Award Abstract # 0948878
Facility Support: The Arizona State University SIMS Laboratories

NSF Org: EAR
Division Of Earth Sciences
Recipient: ARIZONA STATE UNIVERSITY
Initial Amendment Date: June 10, 2010
Latest Amendment Date: September 29, 2014
Award Number: 0948878
Award Instrument: Continuing Grant
Program Manager: David Lambert
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: June 15, 2010
End Date: September 30, 2015 (Estimated)
Total Intended Award Amount: $909,546.00
Total Awarded Amount to Date: $970,258.00
Funds Obligated to Date: FY 2010 = $289,451.00
FY 2011 = $302,389.00

FY 2012 = $317,706.00

FY 2014 = $60,712.00
History of Investigator:
  • Richard Hervig (Principal Investigator)
    hervig@asu.edu
  • Peter Williams (Co-Principal Investigator)
  • Lynda Williams (Co-Principal Investigator)
Recipient Sponsored Research Office: Arizona State University
660 S MILL AVENUE STE 204
TEMPE
AZ  US  85281-3670
(480)965-5479
Sponsor Congressional District: 04
Primary Place of Performance: Arizona State University
660 S MILL AVENUE STE 204
TEMPE
AZ  US  85281-3670
Primary Place of Performance
Congressional District:
04
Unique Entity Identifier (UEI): NTLHJXM55KZ6
Parent UEI:
NSF Program(s): Instrumentation & Facilities
Primary Program Source: 01001011DB NSF RESEARCH & RELATED ACTIVIT
01001112DB NSF RESEARCH & RELATED ACTIVIT

01001213DB NSF RESEARCH & RELATED ACTIVIT

01001415DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s):
Program Element Code(s): 158000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This award will partially fund the ASU secondary ion mass spectrometry (SIMS) laboratories as an NSF national, multi-user facility. The laboratories support researchers by facilitating SIMS microanalyses for trace elements and isotope ratios. Examples of commonly requested analyses include: 1) the measurement of H2O, CO2, and trace element contents of glassy melt inclusions trapped in crystals recovered from explosive volcanic eruptions, 2) boron and lithium amounts and isotopic ratios in clay minerals, 3) a wide range of trace element microanalyses on minerals from low- and high-temperature environments, and 4) depth profile analyses of experimentally-derived samples to determine trace element diffusion coefficients. This support also takes the form of training visitors to use the SIMS technique and development of new analytical protocols in response to the needs of researchers. Visitors include undergraduate and graduate students, post-doctoral researchers and faculty from a wide range of Earth Science institutions.

