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Lecture topics
- Urolithiasis is stone formation in the urinary tract
- Supersaturation is a qualitative threshold
- Absorptive hypercalciuria
- Idiopathic calcium stone disease is a real category
- Radiographic distinction: Calcium versus uric acid
- Many renal-pelvis stones are small
- Hydronephrosis is dilation with progressive atrophy
- Primary source and scope
Slide index & full transcript (71 slides)
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Slide 1 · Urolithiasis
Renal calculi and urinary tract stones
Etiology • crystal formation • morphology • clinical consequences
Dr Abu Suraih Sakhri
MBBS, MD (Pathology)
www.abusuraihsakhri.com
Slide 2 · Learning objectives
Explain why urinary supersaturation favors calculus formation.
Distinguish calcium, struvite, uric acid, and cystine stones.
Connect stone composition and morphology with clinical injury.
Interpret short clinicopathologic teaching cases.
Slide 3 · Urolithiasis is stone formation in the urinary tract
Most stones arise in the kidney, although calculi can occur throughout the urinary tract.
Stone disease spans silent incidental findings, renal colic, infection, and structural damage.
Slide 4 · Sites of calculus formation
Renal calyces and pelvis are important stone-forming locations.
Calculi can also occur in the bladder and elsewhere in the urinary tract.
Slide 5 · Lifetime occurrence in the United States
5%–10%
This lifetime range for the U.S. Population; It is a textbook figure, not a new population estimate.
Slide 6 · Age and sex distribution
Sex pattern
Males are affected more often than females.
Age at onset
Peak age at onset is reported between 20 and 30 years.
Slide 7 · A familial predisposition can underlie stone disease
Familial or hereditary predisposition
Altered handling of stone-forming substances
Increased excretion and crystal risk
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 8 · Two inherited metabolic examples
Cystinuria
Abnormal renal reabsorption increases urinary cystine.
Primary hyperoxaluria
An inherited metabolic disorder increases oxalate burden.
Slide 9 · Four principal stone classes
Class
Principal constituent
Approximate share in Robbins
Calcium
Calcium oxalate ± phosphate
~70%
Struvite
Magnesium ammonium phosphate
5%–10%
Uric acid
Uric acid
5%–10%
Cystine
Cystine
1%–2%
Slide 10 · Calcium stones predominate
Calcium
~70%
Struvite
5%–10%
Uric acid
5%–10%
Cystine
1%–2%
Struvite, uric acid, and cystine shown at reported upper bounds; Bars are not parts of a normalized whole.
Slide 11 · Every calculus contains an organic matrix
A mucoprotein matrix accounting for approximately 1%–5% of stone weight.
Stones are not simply pure, freely precipitated inorganic crystals.
Slide 12 · The central process is urinary supersaturation
Urinary solute concentration rises
Solubility of constituent is exceeded
Crystal formation becomes favorable
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 13 · Supersaturation is a qualitative threshold
Below constituent solubility limit
Below solubility limit: The constituent remains in solution.
Above constituent solubility limit
Above solubility limit: Precipitation becomes thermodynamically favorable.
Slide 14 · Low urine volume can increase crystal risk
Lower urine volume
Greater urinary solute concentration
Increased tendency to supersaturation
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 15 · Several variables influence calculi
Urinary chemistry
Constituent concentration and urinary pH
Urinary environment
Urine volume, bacteria, and crystal inhibitors
Slide 16 · A coherent model of stone pathogenesis
Solute load
Ca / oxalate / urate / cystine
Solution state
Volume + pH
Biological modifiers
Bacteria + inhibitors
Outcome
Crystal formation / stone growth
Slide 17 · Calcium stones are chemically heterogeneous
Most contain calcium oxalate or a mixture of calcium oxalate and calcium phosphate.
The same broad stone class can arise through different metabolic disturbances.
Slide 18 · Calcium stone pathways: Two serum-calcium settings
Hypercalcemia with hypercalciuria
One recognized setting; Associated with conditions elevating serum calcium.
Hypercalciuria without hypercalcemia
A larger source-described group; Abnormal urinary calcium despite normal serum calcium.
Slide 19 · Hypercalcemia-associated calcium oxalate stones
About 5%
This subset with both hypercalcemia and hypercalciuria.
Slide 20 · Systemic settings of hypercalcemic stone risk
Hyperparathyroidism increases circulating calcium.
Diffuse bone disease can contribute to hypercalcemia.
Sarcoidosis and other hypercalcemic states are also named.
Slide 21 · Hypercalciuria despite normocalcemia
About 55%
This calcium oxalate stone subgroup without elevated serum calcium.
