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Research

Dr. Elwood Madden in front of a glacier

How do geoscience departments reward faculty, staff, and students who are working to make our field more divers, equitable and inclusive? 

This project aims to identify, empower, and reward diversity, equity, and inclusion (DEI) champions within the geosciences by aligning hiring, promotion, award, and other evaluation systems with goals to promote diversity and inclusion within our field.  Working with with the Southwest Center for Human Relations Studies (SWCHRS), we will learn from and work with national leaders in diversity, equity, and inclusion (DEI) initiatives in higher education to revise and re-envision evaluation and reward structures within academic units that recruit and train the next generations of geoscientists. More information can be found here.

How fast do minerals react with salty water? What secondary minerals form in these environments? Can we detect evidence of high-salinity alteration on Mars and other planetary bodies?

We are working to answer these questions via mineral dissolution experiments in high salinity brines, supported by NASA.  Recent publications include:

Can we use Raman spectroscopy to measure aqueous solutes in high salinity brines? How can we apply  these techniques to measure aqueous solutes remotely on other planetary bodies?

The Fall 2015 GeoWriting class developed initial calibration curves for solutes in high salinity brines. Research is ongoing to continue this investigation.

McGraw LM, McCollom NM, Phillips-Lander CM, Elwood Madden ME (2018) Measuring Sulfate and Perchlorate in High Salinity Planetary Waters using Raman Spectroscopy, ACS Earth and Space Chemistry, 2 (10), 1068-1074. DOI: 10.1021/acsearthspacechem.8b00082

What clues can we observe in fluvial sediments that will help us determine the climate in which these clastic sediments formed?  Do glacially generated sediments weather differently than sediments produced in warmer climates?  How does reactive surface area affect chemical weathering of primary minerals in different climates? 

Through collaborations with sedimentologist Lynn Soreghan and her students, we have conducted five field studies to compare fluvial sediment textures and chemical weathering indicators under different modern climate conditions funded by NSF. Reactive surface area experiments are underway, funded by a follow-up grant from NSF.

How fast does gas react with ice to form clathrates at low temperatures? How quickly do these clathrate compounds dissociate to form ice and gas under low temperature and pressure  conditions? How do gases diffuse through ice and clathrate at low temperatures?

We recently acquired a High Resolution Mapping Raman Microscope/Spectrometer to observe volatile behavior in ice and clathrates under planetary analog conditions. Recent publications include: