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Carbonic acid is a chemical compound with the chemical formula . The rapidly converts to and in the presence of water. However, in the absence of water, it is quite stable at . The interconversion of carbon dioxide and carbonic acid is related to the breathing cycle of animals and the acidification of natural waters.

In biochemistry and physiology, the name "carbonic acid" is sometimes applied to aqueous solutions of . These play an important role in the bicarbonate buffer system, used to maintain acid–base homeostasis. Acid-Base Physiology 2.1 – Acid-Base Balance by Kerry Brandis.


Terminology in biochemical literature
In , the term "carbonic acid" strictly refers to the chemical compound with the formula . Some literature effaces the distinction between carbonic acid and carbon dioxide dissolved in extracellular fluid.

In , carbon dioxide excreted by the may be called volatile acid or respiratory acid.


Anhydrous carbonic acid
At ambient temperatures, pure carbonic acid is a stable gas. There are two main methods to produce carbonic acid: reaction of hydrogen chloride and potassium bicarbonate at 100 K in and of pure solid carbon dioxide. Chemically, it behaves as a Brønsted acid.

Carbonic acid exhibit three conformational isomers: cis–cis, cis–trans, and trans–trans.

At low temperatures and atmospheric pressure, solid carbonic acid is and lacks in X-ray diffraction. But at high pressure, carbonic acid crystallizes, and modern analytical spectroscopy can measure its geometry.

According to neutron diffraction of carbonic acid () in a hybrid clamped cell (/copper-beryllium) at 1.85 GPa, the molecules are planar and form dimers joined by pairs of . All three C-O bonds are nearly equidistant at 1.34 , intermediate between typical C-O and C=O distances (respectively 1.43 and 1.23 Å). The unusual C-O bond lengths are attributed to delocalized in the molecule's center and extraordinarily strong hydrogen bonds. The same effects also induce a very short O—O separation (2.13 Å), through the 136° O-H-O imposed by the doubly hydrogen-bonded 8-membered rings. Longer O—O distances are observed in strong intramolecular hydrogen bonds, e.g. in , where the distances exceed 2.4 Å.


In aqueous solution
In even a slight presence of water, carbonic acid dehydrates to and , which then further decomposition. For this reason, carbon dioxide can be considered the carbonic .

The equilibrium constant at 25 °C is in pure water

(2025). 9780130399137, Prentice-Pearson-Hall.
and ≈ 1.2×10−3 in . Hence the majority of carbon dioxide at geophysical or biological does not convert to carbonic acid, remaining dissolved gas. However, the equilibrium is reached quite slowly: the are 0.039 −1 for hydration and 23 s−1 for dehydration.


In biological solutions
In the presence of the enzyme carbonic anhydrase, equilibrium is instead reached rapidly, and the following reaction takes precedence: HCO3^- {+} H^+ <=> CO2 {+} H2O

When the created carbon dioxide exceeds its solubility, gas evolves and a third equilibrium CO_2 (soln) <=> CO_2 (g) must also be taken into consideration. The equilibrium constant for this reaction is defined by Henry's law.

The two reactions can be combined for the equilibrium in solution: \begin{align} \ce{HCO3^{-}{} + H+{} <=> CO2(soln){} + H2O} && K_3 = \frac{\ce{H+}\ce{HCO3^-}}{\ce{CO2(soln)}} \end{align} When Henry's law is used to calculate the denominator care is needed with regard to units since Henry's law constant can be commonly expressed with 8 different dimensionalities.


In water pH control
In wastewater treatment and agriculture irrigation, carbonic acid is used to acidify the water similar to and produced by sulfur burners.


Under high CO2 partial pressure
In the beverage industry, sparkling or "fizzy water" is usually referred to as . It is made by dissolving carbon dioxide under a small positive pressure in water. Many treated the same way .

Significant amounts of molecular exist in aqueous solutions subjected to pressures of multiple (tens of thousands of atmospheres) in planetary interiors. Pressures of 0.6–1.6  at 100 , and 0.75–1.75 GPa at 300 K are attained in the cores of large icy satellites such as Ganymede, Callisto, and Titan, where water and carbon dioxide are present. Pure carbonic acid, being denser, is expected to have sunk under the ice layers and separate them from the rocky cores of these moons.


Relationship to bicarbonate and carbonate
Carbonic acid is the formal Brønsted–Lowry of the anion, stable in alkaline solution. The protonation constants have been measured to great precision, but depend on overall . The two equilibria most easily measured are as follows: \begin{align} \ce{CO3^{2-}{} + H+{} <=> HCO3^-} && \beta_1 = \frac{\ce{HCO3^-}}{\ce{H+}\ce{CO3^{2-}}} \\ \ce{CO3^{2-}{} + 2H+{} <=> H2CO3} && \beta_2 = \frac{\ce{H2CO3}}{\ce{H+}^2\ce{CO3^{2-}}} \end{align} where brackets indicate the of species. At 25 °C, these equilibria empirically satisfy (2006). " Stability constants" (database). \begin{alignat}{6} \log(\beta_1) =&& 0&.54&I^2 - 0&.96&I +&& 9&.93 \\ \log(\beta_2) =&& -2&.5&I^2 - 0&.043&I +&& 16&.07 \end{alignat} decreases with increasing , as does . In a solution absent other ions (e.g. ), these curves imply the following stepwise dissociation constants:\begin{alignat}{3} p\text{K}_1 &= \log(\beta_2) - \log(\beta_1) &= 6.77 \\ p\text{K}_2 &= \log(\beta_1) &= 9.93 \end{alignat} Direct values for these constants in the literature include and .

To interpret these numbers, note that two chemical species in an acid equilibrium are when . In particular, the extracellular fluid () in biological systems exhibits , so that carbonic acid will be almost 50%-dissociated at equilibrium.


Ocean acidification
The shows typical equilibrium concentrations, in solution, in , of carbon dioxide and the various species derived from it, as a function of pH. As human industrialization has increased the proportion of carbon dioxide in Earth's atmosphere, the proportion of carbon dioxide dissolved in sea- and freshwater as carbonic acid is also expected to increase. This rise in dissolved acid is also expected to those waters, generating a decrease in pH. It has been estimated that the increase in dissolved carbon dioxide has already caused the ocean's average surface pH to decrease by about 0.1 from pre-industrial levels.


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