CHEMICAL CHANGES LEADING TO SOIL FORMATION FROM BASALTIC BEDROCK IN REYKJANES PENINSULA IN ICELAND
For this project we collected seemingly unaltered and weathered lava samples that erupted during the Reykjanes Fires in Reykjanes, and samples of fresh lava from Fagradalsfjall and Sundnukur to determine overall bedrock chemistry. We also collected samples of hydrothermally altered lava from Fagradalsfjall to search for clay minerals, zeolites and other minerals that could lead to soil formation.
We selected samples based on their alteration colors for powder X-Ray Diffraction (pXRD) analysis to compare the chemistry of unaltered and altered lava. Preliminary results indicate presence of magnesium-rich olivine and calcium-rich plagioclase in the unaltered lava from Fagradalsfjall, while hydrothermally altered samples from the same location show presence of Hydromagnesite, Hydroxylclinohumite, Mordenite, and Laumontite. These rapid chemical changes to the bedrock might also be part of the soil formation processes besides slower weathering processes.
These results provide insight into the first steps of soil production from basaltic lava in Iceland. This is important for agriculture and soil management. This poster will present our data, analytical methods, and implications of our findings.