100 ' DISEASES OF THE HORSE. 



■water freely, and let the food be only such as contains a large propor- 

 tion of liquid, gruels, mashes, turnips, beets, apples, pumpkins, 

 ensilage, succulent grasses, etc. If the acute stage has passed and 

 the presence of the calculus is manifested only by the frequent passage 

 of urine with gritty particles, by stiffness of the loins and hind limbs, 

 and by tenderness to pressure, the most promising resort is a long run 

 at pasture where the grasses are fresh and succulent. The long- 

 continued secretion of a watery urine will sometimes cause the break- 

 ing downi of a calculus, as the imbibition of the less dense fluid bv the 

 organic spongelike framework of the calculus causes it to sAvell and 

 thus lessens its cohesion. The same end is sought by the long-con- 

 tinued use of alkalies (carbonate of potassium), and of acids 

 (muriatic), each acting in a different way to alter the density and 

 cohesion of the stone. But it is only exceptionally that any of these 

 methods is entirely satisfactory. If inflammation of the kidneys 

 develops, treat as advised under that head. 



Stone in the hladder {vesical calculus^ or cystic calcvlus). — These 

 may be of any size up to over a pound in weight. One variety is 

 rough and crystalline and has a yellowish white or deep-brown color. 

 These contain about 87 per cent carbonate of lime, the remainder 

 being carbonate of magnesia, oxalate of lime, and organic matter. 

 The phosphatic calculi are smooth and white and formed of thin 

 concentric layers of great hardness extending from the nucleus out- 

 ward. Besides the phosphate of lime these contain the carbonates of 

 lime and mae-nesia and organic matter. In some cases the bladder 

 contains and may be even distended by a soft pultaceous mass made 

 up of minute round granules of carbonates of lime and magnesia. 

 This, when removed and dried, makes a firm, white, and stony mass. 

 Sometimes this magma is condensed into a solid mass in the bladder 

 by reason of the binding action of the mucus and other organic 

 matter, and then forms a conglomerate stone of nearly uniform con- 

 sistency and Avithout stratification. 



Symptoms of stone in the hladder. — The symptoms of stone in the 

 bladder are more obvious than those of renal calculu . The rough 

 mull^erry calculi especially lead to irritation of the mucous membrane 

 and frequent passing of urine in small quantities and often mingled 

 with mucus or blood or containing minute gritty particles. At times 

 the flow is suddenly arrested, though the animal continues to strain 

 and the bladder is not quite emptied. In the smooth phosphatic 

 variety the irritation is much less marked and may even be altogether 

 absent. With the pultaceous deposit in the bladder there is incon- 

 tinence of urine, which dribbles aAvay continually and keeps the hair 

 on the inner side of the thighs matted with soft magma. In all cases 

 alike the calculus may be felt by the examination of the bladder Avith 

 the oiled hand in the rectum. The pear-shaped outline of the bladder 



