Page 177 - Color_Atlas_of_Physiology_5th_Ed._-_A._Despopoulos_2003
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Reabsorption of Water, Formation of  pertonic towards the papillae (see below) and
       Concentrated Urine              if the vasa recta are permeable to water. Part of
                                       the water diffuses by osmosis from the de-
       The glomeruli filter around 180 L of plasma  scending vasa recta to the ascending ones,
       water each day (= GFR; ! p. 152). By compari-  thereby “bypassing” the inner medulla (! A4).
                          .
       son, the normal urine output (VU) is relatively  Due to the extraction of water, the concentra-
       small (0.5 to 2 L/day). Normal fluctuations are  tion of all other blood components increases as
                      .
       called antidiuresis (low VU) and diuresis (high  the blood approaches the papilla. The plasma
       .
       VU; ! p. 172). Urine output above the range of  osmolality in the vasa recta is therefore con-
    Kidneys, Salt, and Water Balance  plasma and glomerular filtrate is about  rises. Conversely, substances entering the
       normal is called polyuria. Below normal output
                                       tinuously adjusted to the osmolality of the sur-
       is defined as oliguria (! 0.5 L/day) or anuria
                                       rounding interstitium, which rises towards the
                                       papilla. The hematocrit in the vasa recta also
       (! 0.1 L/day). The osmolality (! p. 377) of
       290 mOsm/kg H 2O (= P osm); that of the final
                                       blood in the renal medulla diffuse from the as-
       urine (U osm) ranges from 50 (hypotonic urine in
                                       cending to the descending vasa recta, provided
       extreme water diuresis) to about 1200 mOsm/
                                       the walls of both vessels are permeable to
       kg H 2O (hypertonic urine in maximally con-
                                       them (e.g., urea; ! C). The countercurrent ex-
                                       change in the vasa recta permits the necessary
       centrated urine). Since water diuresis permits
                                       supply of blood to the renal medulla without
       the excretion of large volumes of H 2O without
       the simultaneous loss of NaCl and other sol-
                                       renal medulla and hence impairing the urine
       “free water clearance” (C H 2 O). This allows the
                                       concentration capacity of the kidney.
    7  utes, this is known as “free water excretion”, or  significantly altering the high osmolality of the
       kidney to normalize decreases in plasma
                                        In a countercurrent multiplier such as the
                                       loop of Henle, a concentration gradient be-
       osmolality, for example (! p. 170). The C H 2 O
       represents to the volume of water that could be  tween the two limbs is maintained by the ex-
       theoretically extracted in order for the urine to  penditure of energy (! A5). The countercur-
       reach the same osmolality as the plasma:  rent flow amplifies the relatively small
             .
         C H 2 O " VU (1–[U osm/P osm]).  [7.11]  gradient at all points between the limbs (local
                                       gradient of about 200 mOsm/kg H 2O) to a rela-
       Countercurrent Systems          tively large gradient along the limb of the loop
       A simple exchange system (! A1) can consist of  (about 1000 mOsm/kg H 2O). The longer the
       two tubes in which parallel streams of water flow, one  loop and the higher the one-step gradient, the
       cold (0 #C) and one hot (100 #C). Due to the exchange  steeper the multiplied gradient. In addition, it
       of heat between them, the water leaving the ends of  is inversely proportional to (the square of) the
       both tubes will be about 50 #C, that is, the initially  flow rate in the loop.
       steep temperature gradient of 100 #C will be offset.
         In countercurrent exchange of heat (! A2), the
       fluid within the tubes flows in opposite directions.  Reabsorption of Water
       Since a temperature gradient is present in all parts of  Approximately 65% of the GFR is reabsorbed at
       the tube, heat is exchanged along the entire length.  the proximal convoluted tubule, PCT (! B and
       Molecules can also be exchanged, provided the wall  p. 157 D). The driving “force” for this is the re-
       of the tube is permeable to them and that a concen-  absorption of solutes, especially Na and Cl . –
                                                              +
       tration gradient exists for the substance.  This slightly dilutes the urine in the tubule, but
         If the countercurrent exchange of heat occurs in a
       hairpin-shaped loop, the bend of which is in contact  H 2O immediately follows this small osmotic
       with an environment with a temperature different  gradient because the PCT is “leaky” (! p. 154).
       from that inside the tube (ice, ! A3), the fluid exit-  The reabsorption of water can occur by a para-
       ing the loop will be only slightly colder than that  cellular route (through leaky tight junctions)
       entering it, because heat always passes from the  or transcellular route, i.e., through water chan-
       warmer limb of the loop to the colder limb.  nels (aquaporin type 1 = AQP1) in the two cell
       Countercurrent exchange of water in the vasa  membranes. The urine in PCT therefore re-
       recta of the renal medulla (! A6 and p. 150) oc-  mains (virtually) isotonic. Oncotic pressure
  164
       curs if the medulla becomes increasingly hy-  (! p. 378) in the peritubular capillaries pro-
                                                                   !
       Despopoulos, Color Atlas of Physiology © 2003 Thieme
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