Jaundice: Its Pathology and Treatment: With the Application of Physiological Chemistry to the Detection and Treatment of Diseases of the Liver and PancreasHarley, George
Science
Jaundice: Its Pathology and Treatment: With the Application of Physiological Chemistry to the Detection and Treatment of Diseases of the Liver and Pancreas
Harley, George
Jaundice
I cannot refrain from making a few remarks on what I consider the
injudicious employment of podophyllin. Like every new remedy, it has to
run the risk of falling into disfavour, in consequence of its too
ardent admirers blindly prescribing it in all cases of hepatic disease;
in many of which it must of necessity prove unsuitable, if not even
detrimental. In cases of jaundice, for example, podophyllin is at one,
and the same time, the bane, and the antidote. The bane in _all_ cases
of {114} jaundice from obstruction, the antidote in a _few_ cases of
jaundice from suppression. Having already indicated the cases in which
it may be administered with advantage, I shall now call attention to
one of those where it cannot be employed without injury, and one in
which it is, nevertheless, frequently given. The case I allude to is
that of gall-stones. When once a gall-stone has formed, and is blocking
up the common bile-duct, thereby causing jaundice from obstruction, it
is easy enough to understand why a substance like podophyllin, which
increases the biliary secretion, is to be avoided. It is not, however,
so easy to understand why the remedy is equally counter-indicated,
either during the formation or sojourn of a gall-stone in the
gall-bladder. This, therefore, I must explain. In speaking of the mode
of formation of gall-stones in the gall-bladder (page 43), I have
stated that their formation is due to the deposition of the less
soluble parts of the bile, either as a consequence of these ingredients
being in excess, or in consequence of the solvent, whose duty it is to
retain them in solution, being in reduced quantity. It follows, then,
as a natural result, that the longer bile sojourns in the gall-bladder,
and the thicker it becomes, the more likely are its constituents to be
deposited, and increase the size of the already existing concretion,
{115} or give origin to a new formation. It may be further added, that
the greater the amount of bile secreted, the longer is it likely to
remain in the gall-bladder, and the more concentrated to become; for,
as is well known, there is a constant absorption of the aqueous
particles of the bile going on during the whole time it is stored up in
its reservoir. If, then, during the intervals of digestion, the liver
secretes merely sufficient bile to meet the requirements of the
succeeding meal, by the end of the digestive process the gall-bladder
will be entirely emptied of its contents, and ready to receive a fresh
supply. Whereas, if the liver secretes more bile during the intervals
of digestion than the wants of the system require; after the completion
of each succeeding meal the excess of bile will remain behind in the
gall-bladder, and, while becoming stored up with that subsequently
secreted, of necessity, favour the increase or excite the formation of
gall-stones in persons predisposed to them. There being nothing more
conducive to the deposition of biliary calculi than a well-filled
gall-bladder.
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