Yoo Research Website
It is often viewed that soils are comprised of static organic matter and inorganic minerals that are subject to hydrological, chemical and biological processes. However, biogeochemical processes of minerals and organic matter and their interactions occur as they physically move on the earth surface at the wide range of spatial and temporal scales. My research goal is to quantitatively integrate the interactions among rocks, minerals, and organic matter in motion and to use this understanding to define and resolve fundamental questions in the geochemical and geomorphic evolution of soil covered landscapes and regional to global biogeochemical cycles.
My research approaches span across theoretical/mathematical, laboratory, and field investigations. Additionally, research activities in our group cover diverse locations: Delaware Coastal Plains, Pennsylvania Piedmont, Virginia Ridge and Valley, Sierra Nevada and Coastal Ranges in California, Great Lakes Region in Minnesota, and finally the Arctic Sweden.
Burke Benjamin C., Arjun M. Heimsath, Jean L. Dixon, John Chappell, Kyungsoo Yoo, (2009), Weathering the escarpment: chemical and physical rates and processes, south-eastern Australia, Earth Surface Processes and Landforms, 34, 768–785, DOI: 10.1002/esp.1764
Klaminder Jonatan and Kyungsoo Yoo, (2008) Contaminants as Tracers for Studying Dynamics of Soil Formation: Mining an Ocean of Opportunities. In Donald L. Sparks, editor, Advances in Agronomy, Vol 100. Burlington: Academic Press, pp.15-57. (invited book chapter)
Klaminder, J., K. Yoo, J. Rydberg, and R. Giesler (2008), An explorative study of mercury export from a thawing palsa mire, J. Geophys. Res., 113, G04034, doi:10.1029/2008JG000776.
Yoo, K., S.M. Mudd, (2008), Toward process-based modeling of geochemical soil formation across diverse landforms: A new mathematical framework, Geoderma, doi:10.1016/j.geoderma.2008.05.029
Yoo K. and S.M. Mudd, (2008), The Discrepancy between Mineral Residence Time and Soil Age: Implications for the Interpretation of Chemical Weathering Rates, Geology, v.36; no 1, 35-38, doi: 10.1130/G24285A
Yoo, K., R. Amundson, A. M. Heimsath, W. E. Dietrich, and G. H. Brimhall (2007), Integration of geochemical mass balance with sediment transport to calculate rates of soil chemical weathering and transport on hillslopes, Journal of Geophysical Research, 112, F02013, doi:10.1029/2005JF000402.
Yoo K., R. Amundson, AM Heimsath, WE Dietrich, (2006), Spatial patterns of soil organic carbon on hillslopes: Integrating geomorphic processes and the biological C cycle, Geoderma, 130 (1-2), P47-65, doi:10.1016/j.geoderma.2005.01.008
Yoo K., R. Amundson, AM Heimsath, WE Dietrich, (2005), Process-based model linking pocket gopher (Thomomys bottae) activity to sediment transport and soil thickness, Geology, 33 (11): 917-920 Nov. 2005, doi: 10.1130/G21831.1 (mentioned in Sciencenow.sciencemag.org)
Yoo K., R. Amundson, A. M. Heimsath, W. E. Dietrich (2005), Erosion of upland hillslope soil organic carbon: Coupling field measurements with a sediment transport model, Global Biogeochem. Cycles, 19, GB3003, doi:10.1029/2004GB002271.
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