Diagram of a single vas rectum and single long-looped nephron, illustrating how classic countercurrent multiplication could produce the osmotic gradient.

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Diagram of a single vas rectum and single long-looped nephron, illustrating how classic countercurrent multiplication could produce the osmotic gradient in the outer medulla, and how the “passive mechanism” was proposed to produce the osmotic gradient in th... Diagram of a single vas rectum and single long-looped nephron, illustrating how classic countercurrent multiplication could produce the osmotic gradient in the outer medulla, and how the “passive mechanism” was proposed to produce the osmotic gradient in the inner medulla (23,24). In the outer medulla, active transport of NaCl out of the water-impermeable thick ascending limb (indicated by solid arrows and black dots) creates the small osmotic pressure difference between that limb and the descending limb sufficient for classic countercurrent multiplication to generate the osmotic gradient (approximate osmolalities for rat kidney given by numbers in the black boxes). For the proposed “passive” mechanism in the inner medulla, urea ([urea]) is concentrated ([urea]↑) in urea-impermeable cortical and outer medullary collecting ducts by reabsorption of NaCl and water (broken arrows indicate passive movement). Urea then moves passively out of the inner medullary collecting ducts via vasopressin-regulated urea transporters (UT-A1, UT-A3; open circles and broken lines) into the surrounding inner medulla interstitium. This increased concentration of urea in the inner medullary interstitium draws water from descending thin limbs (DTLs) and inner medullary collecting ducts (IMCDs), thereby reducing inner medullary interstitial concentration of NaCl ([NaCl]↓). These processes result in a urea concentration in the interstitium that is higher than the urea concentration in the ascending thin limbs (ATLs) and a NaCl concentration in the ATLs that is higher than the NaCl concentration in the interstitium. NaCl will then tend to diffuse out of the ATLs (broken arrows) and urea will tend to diffuse into the ATLs (broken arrows). If the permeability of the ATLs to NaCl is sufficiently high and to urea sufficiently low, the interstitial fluid will be concentrated (producing the osmotic gradient) as the ATL fluid is being diluted. Countercurrent exchange of solutes and water helping to preserve this gradient is indicated in the vas rectum. Segments are numbered according to key. William H. Dantzler et al. CJASN 2014;9:1781-1789 ©2014 by American Society of Nephrology