The peritoneum of rabbit was isolated from anterior and posterior walls, colon and omentum andd permeability of the peritoneum for
24NaCl,
42KC1,
14C-Urea and
14C-Glucose was investigated in vitro, getting following results ; 1) No difference of permeability was identified between serosal side and mucosal side. 2) The permebility coefficient was 10
-5 to 10
-6cm sec
-1 which was almost the same as that of cellophane membrane used in artificial kidney. This coefficient showed a tendency to decrease with the increase of molecular weight. 3) The permeability was the highest in omentum among four parts of peritoneum and the lowest in that of colon. Those of anterior and posterior abdominal walls were almost identical, which were they middle of the former two. Passive transport in peritoneum can be assumed since there was no significant difference of permeability between serosal side and mucosal side. The peritoneum may be a porous membrane for it showed the same permeability as cellophane membrane. The filtration coefficient calculated by Pappenheim suggests that the peritoneum supervenes other biological membranes in permeability except the capillary wall of glomerulus.
24NaCl and
131I-Albumin was given to dogs intravenously in order to investigate disappearing curve in the blood and into the peritoneal cavity to investigate appearing curve in the blood. Permeability of the peritoneum in vivo was thus studied. 1) Absorption of
24NaCl and
131I-Albumin from the peritoneal cavity was slower than the movement in capillaries. 2) When vena cava inferior was ligated to make stenosis, absorption of
24NaCl from peritoneal cavity decreased remarkably. The hemodynamics of peritoneal capillary seems to have influence upon absorption of sodium from the peritoneal cavity. 3) On the contrary, absorption of alubumin increased. Increase of lymphatic flow of thoratic duct was noticed, suggesting its influence on absorption of alubumin.
14C-Urea was given to rabbit and man to investigate the distribution of urea. 1) Compartment analysis showed that urea exists in two compartments, extracellular and intracellular fluid, both under normal and uremic conditions. 2) By the calculated rate constants, a simulation of the peritoneal dialysis was modeled. We found the existence of urea disequilibrium in peritoneal dialysis by the Calculation of simulation model. 3) Specific activity of
14C-Urea of various tissues was investigated under uremic condition, and it took more time to attain equilibrium. Exchange of urea between extracellular and intracellular fluid is thus slow under uremic condition. 4) The difference of amount disappeared from blood and that excreted into urine was considered to be due to urea hydrolysis in the gut by bacterial urease. Under normal condition almost the same amount as that excreted into urine is hydrolysed in the gut. Under uremic condition, it is much more acceralated than normal.
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