Stone disease of the urinary tract
Pathophysiology of stone disease
Stones are often formed from a mixture of chemical substances and minerals (e.g. calcium and oxalate) when their concentration exceeds their solubility in urine. Intermittent periods of super-saturation due to dehydration, following meals or medical conditions, can lead to the earliest phase of crystal formation. Lack of crystallisation inhibitors in the urine may also play a role in stone formation. Table 37.1 provides a simple chemical classification showing the relative frequency of stone types and their important clinical characteristics and aetiology. Calcium is present in approximately 80%, as oxalate or phosphate compounds or both. The aetiology of stone disease is multifactorial in most cases.
Clinical features of stone disease
The clinical presentation of stones depends on the size, morphology and site of the stone(s). Many cause no symptoms but represent a potentially serious problem. Other stones produce marked pathological effects which present with acute or chronic symptoms or are discovered incidentally on investigation of unrelated symptoms. The presentation of urinary tract stones is summarised in Box 37.2.