The guiding philosophy of my research. As a graduate student, I am pursuing research on Martian and ocean world chemistry, as well as complex canonical organic material formation.
Mars was once warm and wet. I am investigating the organic chemistry in such an environment and its implications for data detected by rovers today. Formatting of Objectives and Results is ongoing.
Stay tuned.
Stay tuned.
Using data collected by Cassini's Cosmic Dust Analyzer (CDA) and Ion and Neutral Mass Spectrometer (INMS), I am researching the probable organic molecules that could exist within Enceladus's sub-ice shell ocean. My approach utilizes temperature and pressure cycling of basic, reactive material detected by both CDA and INMS (e.g. HCN, CH2O, NH3...). Results have been analyzed at both ELSI and the Frank Postberg laboratory's Laser Induced Liquid Beam Ion Desorption - Mass Spectrometer (LILBID-MS) in Berlin, DE.
What molecules were detected by Cassini? Are there any simple canonical molecules that were obscured in the spectra? What material on chondritic bodies can be explained by an aqueous phase? These are all questions that we are considering during this project.
Paper is in preparation. So far, temperature has played the most vital role in chemical abundance, but not chemical diversity. A steady color change can be observed in our mixtures. A wide array of amino acids and other organic compounds formed, aligning with predicted pathways.
We're trying our best to open the pressure chamber.
Image credit: Minori Koga
As impossible as it may seem, I am currently investigating the potential of a frozen solution to act as a "drying phase". Miyakawa et al., The Cold Origin of Life (2002) showed the formation of many purine and pyrimidine molecules through simply freezing of an ammonium cyanide solution. More recently, Zandanel et al., Nature Astronomy (2022) showed that ammonia solutions can aqueously alter olivine at temperatures as low as -20 C. This type of chemistry and its mechanisms could have great implications for icy bodies like Enceladus, Ryugu, or even early Earth.
One way I think it could work is through forming highly concentrated nuclei in the ice matrix, demonstrated in the figure below:
What molecules can we form from the material found in Enceladus's plume? Could we find this on its ice shell? Do we see any of these molecules in the recent Hayabusa 2 samples? What are the formation pathways of these materials?
Analysis is currently ongoing, and a paper is in preparation. Stay tuned.
Questions, comments, suggestions, concerns? Shoot me an email at the address below!
Header image credit: ELSI