Transport of solutes from peritubular capillaries to tubular fluid, active or passive transport, H+ secreted via Na+/H+ antiporter, K+ secreted in DCT and collecting duct, ammonium ions synthesized in renal epithelial cells and diffuse into tubular fluid
1. H2O diffuses from the lumen of the descending thin limb into the interstitial fluid = tubular fluid increases in osmotic concentration as it descends to the inner most region of the medulla
2. When the tubular fluid enters the ascending thin limb (permeable to solute and not to H2O), NaCl diffuses out into the inner medullary interstitial fluid and urea diffuses into the tubular fluid
3. Continued active secretion by the ascending thick limb, concentration of tubular fluid in the descending thin limb and diffusion from the lumen of the ascending thin limb into the medullary interstitial fluid establishes an osmotic gradient
1. The vasa recta is permeable to water, salts and urea
2. Descending limb of the vasa recta: H2O moves, via osmosis, from the plasma of vasa recta to the hyperosmotic peritubular fluid (created by counter current multiplier) and the solutes diffuse from the peritubular fluid into the vasa recta
3. Ascending limb: Solutes diffuse back into the peritubular fluid and H2O moves, via osmosis, back into the vasa recta
4. Net result is that the solutes responsible for medullary gradient are mostly retained in the medulla and the vasa recta carry only slightly more solutes than are brought to them