Whii \ r. « OMPOSITION, AND ' BAR ■ OP i RIN 



is a large amounl of the disodium hydrogen phosphal lalcium 



and magnesium phosphates are mo i nble than the diphosphat 



the same metals, deposits of tl arthj phosphati I i" 



neutral or alkaline urines. When the urine is heated, the diphospl 

 of calcium breaks up into the mono-calcium and a fcri-calcium pi 



phate, which at nuts Eor the fine turbidity often taken for albumin in 



the flame test. Addition of arid will cause this to disappear. Th< 



tals of triple phosphates which occur in alkaline urine are ammonium 



magnesium phosphate, N 'I I Mg I' 1 1 



KIDNEY REFERENCE 



Monographs 



Beddard, A. P.: Recenl Advances in Physioloj 



L906. 

 Cushny, A. B.: Secretion of Urine, Longmans, Green ..v I '17. 



(Original Pape 



iBrodie, T. G., and Mackenzie, J. J.: Proc. Ro - . L914, lxzxvii, I 

 -•'ushiiv, A. I;.: Secretion of Urine, 1917, |>. I s . 

 sAddia and Watanabe: Jour. Biol. Chem., 1916, x\i\, 2 

 Mosenthal, II. O.: Arch. [nt. Med., 1915, xvi, 733. 



Lmbard and Weil: Physiologie normale el pathologique des reins, Par 

 .1. B. Bailliere el fils. 

 BMaclean, P. C.: Jour. Exper. Med., 1915, xxii, 212. 

 • ('Ii.-isc and Meyers: Jour. Am. Med. Assn., 1916, Ixvii, 931. 

 JVan Slyke, D. D., and Meyer, G. M.: Jour. Biol. Chem., 1912, ■: and I 



xvi, 197, 213 and 231. 

 »Knowlton, I'. P.: Jour. Physiol., 1911, xliii, 219. 

 Baxcroft, J., and Straub, II.: Jour. Physiol., 1910, xli, ' 

 uRowntree and Geraghty: Jour. Pharm. and Exper. Therap., 1910, i. 57 

 i2Asher and Pearce, R. G.: Zeitschr. f. Biol., 1913, Ixiii, - 

 ispearce. R. G., and Carter, E. P.: Am. Jour. Physiol., 1915, \\\ 



