Ganong's Review of Medical Physiology, 23rd Edition

(Chris Devlin) #1
CHAPTER 38Renal Function & Micturition 655

leading to the normal equilibrium condition, although the steps
do not occur in vivo. It is also important to remember that the
equilibrium is maintained unless the osmotic gradient is washed
out. These steps are summarized in Figure 38–16 for a cortical
nephron with no thin ascending limb. Assume first a condition
in which osmolality is 300 mOsm/kg of H 2 O throughout the
descending and ascending limbs and the medullary interstitium
(Figure 38–16A). Assume in addition that the pumps in the
thick ascending limb can pump 100 mOsm/kg of Na+ and Cl–
from the tubular fluid to the interstitium, increasing interstitial
osmolality to 400 mOsm/kg of H 2 O. Water then moves out of
the thin descending limb, and its contents equilibrate with the
interstitium (Figure 38–16B). However, fluid containing 300
mOsm/kg of H 2 O is continuously entering this limb from the
proximal tubule (Figure 38–16C), so the gradient against which
the Na+ and Cl– are pumped is reduced and more enters the
interstitium (Figure 38–16D). Meanwhile, hypotonic fluid flows
into the distal tubule, and isotonic and subsequently hypertonic
fluid flows into the ascending thick limb. The process keeps
repeating, and the final result is a gradient of osmolality from
the top to the bottom of the loop.
In juxtamedullary nephrons with longer loops and thin
ascending limbs, the osmotic gradient is spread over a greater


distance and the osmolality at the tip of the loop is greater. This
is because the thin ascending limb is relatively impermeable to
water but permeable to Na+ and Cl–. Therefore, Na+ and Cl–
move down their concentration gradients into the interstitium,
and there is additional passive countercurrent multiplication.
The greater the length of the loop of Henle, the greater the
osmolality that can be reached at the tip of the medulla.
The osmotic gradient in the medullary pyramids would not
last long if the Na+ and urea in the interstitial spaces were
removed by the circulation. These solutes remain in the pyra-
mids primarily because the vasa recta operate as countercurrent
exchangers (Figure 38–17). The solutes diffuse out of the ves-
sels conducting blood toward the cortex and into the vessels
descending into the pyramid. Conversely, water diffuses out of
the descending vessels and into the fenestrated ascending ves-
sels. Therefore, the solutes tend to recirculate in the medulla
and water tends to bypass it, so that hypertonicity is main-
tained. The water removed from the collecting ducts in the pyr-
amids is also removed by the vasa recta and enters the general
circulation. Countercurrent exchange is a passive process; it
depends on movement of water and could not maintain the
osmotic gradient along the pyramids if the process of counter-
current multiplication in the loops of Henle were to cease.

FIGURE 38–16 Operation of the loop of Henle as a countercurrent multiplier producing a gradient of hyperosmolarity in the
medullary interstitium (MI). TDL, thin descending limb; TAL, thick ascending limb. The process of generation of the gradient is illustrated as oc-
curring in hypothetical steps, starting at A, where osmolality in both limbs and the interstitium is 300 mOsm/kg of water. The pumps in the thick
ascending limb move Na+ and Cl– into the interstitium, increasing its osmolality to 400 mOsm/kg, and this equilibrates with the fluid in the thin
descending limb. However, isotonic fluid continues to flow into the thin descending limb and hypotonic fluid out of the thick ascending limb. Con-
tinued operation of the pumps makes the fluid leaving the thick ascending limb even more hypotonic, while hypertonicity accumulates at the
apex of the loop. (Modified and reproduced with permission from Johnson LR [editor]: Essential Medical Physiology, Raven Press, 1992.)


312
375
375
425
425
513
513
700

300
325
325
425
425
425
425
600

300
300
300
300
300
300
300
300

300
300
300
300
300
300
300
300

300
300
300
300
300
300
300
300

A
400
400
400
400
400
400
400
400

400
400
400
400
400
400
400
400

200
200
200
200
200
200
200
200

B

TDL MI TAL

300
300
300
300
400
400
400
400

300
300
300
300
400
400
400
400

200
200
200
200
400
400
400
400

C
350
350
350
350
500
500
500
500

350
350
350
350
500
500
500
500

150
150
150
150
300
300
300
300

D

300
300
350
350
350
350
500
500

300
300
350
350
350
350
500
500

150
150
300
300
300
300
500
500

E
325
325
425
425
425
425
600
600

125
125
225
225
225
225
400
400

F
300
325
325
425
425
425
425
600

125
225
225
225
225
400
400
600

G
312
375
375
425
425
513
513
700

112
175
175
225
225
313
313
500

H
325
325
425
425
425
425
600
600
Free download pdf