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Uranium (Ur)
Uranium is a
radioactive element having 10 isotopes with half lives that exceed
one hour. Uranium 238 constitutes about 99% of the naturally-occurring
Uranium and this is the isotope measured. Uraunium 238 has a half life of
4.5 X 10 to the ninth years. Uranium 238 decays by alpha emission to produce
thorium, Thorium 234, the initial step in a decay chain that eventually
leads to lead. Alpha, beta and gamma emissions occur during this
decay process. Because of the very long half life, the radioactivity
danger is only slight. However, exposure to enriched or nuclear fuel
grade Uranium (high in Uranium 235) does pose a health hazard. The measured
result (Uranium 238) does not reflect or imply exposure to enriched
Uranium. The major
concern for (natural) Uranium excess is chemical toxicity rather
than radiological.
Uranium is a chemically-reactive element, has four valences (3,4,5
or 6), and may combine with:
carbonate, phosphate, citrate, pyruvate, malate, lactate,
etc. in body tissues. When not excreted in urine, Uranium may accumulate
in the kidneys, spleen, liver, and in bone (substituting for calcium
in hydroxyapatite causing osteoporosis). Uranium is nephrotoxic, causing damage to the
glomeruli and proximal tubules of the kidneys.
An early sign of Uranium excess is general fatigue. Kidney
damage is reflected by excess protein, amino acids, or glucose in
the urine. Albuminuria and
urinary catalase are findings consistent with Uranium excess.
Elevated hair Uranium is a confirmatory finding; whole blood and
fecal analyses may corroborate recent or ongoing exposures.
Uranium is more common than mercury, silver or cadmium in the
earth’s rock strata, and may be present, at low levels, in drinking water
(ground well water). Most commercial use of Uranium is for nuclear
fuel, but it may be present in ceramics or colored glass, especially
ancient or antique, yellow-colored glass.