Kidney stones

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Kidney stones

RENAL

RENAL

Posterior urethral valves
Hypospadias and epispadias
Vesicoureteral reflux
Bladder exstrophy
Urinary incontinence
Neurogenic bladder
Lower urinary tract infection
Transitional cell carcinoma
Non-urothelial bladder cancers
Congenital renal disorders: Pathology review
Renal tubular defects: Pathology review
Renal tubular acidosis: Pathology review
Acid-base disturbances: Pathology review
Electrolyte disturbances: Pathology review
Renal failure: Pathology review
Nephrotic syndromes: Pathology review
Nephritic syndromes: Pathology review
Urinary incontinence: Pathology review
Urinary tract infections: Pathology review
Kidney stones: Pathology review
Renal and urinary tract masses: Pathology review
Osmotic diuretics
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ACE inhibitors, ARBs and direct renin inhibitors
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Plasma anion gap
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Multicystic dysplastic kidney
Proximal convoluted tubule
Loop of Henle
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Tubular reabsorption and secretion
Tubular secretion of PAH
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Urea recycling
Tubular reabsorption and secretion of weak acids and bases
Renin-angiotensin-aldosterone system
Antidiuretic hormone
Kidney countercurrent multiplication
Vitamin D
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Renal agenesis
Horseshoe kidney
Potter sequence
Hyperphosphatemia
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Renal tubular acidosis
Minimal change disease
Diabetic nephropathy
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Poststreptococcal glomerulonephritis
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Nephroblastoma (Wilms tumor)
WAGR syndrome
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Urinary tract infections: Clinical
Hypokalemia: Clinical
Goodpasture syndrome
Syndrome of inappropriate antidiuretic hormone secretion (SIADH)
Diabetes insipidus and SIADH: Pathology review

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With nephrolithiasis, “nephro-” refers to the kidneys, and “-lithiasis” means stone, so nephrolithiasis means kidney stones, sometimes also referred to as renal calculi or urolithiasis.

Kidney stones form when solutes in the urine precipitate out and crystalize, and although these most commonly form in the kidneys themselves, they can also form in the ureters, the bladder, or the urethra.

Now, urine’s a combination of water, which acts as a solvent, and all sorts of particles, or solutes.

In general, when certain solutes become too concentrated in the solvent, they become supersaturated.

Urinary supersaturation of certain solutes results in precipitation out of the solution and formation of crystals.

Those crystals then act as a nidus, or place where more solutes can deposit and over time it builds up a crystalline structure.

This can happen if there’s an increase in the solute, or a decrease in the solvent, as would be the case with dehydration.

In addition, there are substances like magnesium and citrate that inhibit crystal growth and aggregation, preventing kidney stones from forming in the first place.

In the majority of cases, the inorganic precipitate is calcium oxalate, formed by a positively charged calcium ion binding to a negatively charged oxalate ion, which results in a black or dark brown colored stone that is radio-opaque on an Xray, meaning that it shows up as a white spot.

Sometimes, instead of oxalate, the calcium binds a negatively charged phosphate group to form calcium phosphate stones which are dirty white in color and also radiopaque on an X-ray.

Calcium oxalate crystals are more likely to form in acidic urine, whereas calcium phosphate crystals are more likely to form in alkaline urine.

The exact reason why these stones form is usually unknown, but there are some known risk factors like hypercalcemia and hypercalciuria, having too much calcium in the blood and urine, respectively.

Hypercalcemia can result from increased calcium absorption in the gastrointestinal tract as well as hormonal causes like primary hyperparathyroidism.

Hypercalciuria can result from impaired renal tubular reabsorption of calcium, which leaves a lot of calcium behind in the tubule.

For the calcium oxalate stones, hyperoxaluria is a risk factor as well, and it can be due to a genetic defect that increases oxalate excretion, a defect in liver metabolism, or a diet heavy in oxalate-rich foods like rhubarb, spinach, chocolate, nuts, and beer.

There are also uric acid stones which are red-brown in color and radiolucent under an Xray, meaning that they’re transparent to x-rays and don’t show up very well.

At a physiologic pH, uric acid loses a proton and becomes a urate ion, which then binds sodium, forming monosodium urate which crystallizes and ultimately forms uric acid stones.

Since uric acid is a breakdown product of purines, a very common reason for high levels of uric acid is consuming lots of purines.

Purine-rich foods include shellfish, anchovies, red meat or organ meat.

Sources

  1. "Robbins Basic Pathology" Elsevier (2017)
  2. "Harrison's Principles of Internal Medicine, Twentieth Edition (Vol.1 & Vol.2)" McGraw-Hill Education / Medical (2018)
  3. "Pathophysiology of Disease: An Introduction to Clinical Medicine 8E" McGraw-Hill Education / Medical (2018)
  4. "CURRENT Medical Diagnosis and Treatment 2020" McGraw-Hill Education / Medical (2019)
  5. "Prospective Study of Beverage Use and the Risk of Kidney Stones" American Journal of Epidemiology (1996)
  6. "HELICAL CT OF URINARY TRACT STONES" Radiologic Clinics of North America (1999)
  7. "Diagnosis and Management of Acute Ureterolithiasis" American Journal of Roentgenology (2000)
  8. "Kidney stone disease" Journal of Clinical Investigation (2005)
  9. "An Update and Practical Guide to Renal Stone Management" Nephron Clinical Practice (2010)