As has already been stated, it is probable that symptoms closely

resembling if not identical with those of the passage of a calculus may

occur when the substantial cause of them does not make its appearance;

and although many of these may perhaps be accounted for by the

ill-success of the search or by the calculus having ceased to pursue

its downward course and having become quiescent in the kidney, yet it

is well for the practitioner to be prepared for an occasional

disappointment in obtaining tangible proof of the nature of the attack.

Time may be required to decide whether an attack is due to calculus, or

is simply one of the spasmodic or neuralgic paroxysms mentioned above.

If after careful watching no stone makes its appearance, and on the

other hand the pain does not continue and no pus gives evidence of

pyelitis, it is highly probable that no stone is or has been present.

A true neuralgia of the kidney may undoubtedly exist. Lumbago and

lumbar neuralgia may simulate renal colic, but are almost always much

less severe, the pain less sharp and more dull and aching, aggravated

by movement, while the sympathetic phenomena, especially those

connected with the urinary apparatus, are wanting.

The diagnosis of the character of the calculus can sometimes be made

with a reasonable degree of probability. If crystals of uric acid or of

oxalate of lime have been or are present in considerable quantity, it

is highly probable that a possible stone may consist of those

substances. These crystals, however, are of little value in proving the

presence of a stone.

The important diagnosis of the occlusion of a ureter by a calculus, and

at the same time that of the soundness of the opposite kidney, may be

made with great certainty if the urine, which has previously been

purulent, bloody, or containing renal epithelium or casts, suddenly

becomes {45} clear coincidently with the occurrence of symptoms of the

impaction of a stone.

It is not of course necessary that in every case of impaction the flow

of urine from the affected side should be entirely stopped, since the

calculus may be of such a shape as to permit the passage of urine past

it.

The PROGNOSIS in this affection is extremely favorable, so far as the

recovery from the individual attack is concerned, since if the stone is

small enough to enter the ureter it will probably be successful in

forcing its way through sooner or later. It is of course possible that

this pain, like any other of excessive severity, might cause death, but

such an occurrence must be extremely rare.

Perforation of the ureter may occur, with consequent peritonitis. A

permanent plugging of the ureter from failure of the calculus to pass

will give rise to changes in the kidney to be subsequently described.

In cases where only a single kidney exists, and this becomes

obstructed, the symptoms of suppression of the urine may come on,

including death by coma if the obstruction is not relieved. Ten days is

the limit assigned by Ebstein beyond which recovery is not to be

expected, but he mentions a case in which it took place after thirteen

days of anuria. It must be remembered that a painful obstruction, or in

fact any severe shock to one kidney, may produce a very great

diminution in the amount of urine even when the other is sound. This is

undoubtedly the result of nervous sympathy.

One attack of renal colic renders another very probable, either

immediately or after months or years. Several hundred small calculi may

follow each other in rapid succession, or, on the other hand, a single

one may leave the patient in peace for a long time. Much depends on the

character of the calculus, the diathesis and habits of the patient, and

upon the treatment.

The subsequent history of the renal calculus belongs to surgery. After

it has reached the bladder and failed to be discharged, it increases in

size and is removed by lithotomy or lithotrity. The urethra, however,

will usually permit to pass any stone which has come through the

ureter. The patient who has just experienced relief from renal colic

should be instructed to pass his water into a vessel which can be

examined, and if the calculus do not soon make its appearance he should

void the urine when stooping forward or even lying on his face, so as

to bring the stone to the orifice of the urethra. It may catch in the

urethra and demand surgical interference.

The TREATMENT of the paroxysm consists chiefly in relieving the pain,

which may be partly done by the hot bath or hot applications. Opium, or

preferably morphine subcutaneously, is likely to be called for in large

doses. Attention has been called to the danger of morphine in

sufficient dose to relieve severe pain in cases where, as in renal

colic, the pain is likely to be suddenly terminated by the natural

progress of the affection, thus destroying the physiological antagonism

which exists between pain and morphine, and allowing the drug to

exercise its full power to an extent which may be over-narcotic. The

use of atropine with the morphine will mitigate to some extent its

danger, without interfering with its analgesic effects.

