Net transtubular movement of water and urea in saline diuresis
Autor: | Margaret Mylle, Carl W. Gottschalk, William E. Lassiter |
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Rok vydání: | 1964 |
Předmět: |
medicine.medical_specialty
Physiology Sodium Renal urea handling Diuresis chemistry.chemical_element Sodium Chloride Urine Urine sodium Excretion chemistry.chemical_compound Physiology (medical) Internal medicine medicine Loop of Henle Urea Carbon Isotopes Reabsorption Research Inulin Water Rats Kidney Tubules Endocrinology medicine.anatomical_structure chemistry |
Zdroj: | American Journal of Physiology-Legacy Content. 206:669-673 |
ISSN: | 0002-9513 |
DOI: | 10.1152/ajplegacy.1964.206.4.669 |
Popis: | Anesthetized rats were given urea-C14 intravenously and infused with 5% NaCl solution containing inulin-methoxy-H3. Fluid was collected by micropuncture from surface tubules for simultaneous determination of H3 and C14 activities and osmolality. Inulin clearances, plasma and urine sodium, urine volume, and urea excretion were all greatly increased, but fractional water and urea reabsorption in the proximal convolution was similar to that in nondiuretic rats. Inulin fluid/plasma ratios in hypotonic early distal samples were slightly lower than those observed in nondiuretic rats. Urea/inulin ratios in distal samples and in ureteral urine were similar to the late proximal convolution, indicating little or no addition of urea in the loop of Henle or loss from distal convolution or collecting ducts, in contrast to nondiuretic rats. These results suggest that in the proximal convolution sodium (and therefore water) reabsorption is proportional to the rate of delivery of sodium to the tubule. Furthermore, the absence of demonstrable net transtubular movement of urea beyond the proximal convolution under conditions in which concentration gradients are reduced is consistent with the hypothesis that urea movement is largely passive. |
Databáze: | OpenAIRE |
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