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首页> 外文期刊>Clays and clay minerals >METHODS FOR IN SITU SIMS MICROANALYSIS OF BORON AND ITS ISOTOPES IN PALAGONITE
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METHODS FOR IN SITU SIMS MICROANALYSIS OF BORON AND ITS ISOTOPES IN PALAGONITE

机译:硅钙石中硼及其同位素的原位模拟显微分析方法

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Boron has been shown to be a useful trace element in clay-mineralization reactions, raising the possibility that B studies may provide a means to investigate environmental controls on palagonitization. The objective of the present study was to address calibration, matrix effects, and B exchangeability issues such that meaningful secondary ion mass spectrometry (SIMS) microanalysis of B in thin sections of palagonite will be feasible. Silver Hill illite (IMt-1) was found to be a suitable calibration reference material, based on compositional similarity, relatively high B content, and ease of mounting on thin-section samples for SIMS microanalysis. Matrix effects of borated sideromelane and illite were compared and found to be similar, confirming previous studies which showed no matrix effects for B among minerals. Boron substitutes for Si in tetrahedral sites and also can be adsorbed in exchangeable sites of 2:1 clay minerals. Similarly, B can be found in tetrahedral and exchangeable sites within palagonite, which consists of both layered and amorphous volumes. In order to measure tetrahedral B content and isotopic ratio in the palagonite, exchangeable B was removed by soaking sample thin sections in a 1 M NH_4Cl solution until exchangeable cation concentrations were constant. Treated samples showed decreases in B content and isotopic ratio with exchange. Extraction of exchangeable B permits the direct measurement of tetrahedral B content and isotopic ratio. The exchange technique devised and tested here should have broad applicability to thin-section microanalysis of B in clay and clay-like materials where cation exchange can be used for surface-analytical techniques. The present study represents an initial attempt to address sample-preparation, calibration, and potential matrix-effects problems for analyses by SIMS. Further refinements may improve the accuracy of the measurements, but the results presented here indicate that meaningful measurements are possible.
机译:硼已被证明是在粘土矿化反应中有用的微量元素,这增加了B研究可能为研究环境控制泛滥的可能性提供了可能性。本研究的目的是解决校准,基质效应和B交换性问题,以便在方石的薄片中对B进行有意义的二次离子质谱(SIMS)微分析将是可行的。基于成分相似性,相对较高的B含量以及易于在薄片样品上进行SIMS微分析的原因,发现银山伊利石(IMt-1)是合适的校准参考材料。比较了硼酸化的铁硼硅藻土和伊利石的基质效应,发现是相似的,证实了先前的研究表明矿物中B对基质没有效应。硼在四面体位点上替代了Si,也可以吸附在2:1粘土矿物的可交换位点上。类似地,B可以在方晶石的四面体和可交换位点中发现,该方石由层状和无定形两种体积组成。为了测量方石中四面体B的含量和同位素比,通过将样品薄片浸泡在1 M NH_4Cl溶液中直到可交换的阳离子浓度恒定来除去可交换的B。处理后的样品显示B含量和同位素比随交换降低。提取可交换的B可以直接测量四面体B的含量和同位素比。在此设计和测试的交换技术应具有广泛的适用性,适用于粘土和类似粘土的材料中B的薄层显微分析,其中阳离子交换可用于表面分析技术。本研究代表了解决样品制备,校准和潜在的基质效应问题以进行SIMS分析的初步尝试。进一步的改进可以提高测量的准确性,但是此处显示的结果表明有意义的测量是可能的。

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