On Digestive Proteolysis: Being the Cartwright Lectures for 1894Chittenden, R. H. (Russell Henry)
Science
On Digestive Proteolysis: Being the Cartwright Lectures for 1894
Chittenden, R. H. (Russell Henry)
Digestion; Digestive enzymes; Enzymes
NaH_{2}PO_{4} + NaCl = Na_{2}HPO_{4} + HCl.
It is also to be noted that the disodium hydrogen phosphate, may,
likewise, give rise to hydrochloric acid through its action on calcium
chloride, as indicated by the following equation:
2Na_{2}HPO_{4} + 3CaCl_{2} = Ca_{3}(PO_{4})_{2} + 4NaCl + 2HCl.
It is thus evident that hydrochloric acid may originate in the
inter-reaction of these several salts which are known to be present
in the blood; but obviously, the above reactions cannot take place
in the blood itself, and we must look to the selective power of the
epithelial cells of the gastric glands, as suggested by Gamgee,[96] for
the withdrawal of the needed salts from the blood. Once present in the
acid-forming cells, and perhaps aided by the inherent qualities of the
protoplasm, the necessary chemical reactions may be assumed to take
place, after which the newly formed acid may pass from the gland-cells
into the secretion of the gland.
[96] Physiological Chemistry of the Animal Body, vol. 2, p. 113.
A later theory regarding the formation of the acid of the gastric juice
emanates from Liebermann.[97] This investigator claims the existence in
the mucous membrane of the stomach of an acid-reacting, nuclein-like
body, which is apparently a combination of the phosphorized substance
lecithin with a proteid. To this compound body Liebermann gives
the name of lecithalbumin. It is apparently located in the nuclei
of the gastric cells, is strongly acid in reaction, and, according
to Liebermann, is an important agent in the production of the free
hydrochloric acid of the gastric juice, although its action is somewhat
indirect. According to this theory, the free acid is formed in the
mucous membrane of the stomach from sodium chloride, through the
dissociating action of the carbonic acid coming from normal oxidation.
The thus-formed acid then diffuses in both directions, viz., through
the lumen of the gland into the stomach-cavity, and in part in the
opposite direction into the veins and lymphatics. It is the assumed
function of the lecithalbumin to react with the alkaline sodium
carbonate, produced simultaneously with the hydrochloric acid. This
naturally gives rise to the liberation of carbonic acid and to the
formation of a non-diffusible sodium-lecithalbumin compound, which
is retained for the time being in the body of the cell. When the
circulation of the blood, accelerated by the digestive process, returns
to its ordinary pace, this latter compound is slowly decomposed by
the carbonic acid with formation of the readily diffusible sodium
carbonate, which passes into the blood-current. The rate of this
latter reaction is impeded, or, perhaps regulated, by the swelling up
of the lecithalbumin-containing cells, thus rendering the imbibition
of the carbonic acid a slow process. The rate of production of the
hydrochloric acid by this hypothetical process depends primarily upon
the blood supply, and the oxidative changes by which carbonic acid is
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