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	<title>PCO2 - Revision history</title>
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	<updated>2026-09-09T19:50:37Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>http://debianws.lexgopc.com/wiki143/index.php?title=PCO2&amp;diff=6089065&amp;oldid=prev</id>
		<title>imported&gt;GreenC bot: Rescued 2 archive links. Wayback Medic 2.5 per WP:URLREQ#climate.gov</title>
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		<updated>2025-06-30T15:03:35Z</updated>

		<summary type="html">&lt;p&gt;Rescued 2 archive links. &lt;a href=&quot;/wiki143/index.php?title=User:GreenC/WaybackMedic_2.5&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;User:GreenC/WaybackMedic 2.5 (page does not exist)&quot;&gt;Wayback Medic 2.5&lt;/a&gt; per &lt;a href=&quot;/wiki143/index.php?title=WP:URLREQ&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;WP:URLREQ (page does not exist)&quot;&gt;WP:URLREQ#climate.gov&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{short description|Partial pressure of carbon dioxide, often used in reference to blood}}&lt;br /&gt;
{{DISPLAYTITLE:pCO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;}}&lt;br /&gt;
[[File:Carbon-dioxide-3D-vdW.svg|thumb|[[Carbon dioxide]] molecule.]]&lt;br /&gt;
&amp;#039;&amp;#039;&amp;#039;&amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;, pCO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;#039;&amp;#039;&amp;#039;, or &amp;lt;math chem=&amp;quot;&amp;quot;&amp;gt;P_\ce{CO2}&amp;lt;/math&amp;gt; is the [[partial pressure]] of [[carbon dioxide]] (CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;), often used in reference to [[blood]] but also used in [[meteorology]], [[Climatology|climate science]], [[oceanography]], and [[limnology]] to describe the fractional pressure of CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; as a function of its concentration in gas or dissolved phases.   The units of &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; are [[Millimetre of mercury|mmHg]], [[Standard atmosphere (unit)|atm]], [[torr]], [[Pascal (unit)|Pa]], or any other standard unit of [[atmospheric pressure]].  The &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; of [[Earth|Earth&amp;#039;s]] atmosphere has risen from approximately 280 ppm ([[Parts-per notation|parts-per-million]]) to a mean 2019 value of 409.8 ppm as a result of [[Climate change|anthropogenic]] release of carbon dioxide from [[fossil fuel]] burning.&amp;lt;ref&amp;gt;{{Cite web|last=Lindsey|first=Rebecca|date=2020|title=Climate Change: Atmospheric Carbon Dioxide|url=https://www.climate.gov/news-features/understanding-climate/climate-change-atmospheric-carbon-dioxide|archive-url=https://web.archive.org/web/20130624204311/http://www.climate.gov/news-features/understanding-climate/climate-change-atmospheric-carbon-dioxide|url-status=dead|archive-date=June 24, 2013|access-date=2021-02-25|website=www.climate.gov|language=en}}&amp;lt;/ref&amp;gt; This is the highest atmospheric concentration to have existed on Earth for at least the last 800,000 years.&amp;lt;ref&amp;gt;{{Cite web|last=Lindsey|first=Rebecca|date=2020|title=Climate Change: Atmospheric Carbon Dioxide|url=https://www.climate.gov/news-features/understanding-climate/climate-change-atmospheric-carbon-dioxide|archive-url=https://web.archive.org/web/20130624204311/http://www.climate.gov/news-features/understanding-climate/climate-change-atmospheric-carbon-dioxide|url-status=dead|archive-date=June 24, 2013|access-date=2021-02-25|website=www.climate.gov|language=en}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Medicine ==&lt;br /&gt;
{{Main|Hypercapnia|Hypocapnia}}&lt;br /&gt;
In medicine, the partial pressure of carbon dioxide in [[arterial blood]] is called &amp;#039;&amp;#039;&amp;#039;&amp;lt;math chem=&amp;quot;&amp;quot;&amp;gt;P_{a_\ce{CO2}}&amp;lt;/math&amp;gt;&amp;#039;&amp;#039;&amp;#039; or &amp;#039;&amp;#039;&amp;#039;PaCO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;#039;&amp;#039;&amp;#039;. Measurement of &amp;lt;math chem=&amp;quot;&amp;quot;&amp;gt;P_{a_\ce{CO2}}&amp;lt;/math&amp;gt; in the [[systemic circulation]] indicates the effectiveness of [[ventilation (physiology)|ventilation]] at the lungs&amp;#039; [[pulmonary alveolus|alveoli]], given the [[diffusing capacity]] of the gas. It is a good indicator of respiratory function and the closely related factor of [[acid–base homeostasis]], reflecting the amount of acid in the blood (without lactic acid).  Normal values for humans are in the range of 35–45 [[Millimetre of mercury|mmHg]].  Values less than this may indicate [[hyperventilation]] and (if blood [[pH]] is greater than 7.45) [[respiratory alkalosis]].  Values greater than 45 mmHg may indicate [[hypoventilation]], and (if blood pH is less than 7.35) respiratory [[acidosis]].&amp;lt;ref&amp;gt;[https://www.nlm.nih.gov/medlineplus/spanish/ency/article/003855.htm Dugdale DC, Zieve D. Gasometría arterial. Medline Plus. 09/01/2012.]&amp;lt;/ref&amp;gt;&amp;lt;ref&amp;gt;[http://www.redentor.inf.br/arquivos/pos/publicacoes/21082012Microsoft%20Word%20-%20trabalho%20conclusao%20de%20curso.pdf Leticia Godoy Dias Sanderson. Gasometria arterial - Artigo de revisão. Fevereiro 2012.] {{webarchive|url=https://web.archive.org/web/20141017103958/http://www.redentor.inf.br/arquivos/pos/publicacoes/21082012Microsoft%20Word%20-%20trabalho%20conclusao%20de%20curso.pdf|date=2014-10-17}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== Aquatic sciences ==&lt;br /&gt;
