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Density measurements of IAPSO Standard Seawater by hydrostatic weighing

机译:用静水称重法测量IAPSO标准海水的密度

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摘要

In metrological terms, salinity of seawater remains one of the most problematic quantity used in the frame of ocean science. The main reason is because, despite a clear definition of salinity, the realization of the unit is still linked to the use of artifact of natural origin characterized by measurements of conductivity. The latter seems to be the only quantity capable to guarantee the necessary accuracy at the moment. However, the concept of salinity, but not the definition, is linked to the quantity of substance contained in seawater, that is not pure water, and conductivity measurement can only partially cover the physico-chemical aspects characterizing the thermodynamic behavior of seawater. In these cases, the measurement of the density is more appropriate and, thanks to its recent progresses, it seems to be a promising way to guarantee the traceability of salinity measurement in seawater. This work is a contribution to the measurement of the density of IAPSO standard seawater, using the method of hydrostatic weighing. Despite this method is limited to work at atmospheric pressure, it is the best approach in term of accuracy. The measurement method is, mainly, analyzed from the metrological point of view, focusing on the traceability chain supporting the reliability of the obtained results.
机译:用计量学的术语来说,海水的盐度仍然是海洋科学框架中使用最多的问题之一。主要原因是,尽管对盐度有明确的定义,但该单元的实现仍与使用以电导率测量为特征的自然人工制品有关。后者似乎是目前唯一能够保证必要准确性的数量。但是,盐度的概念而不是定义与海水中所含物质的数量有关,即不是纯净的水,电导率测量只能部分覆盖表征海水热力学行为的理化方面。在这些情况下,密度的测量更为合适,并且由于其最新进展,这似乎是一种保证海水中盐度测量可追溯性的有前途的方法。这项工作对使用静水称量法测量IAPSO标准海水的密度做出了贡献。尽管此方法仅限于在大气压下工作,但就准确性而言,它是最佳方法。主要从计量学角度分析测量方法,重点放在支持所获得结果可靠性的可追溯性链上。

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