Blanca en_US
dc.title Geochemical Analysis of Waters in a Tropical Glacial Valley, Cordillera Blanca, Peru en_US
dc.type Thesis en_US
dc.description.embargo No embargo en_US