Anyone can get a urinary tract stone, but some people are more likely to get one. Men are affected more often than women, and Caucasians are more prone to urinary tract stones than African Americans. Age is also a factor. The chance of getting a urinary tract stone rises as men enter their 40s and continues to rise into their 70s. For women, the risk peaks in their 50s.
Experts say that the incidence of urinary tract stones is on the rise. According to the National Health and Nutrition Examination Survey, as of 2012, 10.6% of men and 7.1% of women in the United States are affected by renal stone disease, compared to just 6.3% of men and 4.1% of women that were affected in 1994. Changing socio-economic conditions and subsequent lifestyle may be linked to changes in the prevalence, incidence and distribution for age, sex and type of urolithiasis in terms of both the site and the chemical-physical composition of the calculi.
The urinary tract is the body’s drainage system for removing wastes and extra water. It includes two kidneys, two ureters, a bladder, and a urethra. The kidneys are two bean-shaped organs, each about the size of a fist. Every day, they process about 190 liters of blood to produce about 0.945-1.90 ml of urine.
Urolithiasis refers to the presence of calculi anywhere along the course of the urinary tracts. The terms urolithiasis, nephrolithiasis and renal or urinary tract stones are used interchangeably, although there are slightly varying definitions of each (nephrolithiasis refers to calculi in the kidneys). Because these cases share most of the disease process, they are often discussed in conjunction.
A urinary tract stone or calculus is one of the most common disorders of the renal system. A solid piece of material that forms in a kidney, ureter or bladder when substances that are normally found in the urine become highly concentrated due to dehydration and poor diet. A stone may stay in the kidney or travel down the urinary tract.
Most urinary tract stones are small enough to be passed out in the urine without any complication. However, some stones are large to amount that require treatment. The most important aspect of medical therapy is maintaining a high fluid intake and subsequent high urinary volume.
Urolithiasis is the medical term used to describe stones occurring in the urinary tract, primarily in the kidney (nephrolithiasis) or ureter (ureterolithiasis), and may also form in or migrate into the lower urinary system (bladder or urethra). The result are small, hard mineral deposits that may stay in the tract or pass through the urine, based on its size and hydration status.
Urinary tract stones form when the urine contains more crystal-forming substances - such as calcium, oxalate, uric acid and phosphorus - than the fluid in the urine can dilute. At the same time, the urine may lack substances that prevent crystals from sticking together, such as nephrocalcin and uropontin, creating an ideal environment for the stones to scheme.
A low fluid intake with a subsequent low volume of urine production, produce high concentrations of stone-forming solutes in the urine. When the chemical concentration levels reach the point at which they no longer dissolve, these substances form crystals that may fix to surfaces of renal filtering and passing structures, thus creating the nidus for subsequent stone growth. Urothelial injury and repair after a stone episode may increase surface expression of these molecules to favor further crystal adhesion, which may increase the chances of recurrence.
A urinary tract stone may not cause symptoms until it moves around within the kidney or passes into the ureter. Pain is the major symptom of urinary tract stone. This pain could be:
Other symptoms for urinary tract stones rather than pain may include:
Most urinary tract stones eventually pass out of the body during urination. But some can grow large enough to begin blocking the flow of urine and cause severe discomfort. Treatment for urinary tract stones usually depends on their size and what they are made of, as well as whether they are causing pain or obstructing the urinary tract. The ureter is the smallest diameter structure of the urinary tract and is the area most prone to obstruction. The consequence of stone is determined in this chart:
Stone size (mm) |
Number of days to pass through ureter (mean) |
% Likelihood of eventual need for intervention |
2 or less |
8 |
3 |
3 |
12 |
14 |
4-6 |
22 |
50 |
More than 6 |
-- |
99 |
Between 80-85% of crystals remain tiny enough to travel through the urinary tract and leave the body in the urine without being noticed. Larger stones are able to be eliminated throw seeking medical care with many procedures. Without treatment, calcium stones recur in 50% of patients within 5 years of the first attack, and in 70% of patients or more within 10 years. The individual risk for recurrence varies depending on the stone kind and the underlying condition.
Medical therapy is generally effective at delaying (but perhaps not completely stopping) the tendency for stone formation. Metabolic evaluation and treatment are indicated for patients at greater risk for recurrence, including those who present with multiple stones, who have a personal or family history of previous stone formation, who present with stones at a younger age, or who have residual stones after treatment.
Anyone can get a urinary tract stone, but some people are more likely to get one. Men are affected more often than women, and Caucasians are more prone to urinary tract stones than African Americans. Age is also a factor. The chance of getting a urinary tract stone rises as men enter their 40s and continues to rise into their 70s. For women, the risk peaks in their 50s.
Experts say that the incidence of urinary tract stones is on the rise. According to the National Health and Nutrition Examination Survey, as of 2012, 10.6% of men and 7.1% of women in the United States are affected by renal stone disease, compared to just 6.3% of men and 4.1% of women that were affected in 1994. Changing socio-economic conditions and subsequent lifestyle may be linked to changes in the prevalence, incidence and distribution for age, sex and type of urolithiasis in terms of both the site and the chemical-physical composition of the calculi.