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<a href=showthread.php?s=&postid=9588470#post9588470 target=_blank>Originally posted</a> by jdieck
Hope this helps to clarify the issue.
Not really. I follow what you are saying, but based on the graph from fig 23, the slopes actually appear to be very similar. Given the margin for error for a refracto in obtaining accurate readings, it seems as though you would have a wider range salinities that could be measured than. In addition, the NaCl solutions I made up track appropriately -- i.e. both appear dead-on when calibrated with the 36.5 ppt solution to either 36.5 ppt or 35 ppt (seawater). That lends credence to the slopes being very much the same. So the refracto appears to track well for NaCl salinity readings as well as the adjustment for seawater.
Perhaps what you are saying is that at lower salinities, the refractive index of the 1.009 solution I made up with NaCl is quite off from where seawater would be at 1.009 and that the slope I am seeing is an NaCl slope. If so, that would be puzzling, because the offset at 35ppt appears very close to the offset I see with RO/DI once calibrated to 35ppt using Randy's solution. I.e. both appear to be linear to me, and to have substantially similar slopes. What I mean is, I run hyposalinity in my QT, and the dilution needed to create a mathematical 1.009 from a measured 35 ppt, matches the NaCl 1.009 standard.