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Published on: February 28, 2017
Routine analysis of urinary calculi by scanning electron microscopy
Summary
Calcium phosphate in kidney stones, particularly oxalate-rich ones, suggests a primary core. This finding supports a new model for urinary stone formation by combining existing theories.
Area of Science:
- Nephrology
- Biochemistry
- Materials Science
Background:
- Urinary calculi (kidney stones) are a significant health issue.
- Current theories on stone formation, such as the primary nidus theory and the matrix theory, are often considered contradictory.
- Understanding the initial steps of stone formation is crucial for developing effective prevention and treatment strategies.
Purpose of the Study:
- To investigate the composition and structure of urinary calculi.
- To identify the initial components involved in kidney stone formation.
- To propose a unified model for urinary stone genesis.
Main Methods:
- Analysis of 529 urinary calculi using Scanning Electron Microscopy with Energy Dispersive X-ray Analysis (SEM/EDXA).
- X-ray diffraction was employed to determine the mineralogical composition of the stones.
- Characterization of calcium phosphate-rich microspherules in calculi, urine, and kidney tissue.
Main Results:
- Oxalate-rich stones consistently contained calcium phosphate, often in the central core (in over 75% of cases).
- Calcium phosphate-bearing microspherules were abundant in urinary calculi and urine of stone formers.
- Similar microspherules were identified in human kidney tissue, suggesting a common origin.
- The findings support the existence of a primary nidus in stone formation.
Conclusions:
- Calcium phosphate plays a critical role as a primary nidus in the formation of urinary calculi, including oxalate-rich stones.
- The presence of calcium phosphate microspherules provides insight into the physico-chemical nature of the initial stone-forming aggregate.
- A novel model is proposed that integrates previously disparate theories of urinary stone genesis.
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