Show simple item record

dc.contributor.authorAguirre, Andresen_US
dc.contributor.authorDerry, Louisen_US
dc.contributor.authorKurtz, Andrewen_US
dc.coverage.spatialBoston, MAen_US
dc.date.accessioned2019-09-16T13:44:00Z
dc.date.available2019-09-16T13:44:00Z
dc.date.issued2018-04-02
dc.identifierhttps://whiteiron.org/uploads/conferences/28/program/programVolume.pdf
dc.identifier.citationAndres Aguirre, Louis Derry, Andrew Kurtz. 2018. "Ge/Si as a tracer for Si in paired catchments of the Luquillo CZO." Goldschmidt Conference. Boston, MA, 2018-08-12 - 2018-08-17.
dc.identifier.urihttps://hdl.handle.net/2144/37791
dc.description.abstractCatchment lithology is a significant factor influencing the generation and transport of solutes in the critical zone. In the Luquillo Mountains of Puerto Rico, the Quebrada Guaba and Bisley catchments are studied to understand how lithology affects concentration-discharge (C-Q) relationships. Ge/Si ratios in pore water and stream samples are used to identify sources of Si to streams in the Bisley 1 watershed. Quebrada Guaba is underlain by quartz diorite and is characterized by strong Si dilution behavior (power law slope = -0.47)^1. During baseflow, Ge/Si = 0.27-0.47 μmol mol^-1 due to weathering of plagioclase and precipitation of Ge enriched kaolinite in the bedrock-saprolite interface2. During storms, hydrologic pathways shift to shallower flow paths with lower Si concentrations and higher Ge/Si (1.0-4.0 μmol mol^-1)^3. The shift to saprolite-dominated flow paths carrying dilute Si end-members drives the Si-Q pattern in this catchment. The volcaniclastic sub-catchment of Bisley 1 has a more chemostatic Si-Q relationship (power law slope of = -0.30)^1. In this study, lysemeters at the Bisley sites of B1S1, B1S2 and B1R show higher Si pore water concentrations than the LG sites at Quebrada Guaba. Ge/Si ratios for Bisley are lower than Guaba except for 200-300 cm depth were ratios increase to 2.87 μmol mol^-1 (B1S1). Dissolved Si concentrations increase markedly from 200 cm to the surface at B1S1 and B1S2. Ge/Si shows the opposite trend with ratios decreasing from 2.87 to 0.86 μmol mol^-1. This pattern of increased pore water Si and low Ge/Si may be due to phytolith dissolution also observed in Quebrada Guaba^2,4. Bisleys greater Si depletion near the surface may result in more sensitivity to phytolith inputs. Stream samples from Bisley 1 will be analyzed for major cations and Ge/Si to understand how pore water or other shallow surface reservoirs influence Si-Q patterns in this catchment.en_US
dc.description.urihttps://whiteiron.org/uploads/conferences/28/program/programVolume.pdf
dc.language.isoen_US
dc.titleGe/Si as a tracer for Si in paired catchments of the Luquillo CZOen_US
dc.typeConference materialsen_US
dc.description.versionPublished versionen_US
pubs.elements-sourcemanual-entryen_US
pubs.notesEmbargo: Not knownen_US
pubs.organisational-groupBoston Universityen_US
pubs.organisational-groupBoston University, College of Arts & Sciencesen_US
pubs.organisational-groupBoston University, College of Arts & Sciences, Department of Earth & Environmenten_US
pubs.publication-statusPublisheden_US
dc.identifier.mycv442084


This item appears in the following Collection(s)

Show simple item record