The application of staiidaidization coiTcctions necessary to conform 

 to these vahies reciuires the followin^i' corrections to tlie pubhslied 

 sahnities. It will he noted that while the corrections are tabulated 

 below to the nearest 0.001 °/oo, the salinities published were given to 

 the nearest 0.01°/oo and the pi-ecision of the measurenients was 

 0.0057oo. 



It is now of iiilcirsl 1() cxii iiiiiir I lie departures of ( 'opcnhagen 

 watei- from tbe conihictiNity-chlorinit \- relationsliip existing in actual 

 sea wafer which has not been stored in glass containers, as represented 

 by I lie (bscrcpancies between the sahnities correspon(nng to the stated 

 chlorinities of the ("openhageii water and the salinities corresponding 

 to the X-<nal readings of the Copenliagen water as given above. 

 The coin])arison follows. 



39 



