Wei Wei , Thomas Algeo , Lin Chen , Zhiquan Li , Cody Lazowski , Katherine Snihur , Daniel Alessi , Kurt Konhauser
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引用次数: 0
Abstract
Elemental boron (B) concentrations have been shown to be useful in reconstruction of paleosalinity conditions. Accurate measurement of the B content of a sample is critical for this purpose, but B is a light and relatively volatile element, substantial amounts of which can be lost through sample preparation protocols that fail to take this property of B into consideration. Here, we evaluate the effects of four commonly used sample preparation protocols on measured B concentrations. The Conventional Acid Method uses concentrated HNO3 and HF, but the latter acid can cause volatilization of B. A second method, the modified Conventional Acid Method, uses the same acids but with the addition of H3PO4 to reduce B volatility. Two further methods eliminate HF entirely: the Ammonium Digestion Method makes use of NH4F/NH4HF2, and the Alkali Fusion Method fuses the sample with Na2O2. We tested 9 samples and 4 standards using these four pretreatment methods. Our results show that the Alkali Fusion Method consistently has the highest B yields, with an average recovery rate of ∼98 %, whereas the other methods have average yields ranging from 72 % to 92 %. Owing to the potential for incomplete B recovery using these other methods (especially the Conventional Acid Method, which has the lowest recovery rate), salinity values based on those methods are likely to be underestimated. Given the dominant use of the Conventional Acid Method in older studies reporting B concentrations, paleosalinity estimates based on those studies will require re-evaluation. In the future, we recommend that all studies measuring B concentrations make use of the Alkali Fusion Method in order to achieve near-quantitative recovery, and to provide for maximum robustness and comparability of paleosalinity estimates among studies.
期刊介绍:
Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry.
The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry.
Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry.
The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.