Kidney stones

Kidney stones

Renal

Renal

Development of the renal system
Potter sequence
Horseshoe kidney
Renal agenesis
Multicystic dysplastic kidney
Posterior urethral valves
Renal system anatomy and physiology
Body fluid compartments
Glomerular filtration
Renal clearance
Regulation of renal blood flow
Movement of water between body compartments
Tubular secretion of PAH
Tubular reabsorption of glucose
Proximal convoluted tubule
Loop of Henle
Distal convoluted tubule
Osmoregulation
Urea recycling
Renin-angiotensin-aldosterone system
Measuring renal plasma flow and renal blood flow
Erythropoietin
Hyperkalemia
Hypokalemia
Hypernatremia
Hyponatremia
Hypermagnesemia
Hypomagnesemia
Hyperphosphatemia
Hypophosphatemia
Hypercalcemia
Hypocalcemia
Hyperaldosteronism
Physiologic pH and buffers
Acid-base map and compensatory mechanisms
Plasma anion gap
Metabolic acidosis
Metabolic alkalosis
Respiratory acidosis
Respiratory alkalosis
The role of the kidney in acid-base balance
Renal tubular acidosis
Kidney stones
Hydronephrosis
Vesicoureteral reflux
Urinary incontinence: Pathology review
Neurogenic bladder
Poststreptococcal glomerulonephritis
Rapidly progressive glomerulonephritis
Goodpasture syndrome
Lupus nephritis
IgA nephropathy (NORD)
Alport syndrome
Membranoproliferative glomerulonephritis
Minimal change disease
Focal segmental glomerulosclerosis (NORD)
Membranous nephropathy
Diabetic nephropathy
Urinary tract infections (UTIs): Nursing process (ADPIE)
Urinary tract infections: Pathology review
Acute kidney injury: Clinical
Renal azotemia
Prerenal azotemia
Postrenal azotemia
Renal cortical necrosis
Chronic kidney disease
Renal artery stenosis
Angiomyolipoma
Renal cysts and cancer: Clinical
Polycystic kidney disease
Medullary cystic kidney disease
Renal cell carcinoma
WAGR syndrome
Non-urothelial bladder cancers
Transitional cell carcinoma
Renal and urinary tract masses: Pathology review
Loop diuretics
Thiazide and thiazide-like diuretics
Hyperkalemia: Clinical
ACE inhibitors, ARBs and direct renin inhibitors

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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)