41 year old Peter Horvath presents with severe left sided loin pain, it has been coming and going for the last 2 hours and has now become more constant and severe. He has vomited twice and feels very faint and unwell.
Vital Signs: Afebrile; HR: 100 bpm; BP 140/80; RR 20/min
The patient is suddenly aware of pain in the loin, which radiates anteroinferiorly to the groin and often into the testis or labium, in the sensory distribution of the first lumbar nerve. The pain steadily increases in intensity to reach a peak in a few minutes. The patient is restless, and generally tries unsuccessfully to obtain relief by changing position or pacing the room. Frequency, dysuria and haematuria may occur. The pain is usually constant during attacks, although slight fluctuations in severity may occur. Subsequent to an attack of renal colic there may be intermittent or constant dull ache in the loin or back.
History of previous renal colic (family history of renal calculi)
Distension of the renal pelvis seems to be responsible for the development of renal colic. The rise in pelvic pressure due to a ureteric calculus can result from various mechanisms such as increased diuresis, inflammatory oedema around the stone and increased frequency of ureteric contractions. Prostaglandins can play an important role in these mechanisms, therefore inhibition of prostaglandin synthesis by drugs such as non-steroidal anti-inflammatory drugs could contribute to the lowering of pelvic pressure and distension, and thus to the relief of renal colic.
Renal calculi consist of aggregates of crystals containing small amounts of proteins and glycoprotein that can lodge anywhere along the course of the urinary tract. Human urine is often saturated to the limit with uric acid, phosphates and calcium oxalate. Normally due to the secretion of various protective compounds – proteins, glycosaminoglycans, pyrophosphate and citrate – and natural mechanisms that control the pH of urine, these substances remain suspended in solution. If the protective compounds are overwhelmed or immunity becomes depressed, the substances may crystallize and the crystals may begin to clump together, eventually forming calculi.
Four basic kinds of renal calculi:
About 90% of all calculi contain calcium as the chief constituent. In Europe, 80% of calculi are calcium oxalate.
Environmental and dietary:
Acquired causes:
Congenital and inherited causes:
The classic patient with renal colic is writhing in pain, pacing about, and unable to lie still, in contrast to a patient with peritoneal irritation, who remains motionless to minimize discomfort. There may be pallor, sweating and often vomiting. Fever is not part of the presentation of uncomplicated nephrolithiasis. The most common finding in ureterolithiasis is loin tenderness due to the dilatation and spasm of the ureter from transient obstruction as the calculus passes from the kidney to the bladder. Abdominal examination is usually unremarkable. Bowel sounds may be decreased, a reflection of mild ileus.
Urinalysis:
Consider the use of MET – active medical expulsive therapy – in any patient with a reasonable probability of calculus passage. It is probably most useful in calculi 3 – 10mm in size as those ≤ 3mm have an 85% chance of passing spontaneously. Overall, MET is associated with a 65% greater likelihood of calculus passage. The calcium blocker nifedipine relaxes ureteral smooth muscle and enhances calculus passage. Alpha-1 selective blockers, such as tamsulosin also relax musculature of the ureter and lower urinary tract.
CT KUB should be arranged if not already performed and further management determined pending result.
A 24 hour urine analysis for urea, creatinine clearance, sodium, calcium, oxalate; magnesium and citrate (both important chemical inhibitors of calculus formation esp. citrate), pH (some stones are Ph dependent e.g. uric acid and struvite) should be performed if:
Recommend measures to prevent calcium calculus formation:
Calculus in the renal pelvis or kidney:
Calculus in the upper ureter:
Calculus in the lower ureter:
Calculus in the bladder: