The contact of a gall-stone, especially of a polyangular stone, may cause ulceration of the mucous membrane. This is the more apt to occur if the muscular layer of the gall-bladder is hypertrophied, especially if certain fasciculi are thickened and overacting, leaving intervening parts weak and yielding to the pressure of the stone forced in by the spasmodically contracting muscles. Finally yielding, the stone and other contents of the gall-bladder escape into the cavity of the abdomen. Adhesions to neighboring parts may prevent rupture. Such adhesions are contracted with the colon, the duodenum, the stomach, and other organs. In some rare instances the closed gall-bladder has undergone a gradual process of calcification, the mucous membrane losing its proper structure, the muscular layer degenerating, and a slow deposit of lime salts taking place, the ultimate result being that the biliary concretions are enclosed in a permanent shell.
As above indicated, biliary concretions may remain where deposited for an indefinite period. Very often they migrate from the point of formation, the gall-bladder, into the duodenum, producing characteristic symptoms called hepatic colic. As the size of the ducts increases from above downward, obviously but little vis a tergo is needed to propel the concretions onward. The chief agency in the migration of these bodies is the discharge of bile. Common observation shows that the symptoms of hepatic colic usually declare themselves in two or three hours after a meal—at that time when the presence of the chyme in the duodenum solicits the flow of bile. The gall-bladder contracts on its contents with an energy in direct ratio to the amount of bile present, and with the gush of fluid the concretion is whirled into the duct. Once there, the cystic duct being unprovided with muscular fibres, the onward progress of the stone must depend on the flow of bile; and, as the canal is devious, this may not always carry the concretion into the common duct. Just behind the neck of the gall-bladder the duct makes an angle somewhat abrupt, and here also its folds project into the canal, so that at this point the stone is apt to lodge; but much depends on the size and shape of the calculus. If it pass through the cystic duct, the inflammation resulting may close the canal, several instances of which have fallen under my observation. The next point where stoppage of the migrating calculus may, and frequently does, occur is the orifice of the common duct in the duodenum. This orifice has a funnel shape, the smaller extremity toward the intestine, the object of this being to prevent the entrance into the duct of foreign bodies from the intestine. A diverticulum is thereby made (Vater's) in which a concretion may lodge, partly or wholly preventing the escape of bile into the bowel. The various forces concerned in the propulsion of the concretion onward from the common duct into the intestine are the discharges of bile, the contraction of the few muscular fibres in the walls of the duct, the respiratory movements, especially forced expiration, coughing, sneezing, vomiting, defecation—in fact, all of those acts in which the abdominal muscles, the diaphragm, and the sphincters are simultaneously brought into strong contraction. The symptoms produced by the migration and stoppage of a concretion will vary according to the size and shape of the stone, and the consequent diminution in the amount of bile discharged or its complete arrest. In other words, the stone may be firmly wedged in, completely closing the canal against the passage of bile, or it may lie loosely in the diverticulum Vateri, acting as a sort of ball valve, now permitting a gush of bile, and now stopping the passage-way more or less tightly.
The migration of calculi may take place by ulcerating through into neighboring hollow organs. Usually the first step consists in stoppage of the bile. To the accumulating bile mucus is added, and the gall-bladder or the duct—usually the common or cystic duct—dilates, often to a considerable extent, and, adhesions forming, discharge ultimately takes place through some neighboring hollow organ. The routes pursued by such fistulous communications are various. The organs most frequently penetrated are the stomach, duodenum, and colon, less often the urinary passages, and very rarely the portal vein. Numerous examples of external discharge of calculi have been reported. The most usual, as it is the most direct, is the fistulous connection of the gall-bladder or common duct with the duodenum. Solitary stones of immense size have been thus discharged. Murchison167 gives references to many interesting examples, and the various volumes of Transactions of the Pathological Society are rich in illustrative cases. The symptoms produced by the migration of calculi by the natural route and by ulceration into other organs will be hereafter considered.
