Award Abstract # 2041484
Upgrade of Research Equipment for the UNM Volatiles Laboratory

NSF Org: EAR
Division Of Earth Sciences
Recipient: UNIVERSITY OF NEW MEXICO
Initial Amendment Date: July 29, 2021
Latest Amendment Date: August 17, 2023
Award Number: 2041484
Award Instrument: Standard Grant
Program Manager: David Lambert
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: August 15, 2021
End Date: July 31, 2023 (Estimated)
Total Intended Award Amount: $193,204.00
Total Awarded Amount to Date: $208,049.00
Funds Obligated to Date: FY 2021 = $193,204.00
FY 2022 = $14,845.00
History of Investigator:
  • Tobias Fischer (Principal Investigator)
    fischer@unm.edu
  • Laura Crossey (Co-Principal Investigator)
Recipient Sponsored Research Office: University of New Mexico
1 UNIVERSITY OF NEW MEXICO
ALBUQUERQUE
NM  US  87131-0001
(505)277-4186
Sponsor Congressional District: 01
Primary Place of Performance: University of New Mexico
200 Yale Blvd
Albuquerque
NM  US  87131-0001
Primary Place of Performance
Congressional District:
01
Unique Entity Identifier (UEI): F6XLTRUQJEN4
Parent UEI:
NSF Program(s): Instrumentation & Facilities,
XC-Crosscutting Activities Pro
Primary Program Source: 01002223DB NSF RESEARCH & RELATED ACTIVIT
010V2122DB R&RA ARP Act DEFC V
Program Reference Code(s): 1580, 9150
Program Element Code(s): 158000, 722200
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This award is funded in whole or in part under the American Rescue Plan Act of 2021 (Public Law 117-2). It will build scientific infrastructure at the University of New Mexico (UNM) to enable the measurements of the composition of the noble gas helium in volcanic emanations and thermal springs. Currently there are very few laboratories in the US that have the ability to make these measurements in volcanic gases. The noble gas helium is used in the geosciences as a messenger of information from deep in the Earth?s interior. Changes in the composition of helium emitted from volcanic vents and thermal springs have been shown to signal the arrival of new magma into a volcanic system or the accumulation of gas pressure that can lead to volcanic eruptions. This project focusses on the helium composition emitted from the Valles Caldera in New Mexico, a super volcano that produced a massive eruption about one million years ago. This volcano still hosts a large magma body at depth and a system of thermal springs in the crater. Samples will be collected at these springs throughout the caldera and compared to recent earthquake and imaging studies to understand better the dynamics of the Valles Caldera volcanic system. What we expect to learn from the project can then be applied to other more active volcanic systems to improve our ability to forecast volcanic eruptions to save life and property. The project also supports education of traditionally underrepresented groups in the geosciences by offering a 4-week seminar on the topic of helium in the earth sciences and a field trip to a nearby helium plant that extracts this valuable commodity for commercial uses.

This project focusses on an upgrade of the UNM Volatiles Laboratory to enable the analysis of noble gas isotopes in gas samples from volcanic and hydrothermal systems. The electronics and vacuum system upgrade will significantly expand our current analytical capabilities which are limited to the relative abundance analyses of major and trace gases by gas chromatography and quadrupole mass spectrometry and to carbon stable isotope analyses by infrared isotope ratio spectrometry. The immediate application of the upgraded laboratory will be to collect and analyze a large number of gas samples from Valles Caldera, New Mexico to constrain the mantle volatile input into the magmatic-hydrothermal system through space and time. The helium isotope data collected for this purpose will be correlated spatially with newly acquired seismic tomography data to elucidate the dynamics of the magmatic system under the caldera. A temporal sampling program of gas discharges from the Valles Caldera system will enable us to develop models that can eventually inform processes leading to volcanic eruptions and improve our understanding of volatile sources (crustal versus mantle) in large caldera systems. Our broader impact activities include the teaching of an undergraduate seminar on the utility of helium isotopes in the Earth Sciences as well as helium as a resource in modern society. The seminar will target traditionally underrepresented students from UNM branch campuses and offer the opportunity to visit a helium plant to see first-hand the process of extraction of this valuable natural resource.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

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 award funded the upgrade of instrumentation in the volcanic gas analyses laboratory at the University of New Mexico. The laboratory's capabilities include the chemical analyses of gases emitted from volcanoes and active hydrothermal systems. Applications of the data obtained from the laboratory include advancing our understanding of volcanic processes that lead to hazardous eruptions and estimating deep temperatures in hydrothermal systems that can lead to insights regarding the energy potential for a hydrothermal energy generation project. The awarded grant allowed for the construction of equipment to purify volcanic and hydrothermal gases for the analyses of helium isotopes. 

The intellectual merit of this upgrade is that helium isotopes are the best tracer gases for deep Earth contributions to emissions at the Earth's surface. The ratio of the isotope helium-3 to helium-4 allows one to compute the relative contribution of helium from the deep earth and the shallower crust. Along with helium from these two sources, other important gases such as carbon dioxide and sulfur are transported from depth to the surface, therefore the relationships between these gases and the helium isotopes enables accurate characterization of the sources of these emissions. 

The broader impacts of the upgrade include applications to understand the injection of deep earth helium and other gases into volcanic systems that may indicate increased volcanic activity that could lead to hazardous eruptions. Another important broader impact is that the data on helium sources can be used to understand the formation of helium reservoirs. Helium is an importantcommodity and a limited resource with many uses in moder society. The award also trained a graduate student on the use of the instrument, including calibration and analyses of hydrothermal gas samples. In addition, undergraduate students were trained in field sampling of these gases which is the first step in obtaining valuable data. 

 


Last Modified: 12/14/2023
Modified by: Tobias P Fischer

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