Boomer
Your equation is strictly not true:
53 ms @25 C KCl (32.4356 grams of Potassium Chloride ) = 35 ppt NSW @25 C
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Both sides of the equation use different units with one side in mS the other ppt....you are actually making the same conceptual jump that I am making i.e. relating practical salinity with real or absolute salinity (ppt). What is really meant is that if the conductivity of a seawater sample is equal to the conductivity of a standard KCL cell (each at STP), then the salinity of the sample is 35
by definition of the practical salinity scale. The conductivity of ratio of one is mapped to the number 35 in order for the practical salinity scale to be consistent with the prior chlorinity scale. When the definition of the practical salinity scale was made, a sample of standard seawater with exactly 35 ppt of dissolved salt (calculated from chlorinity) was used to standardize the needed KCL mass to create a conductivity ratio of one.
A standard solution of KCL (32.4356 grams of KCL) would have a real or absolute salinity of 32.4356 ppt....but a conductivity ratio of 1 with another standard KCL cell. I am not saying that a seawater sample with a practical salinity of 35 has exactly 35 ppt....but it will be very, very close because of constant composition of seawater.
Salinity is defined as the ratio of the mass of dissolved material in sea water to the mass of sea water (IAPSO Publication Scientifique, no. 32, 1985). The 'practical salinity' (S) of a seawater sample is defined as the ratio of the electrical conductivity of the sample (at 15 °C, and one standard atmospheric pressure) to that of a standard solution of potassium Chloride (KCl). A ratio of 1 is equivalent to a 'practical salinity' of 35 (UNESCO technical papers in marine science, no. 45, 1985).
Salinity is an important variable in the International Equation of State (EOS-90 ), the officially recognized equation used by oceanographers to calculate the
density of seawater. Without the context of you are dealing with seawater and seawater's constant composition assumption, measurement of conductivity as a reflection of real or absolute salinity, the EOS-90 is meaningless.
The current definition of salinity by IAPSO assumes you are dealing with seawater.....not a bucket of resistors with a conductivity ratio of 1.
What I should have said was:
For example a standard KCL reference cell with a conductivity of exactly 35 ***would not have the same
real or absolute salinity (wt/kg seawater) as normal seawater with a conductivity of exactly 35***, despite the definition of salinity in terms of conductivity ratio.
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Other quotes and crap to further pad this excessively long post on a very esoteric subject and semantic argument.
...Since the relative composition of ocean waters is nearly constant, it is possible to characterize the composition by measuring only one component that is easy to measure and is conservative in its behavior. A conservative component of seawater is one that is unreactive and for which the changes from place to place are due to the addition or loss of water.
Millero Chemical Oceanography 3rd Ed pg 56-57
A complete chemical analysis of seawater is the only reliable way to determine the true or absolute salinity of seawater (S t in parts per thousand). This method, however, is too time consuming for routine studies.
Millero Chemical Oceanography 3rd Ed pg 63
...In practice, any physical property (density, refractive index, sound speed, etc ) at a fixed temperature and pressure can be used to determine salinity...
Millero Chemical Oceanography 3rd Ed pg 67
...The relationship between conductivity and salinity has an accuracy of around ± 0.003 in salinity....
http://oceanworld.tamu.edu/resources/ocng_textbook/chapter06/chapter06_01.htm