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1 Division of Nephrology, University of Maryland School of Medicine, Baltimore, Maryland 21201; 2 Department of Human Anatomy and Cell Biology, University of Liverpool, Liverpool L69 3GE, United Kingdom; 3 Department of Chemical and Biological Engineering, Tufts University, Medford, Massachusetts 02155; and 4 Division of Nephrology, Stanford University School of Medicine, Stanford 94305 and Veterans Affairs, Palo Alto Health Care System, Palo Alto, California 94304
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ABSTRACT |
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GENERAL...
GENERAL...
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The microcirculation of the renal medulla traps NaCl and urea deposited to the interstitium by the loops of Henle and collecting ducts. Theories have predicted that countercurrent exchanger efficiency is favored by high permeability to solute. In contrast to the conceptualization of vasa recta as simple "U-tube" diffusive exchangers, many findings have revealed surprising complexity. Tubular-vascular relationships in the outer and inner medulla differ markedly. The wall structure and transport properties of descending vasa recta (DVR) and ascending vasa recta (AVR) are very different. The recent discoveries of aquaporin-1 (AQP1) water channels and the facilitated urea carrier UTB in DVR endothelia show that transcellular as well as paracellular pathways are involved in equilibration of DVR plasma with the interstitium. Efflux of water across AQP1 excludes NaCl and urea, leading to the conclusion that both water abstraction and diffusion contribute to transmural equilibration. Recent theory predicts that loss of water from DVR to the interstitium favors optimization of urinary concentration by shunting water to AVR, secondarily lowering blood flow to the inner medulla. Finally, DVR are vasoactive, arteriolar microvessels that are anatomically positioned to regulate total and regional blood flow to the outer and inner medulla. In this review, we provide historical perspective, describe the current state of knowledge, and suggest areas that are in need of further exploration.
vasa recta; microperfusion; microcirculation; water channel; urinary concentration; permeability
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INTRODUCTION |
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GENERAL...
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SINCE THE EXPERIMENTAL FINDINGS of Wirz et al. (147) led to the countercurrent theory of the urinary concentrating mechanism, as described by Hargitay and Kuhn (31), most subsequent research has focused on the countercurrent multiplier function of the loops of Henle. According to the theory, a small difference in osmotic pressure (the single effect) is multiplied by countercurrent flow in adjacent channels of the limbs of Henle's loop to produce a large axial difference in osmotic pressure between the renal cortex and the tip of the renal papilla; that is, the multiplier generates a hypertonic renal medulla. Less attention has been paid to countercurrent exchange, which is thought to preserve medullary hypertonicity rather than create it. It is generally accepted that the microcirculation of the renal medulla functions as a countercurrent exchanger that traps NaCl and urea deposited to the interstitium by the loops of Henle and collecting ducts, respectively. Early hypothetical descriptions of this process envisioned a system in which descending vasa recta (DVR) and ascending vasa recta (AVR) are parallel tubes that equilibrate by diffusion. According to that notion, blood flowing from the corticomedullary junction toward the papillary tip in DVR is concentrated by diffusive influx of NaCl and urea, and, conversely, blood flowing away from the papillary tip toward the corticomedullary junction in AVR is diluted by diffusive efflux. That theory predicts that solute is trapped due to recycling between DVR and AVR and that net rate at which solute is removed from the medulla is primarily dependent on the AVR-DVR concentration difference at the corticomedullary junction (13, 39, 40, 91, 145).
Micropuncture studies demonstrated that AVR plasma is more concentrated than adjacent DVR plasma, providing key evidence that vasa recta are countercurrent exchangers (38, 113, 114). In contrast, fluid obtained from descending thin limbs of Henle is more concentrated than that from ascending thin limbs, supporting the conclusion that the loops of Henle function as the countercurrent multiplier responsible for generating corticomedullary osmotic gradients (38-41). Subsequent studies unraveled an unexpected degree of complexity. DVR and AVR wall structures were found to be distinct and to have characteristics that vary as function of corticomedullary axis (39, 59, 91, 121). In vivo measurements of plasma protein concentrations in DVR unexpectedly revealed efflux of water from the DVR lumen to the papillary interstitium, a finding that presented two paradoxes. First, the physiological benefit derived from depositing water from DVR to medullary interstitium was enigmatic. Second, measurements of Starling forces (hydraulic and oncotic pressure) failed to predict the observed direction of DVR transmural water movement (113, 114).
Recent physiological investigations continued to show unexpected complexity while shedding some light on the paradoxes associated with DVR equilibration. Specifically, physiological and immunochemical measurements verified that aquaporin-1 (AQP1) water channels and the facilitated urea carrier (UTB) are significant transport pathways in DVR endothelia. Unusual intracellular signaling pathways have been found in DVR endothelia (94, 99, 106). A few recent measurements of AVR properties have been obtained that show striking differences from DVR (81-83, 90, 95-98, 133). Overall, AVR remain poorly characterized because they cannot be isolated for in vitro studies. Taken together, these studies of microanatomy, tubular-vascular relationships, and transport properties demonstrate complexity and lead to the conclusion that the depiction of vasa recta as simple diffusive "U-tube" exchangers leads to conceptual errors. In this review, we will summarize the pertinent literature and, to the extent possible, give functional perspective to these observations.
In view of his numerous contributions to the urinary concentrating mechanism, among which were the introduction of the countercurrent multiplier theory of Werner Kuhn and the companion countercurrent exchange theory of the medullary circulation to American readers and the experiments by him and his coworkers testing those theories, we wish to dedicate this review to Robert W. Berliner, who died February 6, 2002.
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TUBULAR-VASCULAR RELATIONSHIPS AND MICROANATOMY |
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GENERAL...
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Outer medulla.
Blood flow to the renal medulla is largely derived from the
efferent arterioles of juxtamedullary glomeruli (9, 10, 59, 73, 91, 93, 99), in addition to which a portion of the flow may
traverse periglomerular "shunt" pathways (16) (Fig. 1). Afferent arterioles that supply
juxtamedullary glomeruli arise from the cortical interlobular arteries
at a steep recurrent angle. Those afferent arterioles are composed of
one to three layers of smooth muscle cells surrounding the media and
endothelial layers. Efferent arterioles of juxtamedullary glomeruli are
larger in wall thickness, diameter, and length than efferent arterioles of superficial glomeruli (9, 10, 39, 91). As efferent arterioles penetrate across the corticomedullary junction to the outer
stripe of the outer medulla, the muscular layer decreases and is
replaced by smooth muscle remnants known as "pericytes" (Fig. 1).
In an arrangement compared with a "horse's tail," juxtamedullary efferent arterioles then give rise to as many as 30 DVR
(73). The diameter of rat DVR is generally one-half that
of the parent efferent arteriole (~12 µm ID), but some larger
vessels continue beyond the outer medulla to perfuse the deep inner
medulla (51). When efferent arterioles become DVR, smooth
muscle is replaced by pericytes and the medial layer interposed between
smooth muscle and endothelium disappears. As DVR continue into the
inner medulla, the pericytes become sparse but are present
(101). The transition from arteriole to capillary is most
gradual in the DVR that penetrate furthest into the inner medulla
(39, 91, 121).
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Inner medulla. Shortly after passing the inner-outer medullary junction, the vascular bundle architecture disappears and vasa recta become more evenly dispersed among nephrons and collecting ducts (39, 73, 91). In the outer medulla, interstitial space between adjacent vessels is minimal (Fig. 2B). From the inner-outer medullary junction to the papillary tip, the fraction of medullary tissue that is interstitium increases from 5 to ~30% (49). Numerous inner medullary interstitial cells, arranged horizontally like rungs of a ladder, are tethered between vessels and nephrons so that they might inhibit axial diffusion and retard dissipation of corticomedullary gradients (58). As in the outer medulla, AVR outnumber DVR. Their ratio has been reported as 1.7 to 1 in hamsters and 2.3 to 1 in the rat (35, 67, 155). DVR terminate at various levels in a sparse capillary plexus that coalesces to form AVR. DVR have a continuous, nonfenestrated endothelium and zona occludens (72, 121). Toward the termination of the DVR, fenestrations appear that characterize the wall of the subsequent capillary plexus and AVR. In the inner medulla, the fraction of the AVR wall covered by fenestrations is ~50%. That fraction decreases toward the outer medulla to ~15-30% (39, 91). On electron micrographs, fenestrations have diameters of 530 to 1,000 Å and are bridged by a 40-Å-thick diaphragm. The diaphragm has one or two concentric rings interconnected by radiating fibers and a central density (68).
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COUNTERCURRENT EXCHANGE GENERAL CONCEPTS AND EVOLUTION OF
UNDERSTANDING |
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GENERAL...
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Countercurrent exchange in nature.
The idea of countercurrent exchange can be traced back to Claude
Bernard (14), who observed "wherever a peripheral artery flows alongside a vein there is likely to be a heat gradient between them and a transfer of heat from artery to
vein ... [This] ... thermal short circuit ... carries
some of the arterial heat back into the body before it reaches the
periphery" [cited by Scholander and Krog
(119)]. As pointed out by Scholander and Krog
(119), this simple arteriovenous arrangement can become
much more complex with the artery dividing into arterioles or
capillaries and the vein dividing into venules or capillaries to
provide an enormous area for heat exchange between arterial and venous
blood, the rete mirabile (Fig. 3). The
sloth is a slow-moving arboreal animal that inhabits treetops in
tropical jungles. Scholander and Krog (119) dissected the
brachial rete of a sloth, a 1-cm-thick bundle of parallel arteries and
veins with 20-30 arteries and fewer veins. A 4-cm portion of a
rete was freed, and a thermocouple probe was threaded along its length.
The temperature decline in a direction away from the body was 1°C per
centimeter of length, 30 times steeper than that along the human
brachial artery. When the venous blood flow returning through the rete
was slowed by constricting a ligature, the gradient was greatly
reduced.
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200 atmospheres, equaling the weight of the
surrounding water. Located in the bladder neck, the rete traps oxygen
to prevent its escape from the bladder. The "... outgoing veins,
highly charged with oxygen, give it up to adjacent incoming arteries"
(119). For example, the rete from a common eel weighs
~65 mg and has 100,000 arterial capillaries and about the same number
of venous capillaries. The capillaries are ~4-mm long, meaning the
cumulative total length of each kind of capillary is 400 m.
Because the capillary diameter is 7-10 µm, the total wall
endothelial surface area exceeds 20 cm2 (54).
Scholander (118) calculated that the oxygen pressure across a
rete 1 cm long is reduced by a factor of 3,000, which means that oxygen
would be completely extracted from the venous blood flowing out through
the bladder neck and returned to the inflowing arterial blood.
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Countercurrent exchange in the renal medulla.
The idea that the counterflow arrangement of vasa recta enables
efficient exchange of solutes and water originated with Kuhn and his colleagues (31, 55) and Wirz and colleagues
(145-147). But for many, the introduction to
countercurrent multiplication and countercurrent exchange was, at least
in the United States, provided by Berliner et al. (13).
The countercurrent multiplier explained the exponential rise in osmotic
pressure of the renal medullary tissue from the corticomedullary
junction to the papillary tip. But this implied that the osmotic
pressure of blood entering the medulla also rises concomitantly, which
posed the dilemma that even if only 5% of renal blood flow entered the
medulla, the concentrating mechanism would have to concentrate a very
large volume of blood to concentrate a much smaller volume of urine, severely limiting the mechanism's efficiency. The explanation that the
medullary circulation functions as a countercurrent exchanger resolved
the dilemma. Wirz (146) wrote, "all the blood irrigating the medulla enters and leaves the medulla at the corticomedullary boundary, i.e., in an essentially isotonic [to systemic blood] region. In between it may adapt itself to the osmotic pressure of the
surroundings by a passive uptake (on its way down) and release (on its
way up) of osmotically active solutes." Berliner et al.
(13) described countercurrent exchange using the analogy of a heat exchanger, depicted in Fig. 4.
In Fig. 4A, water flowing at 10 ml/min passes a heat source
that supplies heat at a rate of 100 calorie/min. Accordingly, the
temperature of the stream increases from 30 to 40°C. Figure
4B shows a hypothetical idealized counterflow heat exchanger
created by opposing the limbs upstream and downstream from the heat
source. In that case, consistent with the requirement of energy
conservation, water exits the exchanger at a temperature 10°C higher
than the inflow, but an axial temperature gradient is created by the
warming of water before its arrival at the heat source by the
outflowing heated water. This large axial temperature gradient is
established and maintained by thermal diffusion between the two limbs
and by heat trapping due to countercurrent flow. The graph
inset compares the temperature along flow tubes in each
system. In Fig. 4C, countercurrent flow principle is applied to an idealized capillary loop in the medulla representing a descending vas rectum and ascending vas rectum. Note that the exchange occurs between capillary and interstitium of the medulla rather than between
two adjacent capillary loops. Solute diffuses from the medullary
interstitium to the blood flowing down the descending vas rectum. As
blood returns in the ascending vas rectum, the solute concentration
difference is reversed and solute diffuses into the interstitium. This
effectively "traps" solute in the interstitium by recycling between
ascending and descending capillary. In this way, blood circulates
through the renal medulla without "washing out" its hypertonicity.
