Undergraduate Geology & Geography Student
Dept. Geology & Environmental Earth Science
Dept. Geology & Environmental Earth Science
Dept. Geology & Environmental Earth Science
Nickel (Ni), Cobalt (Co), and Chromium (Cr) are useful critical metals in industry, specifically in manufacturing rechargeable batteries, stainless steel, and superalloys. As many countries are transitioning to alternative forms of energy, critical metals are becoming even more important, with the demand for these elements projected to increase significantly. Since Ni, Co, and Cr are not unlimited resources, finding more efficient and environmentally conscious extraction mechanisms to facilitate the transition to a sustainable world is incredibly valuable. Critical mineral data was collected using sequential extraction methods to characterize the mineral host phases for these metals. Ultramafic rocks of variable alteration mineralogy, such as serpentinite/saprolite (Puerto Rico, Oman), laterite (Puerto Rico), talc-rich soapstone (Oman), and carbonated ultramafics (Oman), were used for analysis. Ultramafic rocks are ideal sources as they are widespread and tend to contain significant amounts of Ni, Co, and Cr compared to other available rocks. Samples were chemically treated with reagents that sequentially leached out metals from 6 fractions: exchangeable, absorbed/carbonate, organic, amorphous oxyhydroxide, crystalline oxides, and residual silicates. Each round of treatment went through an X-ray diffractometer (XRD) for mineralogical compositions. A high resolution inductively coupled plasma mass spectrometer (ICP-MS) was used to determine concentrations of Ni, Co, and Cr. Initial XRD data shows that after each extraction, there is a decrease in sharp peaks. Minerals identified include chromite, lizardite, andradite, chrysotile, and goethite. Initial ICP-MS data depicts a significant contrast between Ni, Co, and Cr during extraction. The laterite samples show that 45-65% of Ni and >97% of Co remain in the residual for each sample. In contrast, less than 30% and 43% of Co remain in the residual in the serpentinized bedrock and saprolite layer, respectively. As for Cr, 82-98% remains in the residual with the larger percent in the laterite layers. If these ultramafic samples contain sufficient concentrations of Ni, Co, and Cr in specific mineral phases, an alternative and targeted method for metal extraction may be explored to aid future energy transition goals.
Inductively Coupled Plasma Mass Spectrometry
Sequential Extraction using Chemical Reagents
X-ray Diffraction
Initial XRD data shows that after each extraction, there is a decrease in sharp peaks. Minerals identified include chromite, lizardite, andradite, chrysotile, and goethite. Initial ICP-MS data depicts a significant contrast between Ni, Co, and Cr during extraction. The laterite samples show that 45-65% of Ni and >97% of Co remain in the residual for each sample. In contrast, less than 30% and 43% of Co remain in the residual in the serpentinized bedrock and saprolite layer, respectively. As for Cr, 82-98% remains in the residual with the larger percent in the laterite layers. If these ultramafic samples contain sufficient concentrations of Ni, Co, and Cr in specific mineral phases, an alternative and targeted method for metal extraction may be explored to aid future energy transition goals.
The chemical reagents utilized need to be altered to result in a better extraction. The reagents were based on the Canadian Geological Society standards and can be adapted based on other researchers' and organizations' findings. Research will be continued through PhD student Lucas Abernathy.
The following is an image of poster presented at the 2026 Undergraduate Research Forum
GSA North-Central Section Research Grant, Miami University Dean's Scholar Research Grant, Kaiya Bensing, Lucas Abernathy
Falk, E. S., & Kelemen, P. B. (2015). Geochemistry and petrology of listvenite in the Samail ophiolite, Sultanate of Oman: Complete carbonation of peridotite during ophiolite emplacement. Geochimica et Cosmochimica Acta, 160, 70–90.
Kelemen, P. B., Carlos de Obeso, J., Leong, J. A., Godard, M., Okazaki, K., Kotowski, A. J., et al. (2022). Listvenite Formation During Mass Transfer into the Leading Edge of the Mantle Wedge: Initial Results from Oman Drilling Project Hole BT1B. Journal of Geophysical Research: Solid Earth, 127(2), e2021JB022352.
Delina, R. E., Arcilla, C., Otake, T., Garcia, J. J., Tan, M., & Ito, A. (2020). Chromium occurrence in a nickel laterite profile and its implications to surrounding surface waters. Chemical Geology, 558, 119863.
Butt, C. R., & Cluzel, D. (2013). Nickel laterite ore deposits: weathered serpentinites. Elements, 9(2), 123-128. Zauyah, S., Schaefer, C. E., & Simas, F. N. (2010). Saprolites. In Interpretation of micromorphological features of soils and regoliths (pp. 49-68). Elsevier.
Kumar, A., & Maiti, S. K. (2013). Availability of chromium, nickel and other associated heavy metals of ultramafic and serpentine soil/rock and in plants. International Journal of Emerging Technology and Advanced Engineering, 3(2), 256-268.
Emam, A., & Zoheir, B. (2013). Au and Cr mobilization through metasomatism: Microchemical evidence from ore-bearing listvenite, South Eastern Desert of Egypt. Journal of Geochemical Exploration, 125, 34-45.
Mistikawy, J. A., Mackowiak, T. J., Butler, M. J., Mischenko, I. C., Cernak Sr, R. S., & Richardson, J. B. (2020). Chromium, manganese, nickel, and cobalt mobility and bioavailability from mafic-to-ultramafic mine spoil weathering in western Massachusetts, USA. Environmental Geochemistry and Health, 42(10), 3263- 3279.
Technology: I expanded my knowledge on XRD and ICP-MS while learning new instrumentation via sequential extraction. The experiment had many different components that had to be changed throughout, so learning how to adapt was an important skill to form.
Teamwork: I worked with each member of the project to determine the scope of my responsibilities and goals for the project. We created a timeline that works best for all involved to have a successful product. Since I had to leave for 3 weeks for a summer study-away course, we communicated effectively to determine the best course of action for the project.
Communication: Through this project, I presented at 3 times at different levels (nationally, university-wide, and within my department). I am currently working with the PhD student Lucas Abernathy to summarize the findings in a concise paper. I learned when to ask questions and get help from others working on the project with me.
Career & Self Development: I learned how to conduct an in-depth experiment that is within my field of interest and prepared me for my summer 2026 internship. I determined where my strengths lie within research and what I should improve upon. Because of this project, I decided to develop a stronger background in the literature within this discipline to understand what I am working on better.
Trainings were conducted by Dr. Marion Lytle. Each step of sequential extraction was monitored and aided by Dr. James Leong. There were no external protocols that were required.