Compressibility of distilled water and seawater

Alvin Bradshaw , Karl Schleicher
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引用次数: 24

Abstract

The compressions of distilled water and of seawater of approximately 31, 35, and 39% salinity were measured at 10°C for pressures up to 1000 bars. The data were summarized by a ‘best’ least-square fit polynomial in pressure and salinity. The summary formula was combined withBryden's (Deep-Sea Research,20, 401–408, 1973) similar type fit to our earlier thermal expansion data (Bradshaw andSchleicher, Deep-Sea Research,17, 691–706, 1970) andFofonoff andBryden's (Journal of Marine Research, in press) recent empirical formula for sigma-0 of seawater to give an expression for the specific volume of seawater as a function of temperature, pressure and salinity in the salinity range 31 to 39%. At 35% specific volumes from this expression in the oceanographic range of temperature and pressure agree within 15 × 10−6cm3g−1 with those computed using sound velocities (Wang andMillero, Journal of Geophysical and Research,78, 7122–7128, 1973). Our mean compressibilities for distilled water at 10°C also agree with those from sound velocities (to within 0·05%) but disagree with those ofKell andWhalley (Philosophical Transactions of the Royal Society of London, A,258, 565–614, 1965) by about 0·3%.

蒸馏水和海水的可压缩性
在10°C下,在压力高达1000巴的情况下,测量了蒸馏水和盐度约为31、35和39%的海水的压缩。数据通过压力和盐度的“最佳”最小二乘拟合多项式进行总结。总结公式与bryden的(深海研究,1973年,20,401-408)与我们早期热膨胀数据的类似拟合(Bradshaw和schleicher,深海研究,17,691-706,1970)和fofonoff和bryden的(海洋研究杂志,已出版)最近的海水sigma-0经验公式相结合,给出了海水比体积在盐度范围31至39%内作为温度、压力和盐度函数的表达式。在海洋温度和压力范围内,该表达式的35%比体积与使用声速计算的结果在15 × 10−6cm3g−1范围内一致(Wang和millero, Journal of Geophysical and Research,78, 7122-7128, 1973)。我们在10°C下蒸馏水的平均可压缩性也与声速计算结果一致(误差在0.05%以内),但与kell和whalley(伦敦皇家学会哲学学报,A,258, 565-614, 1965)的结果相差约0.3%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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