The greater the solute permeability of the capillary, the more complete
the exchange. In the absence of a high solute permeability, at any
given level, osmotic equilibrium may not be completely achieved;
consequently, the contents of the blood at the cortical medullary
junction may be slightly hypertonic to the isotonic interstitium.
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Water uptake by the medullary microcirculation. The foregoing models neglect the exchange of water in the medulla. In reality, water is supplied to the medullary interstitium by reabsorption from the pars recta of the proximal tubule in the outer medulla, the descending thin limb of Henle's loop in the inner medulla, and the collecting duct. Since the epithelium of the ascending thin and thick limb of Henle's loop is impermeable to water and there are no lymphatics in the inner medulla and few in the outer medulla, any water added to the interstitium must be removed by AVR.
Ullrich et al. (136) derived a model for the countercurrent exchanger similar to Berliner's except that solute is added along the length of the exchanger instead of being added only at the tip of the loop. The differential equations are the same (126). In rodents, measurements of hydrostatic pressure in the DVR averaged 17 mmHg (136, 137). Ullrich postulated that this would drive water from DVR, short-circuiting water along with permeable solutes to AVR and concentrating plasma protein in the DVR. In accord with this hypothesis, the ratio of vasa recta plasma to systemic plasma protein was found to be >1, ranging from 1.08 to 1.40. (However, as the authors noted, an alternative explanation for the high plasma protein is ultrafiltration upstream in juxtamedullary glomeruli.) The authors predicted that addition of water in the AVR would reduce plasma protein to its preglomerular capillary value. Micropuncture of the vasa recta in antidiuretic rats (41, 113, 114) and hamsters (30) near the papillary tip confirmed the findings of Ullrich et al. (136) that the plasma protein concentration at the end of the DVR is elevated above that of the blood entering the medulla. Sanjana and colleagues (113, 114) analyzed the driving forces and transmembrane volume movement. In young rats with a systemic plasma protein concentration of 4.1 g/dl, micropuncture of DVR and AVR at the base of the exposed papilla revealed mean plasma protein concentrations of 7.1 and 5.6 g/dl, respectively. Assuming the vasa recta are impermeable to protein, this finding implies dilution of plasma proteins by fluid uptake between the DVR and AVR, a finding corroborated by Zimmerhackl et al. (155). In contrast, micropuncture of the DVR at the base and tip of the exposed papilla revealed protein concentrations of 5.6 and 6.4 g/dl, respectively, indicating net fluid loss from the DVR. Water uptake in the AVR exceeded water removal from the DVR. The difference accounted for the water added to the medulla from the descending limb of Henle and collecting duct and confirmed mass balance for fluid volume movement in the inner medulla. After the blood begins to ascend in AVR toward the cortex, the solute concentration in the plasma lags in equilibration with the continuously decreasing axial concentration of interstitial solute. At some point the direction of the transendothelial small solute concentration difference will reverse and the luminal solute concentration will exceed that in the interstitium and, if anything, will augment the Starling forces, favoring water uptake by the capillary. The analysis is confounded, however, by anatomic and structural differences between AVR and DVR. First, AVR outnumber DVR between 2 and 2.5 to 1 (35, 155). The transit time of plasma flow through AVR is thereby increased, which allows more time for equilibration of small solutes between plasma and interstitium. Second, the endothelium of AVR is fenestrated so that reflection coefficients for small solutes are likely to be lower than in DVR, which has a continuous endothelium. Comparisons of oncotic pressure exerted by plasma protein with hydraulic pressure revealed that volume efflux from the DVR occurred despite an oncotic pressure that exceeds hydraulic pressure. This was in apparent conflict with conventional wisdom with regard to transcapillary forces that determine water movement across the capillary endothelium, as derived by Starling (124)
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(1) |
is the oncotic pressure,
and the subscripts c and i refer to values in the capillary lumen and
interstitium, respectively. As illustrated in the model exchanger (Fig.
4C) and confirmed by Jamison et al. (38),
plasma concentrations of "small" (nonprotein) molecules such as
NaCl lag in osmotic equilibration with the surrounding interstitium,
creating a transendothelial difference in concentration. Sanjana et al.
(114) hypothesized that such a gradient of small solutes
might provide the additional osmotic driving force required for volume
efflux from the DVR. According to nonequilibrium thermodynamics, volume
flux across a membrane is defined by the following equations (44)
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(2) |
P is the transmembrane hydraulic pressure difference,

i is the transmembrane osmotic pressure difference
due to the ith solute, and
i is the
reflection coefficient of the membrane to the ith solute.
The equation states that volume flux occurs in response to a
transmembrane hydraulic pressure difference and the sum of the
transmembrane osmotic pressures exerted by all solutes that are
osmotically active across the membrane. Applying this to the DVR
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(3) |
pr and
ss are the reflection
coefficients of the capillary membrane to proteins and small solute,
respectively, and 
pr and 
ss are the
transmembrane osmotic pressure due to protein and small solutes,
respectively. From Van't Hoff's law
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(4) |
Css is approximately twice the
transmembrane difference in sodium concentration, reflecting its
univalent anion partner. RT = 19.3 mmHg/mM at T = 37°C. For
example, the
ss = 0.07 for NaCl in capillaries of
the frog mesentery (21). It has been found that the NaCl
concentration of the blood in DVR in the inner medulla is less than
that of the surrounding interstitium due to a lag in equilibration (see
below). Assume the transcapillary membrane concentration difference in
NaCl is 25 mmol/l and
ss = 0.07 for NaCl. This
would result in 67.5-mmHg driving force for volume efflux from the DVR
into the interstitium. To test this hypothesis, Pallone et al.
(98) administered diuretics to rats to eliminate the axial
corticomedullary osmotic gradient (and therefore eradicate the
transendothelial NaCl gradient between interstitium and DVR blood). As
predicted, volume efflux from the DVR was abolished. Accessible DVR
near the surface of the papilla were perfused with buffers differing in
osmolality from the interstitium. Perfusion with solutions made
hyperosmotic or hyposmotic to the interstitium, by addition or removal
of NaCl, was accompanied by water uptake into the capillary and efflux from the capillary, respectively (85).
Equation 3 describes transport of water across the DVR
wall as a whole, simulating it as though it occurs through a single pathway, the hydraulic conductivity of which is Lp. More
recently the discovery of water channel proteins, the aquaporins, has
provided the long sought after biophysical explanation for selective
water permeability of biological membranes (2, 3, 76-78,
103, 108, 115). It is now understood that AQP1 is expressed by
DVR endothelia and is the transport pathway across which small
hydrophilic solutes such as NaCl and urea drive water flux. As will be
discussed in subsequent sections, transport of water across the DVR
wall is more rigorously described by simulating parallel pathways. One
pathway is the highly selective AQP1 molecule (
ss = 1.0) and a parallel pathway that conducts both water movement as
well as convective and diffusive flux of small solutes
(
ss
0) (77, 87, 89, 95, 135).
