RENAL PHYSIOLOGY: RENAL MECHANISMS |
Loop of Henle & Initial Distal Tubule Transport
A. Role: establishes an appropriate osmotic environment for the adjustment of fluid balance
B. Active Reabsorption
Sodium ion about 75% of amount entering loop
Chloride ion about 70% of amount entering
C. Passive Reabsorption
Water about 25% of amount entering
D. No Transport
Inulin
Creatinine
Summary: Because the reabsorption of sodium and chloride (the major dissolved substances) is much more rapid than the reabsorption of water, the tubular fluid becomes quite hypo-osmotic (100 mOsm/kg, about one-third the osmolality of plasma). Thus, a hypo-osmotic fluid leaves the loop of Henle (and enters the distal tubule) at the rate of about 20 ml/min.
Later Distal Tubule & Colleting Duct Transport
A. Role: Final adjustment of the fluid to be excreted in order to maintain homeostasis
B. Reabsorption (variable)
1. Active transport
Na+ osmotic and electrolyte balance
Cl- osmotic and electrolyte balance
2. Passive electrochemical diffusion or osmosis
urea body fluid balance
H2O osmotic and body fluid balance
3. Associated with renal metabolism
HCO3- acid-base balance
C. Secretion (variable)
1. Active transport
K+ electrolyte balance
H+ acid-base balance
2. Associated with renal metabolism
NH4+ acid-base balance
D. No Transport
1. Tubule impermeable
inulin
creatinine
Summary: leaving the collecting duct (to be excreted as urine) is a fluid of varying composition, varying osmolality (hyper-, hypo-, or iso-osmotic; range 100-1200 mOsm/kg), varying pH, and varying volume (0.2 to 20 ml/min), as required to satisfy homeostasis.
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