This historical review highlights the shift in understanding edema formation in heart failure from purely hemodynamic factors to renal sodium and water retention.
Supports renal focus in historical HF edema models; leaves open integration with contemporary hemodynamic therapies.
Shifts of fluid from the intravascular to the extravascular compartment are facilitated by appropriate changes in venous pressure, colloidal osmotic pressure, capillary permeability, and "tissue pressure." Development and subsidence of generalized edema cannot easily be explained on the basis of these factors alone. Starling¹invoked diminished excretion by the kidneys to explain the "hydremic plethora" found in chronic congestive heart failure. Schroeder found that the capacity to excrete sodium chloride was greatly reduced in the edematous patient.²Restriction of salt intake to a level below urine output arrested edema accumulation or caused diuresis. Warren and Stead³administered sodium chloride to edema-forming patients and noted extracellular fluid accumulated before any increase in venous pressure was detected. They concluded that the edema of congestive failure resulted from failure of the kidneys to excrete salt and, secondarily, water for reasons then unkonwn. Acute reduction in glomerular filtration rate in the
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Amos H. Lieberman (1958) studied this question.
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