BIOC34H3 Lecture Notes - Lecture 19: Distal Convoluted Tubule, Nephron, Renal Medulla

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29 May 2019
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Lecture 19: the medullary osmotic gradient, urine formation and acid-base balance: the medullary osmotic gradient. Osmolarity of peritubular fluid at cortex/medulla boundary is 300 mosm. It increases from 300 to 1400 in the inner core of kidney. This osmotic gradient is what allows kidney to produce a concentrated urine (greater than 300 mosm): medullary osmotic gradient is established by loop of henle which has different permeability to water and ions between ascending and descending sections. Descending limb is permeable to h2o, but impermeable to ions like, Blood supply to loop of henle is involved in formation and maintenance of medullary osmotic gradient. Maintenance of the gradient: the vasa recta: vasa recta is the capillary network that surrounds loop of henle. It is a vessel that flows down into core of kidney and back up again (same as loop of henle). It functions as a countercurrent exchanger and helps to maintain medullary osmotic gradient.

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