Expression of AQP1 in DVR has been hypothesized to play an
important role in the optimization of renal medullary countercurrent
exchanger function (87).
The finding that urea transport across the collecting duct in the
presence of AVP is much greater than can be explained by diffusion and
is reduced by phloretin and urea analogs led to the discovery of a
transporter that facilitates urea movement. In the last decade, two
families of urea transporters have been identified (5,
17), UTA and UTB. UTA isoforms are present in the collecting
duct and descending limb of Henle's loop (133), and UTB
is found in erythrocytes and DVR (8, 80, 97). In subsequent sections, the role of UTB (Fig.
5) and AQP1 (Fig.
6) in the optimization of urinary
concentrating ability will also be considered.
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TRANSPORT PROPERTIES GENERAL DEFINITIONS |
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GENERAL...
GENERAL...
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To understand the physiology of microvascular exchange in the
renal medulla and review the associated literature, one must grapple
with a few of the fundamentals of membrane transport theory. As
described above in association with Equations 1-4, DVR
equilibrate with the medullary interstitium by passive transport of
solutes and water through a variety of pathways. In this section, we
provide definitions of key parameters that define the properties of
those pathways. Measurement of those parameters has been the goal of many studies (Tables 1 and 2). Some description of the essentials is
provided in the APPENDIX and the reader is directed to
authoritative sources (4, 19, 26, 44, 69, 71, 102, 120,
144).
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Water and solutes permeate the walls of microvessels, including DVR, by
passive convection and diffusion, driven by gradients of potential
energy provided by transmural differences in hydrostatic and
osmotic pressure (19, 69, 71). Quantitative analysis of
passive transport is based on nonequilibrium thermodynamics, which
states that fluxes through a membrane are proportional to driving
forces if they are small enough and if the system is not too far from
equilibrium (19, 44, 120). Permeability coefficients quantify relationships between transmembrane fluxes and forces or
between different fluxes. Hydraulic permeability (Lp)
relates the total flux of solvent (water) plus solute through a
membrane (volume flux, Jv) to the difference in
hydrostatic pressure between the two sides of the membrane (
P).
Lp equals (Jv/
P), when the transmembrane difference in solute concentration (
C) and therefore in osmotic pressure difference (
) is 0. The resistance of a membranous pathway to transport of water is alternately expressed as
osmotic water permeability (Pf). Lp and
Pf are related; Pf = (Lp
Vw)/(RT), where Vw is the partial molar volume
of water.
Diffusional permeability to a solute (Ps) relates the net
molar flux of solute through a membrane (Js) to
the transmural concentration difference,
C, when transmural volume
flux (Jv) and therefore convective solvent drag
is zero. Under these conditions, Ps simply equals
(Js/
C) and can be viewed as the
"resistance" of the membrane to diffusion of the solute. Transport
of solute across a membrane can have both diffusional and convective
components the directions of which need not be the same. Equations that
describe this more complex scenario are provided in the
APPENDIX.
Osmotic reflection coefficient (
d) is a property of a
membranous pathway that describes the selectivity of the pathway for solvent vs. solute.
d Can take on values between zero
and one.
d Is one for a semipermeable membrane that
sieves or "reflects" all solute from solution, but zero for a
nonselective membrane that does not distinguish between solute and
solvent. An ultrafiltration coefficient (
f) is the ratio
of the convective solute flux reflected at a membrane to that carried
through the membrane, given by [1
(Js/JvC1)],
where C1 is the solute concentration at the upstream surface of the membrane and
C is zero. For practical purposes in
physiological dilute solutions,
d and
f
are equal. The equality is, however, only approximate for nonideal
solutes, such as albumin (19, 69). As illustrated by
Equations 2 and 3, when the reflection coefficient to the ith solute (
i) < 1.0, a transmural gradient of the solute will exert less than its total
ideal osmotic driving force for water movement. When
i = 1, solvent traversing the membrane will be
rendered solute free at the downstream membrane surface (complete
sieving). Conversely, when
i = 0, movement of water
across the membrane carries solute freely, without restriction.
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TRANSPORT OF WATER THROUGH THE DVR WALL |
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GENERAL...
GENERAL...
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Water moves through the walls of DVR via pathways of at least two
kinds (77, 89, 90, 135). Analysis of the permeabilities of
DVR indicates that a "shared" transmural pathway for water and
hydrophilic solutes exists in parallel with a "water only" pathway
(
1.0) that excludes hydrophilic solutes.
Shared pathway.
Evidence for a shared pathway conducting diffusion of hydrophilic
solutes through the walls of DVR comes from measurements of the
correlations between the diffusional permeabilities of these
microvessels to 22Na (PNa) and to tritiated
water (PD), 36Cl, [3H]raffinose
(Praf), [14C]urea, and
[14C]inulin (90). The simplest
interpretation of correlated variations in diffusional permeability to
hydrophilic solutes is that they arise from variations in a shared
aqueous (porous) pathway. Simultaneous measurement of permeability to
two solutes was obtained by perfusing DVR in vitro with pairs of
radioactive tracers and calculating both permeabilities (e.g.,
PNa and Praf) from lumen-to-bath efflux using
dual isotope detection methods in the perfusate and collectate (Figs.
5-8, Table
2).
From Fick's first law (see APPENDIX), the diffusional permeability of a porous membrane to a solute (Ps) is given
by
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(5) |
) is
the equilibrium ratio of solute concentration in a pore to that in bulk
solution, and Ap is the fraction of the membrane area
occupied by pores and
x is pore length (19, 66). Using
Equation 5, it can be predicted that, for diffusion of small
hydrophilic solutes in large pores, the ratio of the permeabilities to
those solutes should be equal to the ratio of their diffusion
coefficients in bulk solution. This was verified in DVR for several
pairs of tracers (Table 2) (90). It was experimentally
possible to demonstrate the correlations in rat DVR because the
permeability of individual vessels varies. The variation in
Ps between DVR is probably attributable to variations in
Ap/
x, because the shared pathway in these microvessels does not significantly sieve small hydrophilic solutes (see below).
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alb) was calculated from volume flux (Jv) driven by the known transmural osmotic
pressure difference provided by albumin (
alb) when
P was negligible. Lp
alb correlates with
Praf in DVR, with an intercept close to zero (Fig.