{46} In the milder cases ether and chloroform may be of value given by

the mouth, while in excessively severe ones anæsthetics by inhalation

may be called for, and their use continued for hours. This course also

is not without its inconveniences. The writer has seen a case where a

somewhat prolonged maniacal attack, with delusions lasting several

days, came on after the long-continued use of chloroform to relieve the

pain incident to the passage of a multitude of small uric-acid calculi.

The use of diluents has been suggested as hastening the passage, but

there is no reason to doubt that the pressure upon the calculus is

always sufficient to move it forward as rapidly as its shape and size

will permit. The relaxation of the spasmodically contracted ureter is

of much more importance than an excessive vis-a-tergo applied to the

calculus.

The treatment of the incipient calculus in the kidney or of the

condition which gives rise to it must naturally vary according to its

chemical constitution, which can only be certainly determined after its

discharge, but as to which an approximate opinion can be formed from a

knowledge of the tendencies and diseases of the patient and from an

examination of the urine.

The use of a largely-diluted solution of citrate of lithia or of

acetate, citrate, or tartrate of potassium will probably prevent the

deposition of uric-acid sand, and might even dissolve a small calculus,

although the proofs of this having actually been done are not

conclusive. If the urine be largely diluted the risk of the formation

of a calculus of another kind--_i.e._ phosphatic--is not great. Simple

water would be of great value in many cases, both as dissolving uric

acid and as promoting the metamorphosis of tissue, upon some

abnormality of which the accumulation of uric acid is supposed to

depend. The benzoate of lithia, by the destructive action which Garrod

has shown benzoic acid or its derivative hippuric acid to have upon

uric acid and the solvent action of the lithia, may be of value. The

phosphatic deposit, on the other hand, although beneficially influenced

by a sufficient supply of water, is not so amenable to chemical

influence as the other form, because it is much easier to render the

urine alkaline than acid when any irritation of the urinary passages is

present.

The vegetable acids, however, pass into the urine, and may render it

acid if in sufficient quantity. Benzoic acid becomes hippuric acid, and

can be used to make the urine more acid, as it causes very little

gastric irritation even in considerable doses. Boric acid also passes

into the urine, and acidifies as well as disinfects it, and might

perhaps be used to promote the solution of a phosphatic stone, though

the writer is unaware of any instance in which this has actually been

done. It does much toward diminishing suppuration in the urinary

passages, upon which phosphatic urine largely depends.

The conditions which lead to the deposit of oxalate of lime are not

sufficiently well known to make the prophylaxis of this calculus easy

by any chemical means, except by dilution of the urine and by a general

tonic regimen with abundant exercise.

Although it is not usual for a calculus to be arrested in the ureter

after having once fairly entered, this sometimes occurs, and the result

is stoppage of the flow of urine upon that side, dilatation of the

ureter, followed in turn by dilatation of the pelvis, and finally

atrophy of the {47} renal substance. This does not happen suddenly,

however. The urinary passages do not rapidly dilate to any considerable

extent, and their increase in calibre under pressure from within has

been considered a growth rather than a distension. This condition will

be treated under the head of Hydro-nephrosis.

Calculous Pyelitis.

When a calculus remains in the pelvis of the kidney without completely

obstructing the flow of urine, it usually increases in size, while the

resulting irritation may be the cause of fresh deposits either upon the

surface of the original calculus or in the form of new concretions. In

this way immense deposits of urinary salts may be formed. Thus, in a

case given in detail in the second series of _Boston City Hospital

Reports_ there was found upon the one side a calculus which when

perfectly clean and dry weighed 204 grammes, filling the whole dilated

pelvis and sending prolongations into the calices, so that its shape

was compared to that of a hippopotamus. The resemblance was made more

complete by the wrinkling and roughness of the exterior. In the other

kidney were several hundred calculi, from the size (and shape) of a

large almond down to that of white mustard-seed. The latter were

composed of two apparently distinct substances--one a reddish-brown,

looking like uric acid, and the other of the color and polish of white

marble; both, however, were phosphates.

