In Surah Fatir (35:12), the Quran declares: "And not alike are the two seas. One is fresh and sweet, palatable for drinking, and one is salty and bitter" (ููู ูุง ููุณูุชูููู ุงููุจูุญูุฑูุงูู ููุฐูุง ุนูุฐูุจู ููุฑูุงุชู ุณูุงุฆูุบู ุดูุฑูุงุจููู ููููุฐูุง ู ูููุญู ุฃูุฌูุงุฌู).
This verse clearly distinguishes fresh waters from salty waters, a reality that modern oceanography has precisely characterized.
The salinity of the oceans
The average salinity of seawater is about 35 parts per thousand (35 g of salt per liter of water). This salinity varies by region: Red Sea (~40 ppt), Atlantic Ocean (~35-37 ppt), Pacific Ocean (~34-35 ppt), Baltic Sea (~7-8 ppt).
Distinct water masses
Modern oceanography has discovered that oceans are composed of distinct water masses, each with its own temperature, salinity, and density. These water masses do not mix easily: Atlantic and Mediterranean waters have different characteristics, and at the Strait of Gibraltar, the more saline and dense Mediterranean waters dive beneath the Atlantic waters.
Verse 25:53 also mentions: "And it is He who has released [simultaneously] the two seas, one fresh and sweet and one salty and bitter, and He placed between them a barrier and prohibiting partition" (ูููููู ุงูููุฐูู ู ูุฑูุฌู ุงููุจูุญูุฑููููู ููุฐูุง ุนูุฐูุจู ููุฑูุงุชู ููููุฐูุง ู ูููุญู ุฃูุฌูุงุฌู ููุฌูุนููู ุจูููููููู ูุง ุจูุฑูุฒูุฎูุง ููุญูุฌูุฑูุง ู ููุญูุฌููุฑูุง).
The term barzakh (ุจูุฑูุฒูุฎูุง) designates a barrier or intermediate zone. Oceanography has confirmed the existence of such transition zones where water masses meet without completely mixing.
This knowledge of distinct water masses was only scientifically established from the HMS Challenger expedition (1872-1876), the first major oceanographic expedition, and deepened in the 20th century.