167 Clinical Lectures on the Diseases of the Liver, 2d ed., p. 487 et seq.
SYMPTOMS DUE TO THE PRESENCE OF GALL-STONES AT THEIR ORIGINAL SITE.—Very large calculi or numerous small ones may be present in the biliary passages without causing any recognizable symptoms. The migration of these bodies by the natural channel and by ulceration into the duodenum may also be accomplished without any local or systemic disturbance.168 That the retention of calculi may not induce any characteristic reaction by which they may be recognized is probably due to the fact that the gall-bladder, in which they chiefly form, possesses but slight sensibility, and as it is in a constantly changing state of distension or emptiness according to the amount of bile present, it is obvious that a foreign body made up of the biliary constituents, and having nearly the same specific gravity as the bile, is not likely to cause any uneasiness or recognizable functional disturbances. Furthermore, the slowness with which biliary concretions form enables the organ to accommodate itself to the new conditions. The lack of sensibility which is a feature of the gall-bladder, and which I have had the opportunity to ascertain by actual puncture in an individual not anæsthetized, is in some instances supported by a general state of lowered acuteness of perception. There are great differences in respect to readiness of appreciation and promptness of response to all kinds of excitation in different individuals. To what cause soever we may ascribe the lack of sensibility, the fact remains that in not a few cases of gall-stones in the gall-bladder there are no symptoms to indicate their presence. On the other hand, there are some disturbances that have a certain significance.
168 Amongst the numerous examples of this kind to be found recorded may be mentioned the case reported by M. L. Garnier, Agrégé à la Faculté de Médecine de Nancy (Archives de Physiologie normale et pathologique, No. 6, 1884, p. 176): An hepatic calculus, weighing 24.5 grammes, was discharged without any symptoms or even consciousness on the part of the patient, a man of sixty years. He had had colic and jaundice, but these subsided entirely, and there was no further disturbance. As has happened in so many instances, this stone must have ulcerated through into the bowel without causing any recognizable symptoms.
The subjective signs are uneasiness—a deep-seated sensation of soreness—felt in the right hypochondrium, increased by taking a full inspiration and by decubitus on the left side. Pain or soreness, sometimes an acute pain, is experienced under the scapula near the angle, at or about the acromion process, and sometimes at the nape of the neck. In one case under my observation within the past year a patient who had had several attacks of hepatic colic, the usual polyangular stones having been recovered, had from time to time severe pain over the right side of the neck, shoulder, and scapula, accompanied by a severe herpes zoster in the district affected by the pain. This is of course an extreme example, but it is very suggestive of the relation which may exist between hepatic disturbances and shingles. Attacks of gastric pain coming on some time after food, and not soon after, as is the case in true gastralgia, are usual in the early stage of the disease—are constant, according to Cyr,169 who quotes approvingly an observation of Leared on this point. Migraine or sick headache and vertigo occur in many cases, but it may well be doubted whether these symptoms are not due to the accompanying gastro-duodenal catarrh, which is a nearly constant symptom. Acidity, flatulence, epigastric oppression, a bitter taste, a muddy rather bilious complexion, and constipation are symptoms belonging to catarrh of the gastro-duodenal mucous membrane. Most of these symptoms are rather indefinite. Some additional information may be supplied by palpation. When the gall-bladder is distended with gall-stones, or is in the enlarged state which occurs when the common duct is obstructed, it may project beneath the inferior border of the liver far enough to be felt. In thin persons a grating sound, produced by the friction of the calculi, may be heard, the stethoscope being applied as palpation is made over the hypochondrium. It is rare that these symptoms can be elicited, since the calculous affection of the liver occurs for the most part in persons of full habit, in whom the abdominal walls are too thick to allow of the necessary manipulation. There may be also some tenderness on pressure along the inferior margin of the ribs, especially in the region of the gall-bladder.
169 Traité de l'Affection calculeuse du Foie, p. 71.
SYMPTOMS DUE TO THE MIGRATION OF GALL-STONES BY THE NATURAL CHANNELS.—A calculus passing into the cystic duct from the gall-bladder causes the disturbance known as hepatic colic or bilious colic, because of the jaundice which accompanies the major part of these seizures. But jaundice is not a necessary element in these cases; it is not until the concretion reaches the common duct that the passage of bile into the intestine is interfered with. The gall-bladder has a function rather conservative than essential, for its duct may be permanently closed without apparently affecting the health.
The time when an attack of hepatic colic is most likely to occur would seem to be determined by the flow of bile; for this, as has been stated, is the chief factor in moving calculi along the ducts. As, no doubt, the presence of the chyme in the duodenum is the stimulus for the production of bile and also for the contractions of the gall-bladder, it follows that a few hours after meals is the time when the attacks of hepatic colic would a priori be expected. This is in accord with experience, but there are exceptions. In one of the most formidable cases with which the writer has had to deal—the diagnosis confirmed by the recovery of the calculi—the most severe attacks occurred in the early morning. According to Harley,170 colic from the passage of inspissated bile occurs when the stomach and duodenum are most nearly empty—from ten at night until ten in the morning—and this he relies on as a means of diagnosis, but the exceptions are too numerous to assign much importance to this circumstance.