9), indicating that most
Jv driven by 
alb goes through
the shared pathway. The shared pathway is insensitive to mercurial
compounds, unlike the exclusive water pathways described below, because
p-chloromercuribenzenesulfonate (pCMBS; see Fig. 6) does not
change Lp
alb in glutaraldehyde-fixed DVR
(89). Fixation of DVR by brief exposure to glutaraldehyde prevents damage by mercurials or hyperosmolar solutions and does not
change permeabilities (77, 87, 89).
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alb,
Praf, and PNa correlate with perfusion rate in
isolated DVR, but the ultrafiltration coefficient for albumin does not
(89, 90, 135). Mean Lp values reported for DVR
are >1.4 × 10
6
cm · s
1 · mmHg
1
in vivo (96) and 1.56 × 10
6
cm · s
1 · mmHg
1
in vitro (if
alb is 1) (135) (Table
3).
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close to 1, Equation 5), then this implies
that their solutions undergo little ultrafiltration and exert only
small fractions of their total osmotic pressures across this pathway.
Mathematical modeling indicates that osmotic reflection and
ultrafiltration coefficients are ~(1
)2 for
porous membranes or for fibrous networks (such as the glycocalyx lining
microvessels) and therefore are small if
is close to one (19,
29, 69, 71). Osmotic reflection coefficients for NaCl solutions
at the walls of rat DVR are indeed small, estimates being 0.032 in
vitro (135) and <0.05 in vivo (85). These
values are calculated from the relative abilities of NaCl and albumin solutions to drive transmural volume flux in unfixed DVR, assuming that
alb is one. They are probably overestimates of the
osmotic reflection coefficient of NaCl (
s) at the shared
pathway, because they describe molecular sieving by whole DVR, which
occurs at highly selective exclusive water pathways as well as at the
shared pathway (see below and APPENDIX). In fact, transport
of water across the DVR wall may be better described by simulating
parallel transport through the shared pathway (
s
0)
and water channels (
s
1.0).
Molecular sieving by a shared pathway in DVR is poorly defined even in
microvessels from AQP1 knockout mice, which retain only minimal
exclusive water pathways (87). Osmosis drives volume efflux from these DVR through a mercurial-insensitive pathway, which
appears to show increased sieving of progressively larger hydrophilic
solutes. Hyperosmolar solutions of NaCl are ineffective, but urea,
glucose, and raffinose are increasingly able to drive volume efflux
from unfixed and fixed AQP1 knockout DVR (Fig. 6B). pCMBS
does not inhibit raffinose-driven volume efflux from these microvessels. Similarly, AQP1 knockout DVR apparently do not
ultrafilter luminal 22Na, but do retain some
[3H]raffinose and [14C]inulin during volume
efflux driven by hyperosmolar raffinose. Unfortunately, mathematical
simulations of ultrafiltration and transmural diffusion along mouse DVR
do not yield reliable estimates of osmotic reflection or
ultrafiltration coefficients for small hydrophilic solutes because of
the high diffusional permeabilities of mouse DVR to these tracers
(87). Hence, the appearance of size-dependent molecular
sieving by AQP1 knockout DVR, although attributable to a shared
pathway, is equally consistent with complete sieving at remaining
exclusive water pathways, combined with slower transmural diffusion of
larger solutes.
In contrast with small hydrophilic solutes, the macromolecule albumin
undergoes considerable sieving at the shared pathway in DVR. The mean
ultrafiltration coefficient of albumin solutions at whole DVR is 0.89 (and not significantly different from 1), according to retention of
fluorescently labeled perfusate albumin during volume efflux driven by
unlabeled albumin (135). This probably is close to the
ultrafiltration coefficient of albumin solutions at the shared pathway,
because this pathway dominates the Lp of DVR.
Exclusive water pathways. Water apparently diffuses through the walls of DVR via pathways that exclude hydrophilic solutes, as well as via shared pathways, because the permeability to tritiated water (PD) of these microvessels is always high, even when PNa is low (90) (Fig. 8B).
Exclusive water pathways also conduct most of the convection driven through the walls of DVR by transmural osmotic pressure gradients due to small hydrophilic solutes (85, 89). Evidence for this is that mathematical simulations of ultrafiltration and transmural diffusion along rat DVR, during volume efflux driven by hyperosmolar NaCl, most accurately predict the observed retention of 22Na and [3H]raffinose when ultrafiltration and osmotic reflection coefficients are assumed to be one at the convective pathway (135) (Fig. 10).
|
css) can be
described by
|
(6) |
ss is the osmotic reflection coefficient for a small
hydrophilic solute, A is the fractional area of a pathway, and the
subscripts a, w, and p denote values for the whole microvessel for
exclusive water and for shared pathways, respectively, so that
|
(7) |
Css due to NaCl, because of the evidence that osmotic
reflection coefficient of NaCl is one at the exclusive water pathway
(
ss,w) but low at the shared pathway
(
ss,p). This evidence implies that NaCl drives volume flux mainly through the exclusive water pathway, because it exerts little effective osmotic pressure across the shared pathway. From Equation 6, Jv
Pf,wAwV
Css if
ss,p
0. Flow apparently does not modulate
Pf,wAw in glutaraldehyde-fixed DVR
(89), as it does Pf,a in the unfixed
microvessels (135) or PNa in unfixed (90) or fixed (89) DVR.
The osmotic permeability of exclusive water pathways in DVR
(Pf,wAw) is one order of magnitude lower than
that of the shared pathway (Pf,pAp) (Table 3).
This follows because an osmotic permeability for whole DVR
(Pf,a) of 16,700 µm/s can be calculated from the mean
Lp of 1.56 × 10
6
cm · s
1 · mmHg
1
for microvessels in vitro (89, 135). These permeabilities are of the shared plus exclusive water pathways in DVR, because this
Lp is calculated from Jv driven by
albumin solutions, which apparently have osmotic reflection
coefficients close to one at both pathways.
The low osmotic reflection coefficient of NaCl solutions at whole DVR
(85, 135) is consistent with the osmotic permeabilities and molecular sieving properties attributed to these shared and exclusive water pathways. For parallel pathways (19), from
Equations 6 and 7
|
(8) |
ss,a
0.06, if
ss,p is zero,
ss,w is one,
Pf,wAw is 1,000 µm/s, and Pf,a is
16,700 µm/s, which agrees reasonably well with experimental values
for
ss,a < 0.05 for NaCl solutions (Table 3)
(85, 135). Note that
ss,a (Equation 8) is the same as
ss in Equation 3 as
originally applied to the DVR wall by Sanjana et al.
(114).
