A novel method for extracting potassium (K) from K-poor and sodium-rich samples for high-precision stable K isotope analysis†

IF 3.1 2区 化学 Q2 CHEMISTRY, ANALYTICAL Journal of Analytical Atomic Spectrometry Pub Date : 2024-07-15 DOI:10.1039/D4JA00168K
Xin-Yuan Zheng
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Abstract

Reconstruction of stable potassium isotope composition (41K/39K) in ancient seawater has significant implications for our understanding of the fundamental controls on the long-term stability of Earth's climate and ocean chemistry, but the relevant research is hampered by scarce preservation of seawater K in geological records. Marine halite (NaCl) samples are potentially valuable archives of seawater K isotope signatures because they often contain abundant fluid inclusions directly sourced from evaporated ancient seawater. However, the extremely high Na matrix relative to low K concentrations in halite presents a formidable challenge for K isotope analysis. This study reports a novel and efficient K extraction method that can separate K from a high Na matrix by precipitating K as a sparsely soluble salt using sodium tetraphenylborate (TPB). Development of this method was based on an in-depth understanding of the TPB precipitation reaction and solubility equilibrium of relevant TPB salts. Key parameters, including reaction time, precipitate recovery and rinse, and further K purification for isotope analysis, have been optimized through extensive laboratory experiments. It is demonstrated that this new method can extract small quantities of K down to 20 μg from a large quantity of the NaCl matrix up to 1 gram. In addition, preliminary results show that this new extraction method can be also applied to prepare carbonate samples, which represent another important type of sample pertinent to K isotope research, notoriously difficult to analyze due to their low K concentrations and high Ca matrices. For the first time, this study demonstrates the utility of TPB chemistry in preparing challenging K-poor, matrix-rich samples for high-precision stable K isotope analysis.

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从贫钾和富钠样品中提取钾(K)用于高精度稳定钾同位素分析的新方法
重建古海水中稳定的钾同位素组成(41K/39K)对我们了解地球气候和海洋化学长期稳定性的基本控制具有重要意义,但由于地质记录中保存的海水钾元素很少,相关研究受到了阻碍。海洋海绿石(NaCl)样本可能是海水 K 同位素特征的宝贵档案,因为它们通常含有大量直接来自蒸发的古海水的流体包裹体。然而,相对于低 K 浓度而言,海泡石中的 Na 基质含量极高,这给 K 同位素分析带来了巨大挑战。本研究报告了一种新颖高效的钾萃取方法,该方法通过使用四苯基硼酸钠(TPB)将钾沉淀为稀溶盐,从而将钾从高Na基质中分离出来。该方法的开发基于对 TPB 沉淀反应和相关 TPB 盐类溶解平衡的深入理解。通过大量的实验室实验,对包括反应时间、沉淀回收和冲洗以及用于同位素分析的进一步 K 纯化在内的关键参数进行了优化。实验结果表明,这种新方法可以从多达 1 克的大量氯化钠基质中提取低至 20 微克的少量钾。此外,初步结果表明,这种新的萃取方法还可用于制备碳酸盐样品。碳酸盐样品是与钾同位素研究相关的另一种重要样品类型,但由于其钾浓度低、钙基质含量高而难以分析。这项研究首次证明了 TPB 化学在制备具有挑战性的贫钾、富含基质的样品以进行高精度稳定钾同位素分析方面的实用性。
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来源期刊
CiteScore
6.20
自引率
26.50%
发文量
228
审稿时长
1.7 months
期刊介绍: Innovative research on the fundamental theory and application of spectrometric techniques.
期刊最新文献
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