An improved pyrite pretreatment protocol for kinetic and isotopic studies

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Natella Mirzoyan, Alexey Kamyshny, Itay Halevy
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引用次数: 2

Abstract

Pyrite is one of the most abundant and widespread of the sulfide minerals with a central role in biogeochemical cycles of iron and sulfur. Due to its diverse roles in the natural and anthropogenic sulfur cycle, pyrite has been extensively studied in various experimental investigations of the kinetics of its dissolution and oxidation, the isotopic fractionations associated with these reactions, the microbiological processes involved, and the effects of pyrite on human health. Elemental sulfur (S0) is a common product of incomplete pyrite oxidation. Preexisting S0 impurities as unaccounted reaction products are a source of experimental uncertainty, as are adhered fine grains of pyrite and its oxidation products. Removal of these impurities is, therefore, desirable.

A robust standardized pretreatment protocol for removal of fine particles and oxidation impurities from pyrite is lacking. Here we describe a protocol for S0 and fine particle removal from the surface of pyrite by rinsing in acid followed by repeated ultrasonication with warm acetone.

Our data demonstrate the presence of large fractions of S0 on untreated pyrite particle surfaces, of which only up to 60% was removed by a commonly used pretreatment method described by Moses et al. (GCA 51:1561-1571, 1987). In comparison, after pretreatment by the protocol proposed here, approximately 98% S0 removal efficiency was achieved. Additionally, the new procedure was more efficient at removal of fine particles of adhered pyrite and its oxidation products and did not appear to affect the particle size distribution, the specific surface area, or the properties of grain surfaces.

The suggested pyrite pretreatment protocol is more efficient in removal of impurities from pyrite grains, and provides multiple advantages for both kinetic and isotopic investigations of pyrite transformations under various environmental conditions.

Abstract Image

一种用于动力学和同位素研究的改进的黄铁矿预处理方案
黄铁矿是最丰富、分布最广的硫化物矿物之一,在铁和硫的生物地球化学循环中起着核心作用。由于其在自然和人为硫循环中的不同作用,黄铁矿在其溶解和氧化动力学、与这些反应相关的同位素分馏、所涉及的微生物过程以及黄铁矿对人体健康的影响等各种实验研究中得到了广泛的研究。单质硫(S0)是黄铁矿不完全氧化的常见产物。作为未计数的反应产物,先前存在的硫杂质是实验不确定性的来源,黄铁矿及其氧化产物粘附的细颗粒也是如此。因此,需要去除这些杂质。目前还缺乏一种用于去除黄铁矿中细颗粒和氧化杂质的可靠的标准化预处理方案。在这里,我们描述了一个方案,从硫铁矿表面的硫和细颗粒去除酸冲洗,然后用温丙酮反复超声。我们的数据表明,未经处理的黄铁矿颗粒表面存在大量的so0, Moses等人描述的常用预处理方法只能去除其中的60% (GCA 51:1561-1571, 1987)。相比之下,采用本文提出的方案预处理后,S0的去除率约为98%。此外,新方法在去除粘附的黄铁矿及其氧化产物的细颗粒方面更有效,并且似乎不影响颗粒尺寸分布,比表面积或晶粒表面的性质。本文提出的黄铁矿预处理方案能够更有效地去除黄铁矿颗粒中的杂质,并为各种环境条件下黄铁矿转化的动力学和同位素研究提供了多种优势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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