Identification of exclusive water pathways in DVR begins with the
observation that they are mercurial sensitive, unlike the shared
pathway. pCMBS strongly inhibits volume efflux driven by hyperosmolar
NaCl from fixed DVR from rats (89) (Fig. 6A)
and significantly reduces PD without changing
PNa (77). Similarly, pCMBS abolishes volume
efflux driven by NaCl from wild-type mouse DVR and reduces that driven
by raffinose (87). This suggests that aquaporins form a
transcellular exclusive water pathway in DVR, although mercurials do
not block all (2) or only (80) aquaporins.
AQP1 is highly selective for water, mercurial sensitive (2,
3), and expressed by DVR (77, 78) in sufficient
quantity to account for exclusive water pathways (89).
Polyclonal antibodies to AQP1 label the plasma membranes (including
caveolae) of the continuous endothelium of DVR in the inner medulla of
rat kidney, but not the surrounding pericytes or the fenestrated
endothelium of AVR (77). The AQP1 content of rat DVR,
measured by enzyme-linked immunosorbent assay, predicts an osmotic
permeability of 1,344 µm/s, if AQP1 is equally distributed between
luminal and abluminal endothelial plasma membranes in series
(89). This is close to measured osmotic permeabilities for
exclusive water pathways (Pf,wAw) in rat DVR of
between 900 and 1,300 µm/s (89, 135). Deletion of
AQP1 in knockout mice eliminates nearly all volume efflux driven by
hyperosmolar NaCl from fixed DVR, reducing
Pf,wAw by ~50-fold in homozygous animals and
by about twofold in heterozygous animals (Fig. 6B)
(87).
Urea transporters in the DVR wall. The distribution and permeabilities of UTB urea transporters indicate that these proteins may conduct urea through the walls of outer and perhaps inner medullary DVR. Outer medullary DVR express urea transporters, because apparent Purea is high, even in isolated microvessels with low PNa and therefore a poorly permeable shared pathway (90, 97) (Fig. 5A). Also, thiourea, methylurea, phloretin, or pCMBS inhibits the apparent Purea of outer medullary DVR in vitro (Fig. 5B, Table 2) (80, 90, 97). Thiourea at maximal inhibitory concentration (80) reduces the Purea of outer medullary DVR to reveal a strong correlation with PNa attributable to the shared aqueous transmural pathway (80, 97). Inner medullary DVR may lack functional urea transporters, because they show a close correlation between estimated Purea and PNa in vivo, unaffected by thiourea or phloretin, with an intercept near to zero (97). This evidence is not conclusive, because unstirred layers in the renal interstitium might obscure the Purea and PNa of inner medullary DVR in vivo, but this seems unlikely (85, 90, 97). Antibodies to UTB label the continuous endothelium of rat DVR, most strongly in the outer medulla, but not pericytes or the fenestrated endothelium of AVR (47, 131, 148).
Some urea transporters can increase the osmotic permeability of cells, according to swelling or shrinkage experiments (122, 150, 151), although perhaps only at unphysiologically high levels of expression (122). Nevertheless, UTB expressed in Xenopus oocytes apparently has a single channel osmotic permeability approaching that of AQP1, with ultrafiltration and osmotic reflection coefficients for urea of ~0.3 (151). UTB also mediates an appreciable osmotic permeability in erythrocytes, according to data from knockout mice lacking UTB and/or AQP1 (150). The osmotic permeability conferred by UTB is insensitive to mercurials, but inhibited by methylurea (151) or phloretin (150). These reports indicate that UTB might form a shared pathway for water and some small hydrophilic solutes in DVR, but the quantitative importance of such a pathway is unclear. Whether or not water movement through other nonaquaporin membrane proteins (60) contributes to transmural fluxes in DVR is unknown.| |
TRANSPORT OF WATER IN OTHER CONTINUOUS MICROVESSELS |
|---|
GENERAL...
GENERAL...
|
|---|
The shared and exclusive water pathways of DVR apparently resemble those already described in other microvessels with continuous endothelium, although DVR have high Lp values for continuous microvessels (1, 19, 21, 29, 69, 71). Shared aqueous transmural pathways account for the correlation between Lp and Ps to small hydrophilic solutes seen across different microvascular beds, despite large variations in absolute permeabilities. Continuous microvessels sieve small hydrophilic solutes, showing smaller ratios of diffusional permeability to free diffusion coefficient (Ps/D) for tracers of larger molecular radius, indicating greater restriction of diffusion or entry by the shared pathway. Continuous microvessels also sieve macromolecules, displaying high and uniform ultrafiltration or osmotic reflection coefficients, despite wide variations in Lp and Ps to small solutes. The shared pathways in continuous microvessels appear to be extracellular routes through interendothelial clefts containing interrupted strands of tight junction and covered by glycocalyx, which acts principally as a macromolecular filter. The evidence for this comes from quantitative studies of electron-dense tracers, correlations between ultrastructure and permeabilities, and mathematical modeling of pathways. Flow increases diffusional permeabilities in several microvascular preparations, by a mechanism involving nitric oxide synthase in mammalian tissue (20, 71).
Exclusive water pathways seem to mediate <10% of Lp in most continuous microvessels (21, 71). Their existence emerged from comparisons of PD and PNa and from analyses of sieving of small hydrophilic solutes. These exclusive water pathways are probably transcellular, mediated as in DVR by AQP1, which is abundant in continuous microvessels of many tissues (33, 78, 138). Nevertheless, exclusive water pathways might include routes through the tight regions of interendothelial junctions. UTB-mediated transport of urea, and therefore probably of water, seems insignificant in most microvascular beds examined (71), although UTB is widely expressed in vascular endothelium (139).
| |
EQUILIBRATION OF NACL AND UREA ACROSS THE DVR WALL |
|---|
GENERAL...
GENERAL...
|
|---|
As blood flows from the corticomedullary junction toward the papillary tip, rising interstitial concentrations of NaCl and urea are encountered. Those solutes equilibrate with the DVR lumen; however, the lag creates transmural gradients so that interstitial NaCl and urea concentrations exceed their respective concentrations in DVR plasma. Two processes contribute to equilibration. One is diffusion. Diffusive influx of NaCl and urea occurs through an aqueous pathway that provides minimal steric restriction to diffusion or convection of low molecular weight hydrophilic solutes. Diffusive influx of urea also occurs via a transcellular route that employs a facilitated carrier (Fig. 5) (80, 90, 97, 134). Molecular sieving by AQP1 is the second mechanism that concentrates NaCl and urea in the DVR lumen. Driven by transendothelial NaCl and urea gradients, water flows via AQP1 channels from the DVR lumen to the medullary interstitium (76-78, 85, 87, 89, 95) (Fig. 6). The conformation of AQP1 is such that water movement through its central pore excludes NaCl and urea so that transcellular water efflux concentrates NaCl and urea within the DVR lumen.
