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Alkalinity. Sea surface alkalinity (from the GLODAP climatology ). Alkalinity (from Arabic: القلوية, romanized : al-qaly, lit. 'ashes of the saltwort ') [1] is the capacity of water to resist acidification. [2] It should not be confused with basicity, which is an absolute measurement on the pH scale.
Alkali. In chemistry, an alkali ( / ˈælkəlaɪ /; from Arabic: القلوي, romanized : al-qaly, lit. 'ashes of the saltwort ') is a basic, ionic salt of an alkali metal or an alkaline earth metal. An alkali can also be defined as a base that dissolves in water. A solution of a soluble base has a pH greater than 7.0.
In chemistry, pH ( / piːˈeɪtʃ / pee-AYCH ), also referred to as acidity or basicity, historically denotes " potential of hydrogen " (or "power of hydrogen"). [ 1 ] It is a logarithmic scale used to specify the acidity or basicity of aqueous solutions. Acidic solutions (solutions with higher concentrations of hydrogen ( H+) ions) are ...
Ocean acidification. Ocean acidification means that the average seawater pH value is dropping over time. [1] Ocean acidification is the ongoing decrease in the pH of the Earth's ocean. Ocean acidification is a process that occurs when carbon dioxide (CO2) from the atmosphere is absorbed by seawater, leading to a decrease in pH levels.
Carbonate hardness. Carbonate hardness, is a measure of the water hardness caused by the presence of carbonate ( CO2−. 3) and bicarbonate ( HCO−. 3) anions. Carbonate hardness is usually expressed either in degrees KH ( °dKH) (from the German "Karbonathärte" ), or in parts per million calcium carbonate ( ppm CaCO. 3 or grams CaCO.
Soil pH is a measure of the acidity or basicity (alkalinity) of a soil. Soil pH is a key characteristic that can be used to make informative analysis both qualitative and quantitatively regarding soil characteristics. [1] pH is defined as the negative logarithm (base 10) of the activity of hydronium ions ( H+.
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