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长期受制革厂废物污染土壤中六价铬形态的形成与固定。

Formation and Immobilization of Cr(VI) Species in Long-Term Tannery Waste Contaminated Soils.

机构信息

Natural Resources and Environmental Studies Graduate Program, University of Northern British Columbia, Prince George, British Columbia V2N 4Z9, Canada.

Ecosystem Science & Management Program, University of Northern British Columbia, Prince George, British Columbia V2N 4Z9, Canada.

出版信息

Environ Sci Technol. 2020 Jun 16;54(12):7226-7235. doi: 10.1021/acs.est.0c00156. Epub 2020 Jun 5.

Abstract

Chromium speciation in naturally contaminated soils appears more complex than spiked studies have shown. This study characterized Cr speciation (oxidation states; availability; molecular geometry) intended to highlight the genesis of immobile Cr(VI) species in long-term tannery waste-contaminated soils. In a series of samples obtained from Shuitou in China, chemical extraction methods showed that Cr(III) was dominant(>96.7% of total Cr), with Cr(VI) concentration up to 144 mg kg. Of the total Cr(VI) present, immobile Cr(VI) represents >90%. Synchrotron-based X-ray near-edge structure spectroscopy (XANES) showed the occurrence of Cr(VI), which was not removed by phosphate buffer extraction, confirming a significant amount of immobile Cr(VI) fractions in soils. X-ray fluorescence maps exhibited the heterogeneous distribution of Cr in soils associated with both Mn and Fe. Such a distribution suggests Cr(III) oxidation to Cr(VI) by Mn oxides and a possible immobilization of both Cr(III) and Cr(VI) onto Fe (hydr)oxides. Linear combination fitting of XANES spectra revealed that fractional weights (%) in samples were CrFeO (49.3-53.6), CrOOH (22.3-30.8), and CaCrO (13.2-25.3). Our results demonstrate that (i) Cr(VI) is immobilized in soils and (ii) mechanisms of Cr(VI) immobilization are CaCrO precipitation and recrystallization with Fe (hydr)oxides.

摘要

自然污染土壤中的铬形态似乎比添加研究显示的更为复杂。本研究旨在描述 Cr 形态(氧化态;可用性;分子几何形状),以突出长期制革废物污染土壤中不移动的 Cr(VI) 物种的成因。在中国水头获得的一系列样品中,化学提取方法表明 Cr(III) 占主导地位(>总 Cr 的 96.7%),Cr(VI)浓度高达 144mgkg。存在的总 Cr(VI)中,不移动的 Cr(VI) 占>90%。基于同步加速器的 X 射线近边结构光谱(XANES)显示了 Cr(VI) 的存在,其不能被磷酸盐缓冲液提取去除,证实了土壤中存在大量不移动的 Cr(VI) 。X 射线荧光图谱显示了 Cr 与 Mn 和 Fe 相关的土壤中的不均匀分布。这种分布表明 Mn 氧化物将 Cr(III)氧化为 Cr(VI),并且 Cr(III)和 Cr(VI)可能都固定在 Fe(水合)氧化物上。XANES 光谱的线性组合拟合表明,样品中的分重(%)分别为 CrFeO(49.3-53.6)、CrOOH(22.3-30.8)和 CaCrO(13.2-25.3)。我们的结果表明,(i) Cr(VI) 在土壤中被固定,(ii) Cr(VI) 固定的机制是 CaCrO 沉淀和与 Fe(水合)氧化物的再结晶。

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