Which unites with the magnesia derived from the feed
Carbonate of magnesia, another almost constant ingredient of the urinary
calculi of the horse, is formed the same way as the carbonate of
lime from the excess of carbonaceous feed (organic acids) becoming
oxidized into carbon dioxid, which unites with the magnesia derived from
the feed.
The phosphates of lime and magnesia are not abundant in urinary calculi
of the horse, the phosphates being present to excess in the urine in
only two conditions (a) when the ration is excessive and especially
rich in phosphorus (wheat, bran, beans, peas, vetches, rape cake, oil
cake, cottonseed cake); and (b) when, through the morbid, destructive
changes in the living tissues, and especially of the bones, a great
quantity of phosphorus is given off as a waste product. Under these
conditions, however, the phosphates may contribute to the formation of
calculi, and this, above all, is liable if the urine is retained in the
bladder until it has undergone decomposition and given off ammonia. The
ammonia at once unites with the phosphate of magnesia to form a double
salt phosphate of ammonia and magnesia which, being insoluble, is at
once precipitated. The precipitation of this salt is, however, rare in
the urine of the horse, though much more frequent in that of man and
sheep.
Source: Diseases of the Horse