The amount of local disturbance produced in the pelvis of the kidney by

the presence of a foreign body seems to depend somewhat upon the

character of its surface. Rough and uneven calculi, such as oxalate of

lime, are apt to produce inflammation much more rapidly than smooth and

polished ones, but it is seldom that any calculus remains without some

pyelitis. At first only a loss of polish of the mucous membrane, with a

little increase of mucus, may be observed, to which succeed roughening

and suppuration with occasional fibrinous deposit. The pelvis, more or

less dilated, may then contain a quantity of mucopurulent urine, with

perhaps some blood, in which are concealed the stones which have given

rise to this condition, and often phosphatic deposits not converted

into calculi.

Pyelitis is divided by some foreign writers into catarrhal and

diphtheritic--a distinction rather of degree than of kind. The mucous

membrane of the pelvis may, like other mucous membranes rarely, and

like serous membranes often, throw out a fibrinous exudation which

takes the form of false membrane. This indicates intensity of

inflammation, but has no necessary connection with diphtheria. A true

diphtheritic pyelitis, that is, connected with the general disease

known as diphtheria, is of course a conceivable lesion, but certainly

not a common one.

The renal symptoms--especially true albuminuria, so common and of such

grave import in this disease--are due to lesions of the secreting

substance, and not of the pelvis. It is important, but not always easy,

to decide whether there is more albumen present than is to be accounted

for by the pus. The pyelitis may be acute or chronic, being {48}

characterized by the intensity of the attack and the rapidity with

which the symptoms subside. The prospect of a given attack being acute

is decided largely by the supposed cause: a small calculus passing into

the ureter undoubtedly gives rise in most instances to a localized

pyelitis, which subsides after the cause of irritation has disappeared.

An inflammation from a larger one remaining is naturally of slower

development, but may be more acute while the calculus remains rough and

irritating, and partially subside when it becomes covered with a

smoother coating of phosphates. The mucous membrane, however, is not

likely to regain a completely healthy condition.

The mucous membrane in severe pyelitis may be deeply eroded, and even

perforated, so that the contents of the pelvis escape and give rise to

abscess in the perinephritic or prevertebral cellular tissue, which may

be discharged through the loins with resulting cure, or the

establishment of a fistula, from which issues pus and at times calculi.

Among the rarer results of perforation may be mentioned gastro-nephric

and duodeno-nephric fistulæ. These might be diagnosticated by the

presence of food and other intestinal contents in the urine, provided

that the ureter were still pervious. Vomiting of calculi and urine has

been reported by the older writers.

The writer is indebted to J. R. Chadwick for references to two modern

cases--one where such a fistula was diagnosticated during life;[16] and

another where a gastro-nephric fistula was found after death.[17] In

the latter case a diagnosis would have been impossible, as the kidney

was disorganized and the ureter occluded. The extent to which the renal

secreting substance suffers in calculous pyelitis varies considerably,

and is very probably connected with the amount of pressure exercised

either by the calculus itself when it attains a large size or by the

urine in cases of obstruction. It is rare for either pyelitis or

hydro-nephrosis to exist entirely independently.

[Footnote 16: _Giornale di Anat. e Fis. path._, iii. p. 370.]

[Footnote 17: Marquezy, _Thèse de Paris_, 1856.]

The changes which take place are those of atrophy. Interstitial

suppurative nephritis seems to follow this form of pyelitis much less

frequently than that which is due to extension upward of disease in the

lower urinary passages.

Corresponding to the pressure of solid or fluid, the papillæ are eroded

and the straight tubes shortened. In the cortical substance, which soon

becomes diminished in thickness, the interstitial tissue is

hypertrophied, dense, and hard, while the tubes become smaller or in

time disappear. The Malpighian bodies are changed to dense masses of

connective tissue, but are still plainly recognizable, irregularly

crowded together instead of being arranged as usual in more or less

symmetrical double rows. The cortex of the kidney may thus become but

little more than a mere skin stretched over a large stone, with perhaps

here and there a piece of renal structure recognizable and in a

comparatively normal condition.