Slide 22 · Absorptive hypercalciuria
Excess intestinal calcium absorption
Increased calcium entering circulation
Greater urinary calcium excretion
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 23 · Renal hypercalciuria
Intrinsic impairment of tubular calcium reabsorption
Reduced renal conservation of calcium
Hypercalciuria despite normocalcemia
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 24 · Idiopathic fasting hypercalciuria
The calcium-stone differential includes fasting hypercalciuria with normal parathyroid function.
The label does not imply that the underlying transport mechanism has been fully established.
Slide 25 · Uric acid can nucleate calcium oxalate
Increased urinary uric acid
Uric acid crystals in collecting ducts
Calcium oxalate nucleation and growth
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 26 · Hyperuricosuric calcium nephrolithiasis
Up to 20%
Calcium oxalate stones may be associated with increased urinary uric acid, with or without hypercalciuria.
Slide 27 · Two major hyperoxaluria pathways
Primary
Hereditary oxalate overproduction or abnormal metabolism.
Enteric
Acquired intestinal overabsorption in enteric disease.
Slide 28 · Enteric disease and oxalate stones
Enteric disorder
Enhanced intestinal oxalate absorption
Hyperoxaluria
Calcium oxalate risk
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 29 · Primary hyperoxaluria is a hereditary stone risk
Primary hyperoxaluria among inborn errors associated with stones.
For a calcium stone, excess oxalate can be the key abnormal urinary constituent.
Slide 30 · Hypocitraturia removes a protective influence
Reduced urinary citrate
Fewer inhibitor-mediated restraints
Greater calcium crystal risk
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 31 · Clinical contexts of hypocitraturia
Hypocitraturia may be idiopathic.
It may accompany acidosis.
Chronic diarrhea of unknown cause is another association.
Slide 32 · Idiopathic calcium stone disease is a real category
No cause is found in a variable proportion of patients with calcium stones.
Absence of an identified abnormality should not be presented as absence of stone-forming pathophysiology.
Slide 33 · Calcium stone mechanisms: Compare the drivers
Driver
Primary disturbance
Stone-forming consequence
Calcium
Hypercalcemia or hypercalciuria
↑ urinary Ca
Urate
Hyperuricosuria
Ca oxalate nucleation
Oxalate
Primary or enteric hyperoxaluria
↑ urinary oxalate
Citrate
Hypocitraturia
Reduced inhibition
Slide 34 · Struvite is an infection-associated calculus
Struvite consists principally of magnesium ammonium phosphate.
Stone formation is strongly linked to infection by organisms able to split urea.
Slide 35 · Urea-splitting bacteria change urinary chemistry
Bacterial urea splitting
Ammonia generation
Urine alkalinization
Struvite precipitation
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 36 · Which organisms are implicated?
Common example
Proteus species are specifically cited.
Additional example
Some staphylococci can also be urea-splitting.
Slide 37 · Alkaline urine favors struvite precipitation
Ammonia produced by urea splitting raises urinary pH.
The altered pH environment permits magnesium ammonium phosphate salts to precipitate.
Slide 38 · Infection stones can form branching staghorn casts
Progressive salt accretion can occupy large portions of the renal pelvis.
The stone may extend into calyces and mold to the collecting system.
Slide 39 · Uric acid stones: Systemic associations
Hyperuricemia can be present in patients with gout.
High cell turnover, exemplified by leukemia, is another association.
Serum urate alone does not explain most uric acid stones.
Slide 40 · Normal systemic urate does not exclude uric acid calculi
More than half
More than half of patients with uric acid calculi lack hyperuricemia or increased urinary uric acid excretion.
Slide 41 · Acidic urine favors uric acid calculi
Less acidic than the stated risk setting
A tendency to urinary pH below 5.5 in this subset.
Urinary pH < 5.5
Uric acid is poorly soluble in acidic urine.
Slide 42 · Radiographic distinction: Calcium versus uric acid
Calcium stones
Radiopaque on conventional radiography.
Uric acid stones
Radiolucent on conventional radiography.
Slide 43 · Cystinuria produces cystine stones
Hereditary tubular amino-acid reabsorption defect
Increased urinary cystine
Cystine precipitation and stones
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 44 · Cystine stones also favor low urinary pH
Low pH is described in the formation of cystine stones.
The underlying defect is impaired renal reabsorption of cystine-containing amino acids.
Slide 45 · Acidic urine: Two distinct stone mechanisms
Feature
Uric acid
Cystine
Underlying basis
Poor solubility of uric acid
Cystinuria: amino-acid reabsorption defect
Urinary pH
Acidic; Robbins discusses pH < 5.5
Low urinary pH favors formation
Hereditary driver
Not necessary
Intrinsic to cystinuria
Slide 46 · Urinary constituents that inhibit crystals
Low-molecular/ionic inhibitors
Other named inhibitors
Citrate
Glycosaminoglycans
Pyrophosphate
Osteopontin
Diphosphonates
Nephrocalcin (glycoprotein)
Slide 47 · Why similar solute abnormalities need not yield stones
Stone-promoting urinary chemistry
Counteracting inhibitors and local conditions
Variable crystallization outcome
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 48 · A biochemical predisposition is not destiny
Patients with hypercalciuria, hyperoxaluria, or hyperuricosuria often do not develop stones.
