It is a branch of chemistry which studying chemical processes and chemical composition of ocean waters.
Chemistry has contributions in oceanography !For example the chemical study of ocean waters, pollution, interaction atmosphere-ocean, etc.
ocean water chemistry, currents, ocean life, and the shape of the ocean floor
Using methods and instruments of analytical chemistry.
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An increase in carbon dioxide in the atmosphere leads to more CO2 being absorbed by the ocean, causing ocean water to become more acidic. This change in chemistry can harm marine life, particularly organisms with shells or skeletons made of calcium carbonate.
A Oceanographer. We study waves and currents, geology, chemistry and Biology.
Oceanography is considered a physical science. It is the study of the ocean's chemistry, ecosystem and organisms. Other physical sciences include astronomy, physics, chemistry and geology.
Yes, sulfur is found in the ocean in various forms, including sulfates and hydrogen sulfide. These compounds are released into the water through volcanic activity, weathering of rocks, and biological processes. They play important roles in ocean chemistry and the marine ecosystem.
Naturally, seawater in the North Pacific Ocean is more acidic (lower in pH) than in the North Atlantic Ocean. This is related to the circulation, biology and chemistry in the ocean, which involve complicated processes that oceanographers have been studying for decades. The results of these processes are that seawater in the North Pacific in general has lower pH, but higher TCO2 concentrations than that of the North Atlantic at similar latitude. source: WHOI Chemist Aleck Wang at http://funwithkrill.blogspot.com/2012/09/seawater-chemistry-north-atlantic-vs.html]
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Yes, the ocean absorbs both carbon dioxide and heat from the atmosphere. When carbon dioxide enters the ocean, it reacts with seawater to form carbonic acid, which impacts ocean chemistry and marine life. Additionally, the ocean acts as a significant heat sink, absorbing excess heat from global warming, which helps regulate the Earth's climate but also leads to issues like ocean warming and acidification.
A Paleozoic ocean, spanning from about 541 to 252 million years ago, would differ significantly from today's oceans in terms of biodiversity, chemistry, and physical characteristics. During this era, marine life was dominated by invertebrates like trilobites and brachiopods, with the absence of modern fish and mammals. The ocean's chemistry was also different, featuring higher levels of carbon dioxide and lower oxygen concentrations, affecting the types of organisms that could thrive. Additionally, the arrangement of continents and ocean currents would have influenced climate and habitats, resulting in distinct ecosystems compared to contemporary oceans.