单质硫粗化动力学

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geochemical Transactions Pub Date : 2014-08-06 DOI:10.1186/s12932-014-0011-z
Angel A Garcia, Gregory K Druschel
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引用次数: 38

摘要

单质硫以多种形式存在于自然系统中,从溶解形式(记为S8(diss)或水中的S8(aq))到散装单质硫(最稳定的α-S8)。单质硫可以通过几种生物和非生物过程形成,许多是从小的硫氧化物或多硫硫分子开始的,这些分子会粗化成S8环,然后合并成更大的形式。单质硫的形成可以通过两种主要技术来实现,即在水中形成液态硫的乳液,称为硫溶胶,它近似于自然系统中可能形成单质硫的一些机制。这些技术产生疏水(S8(魏玛))和亲水(S8(多硫化物))溶胶,它们以纳米颗粒和胶体悬浮液的形式存在。这些溶胶开始时是小的硫氧化物或多硫硫分子,或溶解的S8(aq)形式,但通过经典成核、聚集过程和/或奥斯特瓦尔德成熟的结合,迅速变成纳米颗粒并变粗成微米大小的颗粒。采用动态光散射(DLS)方法对不同理化条件下单质硫颗粒粗化速率进行了研究。成核速率和初始粗化速率在几秒到几分钟内发生,其速度太快,无法用DLS测量,随后S8(纳米)和S8(溶胶)的粗化与温度密切相关,在75°C时的速率比20°C快20倍。除了已知的这些分子对单质硫溶解度的影响外,表面活性剂的添加(利用离子和非离子表面活性剂作为模型化合物)还显著降低了粗化速率。DLS和冷冻扫描电镜结果表明,粗化主要是成熟过程的产物,而不是颗粒聚集,特别是在较高温度下。将粗化率数据拟合到已建立的奥斯特瓦尔德成熟模型中,进一步支持这是粗化的主要机制。单质硫溶胶在高温下迅速变粗,由于与表面活性剂的相互作用,对溶解度和颗粒变粗动力学都有显著影响。单质硫纳米颗粒和溶胶的生长在很大程度上受奥斯特瓦尔德成熟过程的支配。
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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Elemental sulfur coarsening kinetics

Elemental sulfur exists is a variety of forms in natural systems, from dissolved forms (noted as S8(diss) or in water as S8(aq)) to bulk elemental sulfur (most stable as α-S8). Elemental sulfur can form via several biotic and abiotic processes, many beginning with small sulfur oxide or polysulfidic sulfur molecules that coarsen into S8 rings that then coalesce into larger forms:

Formation of elemental sulfur can be possible via two primary techniques to create an emulsion of liquid sulfur in water called sulfur sols that approximate some mechanisms of possible elemental sulfur formation in natural systems. These techniques produce hydrophobic (S8(Weimarn)) and hydrophilic (S8(polysulfide)) sols that exist as nanoparticle and colloidal suspensions. These sols begin as small sulfur oxide or polysulfidic sulfur molecules, or dissolved S8(aq) forms, but quickly become nanoparticulate and coarsen into micron sized particles via a combination of classical nucleation, aggregation processes, and/or Ostwald ripening.

We conducted a series of experiments to study the rate of elemental sulfur particle coarsening using dynamic light scattering (DLS) analysis under different physical and chemical conditions. Rates of nucleation and initial coarsening occur over seconds to minutes at rates too fast to measure by DLS, with subsequent coarsening of S8(nano) and S8(sol) being strongly temperature dependent, with rates up to 20 times faster at 75°C compared to 20°C. The addition of surfactants (utilizing ionic and nonionic surfactants as model compounds) results in a significant reduction of coarsening rates, in addition to known effects of these molecules on elemental sulfur solubility. DLS and cryo-SEM results suggest coarsening is largely a product of ripening processes rather than particle aggregation, especially at higher temperatures. Fitting of the coarsening rate data to established models for Ostwald ripening additionally support this as a primary mechanism of coarsening.

Elemental sulfur sols coarsen rapidly at elevated temperatures and experience significant effects on both solubility and particle coarsening kinetics due to interaction with surfactants. Growth of elemental sulfur nanoparticles and sols is largely governed by Ostwald ripening processes.

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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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