CO2 produced as a waste product of the oxidation of sugars in the mitochondria reacts with water in a reaction catalyzed bycarbonic anhydrase to formH2CO3, which is in equilibrium with the cationH+ and anionHCO−3. It is then carried to the lung, where the reverse reaction occurs and CO2 gas is released. In the kidney (left), cells (green) lining the proximal tubule conserve bicarbonate by transporting it from the glomerular filtrate in the lumen (yellow) of the nephron back into the blood (red). The exact stoichiometry in the kidney is omitted for simplicity.
With carbonic acid as thecentral intermediatespecies, bicarbonate – in conjunction with water,hydrogen ions, andcarbon dioxide – forms this buffering system, which is maintained at the volatile equilibrium[3] required to provide prompt resistance to pH changes in both the acidic andbasic directions. This is especially important for protectingtissues of thecentral nervous system, where pH changes too far outside of the normal range in either direction could prove disastrous (seeacidosis oralkalosis). Recently it has been also demonstrated that cellular bicarbonate metabolism can be regulated by mTORC1 signaling.[8]
Additionally, bicarbonate plays a key role in the digestive system. It raises the internal pH of the stomach, after highly acidic digestive juices have finished in their digestion of food. Bicarbonate also acts to regulate pH in the small intestine. It is released from thepancreas in response to the hormonesecretin to neutralize the acidicchyme entering theduodenum from the stomach.[9]
Some plants likeChara utilize carbonate and produce calcium carbonate (CaCO3) as a result of biological metabolism.[11]
In freshwater ecology, strongphotosynthetic activity by freshwater plants in daylight releases gaseousoxygen into the water and at the same time produces bicarbonate ions. These shift the pH upward until in certain circumstances the degree of alkalinity can become toxic to some organisms or can make other chemical constituents such asammonia toxic. In darkness, when no photosynthesis occurs, respiration processes release carbon dioxide, and no new bicarbonate ions are produced, resulting in a rapid fall in pH.[citation needed]
The flow of bicarbonate ions from rocks weathered by the carbonic acid in rainwater is an important part of thecarbon cycle.
The parameterstandard bicarbonate concentration (SBCe) is the bicarbonate concentration in the blood at aPaCO2 of 40 mmHg (5.33 kPa), full oxygen saturation and 36 °C.[15]
^ab"hydrogencarbonate (CHEBI:17544)".Chemical Entities of Biological Interest (ChEBI). UK: European Institute of Bioinformatics. IUPAC Names.Archived from the original on 7 June 2015.
^William Hyde Wollaston (1814) "A synoptic scale of chemical equivalents",Philosophical Transactions of the Royal Society,104: 1-22.On page 11, Wollaston coins the term "bicarbonate": "The next question that occurs relates to the composition of this crystallized carbonate ofpotash, which I am induced to call bi-carbonate of potash, for the purpose of marking more decidedly the distinction between this salt and that which is commonly called a subcarbonate, and in order to refer at once to the double dose of carbonic acid contained in it."
^Geor, Raymond J.; Coenen, Manfred; Harris, Pat (31 January 2013).Equine Applied and Clinical Nutrition: Health, Welfare and Performance. Elsevier Health Sciences. p. 90.ISBN978-0-7020-5418-1.The most common indicator of water quality is the concentration of total dissolved solids (TDS)