美国大西洋中部两处农业土壤中遗留磷的多模式微光谱标本分析

Kathryn D. Szerlag, Matthew G. Siebecker, Fatemeh Izaditame, Paul Northrup, Ryan Tappero, Donald L. Sparks
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摘要

要了解磷(P)在农业土壤中的迁移性及其潜在的环境风险,就必须直接测量固相磷的种类。通常情况下,利用块状磷 K 边 X 射线吸收近缘结构 (XANES) 光谱法,然后进行线性组合拟合 (LCF) 来确定土壤中的固态磷相。然而,这种方法可能会将结果限制在几个主要相上。此外,不同 P 物种的 XANES 光谱可能具有非常相似的特征,从而导致高估或低估它们对 LCF 的贡献。在此,通过将多模态微束-X 射线荧光(µ-XRF)绘图与 µ-XANES(微束-X 射线吸收近边缘结构)分析相结合,改进了 P 的标示,从而直接标示出微米尺度上的主要和次要 P 相。为了更好地考虑将 XANES 峰分配给单个化合物的不确定性,我们通过 "光谱特征分析 "完成了更加定量的指纹识别。通过这种分析,报告了拟合的 R 因子。这些结果与传统的 LCF 进行了比较。前沿拟合结果显示,吸附在铁酸盐上的磷酸盐存在双组分前沿特征。此外,与铁酸盐共沉淀的植酸盐(植酸-铁-铜)也有一个前沿特征,表明与铁直接相关。最后,通过多模态制图和 µ-XANES 确定了土壤中与氧化锰相关的独特 P 物种。这些结果有助于更好地预测钾的溶解和流动性。
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Multimodal, microspectroscopic speciation of legacy phosphorus in two US mid-Atlantic agricultural soils

To understand phosphorus (P) mobility in agricultural soils and its potential environmental risk, it is essential to directly measure solid phase P speciation. Often, bulk P K-edge X-ray absorption near edge structure (XANES) spectroscopy followed by linear combination fitting (LCF) is utilized to determine the solid P phases in soil. However, this method may limit results to only a few major phases. Additionally, XANES spectra for different P species may have very similar features, leading to an over- or underestimate of their contribution to LCF. Here, an improved P speciation by pairing multimodal microbeam-X-ray fluorescence (µ-XRF) mapping coupled with µ-XANES (microbeam-X-ray absorption near edge structure) analysis to directly speciate major and minor P phases on the micron scale is provided. We combined maps of both tender (P, sulfur, aluminum, and silicon) and hard energy (calcium, iron [Fe], and manganese) elements to evaluate the elemental co-locations with P. To better account for uncertainty assigning XANES peaks to individual compounds, a more quantitative fingerprinting by “spectral feature analysis” was completed. With this analysis, an R-factor is reported for the fit. These results were compared to traditional LCF. Pre-edge fitting results revealed the presence of a two-component pre-edge feature for phosphate adsorbed to ferrihydrite. Additionally, phytate co-precipitated with ferrihydrite (Phytate-Fe-Cop) had a pre-edge feature, indicating direct association with Fe. Lastly, a unique P species associated with manganese oxide was identified in the soil via multimodal mapping and µ-XANES. These results allow for better prediction of P dissolution and mobility.

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