鳞片岩
针铁矿
铁酸盐
化学
硫化物
萃取(化学)
硫化物矿物
X射线吸收精细结构
无机化学
金属
氧化物
硫黄
铁质
氧化铁
核化学
色谱法
吸附
物理
有机化学
光谱学
量子力学
作者
Man Jae Kwon,Jung‐Seok Yang,Moo Joon Shim,Maxim I. Boyanov,Kenneth Kemner,Edward J. O’Loughlin
摘要
Acid extraction followed by a colorimetric assay is a widely used approach for the determination of the total Fe(II) in samples from suboxic and anoxic environments. Under sulfidogenic conditions, these samples can contain both metal sulfides and iron (hydr)oxides. Our comparisons between 0.5 N HCl extraction and X-ray absorption fine structure (XAFS) analysis of systems containing 40 mM Fe(III) as specific (hydr)oxides and 10 mM FeS showed that the presence of sulfide can result in significant overestimation of the total Fe(II) by acid extraction. The total Fe(II) determined by XAFS was consistent with the added FeS. However, the total Fe(II) determined by extraction was significantly higher and dependent on the nature of the Fe(III) (hydr)oxides; the rates and extent of Fe(II) production were higher with ferrihydrite and lepidocrocite than with goethite. Total Fe(II) concentrations determined following acid extraction might be overestimated when iron (hydr)oxides and sulfide minerals are present in samples.
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