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Si cycling and isotope fractionation: Implications on weathering and . . . The aims of this study are: (1) to understand the fractionation of Si isotopes among rock, soil, water and plants in granitic watersheds; (2) to trace the Si pathways of translocation and identify water Si sources in the watersheds and (3) to further understand soil formation process and mechanisms related to Si cycling in subtropical areas
Iron cycling and isotope fractionation in terrestrial ecosystems Biogeochemical processes taking part in the Fe cycle frequently fractionate stable Fe isotopes, leaving soil, plant and other compartments of the ecosystems with varied Fe isotopic signatures In this work, we reviewed the Fe isotope fractionation processes that have been reported so far for terrestrial ecosystems
自然地理学 - 张甘霖 - 中国科学院南京地理与湖泊研究所 Three-Dimensional Mapping of Organic Carbon using Piecewise Depth Functions in the Red Soil Critical Zone Observatory Soil Science Society of America Journal, 83: 687-696 [13]Yang, Jin-Ling, Zhang, Gan-Lin 2019 Si cycling and isotope fractionation: Implications on weathering and soil formation processes in a typical subtropical area
Physical weathering by glaciers enhances silicon mobilisation and . . . These experiments illustrate the critical role of physical processes in driving isotopic fractionation and biogeochemical weathering in subglacial environments Understanding perturbations in high latitude Si cycling under climatic change will likely depend on the response of mechanochemical weathering to increased glacial melt
Iron Isotope Fractionation and Biogeochemical Cycling in Soils Research in this field has illuminated the intertwined roles of natural weathering, organic matter interactions and both anthropogenic and natural redox processes in shaping isotopic signatures