This facility support award will make the Arizona State University secondary ion mass spectrometry instrumentation, the extensive expertise of the ASU personnel and novel analytical techniques developed at ASU available to researchers from across the US in areas including high and low-temperature geochemistry, geobiology, archaeology, climate science, and the early history of the solar system.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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(Showing: 1 - 10 of 40)
Alves, T. V.; Hermoso, W.; Franzreb, K.; Ornellas, F. R. "Calcium-containing diatomic dications in the gas phase." Physical Chemistry Chemical Physics , v.13 , 2011 , p.18297 10.1039/C1CP20735K
Ardia P., Hirschmann, M.M., Withers, A. C., and Tenner, T.J. "H2O storage capacity of olivine at 58GPa and consequences for dehydration partial melting of the upper mantle." Earth andPlanetaryScienceLetters , v.345-348 , 2012 , p.104-116
Ardia, P., Hirschmann, M.M., Withers, A.C., Stanley, B.D. "Solubility of CH4 in a synthetic basaltic melt, with applications to atmosphere?magma ocean?core partitioning of volatiles and to the evolution of the Martian atmosphere" Geochimica et Cosmochimica Acta , v.114 , 2013 , p.52-71 http://dx.doi.org/10.1016/j.gca.2013.03.028
Bachmann, O; Wallace, PJ; Bourquin, J "The melt inclusion record from the rhyolitic Kos Plateau Tuff (Aegean Arc)" CONTRIBUTIONS TO MINERALOGY AND PETROLOGY , v.159 , 2010 , p.187 View record at Web of Science 10.1007/s00410-009-0423-
Batista, A. P., de Lima, J. C., Franzreb, K.,and Ornellas, F. R. "A theoretical study of SnF2+, SnCl2+, and SnO2+ and theirexperimental search" THE JOURNAL OF CHEMICAL PHYSICS , v.137 , 2012 , p.1-8 http://dx.doi.org/10.1063/1.4758475
Begue, F. B., Deering, C. D.,Gravley, D. M., Kennedy, B. M., Chambefort,I., Gualda, G. A. R., and Bachmann, O. "Extraction, Storage and Eruption of Multiple Isolated Magma Batches in the Paired Mamaku and Ohakuri Eruption, TaupoVolcanic Zone, New Zealand" Journal of Petrology , v.55 , 2014 , p.1653 10.1093/petrology/egu038
Behr, WM; Platt, JP "A naturally constrained stress profile through the middle crust in an extensional terrane" EARTH AND PLANETARY SCIENCE LETTERS , v.303 , 2011 , p.181 View record at Web of Science 10.1016/j.epsl.2010.11.04
Behr, WM; Thomas, JB; Hervig, RL "Calibrating Ti concentrations in quartz for SIMS determinations using NIST silicate glasses and application to the TitaniQ geothermobarometer" AMERICAN MINERALOGIST , v.96 , 2011 , p.1100 View record at Web of Science 10.2138/am.2011.370
Berlo, K; Stix, J; Roggensack, K; Ghaleb, B "A tale of two magmas, Fuego, Guatemala" BULLETIN OF VOLCANOLOGY , v.74 , 2012 , p.377 View record at Web of Science 10.1007/s00445-011-0530-
Bloch, E.Ganguly, J.Hervig, R. L. "176Lu-176Hf geochronology of garnet I. Experimental determination of the diffusion kinetics of Lu3+ and Hf4+ in garnet, closure temperatures, and geochronological implications." Contributions to Mineralogy and Petrology , v.169 , 2015 , p.12 10.1007/s00410-015-1109-8
Brites, V.; Franzreb, K.; Harvey, J.N.; Sayres, S.G.; Ross, M.W.; Blumling, D.E.; Castleman, A.W.; Hochlaf, M. "Oxygen-containing gas-phase diatomic trications and tetracations: ReOz+, NbOz+ and HfOz+ (z=3, 4)" Physical Chemistry Chemical Physics , v.13 , 2011 , p.15233 10.1039/C1CP21566C
(Showing: 1 - 10 of 40)

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.

This NSF grant supported the operation of the Arizona State University secondary ion mass spectrometer (SIMS) laboratories to act as a national facility for earth science researchers. SIMS instruments are commercially available largely because of the demands of the semiconductor industry, but are far too expensive to be commonly available in academic research environments (the replacement cost for the instrument supported by this grant is >$3M).

SIMS is applied to earth science research through its ability to make chemical and isotopic analyses on very small areas (about 1/10th the diameter of a human hair) in natural materials (minerals and glasses contained in sedimentary, igneous, or metamorphic rocks). Some geoscience researchers study processes deep in planetary interiors, conducting experiments at high pressure and temperature to simulate these conditions. Microanalyses of the products of these experiments (often quite small) represent another common task at our SIMS lab. This technique is very sensitive, allowing concentrations of many elements to be quantified at the 1 part-per-million level and below. However, in addition to its expense, the operation of this specialized equipment is quite complex with a steep learning curve to gain mastery.

Our charge is to simplify the operation so that visiting geoscience researchers can be trained to obtain chemical analyses by themselves (with our assistance). We expect visitors to become mostly independent in approximately one to four hours after getting started. We also help them prior to their visit, because the proper preparation of their samples for analysis is very important. During their trip, we help them modify their analysis routine based on what they have learned (to maximize efficiency). During and after their trip we help them interpret their chemical analyses (if requested).

Visitors include undergraduate students, graduate students, post-doctoral researchers, and faculty members from many universities across the U.S. Our lab is busy maintaining the instrument and helping visitors about 2/3 of the available time. If analytical time is available, we also help ASU research engineers characterize experimental photovoltaic and integrated circuit devices. The rest of the instrument time is applied to developing new analytical techniques for future research questions in the geosciences and working at improving the physical capabilities of the instrument (more efficient ion sources, for example). Some of these improvements can result in partnerships with industry. Because of the interest in this type of analysis, we conduct an annual workshop aimed at teaching students more about how SIMS works. The grant supports the travel and lodging costs of U.S. students during the three-day event held each January. 

 


Last Modified: 11/23/2015
Modified by: Richard L Hervig

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