Award Abstract # 1251875
Collaborative research: Quantifying weathering rind formation rates using U-series isotopes along steep gradients of precipitation, bedrock ages, and topography in Guadeloupe

NSF Org: EAR
Division Of Earth Sciences
Recipient: THE PENNSYLVANIA STATE UNIVERSITY
Initial Amendment Date: September 10, 2013
Latest Amendment Date: June 19, 2015
Award Number: 1251875
Award Instrument: Continuing Grant
Program Manager: Enriqueta Barrera
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: September 1, 2013
End Date: August 31, 2017 (Estimated)
Total Intended Award Amount: $52,210.00
Total Awarded Amount to Date: $52,210.00
Funds Obligated to Date: FY 2013 = $39,625.00
FY 2014 = $5,023.00

FY 2015 = $7,562.00
History of Investigator:
  • Susan Brantley (Principal Investigator)
Recipient Sponsored Research Office: Pennsylvania State Univ University Park
201 OLD MAIN
UNIVERSITY PARK
PA  US  16802-1503
(814)865-1372
Sponsor Congressional District: 15
Primary Place of Performance: Pennsylvania State Univ University Park
225B Earth-Engineering Sci Bldg
University Park
PA  US  16802-1503
Primary Place of Performance
Congressional District:
15
Unique Entity Identifier (UEI): NPM2J7MSCF61
Parent UEI:
NSF Program(s): Geobiology & Low-Temp Geochem
Primary Program Source: 01001314DB NSF RESEARCH & RELATED ACTIVIT
01001415DB NSF RESEARCH & RELATED ACTIVIT

01001516DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s):
Program Element Code(s): 729500
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

The process of mechanical and chemical decomposition of volcanic rocks at the Earth's surface (i.e., weathering) regulates the global carbon cycle, releases nutrients to ecosystems, and sculpts landscapes. Despite its fundamental importance, we still lack effective tools and key observations to quantify the weathering rates of volcanic rocks and to understand how they respond to changes in climate and tectonic regime. During weathering, rock fragments in soils commonly form weathering rinds. These rinds can provide an ideal long-term record to help understand the controls of chemical weathering. Investigators propose to combine a novel U-series isotopic technique with bulk chemical, petrographic, and electron microprobe analyses to quantify formation rates of weathering rinds on the tropical volcanic Basse-Terre Island of French Guadeloupe. By comparing weathering rinds from a single watershed, they will understand the controls on weathering rind formation at the micro-scale through processes including dissolution, formation of new phases, and development of porosity. In addition, the field setting at Basse-Terre Island provides a superb natural laboratory with large environmental variables, allowing them to study rind formation along steep gradients of precipitation, bedrock ages and relief at large watershed scale. The combined analysis of weathering rinds will provide a novel and fundamental method to directly determine chemical weathering rates. This will be of broad interests to scientists worldwide studying the Critical Zone or Earth's surface layer extending from the top of the vegetative canopy to the base of groundwater. For example, such an approach provides a direct means to understand the controls on chemical weathering across different spatial scales. The gained insights will also help to understand how changes in precipitation affect mineral dissolution and reaction surfaces in rinds and soils, and how these processes control river chemistry over long time scales.

This project brings together resources and expertise from the U.S., France, and UK. Graduate and undergraduate students at Univ. of Texas at El Paso (UTEP), one of the largest Ph.D.-granting Hispanic Serving Institutes in the U.S., and Dickinson College, an undergraduate-only liberal arts college in Pennsylvania will conduct research at an international Critical Zone research site (Guadeloupe, France) and in research facilities at Pennsylvania State University, Institut de Physique du Globe de Paris, Univ. of Strasbourg, and Univ. of Bristol. This importance is highlighted for UTEP and Dickinson College where the students are rarely exposed to such opportunities at international levels. This project will also support one early career faculty (PI Ma) at UTEP. Educational and outreach activities at UTEP and Dickson College, in collaboration with the NSF funded Pathways and STEP Scholars, as well as Earth Science Day at UTEP, will expose local high school students and general public in the rapidly growing and diverse El Paso region to cutting edge Critical Zone research topics (water, soils, and environments). The project will attract future STEM students who wish to study and solve emerging environmental problems facing the local community.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Engel, Jacqueline M., Ma, Lin, Sak, Peter B., Gaillardet, Jerome, Ren, Minghua, Engle, Mark, and Brantley, Susan "Quantifying chemical weathering rates along a precipitation gradient on Basse-Terre Island, French Guadeloupe: new insights from U-series isotopes in weathering rinds" Geochimica Cosmochimica Acta , v.195 , 2016 , p.29 http://dx.doi.org/10.1016/j.gca.2016.08.040
Lebedeva, M., and Brantley, S. L. "Weathering and erosion of fractured bedrock systems" Earth Surface Processes and Landforms , 2017 10:1002/esp.4177
Lebedeva, Marina I.; Sak, Peter B.; Ma, Lin; and Brantley, Susan L. "Using a mathematical model of a weathering clast to explore the effects of curvature on weathering" Chemical Geology , v.404 , 2015 , p.88 http://dx.doi.org/10.1016/j.chemgeo.2015.03.027
Lebedeva, M. I., P. B. Sak, L. Ma, and S. L. Brantley "Using a mathematical model of a weathering clast to explore the effects of curvature on weathering" Journal publication , v.404 , 2015 , p.88 10.1016/j.chemgeo.2015.03.027
Lebedeva, M.I., P. B. Sak, L. Ma, and S.L. Brantley "Using a mathematical model of a weathering clast to explore the effects of curvature on weathering" Chemical Geology , v.404 , 2015 , p.88

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The research team, which includes multiple PIs and collaborators from US, French, Australia, and UK institutions and graduate/undergraduate students from minority-serving or undergraduate-only institutions, has worked closely to investigate important chemical weathering processes at a tropical volcanic setting. The project has produced one large and comprehensive isotope dataset for weathering rinds, soil profiles, vegetation samples, streams and rivers for the tropical volcanic island. In addition, trace and major element datasets and geophysical profiles were also generated during this project.

         This collective research work has elucidate important controlling mechanisms for weathering rind formation and long term chemical weathering rates: curvature and mean annual precipitation at a watershed scale. Both are important mechanisms operating at timescales of thousands of years. Furthermore, the research reveals the importance of dust and volcanic ash as a critical mineral nutrient source to support ecosystems in highly weathered tropical systems. This observation is consistent with studies in similar tropical volcanic settings around the world. However, this study also finds that despite the importance of dust and volcanic ash to supply critical and insoluble nutrients such as P to surface soils, many soluble nutrient sources (such as Ca, Mg, Sr) are provided dominantly by aerosols from precipitation. This is an unique observation for areas with extremely high precipitation. Solute sources in first order streams change from rainwater-derived to bedrock-derived along the flow path from headwater to steam outlet over a distance of less than 1000m. Such change reveals the presence of two different weathering regimes within small watersheds: a highly weathered and slow weathering regime which occurs near the headwaters where the region is characterized by a thick and depleted soil profile (rain-water dominant chemistry) vs. a high erosion/thin regolith area with active inputs from weathering fronts at low elevation outlet area (bedrock-derived chemistry). The changes along the stream are linked to the longitudinal profile with respect to locations of local knick-points. Such an observation highlights the importance of topography on controlling short-term weathering processes and stream chemistry.


Last Modified: 12/29/2017
Modified by: Susan L Brantley

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