The importance of oxalic acid in medicine derives from the extreme insolubility of its calcium salt in water, at around 12 mg or 0.13 mM per litre, which is affected little by pH above 5, but increases as the pH falls below 5 [I]. Because calcium and oxalate require to be excreted in substantial quantities by the kidneys, averaging 4-5 mM and 0.3 mM per day respectively in the adult, urinary supersaturation with calcium oxalate is the norm. Complex and elaborate mechanisms exist to prevent the formation, growth and agglomeration of crystals in the urinary tract. processes which are believed to be precursors of stone formation.Calcium oxalate is the major constituent of over 70% of upper urinary tract stones. In calcium-containing stones, oxalate is most commonly the major anion, with varying amounts of calcium phosphate. Pure calcium oxalate stones are common, whereas predominantly calcium phosphate stones are less frequent « 10%). It has generally been assumed that the determination of the relative amounts of oxalate versus phosphate in idiopathic calcium stones is of little clinical value. Gault et al. [2], using a semiquantitative infrared analytical method [3 J, have recently addressed this issue in detail, and found that phosphate stones (oxalate: phosphate ratio < I) are commoner in females, tend to be larger than predominantly oxalate stones (oxalate: phosphate> 10), and in about 250/c of patients are associated with a defect in urinary acidification. These patients did not have complete distal renal tubular acidosis, and most did not have hypocitraturia. It is unclear whether these patients should receive different therapy from the commoner idiopathic calcium oxalate stone former [4]. Aside from these idiopathic calcium phosphate stone formers, calcium phosphate stones are usual in complete distal renal tubular acidosis (RTA), and are common (though less so than calcium oxalate) in primary hyperparathyroidism [5].
Sources of urinary oxalateIt is generally stated that in normal man, some 40% of urinary oxalate is derived from serine and glycine via glyoxylate, 40% from ascorbic acid via as yet uncertain metabolic intermediates, and 5-10% from dietary oxalate. An average (Western) 1. Talati et al. (eds) The Manar;ement of Lithiasis. 57-68