A New Albite Microanalytical Reference Material from Piz Beverin for Na, Al and Si Determination, and the Potential for New K-Feldspar Reference Materials

IF 2.7 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Julien M. Allaz, Marcel Guillong, Lorenzo Tavazzani, Georg Spiekermann, Lydia Zehnder, Emma Bullock, Joel DesOrmeau, Michael J. Jercinovic, Joachim Krause, Felix Marxer, William O. Nachlas, John Spratt
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Abstract

Determination of alkali elements is important to Earth scientists, yet suitable and reliable microanalytical reference materials are lacking. This paper proposes a new albite reference material and evaluates the potential for future K-feldspar reference materials. The proposed Piz Beverin albite reference material from Switzerland yields a homogeneous composition at the centimetre- to micrometre-scale for Si, Al and Na with < 2000 μg g-1 total trace elements (mostly heterogeneously distributed Ca, K and Sr). EPMA and LA-ICP-MS measurements confirm a composition of 99.5(2)% albite component, which is supported further by bulk XRF measurements. A round robin evaluation involving nine independent EPMA laboratories confirms its composition and homogeneity for Si, Al and Na. In addition, a set of five distinct clear K-feldspar samples was evaluated as possible reference materials. The first two crystals of adular and orthoclase yield unacceptable inhomogeneities with > 2% relative local variations of Na, K and Ba contents. The three other investigated sets of K-feldspar crystals are yellow sanidine crystals from Itrongay (Madagascar). Despite distinct compositions, EPMA confirms they are each homogeneous at the centimetre to micrometre scale for Si, Al and K and have no apparent inclusions; further investigation to find larger amounts of these materials is therefore justified.

Abstract Image

用于测定 Na、Al 和 Si 的 Piz Beverin 新白云石微量分析标准物质,以及新钾长石标准物质的潜力
碱元素的测定对地球科学家来说非常重要,但目前缺乏合适、可靠的微量分析参考材料。本文提出了一种新的钠长石参考物质,并评价了未来钾长石参考物质的潜力。来自瑞士的Piz Beverin钠长石标准物质在厘米到微米尺度上具有均匀的Si、Al和Na组成,总微量元素(主要是不均匀分布的Ca、K和Sr)为2000 μg -1。EPMA和LA-ICP-MS测量证实其成分为99.5(2)%的钠长石成分,XRF测量进一步证实了这一点。由9个独立EPMA实验室参与的循环评估确认了其Si、Al和Na的组成和均匀性。此外,一组五种不同的透明钾长石样品被评估为可能的参考物质。成年长石和正长石的前两个晶体产生不可接受的不均匀性,Na, K和Ba含量的相对局部变化为> 2%。另外三组被调查的钾长石晶体是来自马达加斯加Itrongay的黄色水晶石晶体。尽管组成不同,EPMA证实它们在厘米到微米尺度上都是均匀的,对于Si, Al和K没有明显的夹杂物;因此,有理由进行进一步调查,以找到更多的这些材料。
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来源期刊
Geostandards and Geoanalytical Research
Geostandards and Geoanalytical Research 地学-地球科学综合
CiteScore
7.10
自引率
18.40%
发文量
54
审稿时长
>12 weeks
期刊介绍: Geostandards & Geoanalytical Research is an international journal dedicated to advancing the science of reference materials, analytical techniques and data quality relevant to the chemical analysis of geological and environmental samples. Papers are accepted for publication following peer review.
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