
NSF Org: |
EAR Division Of Earth Sciences |
Recipient: |
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Initial Amendment Date: | January 7, 2013 |
Latest Amendment Date: | August 13, 2013 |
Award Number: | 1304352 |
Award Instrument: | Continuing Grant |
Program Manager: |
Enriqueta Barrera
EAR Division Of Earth Sciences GEO Directorate for Geosciences |
Start Date: | August 1, 2012 |
End Date: | May 31, 2017 (Estimated) |
Total Intended Award Amount: | $244,448.00 |
Total Awarded Amount to Date: | $244,448.00 |
Funds Obligated to Date: |
FY 2011 = $68,533.00 FY 2013 = $141,547.00 |
History of Investigator: |
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Recipient Sponsored Research Office: |
107 S INDIANA AVE BLOOMINGTON IN US 47405-7000 (317)278-3473 |
Sponsor Congressional District: |
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Primary Place of Performance: |
980 Indiana Ave. Indianapolis IN US 46202-2915 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): |
EDUCATION AND HUMAN RESOURCES, Geobiology & Low-Temp Geochem |
Primary Program Source: |
01001112DB NSF RESEARCH & RELATED ACTIVIT 01001314DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
Greater understanding of redox-active elements like sulfur and iron are key in the processes that affect problems such as ocean transitions through deep time, sour gas and oil evolution, hydrothermal chemistry and the origins of life, the supply of iron to the sea, industrial desulfurization, agricultural sulfur cycling, and metal mobility. Microorganisms have been a potentially important part of sulfur cycling for billions of years (Johnston et al., 2005; Mojzsis et al, 2007), yet many of the fundamental interactions between microorganisms and elemental sulfur are not understood. Advancing our understanding of how these systems behave requires delving into the detailed interactions between cells (bacterial, archaeal, and eukaryotic), minerals (especially nanoparticles), and water chemistry (especially redox speciation).
Intellectual Merit: Elemental sulfur occurs as bulk and nanoparticulate phases and can be utilized by microorganisms for all 3 major catabolic paths through use as an electron acceptor, donor, or essentially both in the case of disproportionation. Dissolved sulfur species also interact with elemental sulfur, and those species can additionally react with metals, most importantly iron. Microorganisms must solubilize elemental sulfur in order to metabolize it, but this mineral is fundamentally different from other minerals where microbe-mineral interactions have been well studied, such as iron oxide minerals (for example Hernandez and Newman, 2001; Childers et al., 2002; Burgon et al., 2003; Lovley, 2008; Newman, 2008). Solubilizing elemental sulfur can be accomplished through interaction with organic ligands or through interactions with other sulfur species to form new soluble intermediates such as polysulfides. Investigator proposes to develop a combined in situ analytical capability to investigate sulfur speciation and elemental sulfur mineralogy in field and laboratory tests to address the following hypothesis: The size and surface character of elemental sulfur is a key component controlling sulfur cycling in biotic and abiotic reactions in many environments.
Broader Impacts: Advances in fundamental cell-mineral-redox interactions in the sulfur system provide an opportunity to integrate some exciting educational experiences to engage stakeholders and professionals in health, policy, and legal fields with research goals that will yield transformative insights of value to the broad study of sulfur-based microorganisms and element cycling through time and in environmentally relevant systems. Sulfur species and minerals are importantly affected by a number of known organisms, but the level of detail proposed for elemental sulfur particle size/character and redox speciation has never been applied. When comparing the wealth of information that has come from years of investigating detailed iron oxide-microbe interactions (Newman, 2008), a detailed investigation of fundamental microbe-mineral-redox interactions involving sulfur may yield critical new insights. The application of the knowledge gained through these investigations of the sulfur system can be applied to broader thinking about similar cell-mineral-redox interactions that affect problems of human health. This opens an opportunity to advance the training of scientists to communicate results with the non-scientific public, and provide training to the medical professionals, policymakers, and legal professionals that utilize mineralogical, geochemical, and microbial information in addressing problems such as asbestos mineral exposure, groundwater arsenic contamination, and selenium toxicity. A series of classes and professional workshops will be developed, alongside a series of learning modules illustrating fundamental cell-mineral-redox interactions, to engage students and professionals in hands-on experiences of how geochemical, mineralogical, and microbial data is gathered, assessed, evaluated, and debated to arrive at reliable information. The participation of stakeholders in the practice of scientific data collection, evaluation, and debate integrated with the training of scientists with better communication skills represents not only an advance in the preparation of scientists, but an advance also in preparing professionals who will work with those scientists.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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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.
Sulfur is a critical element that transforms due to electron transfer reactions into a variety of intermediate chemical forms and a solid form called elemental sulfur. Elemental sulfur can exist in a number of different specific solid forms that vary in size, surface chemistry, and molecular arrangement and can form both abiotically and biotically. We have investigated how these different forms of elemental sulufr, especially forms related to biological formation of elemental sulfur, affect the reactions determining the distribution of different intermediate forms of sulfur (see Figure 1). By developing and refining several methods to characterize sulfur species and elemental sulfur solid forms, and through a series of laboratory experiments, we were able to determine the speed of the reactions controlling sulfur intermediates, and determine that these distributions are consistent with observations of these sulfur intermediates in a variety of natural settings. We then performed a series of experiments, and in collaboration with colleagues in Germany, developed methods to determine how these sulfur intermediates can react with many different organic carbon molecules in water. We were able to determine a whole new set of critical observations showing how sulfur and carbon interact in freshwater and marine waters and sediments.
These reactions, and an understanding of how elemental sulfur solid forms may affect them, is important for processes including how oil, coal, and natural gas deposits form, and how excess sulfur (which can be harmful to the drilling, production, and refining equpment used in energy extraction and refinement) can be more efficiently removed. Additionally, sulfur transformations are key in agricultral fertilization as many fertilizers also add sulfur to stimulate plant growth, in discovering and utilizing metal deposits, in efficient extraction and mobilization of metal contaminants, and in understanding mobility of nanoparticle transport into various water bodies. Sulfur transformations described in this work are also important in interpreting possible biosugnatures associated with life on other planets and in the earth's record of life through deep time in rocks. It is our hope that the fundamental scientific knowledge this advances will have impact in a number of applications - commercial, industrial, and in exploration with positive economic and societal impact.
These advances in interactions between nanoparticle minerals, cells, and dissolved chemical compounds has also been used to develop learning modules in the classroom, and for use in communicating key scientific ideas to the lay and professional public. These modules have addressed fundemental interactions as described above, and those that impact human health as well, with fundamental cell-mineral-redox interactions being a potential part of deleterious health effects associated with inhalation and ingestion of significant quantities of natural and synthetic dust materials. As part of this grant, we have also trained two graduate students in this field, and a number of undergraduate students have participated both directtly with this research and in the classrooom.
Last Modified: 08/27/2018
Modified by: Gregory K Druschel
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