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  1. 9 gru 2019 · The ocean’s chemistry is changing due to the uptake of anthropogenic carbon dioxide (CO2). This phenomenon, commonly referred to as “Ocean Acidification”, is endangering coral reefs and the ...

  2. 9 cze 2020 · Alkalinity, the excess of proton acceptors over donors, plays a major role in ocean chemistry, in buffering and in calcium carbonate precipitation and dissolution. Understanding alkalinity dynamics is pivotal to quantify ocean carbon dioxide uptake during times of global change.

  3. On the basis of laboratory experiments and field studies of naturally elevated CO2 marine environments, widespread biological impacts of human-driven ocean acidification have been posited, ranging from changes in organism physiology and population dynamics to altered communities and ecosystems.

  4. Water and carbon dioxide combine to form carbonic acid (H 2 CO 3), a weak acid that breaks (or “dissociates”) into hydrogen ions (H +) and bicarbonate ions (HCO 3-). Because of human-driven increased levels of carbon dioxide in the atmosphere, there is more CO 2 dissolving into the ocean.

  5. 9 lis 2021 · One third of the carbon dioxide in our atmosphere dissolves in the ocean. It therefore acts as an important buffer against rising temperatures. Carbon is one of the chemical elements in the...

  6. Scientists calculate that the ocean is currently absorbing about one quarter of the carbon dioxide that humans are emitting. When carbon dioxide combines with seawater, chemical reactions occur that reduce the seawater pH, hence the term ocean acidification.

  7. 23 lip 2018 · Long-term trends in OA for the open ocean are a result of the net uptake of CO 2 from the atmosphere by surface waters causing a change in carbonate chemistry. These trends are detectable over...