Quantification of diffusive permeabilities of the DVR wall to NaCl has been achieved by measurement of the rate of efflux of 22Na and [14C]urea from microperfused vessels. Those experiments have been performed both in vivo on the surface of the exposed papilla (Fig. 5A) (67, 75, 83, 85, 96, 97) and in vitro in microperfused DVR isolated from outer medullary vascular bundles (80, 87, 89, 90, 95, 97, 135). A summary of reported permeability measurements is provided in Table 2. Some limitations of the methods employed to obtain the values should be noted. In vivo perfusion can lead to underestimation of permeabilities if the rate of diffusion of the isotopes away from the vessel in the surrounding interstitium is too low. In that case, 22Na or [14C]urea concentrations on the abluminal surface accumulate, violating the assumption of zero abluminal concentration. In vitro perfusion, due to the presence of a continuously flowing bath, is less likely to yield errors from such boundary layer effects, but necessitates the trauma of isolation and exposes the vessel to artificial buffers that could alter transport properties.
As shown in Fig. 7, [3H]raffinose and [14C]inulin permeability of in vitro perfused outer medullary DVR is strongly dependent on perfusion rate (90). Similar behavior is observed when permeability to 22Na is examined. Whether this rate dependence exists in vivo has important implications for the manner in which these vessels equilibrate. For example, if the true NaCl permeability is very low, then abstraction of water across AQP1 might be the dominant mode of NaCl equilibration. As discussed below, that mode of equilibration may reduce blood flow to the deeper regions of the medulla and thereby enhance interstitial osmolality near the papillary tip (87).
Measurement of [14C]urea efflux yields a permeability value that is the sum of transport via the transcellular, carrier-mediated route and other, e.g., pericellular, pathways (80, 90, 97). When the urea carrier in the DVR wall is inhibited by phloretin, pCMBS, or structural urea analogs (thiourea, methylurea), the measured urea permeability falls (Fig. 5B, Table 2) (80, 90). Histochemical evidence and in situ hybridization have identified the DVR urea transporter as the same as that expressed by the RBC-UTB. This carrier is distinct from the vasopressin-stimulated cAMP-responsive transporter of the collecting tubule and the related isoforms found in thin descending limb of Henle (UTA1, UTA2, etc.) (5, 8, 25, 36, 47, 48, 104, 105, 110-112, 131-134, 139, 148-151).
| |
TRANSPORT OF SOLUTES AND WATER ACROSS THE AVR WALL |
|---|
GENERAL...
GENERAL...
|
|---|
Blood ascending toward the cortex in AVR encounters decreasing NaCl and urea concentrations so that the lag in equilibration results in luminal osmolality that exceeds that in the adjacent interstitium. The transmural NaCl and urea gradients generated in vivo are likely to be small. This is because AVR are larger and more numerous than DVR so that the combination of high permeability, large surface area and slower blood flow favors a high degree of equilibrium between AVR plasma and interstitium (35, 39, 67, 91, 155). AVR solute permeability has not been as thoroughly evaluated as that in DVR because AVR have not been isolated and perfused in vitro, owing to technical difficulties. Transport properties have been measured only by the difficult approach of in vivo microperfusion of vessels on the surface of the exposed papilla of rats and hamsters (Table 2) (67, 75, 81, 83). The values so obtained exceed DVR permeabilities but, even so, are probably underestimated. As discussed above, the underestimation is likely because the 22Na and [14C]urea tracers in the perfusate might cross the AVR wall and accumulate in the interstitium to significant levels.
As required for overall mass balance in the medulla, AVR must remove
the water deposited to the interstitium by nephrons, collecting ducts,
and DVR. Transmural oncotic pressure gradients favor water uptake
across the AVR wall and AVR hydraulic conductivity is very high (Table
3) (64, 82, 98, 113, 114). In vivo, transmural gradients
in the AVR generated by the osmotic lag between blood and interstitium
are directed to favor water uptake (luminal concentration > interstitial concentration). For AVR water uptake to be augmented by
those gradients, the AVR wall would have to have nonzero reflection
coefficients to NaCl and/or urea and transmural gradients of those
solutes would need to be of significant magnitude. In the AVR, rigorous
measurements of NaCl and urea reflection coefficients have been
technically impossible to obtain but the general hypothesis that NaCl
might augment transmural volume flux has been tested. In contrast to
similar experiments in DVR (85), in vivo microperfusion of
AVR with buffers made hypertonic or hypotonic to the papillary
interstitium yielded no measurable water flux, a finding that favors
zero reflection coefficients to small hydrophilic solutes
(
SS
0, Equation 3). The variation in the
data from those experiments was large so that low levels of small
solute-driven AVR water transport would not have been readily detected
(83).
| |
TRANSPORT OF UREA AND WATER ACROSS THE PLASMA MEMBRANE OF RED BLOOD CELLS |
|---|
GENERAL...
GENERAL...
|
|---|
In addition to DVR and AVR, red blood cells (RBCs) participate in the medullary recycling of solute and water. The RBC membrane and DVR endothelia express the same transporters for water (AQP1) and urea (UTB) (8, 104, 105, 131-134, 139, 148-151). Thus urea returning from the inner medulla in AVR plasma and RBC cytoplasm has high conductivity transcellular pathways across which it can be returned to the medullary interstitium. Using mathematical simulations, Macey and Yousef (62) concluded that the RBC urea carrier might protect the RBC from osmolar lysis.
| |
TRANSPORT OF LARGE MOLECULES BY THE MEDULLARY MICROCIRCULATION |
|---|
GENERAL...
GENERAL...
|
|---|
It is generally accepted that the renal medulla is devoid of lymphatics (11, 22). As such, the interstitial space must be cleared of large molecules by some other mechanism. Logically, that mechanism must be solvent drag across the AVR wall. Water continuously deposited by loops of Henle, collecting ducts, and DVR must be taken up into AVR (63-65, 86, 141, 153). That water movement will also carry albumin and other large molecules to the AVR wall where they could potentially be carried by convection into the AVR lumen. The related transport issues are complex, because, depending on the "pore" structure of the AVR wall, molecular sieving would tend to limit such permeation and secondarily concentrate macromolecules within the interstitium. Hypothetically, the tendency toward high interstitial oncotic pressure could be offset if deposition of water to the interstitium by nephrons and DVR dilutes macromolecules and raises hydraulic pressure enough to drive water flux across the AVR wall. It has been predicted that a small net transmural driving force would suffice to accommodate mass balance because the AVR wall has a very high hydraulic conductivity (Table 3) (63-65, 70, 81, 82). Commensurate with this notion, AVR tolerate reduction of luminal hydraulic pressure without collapsing (65). With respect to transport of macromolecules, the reflection coefficient of the AVR to albumin has been measured by different methods. Values of 0.59-0.72 and an average of 0.78 were obtained by MacPhee and Michel (64) and Pallone (81), respectively (Table 3). Those nonzero values predict significant sieving of albumin by the AVR wall. Theoretical analysis of macromolecular trafficking has been considered in several studies (64, 86, 141, 153).
| |
INSIGHTS FROM MODELING: THE ROLE OF AQP1 TO ENHANCE EXCHANGER EFFICIENCY |
|---|
GENERAL...
