Abstract
Seasonal hydrochemical studies of the basic salt composition of water in the Partizanskaya R. estuary (Nakhodka Bay, the Sea of Japan), carried out in 2012, showed no within-year changes in the ratio of major ions, and hence the type of mineralization, in the river against a background of a pronounced seasonal variation of total mineralization. The mixing of river and sea water in the estuary is shown to be of a conservative character.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
