Search results
Results from the WOW.Com Content Network
chemistry (ratio of sensible to latent energy absorbed during liquid-vapor phase change) [3] pH = (+) chemistry (the measure of the acidity or basicity of an aqueous solution) van 't Hoff factor: i = + ()
In this case H 0 and H − are equivalent to pH values determined by the buffer equation or Henderson-Hasselbalch equation. However, an H 0 value of −21 (a 25% solution of SbF 5 in HSO 3 F) [5] does not imply a hydrogen ion concentration of 10 21 mol/dm 3: such a "solution" would have a density more than a hundred times greater than a neutron ...
The measurement of pH can become difficult at extremely acidic or alkaline conditions, such as below pH 2.5 (ca. 0.003 mol/dm 3 acid) or above pH 10.5 (above ca. 0.0003 mol/dm 3 alkaline). This is due to the breakdown of the Nernst equation in such conditions when using a glass electrode.
Alkalinity roughly refers to the molar amount of bases in a solution that can be converted to uncharged species by a strong acid. For example, 1 mole of HCO − 3 in solution represents 1 molar equivalent, while 1 mole of CO 2− 3 is 2 molar equivalents because twice as many H + ions would be necessary to balance the charge.
acid + base → salt + water. For example: HCl + NaOH → NaCl + H 2 O. Acidimetry is the specialized analytical use of acid-base titration to determine the concentration of a basic (alkaline) substance using standard acid. This can be used for weak bases and strong bases. [8] An example of an acidimetric titration involving a strong base is as ...
An equivalent (symbol: officially equiv; [1] unofficially but often Eq [2]) is the amount of a substance that reacts with (or is equivalent to) an arbitrary amount (typically one mole) of another substance in a given chemical reaction. It is an archaic quantity that was used in chemistry and the biological sciences (see Equivalent weight § In ...
On this scale, pure H 2 SO 4 (18.4 M) has a H 0 value of −12, and pyrosulfuric acid has H 0 ~ −15. [7] Take note that the Hammett acidity function clearly avoids water in its equation. It is a generalization of the pH scale—in a dilute aqueous solution (where B is H 2 O), pH is very nearly equal to H 0 .
The increase in atmospheric increases H+ ion production because in the ocean reacts with water and produces carbonic acid, and carbonic acid releases H+ ions and bicarbonate ions. [15] Overall, since the Industrial Revolution the ocean has experienced a pH decrease by about 0.1 pH units due to the increase in C O 2 {\displaystyle \mathrm {CO_{2 ...