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

Author:

Allaz Julien M.1ORCID,Guillong Marcel1,Tavazzani Lorenzo1,Spiekermann Georg1,Zehnder Lydia1,Bullock Emma2,DesOrmeau Joel3,Jercinovic Michael J.4,Krause Joachim5,Marxer Felix6ORCID,Nachlas William O.7,Spratt John8

Affiliation:

1. Department of Earth Sciences, Institute of Geochemistry and Petrology ETH Zürich Clausiusstrasse 25, 8092 Zürich Switzerland

2. Carnegie Science Earth and Planets Laboratory 5241 Broad Branch Road, NW, Washington DC 20015 USA

3. Reno, Department of Geological Sciences and Engineering University of Nevada 1664 N. Virginia Street, Reno NV 89557‐0172 USA

4. 154 Morrill Science Center, Department of Geosciences University of Massachusetts 01003 Amherst USA

5. Helmholtz‐Zentrum Dresden‐Rossendorf Helmholtz Institute Freiberg for Resource Technology Chemnitzer Strasse 40,09599 Freiberg Germany

6. Institute of Mineralogy Leibniz University Hannover Callinstrasse 3, 30167 Hannover Germany

7. Madison, Department of Geoscience University of Wisconsin 1215 West Dayton Street, Madison WI 53706 USA

8. The Natural History Museum Core Research Laboratories Cromwell Road, London SW7 5BD UK

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.

Funder

Deutsche Forschungsgemeinschaft

National Science Foundation

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology,Geochemistry and Petrology,Geology

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