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What Are Kidney Stones?

Kidney stones are composed of both matrix and crystals, with crystals making up about 97% and the matrix accounting for the remaining 3%. Since the primary component of stones is crystalline material, they are typically classified based on their crystal composition. The four main types of kidney stones include calcium stones, infection-related stones, uric acid stones, and cystine stones. Each type of stone exhibits distinct physical properties and imaging characteristics, and they can be composed of a single substance or a combination of several components.

Calcium stones can be further divided into calcium oxalate stones, calcium phosphate stones, and brushite stones. On the other hand, infection-related stones include carbonate apatite stones, struvite stones, and newberyite stones. Uric acid stones mainly consist of urate crystals, while cystine stones are a rare type associated with a genetic disorder. Additionally, there are also rare cases of drug-induced stones caused by certain medications.

The formation of kidney stones is a complex process influenced by multiple factors across four key areas: external environmental factors, individual metabolic factors, urinary system conditions, and urine composition. These factors can interact in various ways to promote stone development. As a result, accurate diagnosis and effective treatment require a tailored approach based on the specific composition and underlying cause of each stone type. Understanding the type of stone a patient has is crucial for developing an appropriate prevention and treatment strategy. Medical professionals often analyze stone composition after removal to guide long-term management and reduce the risk of recurrence.

This comprehensive understanding helps improve patient outcomes and supports more effective, personalized care. Advancements in diagnostic imaging and laboratory analysis continue to enhance our ability to identify and manage different types of kidney stones efficiently.

WildHeart2025-07-22 11:49:23
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