BIOC34H3 Lecture Notes - Lecture 19: Oncotic Pressure, Distal Convoluted Tubule, Nephron

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20 Apr 2014
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Lecture 19: the medullary osmotic gradient, urine formation and acid-base balance: the medullary osmotic gradient. Formation of the gradient: the loop of henle. The osmolarity of the peritubular fluid at the cortex/medulla boundary is 300 mosm (milliosmoles). 1400 mosm in the inner core of the kidney. This osmotic gradient is what allows the kidney to produce a concentrated urine (i. e. , to produce a urine with an osmolarity that is greater than 300 mosm; which is the osmolarity of blood). The medullary osmotic gradient is established by the loop of henle which has different permeability to water and ions between the ascending and descending sections of the loop. The descending limb is permeable to h2o, but impermeable to various ions (such as na+, k+ or cl-). The ascending limb is the opposite; permeable to ions and impermeable to water. The seven-step series of slides at the beginning of this lecture illustrate a scheme in which the osmotic gradient is formed.

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