Gilbertus Anglicus - Medicine of the Thirteenth Century by Henry Ebenezer Handerson
page 96 of 105 (91%)
page 96 of 105 (91%)
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Compendium by an abstract of Gilbert's views on vesical calculus and
its treatment, which cover more than fifteen pages of his work. Stone and gravel arise from various viscous superfluities in the kidneys and bladder, which occasion difficulty in micturition. Stone is produced by the action of heat upon viscous moisture, sublimating the volatile elements and condensing the denser portions. Putrefication of stone in the bladder is the result of three causes, viz., consuming heat, viscous matter and stricture of the meatus. For consuming heat acting on viscous material retained by reason of stricture of the meatus, by long action dries up, coagulates and hardens the moisture. This is particularly manifest in boys who have a constricted meatus. Stones are thus generated not only in the kidneys and bladder, but also even in the stomach and the intestines, whence they are ejected by vomiting or in the stools. Indeed they may also be found occasionally in the lungs, the joints and other places. They are comparatively rare in women, in consequence of the shortness of the urethra and the size of their meatus. Sometimes calculi occur in the bladder, sometimes in one kidney and occasionally in both kidneys. The symptoms produced by their presence vary in accordance with the situation of the concretion. If the stone is in the kidney, the foot of the side affected is numb (_stupidus_), the spine on the affected side is sore and there is difficulty of micturition and considerable gravelly sediment in the urine. If the stone is increasing in size, the quantity of sediment also increases, but if the stone is fully formed and confirmed, the amount of sediment decreases daily, and the urine becomes milky both in the kidneys and |
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