scholarly journals Validation of Isotope Dilution Technique for Determination of Bile Acid Synthesis in Man

1974 ◽  
Vol 67 (6) ◽  
pp. 1299-1301 ◽  
Author(s):  
Z.R. Vlahcevic ◽  
D.H. Gregory ◽  
Leon Swell
Lipids ◽  
1982 ◽  
Vol 17 (5) ◽  
pp. 345-348 ◽  
Author(s):  
William C. Duane ◽  
David E. Holloway ◽  
Scot W. Hutton ◽  
Patricia J. Corcoran ◽  
Nancy A. Haas

1978 ◽  
Vol 234 (5) ◽  
pp. F446-F451 ◽  
Author(s):  
Theodore Y. Chin ◽  
A. J. Quebbemann

The contribution of uric acid synthesized in the kidney (nephrogenic uric acid) to the total uric acid excreted in the urine was studied in the chicken by use of the isotope-dilution technique. In the nonfasted chicken the urine-to-plasma specific activity ratio (SAR) of [14C]uric acid was 0.83, suggesting that a minimum of 17% of the uric acid excreted in the urine is synthesized in the kidney. During allopurinol infusion into the renal portal circulation of one kidney the SAR increased to 0.99, indicating that the renal synthesis of uric acid was almost completely inhibited and that the SAR is a valid indicator of the contribution of nephrogenic uric acid excreted into the urine without first entering the circulation. Chickens fasted for 18 h showed a lower rate of renal synthesis of uric acid. Hypoxanthine infusion into the systemic circulation increased the rate of renal synthesis of uric acid in both fasted and nonfasted chickens, suggesting that circulating precursor levels may in part regulate the renal synthesis of uric acid. kidney; specific activity ratio; allopurinol; renal metabolism Submitted on July 14, 1977


1953 ◽  
Vol 31 (10) ◽  
pp. 909-914 ◽  
Author(s):  
R. H. Tomlinson ◽  
A. K. Das Gupta

The mass spectrometer has been used for the estimation of trace quantities of rubidium and strontium. The isotope dilution technique developed by Aldrich has been extended so that 0.01% of rubidium and 0.0001% strontium have been analyzed with 100 mgm. of mineral. The use of small quantities for mass spectrometric determination allows the use of easily available fission strontium and rubidium. The radioactivity of the fission strontium also simplifies the chemical manipulation. No chemical separation from the mineral was required for the rubidium but the strontium was concentrated by ion exchange methods. Ages are presented for one lepidolite and two biotite minerals and their ages compared to those found by other methods. With one of the biotites the effect of weathering on the fractionation of rubidium from strontium has been studied.


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