The extremer grades of hydro-nephrosis do not seem to be met with in

this form of atrophy, but the pelvis is considerably dilated, while its

internal capacity is also added to by the atrophy of the renal

substance. The interior of the cyst thus formed usually retains

distinct traces of its original division into infundibula, and may be,

as already stated, almost filled by the calculus. Kidneys undergoing

this process of degeneration {49} often furnish up to a short time

before death a normal, or even more than normal, amount of urine, and

one is often astonished to find how little disturbance of elimination

has been caused in cases where the true kidney-structure seems to the

naked eye to have been almost entirely destroyed.

The DIAGNOSIS of a calculus remaining in the pelvis of the kidney

depends chiefly on the determination of hæmaturia and pyelitis for

which no other cause can be found, and upon the presence of pain in one

loin. It is naturally greatly assisted by the presence or history of

renal colic. An aching pain in the loins, more or less permanent, is a

frequent but not invariable symptom. It may be such as to prevent the

patient from standing upright, and cause him to assume an habitually

stooping posture in standing or walking. A careful examination of the

urine in conjunction with this symptom, especially if an unusually

abnormal condition has been preceded by an exacerbation of the pain,

may make the diagnosis almost certain. In the beginning of a case

occasional not severe hæmaturia, with some increase of mucus or a

little pus, may be all that can lead to the suspicion of calculus as

the cause of pain. At a later period an increase of these symptoms,

with a considerable quantity of the peculiar irregular epithelium

lining the pelvis, may be observed. The latter constituent, however,

can hardly be looked upon as entirely conclusive of pyelitis, since the

lower urinary passages may give rise to cells of about the same form

and size, and the irregularity is likely to be increased beyond

recognition by the presence of inflammation. They may also undergo

change of form in the urine. The presence of transparent or other casts

denotes the irritation of the renal parenchyma.

The point of chief difficulty in the diagnosis of pyelitis is the

determination of the origin of the pus, whether from the kidney or the

bladder. Cystitis may be only partly excluded by the absence of

dysuria. A point of considerable weight is the reaction of the urine,

that from the kidneys being usually acid, while that from the bladder,

when cystitis of much severity exists, is alkaline or rapidly becomes

so. The pus coming from the kidneys is more intimately mixed with the

often profuse urine than when formed in the bladder. The whole of it

does not in the former case completely subside, but remains in

sufficient quantity to form a turbid or opalescent mixture--the

polyuric trouble of Felix Guyon, according to whom this condition in an

acid urine is strongly indicative of renal as distinguished from

vesical lesion. In cystitis the pus subsides in more or less distinct

masses, but if the urine is alkaline, or when it becomes so, is altered

to a ropy consistency usually spoken of as muco-purulent.

The procedure recommended by Thompson may be resorted to in order to

determine whether the urine comes from the kidneys loaded with cellular

detritus, or whether the addition is made in the bladder. This consists

in washing out thoroughly the bladder with several successive

quantities of water through a single catheter, until the water comes

away clear and the bladder has contracted itself around the instrument,

when the urine from the kidneys will for a time come through direct and

comparatively uncontaminated.

In cases where the urine is alkaline in the kidney, which may happen,

distinctions founded on the reaction cannot be of value, and the same

{50} may be said of cases where cystitis is known to exist, but where

there is in addition a possibility of a renal calculus. In these some

such mechanical procedure as that just described must be resorted to.

The presence of a calculus as a cause of pyelitis cannot always be

demonstrated, but may be more or less strongly suspected according to

the conclusiveness with which any other cause can be excluded, by the

definiteness and character of the local pain, the history of renal

colic, the presence of uric-acid crystals in the urine, and perhaps in

some cases the results of palpation. The exploring-needle may be used,

and may of course, if reaching the calculus and giving a characteristic

grating feeling and sound, give absolutely positive results; but a

failure to strike a stone could hardly be regarded as proof positive of

its absence.

