在278.15 K至308.15 K温度范围内的海水密度测量

R. Romeo, S. Lago, P. A. Giuliano Albo, M. Le Menn
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引用次数: 2

摘要

海水密度在海洋学中具有非常重要的意义,因为如果密度已知并具有必要的准确性,就可以用来测定盐度。为此,本文综述了适用于海水测量的密度测量方法。此外,在环境压力(278.15 ~ 308.15)K的温度范围内,测量了不同实际盐度(9.997 ~ 37.999)下的标准海水密度。测量是通过振动管密度计和替代法(海水和普通水交替取样)进行的。此外,对密度不确定度进行了精确的分析,得到了0.004%的扩展不确定度。用同样的技术进行测量,并与文献中给出的密度结果进行比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seawater density measurements in the temperature range between 278.15 K and 308.15 K at ambient pressure
Seawater density has a great importance in the oceanographic science, since it can be used for salinity determination, if density is known with the necessary accuracy. For that reason, a review of the methods for density measurements suitable for seawater measurements is presented. Furthermore, in this work standard seawater density is measured at different practical salinities (from 9.997 to 37.999) in the temperature range between (278.15 to 308.15) K at ambient pressure. Measurements are carried out by means of a vibrating tube densimeter and following the substitution method (alternating samples of seawater and ordinary water). Besides, an accurate analysis of the density uncertainty has been performed, obtaining an expanded uncertainty of 0.004%. Measurements are carried out and compared with density results given in the literature, performed with the same technique.
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