Regulation of salt and water balance

Author(s):  
Elizabeth H. Holt ◽  
Beatrice Lupsa ◽  
Grace S. Lee ◽  
Hanan Bassyouni ◽  
Harry E. Peery
The Lancet ◽  
2002 ◽  
Vol 359 (9320) ◽  
pp. 1812-1818 ◽  
Author(s):  
Dileep N Lobo ◽  
Kate A Bostock ◽  
Keith R Neal ◽  
Alan C Perkins ◽  
Brain J Rowlands ◽  
...  

1975 ◽  
Vol 228 (6) ◽  
pp. 1847-1855 ◽  
Author(s):  
J Mohring ◽  
B Mohring ◽  
H-J Naumann ◽  
A Philippi ◽  
E Homsy ◽  
...  

In male Sprague-Dawley rats, renal artery constriction in the presence of an inact contralateral kidney induced sodium retention (for 2-3 wk), moderate potassium loss,elevation of blood volume (BV), and an increase in water turnover. It is suggestedthat renal artery constriction activates the renin-angiotensin-aldosterone system, resulting in disordered regulation of salt and water balance and in blood pressure (BP) elevation. Subsequently, sodium balance was reestablished in one group of hypertensive rats. The previously retained sodium was kept in the body, and BV and reninactivity remained elevated. In a second group of animals, a malignant course of hypertension developed: BP surpassed a critical level of about 180 mmHg; sodium, potassium, and water were lost; BV declined; renin activity was further stimulated; and in the contralateral kidney malignant nephrosclerosis occurred. It is assumed that pressure diuresis and natriuresis induce a vicious circle: the increasing renin activity may maintain or further increase BP level, therby inducing further salt and water loss, etc.; high BP levels and high renin activities induce vascular damage and deterioration of renal function.


1970 ◽  
Vol 52 (3) ◽  
pp. 553-564
Author(s):  
W. T. W. POTTS ◽  
MARGARET A. FOSTER ◽  
J. W. STATHER

1. Salmon smolts adapted to sea water maintain a high rate of turnover of both sodium and chloride, but when adapted to fresh water the rate of turnover is low. 2. Only a small part of the influx takes place through the gut. 3. On immediate transfer from sea water to dilute sea water or to fresh water the influxes decline rapidly, but on transfer from fresh water to sea water the restoration of the fluxes takes place slowly. 4. The alternative hypotheses that the rapid changes are due to exchange diffusion or to rapid adjustments of the sodium pump are discussed.


Author(s):  
M. J. McKinley ◽  
D. A. Denton ◽  
M. L. Mathai ◽  
B. J. Oldfield ◽  
R. S. Weisinger

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