scispace - formally typeset
Journal ArticleDOI

A new high pressure equation of state for seawater

TLDR
A new high pressure equation of state for water and seawater has been derived from the experimental results of Millero and coworkers in Miami and Bradshaw and Schleicher in Woods Hole as mentioned in this paper.
Abstract
A new high pressure equation of state for water and seawater has been derived from the experimental results of Millero and coworkers in Miami and Bradshaw and Schleicher in Woods Hole The form of the equation of state is a second degree secant bulk modulus K = Pv0(v0−vp=K0+AP+BP2 K = Kw0+aS+bS32 A = Aw+cS+dS32 B = Bw+eS where ν0 and νP are the specific volume at 0 and P applied pressure and S is the salinity (ℵ) The coefficients KWO, AW, and BW for the pure water part of the equation are polynomial functions of temperature The standard error of the pure water equation of state is 43 × 10−6 cm3 g−1 in νWP The temperature dependent parameters a, b, c, d, and e have been determined from the high pressure measurements on seawater The overall standard error of the seawater equation of state is 90 × 10−6 cm3 g−1 in νP Over the oceanic ranges of temperature, pressure, and salinity the standard error is 50 × 10−6 cm3 g−1 in νP This new high pressure equation of state has recently (1979) been recommended by the UNESCO Joint Panel on Oceanographic Tables and Standards for use by the oceanographic community

read more

Citations
More filters
Journal ArticleDOI

Thermophysical properties of seawater: a review of existing correlations and data

TL;DR: In this paper, a review of the properties of seawater is presented in terms of regression equations as functions of temperature and salinity, and the available correlations for each property are summarized with their range of validity and accuracy.

The thermophysical properties of seawater: A review of existing correlations and data

TL;DR: In this article, a review of the properties of seawater is presented in terms of regression equations as functions of temperature and salinity, and the available correlations for each property are summarized with their range of validity and accuracy.
Journal ArticleDOI

The composition of Standard Seawater and the definition of the Reference-Composition Salinity Scale

TL;DR: Reference Seawater is defined as any seawater that has the Reference Composition and a new Reference-Composition Salinity S R is defined to provide the best available estimate of the Absolute Salinity of both Reference Seawaters and the Standard SeawATER that was used in the measurements of the physical properties as discussed by the authors.
Journal ArticleDOI

A method for computing horizontal pressure-gradient force in an oceanic model with a nonaligned vertical coordinate

TL;DR: A pressure-gradient algorithm that achieves more accurate hydrostatic balance between the two components and does not lose as much accuracy with nonuniform vertical grids at relatively coarse resolution, and generalized the monotonicity constraint to guarantee nonnegative physical stratification of the reconstructed density profile in the case of compressible equation of state.
Journal ArticleDOI

Redfield ratio based on chemical data from isopycnal surfaces

TL;DR: In this article, the composition of the organic matter oxidized within the thermocline of the Atlantic and Indian oceans has been estimated from the chemical data along the σθ 27.0 and 27.2 horizons.
References
More filters
Journal ArticleDOI

Density, thermal expansivity, and compressibility of liquid water from 0° to 150°C: correlations and tables for atmospheric pressure and saturation reviewed and expressed on 1968 temperature scale.

TL;DR: In this article, a review is given of the temperature dependence of the density of liquid water from 40" to 150°C and the error in the calculated compressibilities is estimated as 03 X lO-'bar-' at 4'C and as7 X 100°C at 4''C.
Journal ArticleDOI

Speed of Sound in Pure Water

TL;DR: A sound speed equation of fifth order in temperature is fit with a standard deviation of 0.0028 m/sec to 148 observations between 0.001°C and 95.126°C on the T68 scale as discussed by the authors.
Journal ArticleDOI

Speed of sound in seawater at high pressures

TL;DR: In this article, the effect of pressure on the relative speeds of sound, (UP−UPH2O) ‐UO−UOH2O), have been measured relative to pure water with a Nusonics single-transducer sound velocimeter as a function of salinity (5−40°/00), temperature 0°-40°C, and applied pressure (0-1000 bars).
Journal ArticleDOI

The equation of state of pure water determined from sound speeds

TL;DR: In this article, Chen and Millero used the high pressure sound velocities of Wilson to determine the equation of state of water valid over the range 0 −100°C and 0 −1000 bar.
Journal Article

Density of seawater solutions at one atmosphere as a function of temperature and salinity.

TL;DR: In this article, the relative density (d d) of diluted and evaporated standard seawater solutions have been determined at one atmosphere with a magnetic float densimeter and a suspension balance from 0.5 to 40%0 salinity and 0 to 40°C.
Related Papers (5)