Understanding controls on redox processes in floodplain sediments of the Upper Colorado River Basin.

导出 LinkOut

翻译打印收藏纠错

作者： Vincent,Noël ^[1] ; Kristin,Boye ^[2] ; Ravi K,Kukkadapu ^[3] ; Sharon,Bone ^[1] ; Juan S,Lezama Pacheco ^[2] ; Emily,Cardarelli ^[4] ; Noémie,Janot ^[1] ; Scott,Fendorf ^[4] ; Kenneth H,Williams ^[5] ; John R,Bargar ^[6]

作者单位： Stanford Synchrotron Radiation Lightsource, SLAC National Accelerator Laboratory, Menlo Park, CA 94025, United States. ^[1] Stanford Synchrotron Radiation Lightsource, SLAC National Accelerator Laboratory, Menlo Park, CA 94025, United States; Department of Environmental Earth System Science, Stanford University, Stanford, CA 94305, United States. ^[2] Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, WA 99354, United States. ^[3] Department of Environmental Earth System Science, Stanford University, Stanford, CA 94305, United States. ^[4] Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, United States. ^[5] Stanford Synchrotron Radiation Lightsource, SLAC National Accelerator Laboratory, Menlo Park, CA 94025, United States. Electronic address: bargar@slac.stanford.edu. ^[6]

关键词 Floodplain sediments Iron and sulfur Redox processes Upper Colorado River Basin X-ray absorption spectroscopy