Circadian variation in the urinary excretion of electrolytes and trace elements in men

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Abstract
Three‐hour urine specimens were collected over a period of 27 hours from 11 healthy adult male subjects. Each specimen was analyzed for Na, K, Ca, Mg, and Zn using atomic absorption spectrophotometry. Each sample was also dialyzed, pH 7.35, and subsequently analyzed for Na, K, P, Ca, Mg, Zn, Fe, Pb, Al, Ni, Cu, Mo, Hg, Cr, Cd, and Mn using a multielemental argon‐plasma emission system. The data were evaluated on conventional time plots (chronograms) and as computer‐determined “cosinor” plots. A population circadian rhythm with a statistical significance was detected for total Na, K, Ca, and Mg, and for nondialyzable Na, K, P, Ca, Zn, and Mo. For almost every element studied the increase from lowest to highest 3‐hour group mean along the 24‐hour time scale was more than 100%. The 24‐hour excretion of Na, K, Ca, Mg, and Zn appeared in good agreement with the so‐called “normals.” The nondialyzable levels of Fe, Pb, Al, Ni, Cu, Mo, Hg, Cr, Cd, and Mn were similar to the total urinary excretions reported in the literature.