The diagnosis of renal calculus from lumbago or neuralgia should rest,

in case the pain is severe enough or long-continued enough to really

cause the question to arise, upon an examination of the urine.

A very important point in diagnosis, especially when the question of

operative procedure arises, is that of the soundness of the other

kidney. Accidental circumstances will sometimes permit this to be

determined; as, for instance, when one ureter is suddenly blocked by a

calculus, and at the same time the urine, which has previously been

found purulent, bloody, and containing renal cells and casts, becomes

clear and normal until the obstruction is removed and the abnormal

ingredients reappear. Cases of exstrophied bladder, where of course it

is possible easily to separate the urine of the two kidneys, may be,

from their rarity, practically left out of the account. Various

proposals for obtaining the separate urine of the two kidneys have been

made. A small catheter has been passed into the female ureter through

the dilated urethra. In the female also a finger in the vagina may

succeed in temporarily blocking one ureter, while the secretion of the

other alone is filling the bladder, a catheter with a bent portion at

the end being used for making counter-pressure from the inside. It

would probably remain doubtful in most cases how successful this

manoeuvre had been in completely stopping the flow of urine, although

experiments upon the dead body have been made by Polk,[18] who proposes

the method, with entire success. The male bladder offers greater

difficulties, which are at present insurmountable. A point opposite the

lower end of the ureter can, it is true, be reached with some

difficulty in the rectum, and it is possible that a catheter might be

so adjusted as to make counter-pressure to the finger in this position,

but there could be no certainty that the occlusion was complete.

[Footnote 18: _New York Med. Journ._, Feb. 17, 1883.]

The whole hand in the rectum, after Simon's method, would enable the

object to be accomplished with more certainty, but this procedure has

risks of its own. A staff with flattened extremity, as suggested by

Weir,[19] may more conveniently, though with somewhat less certainty,

be used for pressing from within the rectum on the ureter where it

passes over the brim of the pelvis. A compressorium consisting of an

empty and folded bag, to be introduced into the bladder and there

expanded by the introduction of metallic mercury, has been described

and used, with the result of partly checking the flow of urine.[20] The

proposition to pinch up the extremity of one ureter in the bladder by

means of the lithotrite is still {51} more open to the objection of

great uncertainty, and would, to say the least, demand very special

skill to obtain even a chance of success.

[Footnote 19: _Ibid._, Dec. 27, 1884.]

[Footnote 20: See Weir's article, just quoted.]

None of these procedures have as yet been put to practical use, and it

is doubtful whether any of them, unless we except perhaps the use of a

staff in the rectum, would be justified for purely diagnostic purposes,

considering the great risks involved. For the present, at least, the

possibility of separating the secretion of one kidney from that of the

other must be looked upon as depending chiefly upon accident, and in

case of contemplated operation it is not possible to assure one's self

of the integrity of the other kidney before the abdomen is opened. In

many cases after opening the abdomen both kidneys may be examined

before deciding upon further steps. Lawson Tait considers an

exploratory incision distinctly indicated whenever abdominal disease

not malignant threatens the life of the patient. The soundness of the

other kidney, however, may be considered highly probable if in spite of

demonstrated extensive disease of one kidney a sufficient quantity of

urine with a normal amount of urea and salts continues to be formed.

The SYMPTOMS arising from a large calculus producing destruction of the

renal substance, when both kidneys are affected or one is insufficient

to supplement the partial or total loss of the other, may closely

resemble those of diffuse nephritis, either interstitial or

parenchymatous, or perhaps it would be more correct to say that these

forms of nephritis are the symptoms of such a change. Thus we may have

polyuria, albumen, and casts, dyspnoea, dropsy, and uræmia. The

enormous calculus described above as resembling a hippopotamus had

given rise to no marked symptoms until palpitation, dyspnoea, and

oedema were complained of; the heart was hypertrophied.

A system of practical medicine. By American authors. Vol. 4 · 第 4 / 116 段