Viret Fanny, Grand Stephanie
Faculty of Geosciences and Environment, University of Lausanne.
Faculty of Geosciences and Environment, University of Lausanne;
J Vis Exp. 2019 Feb 15(144). doi: 10.3791/58927.
Combined size and density fractionation (CSDF) is a method used to physically separate soil into fractions differing in particle size and mineralogy. CSDF relies on sequential density separation and sedimentation steps to isolate (1) the free light fraction (uncomplexed organic matter), (2) the occluded light fraction (uncomplexed organic matter trapped in soil aggregates) and (3) a variable number of heavy fractions (soil minerals and their associated organic matter) differing in composition. Provided that the parameters of the CSDF (dispersion energy, density cut-offs, sedimentation time) are properly selected, the method yields heavy fractions of relatively homogeneous mineral composition. Each of these fractions is expected to have a different complexing ability towards organic matter, rendering this a useful method to isolate and study the nature of organo-mineral interactions. Combining density and particle size separation brings an improved resolution compared to simple size or density fractionation methods, allowing the separation of heavy components according to both mineralogy and size (related to surface area) criteria. As is the case for all physical fractionation methods, it may be considered as less disruptive or aggressive than chemically-based extraction methods. However, CSDF is a time-consuming method and furthermore, the quantity of material obtained in some fractions can be limiting for subsequent analysis. Following CSDF, the fractions may be analyzed for mineralogical composition, soil organic carbon concentration and organic matter chemistry. The method provides quantitative information about organic carbon distribution within a soil sample and brings light to the sorptive capacity of the different, naturally-occurring mineral phases, thus providing mechanistic information about the preferential nature of organo-mineral interactions in soils (i.e., which minerals, what type of organic matter).
组合粒度与密度分级法(CSDF)是一种用于将土壤物理分离成粒度和矿物学不同的组分的方法。CSDF依靠连续的密度分离和沉降步骤来分离:(1)游离轻组分(未络合的有机物质),(2)闭蓄轻组分(困于土壤团聚体中的未络合有机物质),以及(3)数量可变的、组成不同的重组分(土壤矿物质及其相关的有机物质)。只要正确选择CSDF的参数(分散能量、密度临界值、沉降时间),该方法就能产生矿物组成相对均匀的重组分。预计这些组分中的每一种对有机物质都具有不同的络合能力,这使得该方法成为分离和研究有机-矿物相互作用性质的有用方法。与简单的粒度或密度分级方法相比,结合密度和粒度分离可提高分辨率,从而能够根据矿物学和粒度(与表面积有关)标准分离重组分。与所有物理分级方法一样,它可能被认为比基于化学的提取方法干扰性或侵蚀性更小。然而,CSDF是一种耗时的方法,此外,某些组分中获得的材料数量可能会限制后续分析。CSDF之后,可对各组分进行矿物组成、土壤有机碳浓度和有机物质化学分析。该方法提供了关于土壤样品中有机碳分布的定量信息,并揭示了不同天然存在的矿物相的吸附能力,从而提供了关于土壤中有机-矿物相互作用优先性质的机制信息(即哪些矿物、何种类型的有机物质)。