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Encyclopedia of Health and Medicine

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urolithiasis 227<br />

liters <strong>of</strong> urine; maximum capacity <strong>of</strong> the bladder is<br />

about 500 ml.<br />

ANURIA<br />

HEMATURIA<br />

URINARY FREQUENCY<br />

URINARY RETENTION<br />

CONDITIONS OF ALTERED URINATION<br />

See also NEUROGENIC BLADDER.<br />

DYSURIA<br />

NOCTURIA<br />

URINARY INCONTINENCE<br />

URINARY URGENCY<br />

urine The liquid the KIDNEYS generate to pass<br />

wastes <strong>and</strong> excess fluid from the body. The typical<br />

adult makes <strong>and</strong> passes between 1,500 <strong>and</strong> 3,000<br />

milliliters (1.5 to 3 liters) <strong>of</strong> urine every 24 hours.<br />

Numerous variables influence the volume <strong>and</strong><br />

composition or urine, though in general urine is<br />

95 percent water <strong>and</strong> 5 percent suspended or dissolved<br />

solids.<br />

Most <strong>of</strong> the solids urine contains are organic<br />

wastes in the forms <strong>of</strong> urea, uric acid, creatinine,<br />

<strong>and</strong> ammonia. These are the nitrogen-based waste<br />

byproducts <strong>of</strong> METABOLISM that the kidneys filter<br />

from the BLOOD. The urine also contains minerals<br />

(electrolytes) the kidneys excrete to maintain the<br />

body’s electrolyte <strong>and</strong> fluid balance. Excreted electrolytes<br />

include sodium, potassium, chloride, magnesium,<br />

phosphate, <strong>and</strong> calcium. Normal urine<br />

may contain small amounts <strong>of</strong> ALBUMIN (protein).<br />

Urine <strong>of</strong> normal concentration is pale yellow<br />

<strong>and</strong> has no odor. Dilute urine is colorless; concentrated<br />

urine can appear dark yellow to orange.<br />

Dietary substances, certain medications, <strong>and</strong> certain<br />

health conditions can alter the color as well as<br />

the odor <strong>of</strong> the urine. Normal urine is slightly<br />

acidic <strong>and</strong> has a specific gravity <strong>of</strong> 1.010 to 1.025,<br />

slightly above that <strong>of</strong> water. Deviations from normal<br />

urine composition <strong>and</strong> concentration suggest<br />

various health conditions <strong>and</strong> may require diagnostic<br />

evaluation.<br />

For further discussion <strong>of</strong> the urine within the<br />

context <strong>of</strong> the urinary system’s structure <strong>and</strong><br />

function please see the overview section “The Urinary<br />

System.”<br />

See also ALBUMINURIA; ANURIA; CYSTINURIA; HEMA-<br />

TURIA; OLIGURIA; UREMIA; UROLITHIASIS.<br />

urolithiasis The formation <strong>of</strong> calcifications (also<br />

called calculi) in the BLADDER. Most bladder stones,<br />

like kidney stones, form <strong>of</strong> calcium in combination<br />

with oxalate (the most common combination),<br />

phosphate, or magnesium. Bladder stones<br />

are less common today than kidney stones<br />

(NEPHROLITHIASIS), though throughout recorded history<br />

bladder stones have been a common urologic<br />

condition. Bladder stones are most likely to form<br />

when URINE remains in the bladder for an<br />

extended time, particularly with URINARY RETENTION<br />

(in which the bladder fails to completely empty<br />

with URINATION). URETHRAL<br />

STRICTURE, CYSTOCELE,<br />

BENIGN PROSTATIC HYPERPLASIA (BPH), long-term BLAD-<br />

DER CATHETERIZATION, <strong>and</strong> NEUROGENIC BLADDER are<br />

among the conditions that contribute to the formation<br />

<strong>of</strong> bladder stones. Chronic DEHYDRATION,<br />

such as occurs with drinking too little water, further<br />

contributes to calcification. Bladder stones are<br />

also common during PREGNANCY.<br />

In urinary stasis the minerals dissolved in the<br />

urine begin to settle out when the urine is static<br />

(not moving), forming crystals. The formed crystals<br />

attract more <strong>of</strong> their composite minerals,<br />

eventually hardening into calculi. Small stones<br />

<strong>of</strong>ten easily pass through the urethra in the urine<br />

without the person’s awareness <strong>of</strong> them. Stones<br />

that are large enough to scrape the walls <strong>of</strong> the<br />

urethra, or s<strong>and</strong>like clumps <strong>of</strong> calculi that surge<br />

through the URETHRA, may cause irritation such as<br />

DYSURIA (burning sensation) with urination. Other<br />

symptoms may include URINARY FREQUENCY, URINARY<br />

URGENCY, <strong>and</strong> urinary hesitation (difficulty starting<br />

urination, or start-<strong>and</strong>-stop urination).<br />

A stone that completely blocks the urethra,<br />

<strong>of</strong>ten at the neck <strong>of</strong> the bladder, causes excruciating<br />

PAIN that may feel as though it arises in the groin or,<br />

in men, in the TESTES (testicles). Often a change in<br />

position relieves the pain, causing the urine to<br />

wash the stone from its point <strong>of</strong> occlusion. A stone<br />

that is larger than the diameter <strong>of</strong> the urethra will<br />

intermittently though persistently obstruct the passage<br />

<strong>of</strong> urine. It may also cause bleeding, resulting<br />

in HEMATURIA (blood in the urine).<br />

The diagnostic path typically includes urinalysis,<br />

ULTRASOUND to detect the presence <strong>of</strong> stones in the<br />

bladder, <strong>and</strong> CYSTOSCOPY. Cystoscopy <strong>of</strong>ten is both<br />

diagnostic <strong>and</strong> therapeutic, allowing the urologist<br />

to confirm the presence <strong>of</strong> stones as well as remove<br />

them from the bladder. Larger stones may require<br />

treatments such as EXTRACORPOREAL SHOCKWAVE

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