This observation supports the importance of inhibitory and local urinary factors.
Slide 49 · Stone determinants must be interpreted together
Solute
Amount excreted
PH
Species solubility
Volume
Concentration
Inhibitors
Crystallization restraint
Slide 50 · Renal calculi are often unilateral
About 80%
Unilateral disease in roughly 80% of patients with stones.
Slide 51 · Typical anatomic distribution
Calyces and renal pelvis are common locations.
Bladder stones are also recognized in the same disease spectrum.
Slide 52 · Many renal-pelvis stones are small
2–3 mm
This average diameter for stones forming in the renal pelvis.
Slide 53 · Calculi differ in surface contour
Smooth contour
Jagged or spiculated contour
Schematic contours only; Not a photograph of stones
Slide 54 · A kidney may contain multiple calculi
Several stones may occupy separate areas in one kidney.
Multiplicity does not imply that both kidneys are involved.
Slide 55 · Staghorn calculi mirror collecting-system shape
Branching structures form with progressive accretion of salts.
Large calculi can cast the pelvis and calyces.
Slide 56 · Clinical course varies widely
Silent disease
A calculus may produce no symptoms.
Symptomatic disease
Renal colic, abdominal pain, hematuria, or renal damage may occur.
Slide 57 · Obstructing calculi can provoke renal colic
Stone lodged in urinary outflow path
Dilation / distention of urinary collecting system
Pain and renal colic
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 58 · A calculus can cause hematuria
Calculus in urinary tract
Local tissue trauma
Blood in urine (hematuria)
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 59 · Stones increase susceptibility to infection
Obstruction and local tissue trauma
Impaired urinary drainage / mucosal injury
Predisposition to superimposed infection
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 60 · Persistent stone obstruction injures the kidney
Outflow obstruction
Pelvicalyceal dilation
Pressure-related parenchymal injury
Progressive renal atrophy
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 61 · Hydronephrosis is dilation with progressive atrophy
Obstruction can dilate the renal pelvis and calyces.
Prolonged pressure is associated with loss of renal parenchyma.
Slide 62 · Chronic obstruction evolves beyond dilation
Sustained obstruction
Interstitial inflammation
Tubular atrophy and fibrosis
Structural renal damage
Conceptual sequence — direction indicates the causal relationship described in the source
Slide 63 · Teaching case: Recurrent calcium-type risk
A patient has calcium oxalate stones and increased urinary calcium, but normal serum calcium.
Question: Which metabolic category is supported? What mechanisms should be considered?
Slide 64 · Case interpretation: Normocalcemic hypercalciuria
The pattern is compatible with hypercalciuria without hypercalcemia.
Possible categories include increased intestinal absorption, tubular reabsorption impairment, or idiopathic fasting hypercalciuria.
Slide 65 · Teaching case: Large branching calculus
A patient has a staghorn-shaped calculus and an infection caused by a urea-splitting organism.
Question: Which stone type is most plausible, and why?
Slide 66 · Case interpretation: Infection-associated struvite
A urease-positive infection can raise urinary pH through ammonia generation.
Alkalinization favors magnesium ammonium phosphate precipitation and large branching calculi.
Slide 67 · Teaching case: Stone invisible on plain radiography
A patient with a stone has persistently acidic urine; The calculus is radiolucent on plain radiography.
Question: What composition is most strongly suggested by Robbins?
Slide 68 · Case interpretation: Uric acid stone
Acidic urine promotes uric acid precipitation.
Radiolucency supports uric acid rather than a typical calcium stone; Serum urate need not be elevated.
Slide 69 · Integrative differential at a glance
Stone class
Most discriminating source-based feature
Calcium
Common; multiple possible urinary metabolic drivers
Struvite
Urea-splitting infection → alkaline urine; may be staghorn
Uric acid
Acidic urine; radiolucent on plain radiography
Cystine
Hereditary amino-acid transport defect; acidic urine
Slide 70 · Clinicopathologic synthesis
Supersaturation is central, but urinary pH and inhibitors modulate crystal formation.
Calcium stones have heterogeneous mechanisms; Struvite, uric acid, and cystine have distinct clues.
Stone shape, location, obstruction, and infection determine clinical consequences.
Stone chemistry and renal morphology should be interpreted together.
Slide 71 · Primary source and scope
Robbins, Cotran & Kumar. Pathologic Basis of Disease. 11th ed. 2026. Chapter 20: The Kidney, pp. 861–862.
The obstructive uropathy section in the same chapter was used for consequences of persistent obstruction.
Figures in this lecture are original editable schematics, not patient specimens or textbook reproductions.