{{see also|Ocean acidification|Freshwater acidification}}&lt;br /&gt;
Oceanographers and limnologists use &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; to measure the amount of carbon dioxide dissolved in water, as well as to parameterize its [[flux]] into (influx) and out of (efflux) the atmosphere.  Carbon dioxide reacts with water to form [[bicarbonate]] and [[carbonate]] ions, such that the relative solubility of carbon dioxide in water is greater than that of other unreactive gasses (e.g. [[Helium]]).  As more carbon dioxide dissolves in water, its &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; rises until it equals the &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; of the overlying atmosphere.  Conversely, a body of water with a &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; greater than that of the atmosphere effluxes carbon dioxide.&amp;lt;ref name=&amp;quot;:0&amp;quot;&amp;gt;{{Cite book|last=Millero|first=Frank J.|url=https://www.worldcat.org/oclc/958798815|title=Chemical oceanography|date=2013|publisher=Taylor &amp;amp; Francis|isbn=978-1-4665-1255-9|edition=4|location=Boca Raton|oclc=958798815}}&amp;lt;/ref&amp;gt;&amp;lt;ref name=&amp;quot;:1&amp;quot;&amp;gt;{{Cite book|last=Zeebe|first=Richard E.|url=https://www.worldcat.org/oclc/246683387|title=CO2 in seawater : equilibrium, kinetics, isotopes|date=2001|others=Dieter A. Wolf-Gladrow|isbn=978-0-08-052922-6|location=Amsterdam|oclc=246683387}}&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
&amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; is additionally affected by water [[temperature]] and [[salinity]].  Carbon dioxide is less soluble in warmer water than cooler water, so hot water will exhibit a larger &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; than cold water with the same concentration of carbon dioxide.  &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; can be used to describe the inorganic carbon system of a body of water, together with other parameters such as pH, [[dissolved inorganic carbon]], and [[alkalinity]].   Together, these parameters describe the concentration and speciation of inorganic carbon species (CO&amp;lt;sub&amp;gt;2 (aq)&amp;lt;/sub&amp;gt;, HCO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;−&amp;lt;/sup&amp;gt;, CO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;2-&amp;lt;/sup&amp;gt;) in water.&amp;lt;ref name=&amp;quot;:1&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Biological processes such as [[Cellular respiration|respiration]] and [[photosynthesis]] affect and can be affected by aquatic &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;.  Respiration degrades [[organic matter]], releasing CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; into the water column and increasing &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;.  Photosynthesis assimilates inorganic carbon, thereby decreasing aquatic &amp;#039;&amp;#039;p&amp;#039;&amp;#039;CO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;.&amp;lt;ref name=&amp;quot;:0&amp;quot; /&amp;gt;&lt;br /&gt;
&lt;br /&gt;
== See also ==&lt;br /&gt;
* [[Acidosis]]&lt;br /&gt;
* [[Alkalosis]]&lt;br /&gt;
* [[Arterial blood gas]]&lt;br /&gt;
* [[Blood gas tension]]&lt;br /&gt;
* [[Chemical equilibrium]]&lt;br /&gt;
* [[Hypercapnia]]&lt;br /&gt;
* [[pH]]&lt;br /&gt;
*[[Carbon cycle|Carbon Cycle]]&lt;br /&gt;
* [[xCO2|xCO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;]]&lt;br /&gt;
&lt;br /&gt;
== References ==&lt;br /&gt;
{{reflist}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Acid–base chemistry]]&lt;br /&gt;
[[Category:Analytical chemistry]]&lt;br /&gt;
[[Category:Equilibrium chemistry]]&lt;br /&gt;
[[Category:Units of measurement]]&lt;br /&gt;
[[Category:Chemical oceanography]]&lt;br /&gt;
[[Category:Limnology]]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
{{CC-notice|cc=by4|url=https://opentextbc.ca/clinicalskills|author(s)=Glynda Rees Doyle and Jodie Anita McCutcheon}}&lt;/div&gt;</summary>
		<author><name>imported&gt;GreenC bot</name></author>
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