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A new and less destructive laboratory procedure for the physical separation of distal glass tephra shards from sediments

机译:一种新的,破坏性较小的实验室程序,用于从沉积物中物理分离远侧玻璃提夫拉碎片

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摘要

Tephrochronology, a key tool in the correlation of Quaternary sequences, relies on the extraction of tephra shards from sediments for visual identification and high-precision geochemical comparison. A prerequisite for the reliable correlation of tephra layers is that the geochemical composition of glass shards remains unaltered by natural processes (e.g. chemical exchange in the sedimentary environment) and/or by laboratory analytical procedures. However, natural glasses, particularly when in the form of small shards with a high surface to volume ratio, are prone to chemical alteration in both acidic and basic environments. Current techniques for the extraction of distal tephra from sediments involve the 'cleaning' of samples in precisely such environments and at elevated temperatures. The acid phase of the 'cleaning' process risks alteration of the geochemical signature of the shards, while the basic phase leads to considerable sample loss through dissolution of the silica network. Here, we illustrate the degree of alteration and loss to which distal tephras may be prone, and introduce a less destructive procedure for their extraction. This method is based on stepped heavy liquid flotation and which results in samples of sufficient quality for analysis while preserving their geochemical integrity. In trials, this method out-performed chemical extraction procedures in terms of the number of shards recovered and has resulted in the detection of new tephra layers with low shard concentrations. The implications of this study are highly significant because (i) the current database of distal tephra records and their corresponding geochemical signatures may require refinement and (ii) the record of distal tephras may be incomplete due to sample loss induced by corrosive laboratory procedures. It is therefore vital that less corrosive laboratory procedures are developed to make the detection and classification of distal glass tephra more secure. (c) 2005 Elsevier Ltd. All rights reserved.
机译:年代学是第四纪序列相关性的关键工具,它依赖于从沉积物中提取提非拉铁碎片,以进行视觉识别和高精度地球化学比较。提菲拉层可靠关联的前提是,玻璃碎片的地球化学组成不会因自然过程(例如沉积环境中的化学交换)和/或实验室分析程序而改变。然而,天然玻璃,特别是当具有高表面积与体积比的小碎片形式时,在酸性和碱性环境中都容易发生化学变化。从沉积物中提取远侧提夫拉的当前技术包括在精确的此类环境中和升高的温度下“清洁”样品。 “清洁”过程的酸性阶段可能会改变碎片的地球化学特征,而碱性阶段会由于溶解二氧化硅网络而导致大量样品损失。在这里,我们说明远侧眼睑容易发生改变和丢失的程度,并介绍了破坏程度较小的提取方法。该方法基于逐步重液浮选,可产生质量足以进行分析的样品,同时保留其地球化学完整性。在试验中,就回收的碎片数量而言,该方法的性能优于化学提取程序,并导致检测到具有低碎片浓度的新提法拉层。这项研究的意义非常重大,因为(i)当前的远端特弗拉记录数据库及其相应的地球化学特征可能需要改进,并且(ii)由于腐蚀性实验室程序引起的样品流失,远端特弗拉记录可能不完整。因此,至关重要的是要开发出腐蚀性较小的实验室程序,以使远端玻璃球菌的检测和分类更加安全。 (c)2005 Elsevier Ltd.保留所有权利。

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