GENERAL...
|
|---|
Mathematical models of the urinary concentration have played an important role in the evolution of our understanding (31, 34, 56, 74, 125-130, 136, 143). The daunting complexity involved in the simulation of both nephrons and the microcirculation has often led investigators to focus on one while neglecting the other. In the case of the vasa recta, there have been many mathematical models of microvascular exchange in the renal medulla. These have been motivated by the desire to simulate countercurrent exchange and account for low oxygen tensions within the medulla (136, 152). The earliest efforts simulated the vasa recta as limbs of a countercurrent exchanger that equilibrates by diffusion either across a simple membrane or via an interposed interstitial space. Those efforts have been previously summarized and will not be reviewed here (91). Instead, we will draw attention to more recent efforts and the insights derived from them.
Most models that focus on vasa recta have specified corticomedullary solute concentration profiles as inputs; however, Wang and Michel (140, 141) recognized that it is more realistic to specify the rate of deposition of NaCl, urea, and water to the medullary interstitium. Mathematically this introduces generation terms into the governing differential equations that account for interstitial mass balance. Their elegant models maintained sufficient simplicity to avoid the need for numerical integration. When shunting of blood flow from DVR to AVR with medullary depth was included as a feature, an exponential increase in corticomedullary solute concentration was predicted, a result that agrees with prior electron probe measurements (50, 140, 142). A weakness of all such models is that they neglect simulation of loops of Henle and collecting ducts (23, 24, 140-142). Solute generation rates in the interstitium are assigned as inputs to the model and interstitial solute concentrations are calculated predictions. Thus variations of transport properties of the microvessels cannot affect the interstitial appearance of NaCl, urea, and water as would occur in vivo. Convincing evidence has been provided that structure and properties of nephrons can abruptly vary with medullary depth (100). The effects of such variation cannot be accounted for by models that focus solely on the microcirculation.
Many of the key parameters needed for a detailed theoretical model to
describe microvascular exchange in the renal medulla (solute
permeabilities, reflection coefficients, hydraulic conductivities) have
been experimentally measured over the last two decades. That information has been combined with anatomic detail and recent insights
concerning transcellular pathways for urea and water transport in DVR
endothelia to enable increasingly realistic simulations by mathematical
modeling. Recent work incorporated a description of AQP1- and
UTB-mediated urea and water transport into an evaluation of
microvascular exchange in the renal medulla by accounting for parallel
pathways for transport of water described above. Following the lead of
Wang and colleagues (140, 142), mass balance equations incorporated the rate of introduction of NaCl, urea, and water into the
medullary interstitium as a function of corticomedullary axis. As a
result, interstitial solute concentrations and the magnitude of
corticomedullary gradients were predicted rather than specified as
inputs (23, 24, 87). Commensurate with the demonstration
that collecting duct urea permeability rises markedly in the inner
medulla (111), the rate of generation of urea was assumed
to rise exponentially toward the papillary tip. The predictions showed
that AQP1 might play an important role to raise medullary interstitial
osmolality by driving water efflux from DVR to the medullary
interstitium across AQP1 water channels, effectively shunting DVR
plasma volume to the AVR and reducing blood flow to deeper regions of
the medulla. The lowering of blood flow favors high exchanger
efficiency in the inner medulla where urea is added to the interstitium
from the collecting duct. It also reduces the volume of fluid to be
concentrated (13, 39). The net effect is optimization of
interstitial osmolality (Fig. 11).
Without AQP1, the model predicts that water influx will occur into DVR
along its length, driven by Starling forces, with reduction of
interstitial osmolality throughout the medulla. Thus the effect of
water channels is to reduce blood flow rate to the inner medulla to
improve solute trapping and interstitial osmolality in that region
(87). Interest in this intriguing prediction is heightened by the observation that transmural water flux can be driven across the
wall of AQP1 null mice by solutes other than NaCl (Fig. 6). If the
non-AQP1 pathway is important in vivo, it might represent another route
through which water is shunted from DVR to AVR in the medulla.
|
| |
SUMMARY AND FUTURE DIRECTIONS FOR RESEARCH |
|---|
GENERAL...
GENERAL...
|
|---|
The primary lesson from recent studies is that the tendency to conceptualize vasa recta as a diffusive U-tube countercurrent exchanger is a misleading oversimplification. In the case of purely diffusive equilibration between lumen and interstitium, countercurrent exchanger efficiency would be enhanced by high permeability, high surface area, and low flow rate. Each of those factors tends to decrease the transmural gradient generated by osmotic lag with the interstitium and therefore the difference in solute concentration between descending and ascending limbs (Fig. 4). If vasa recta were purely diffusive exchangers, the difference in concentration at the corticomedullary junction would govern the overall rate of solute removal from the medulla. Due to high rates of equilibration, it is likely that AVR solute concentrations only slightly exceed those in DVR and that the extent to which AVR blood flow rate exceeds DVR blood flow rate actually serves as the major determinant of overall solute removal.
Expression of the UTB urea transporter results in high DVR urea permeability and minimization of transmural urea gradients. In contrast to transport of urea, the permeability of at least some DVR to NaCl is low (Fig. 5A), favoring equilibration of NaCl by AQP1- mediated water efflux. We conclude from this that a tradeoff has probably evolved to optimize urinary concentrating ability. Relatively low DVR NaCl permeability favors shunting of water from DVR to AVR via AQP1, the purpose of which may be to lower blood flow rate toward the papillary tip. When the net outcome is fully analyzed by mathematical simulation, the prediction is that AQP1-mediated shunting of water could enhance medullary interstitial osmolality (Fig. 11) (87). Stated another way, the continuous shunting of water across AQP1 in DVR, driven primarily by transmural gradients of NaCl, might serve to reduce blood flow, thereby both enhancing equilibration near the papillary tip (where the need to preserve steep corticomedullary gradients is greatest) and reducing the overall flow that needs to be concentrated.
It has been technically feasible to isolate outer medullary DVR (OMDVR) by microdissection from vascular bundles. These vessels have been extensively characterized with respect to their solute and water transport properties and vasoactive characteristics. In contrast, inner medullary DVR (IMDVR) have not been so thoroughly evaluated because they cannot be readily dissected from the rat medulla and subjected to in vitro experimentation. Solute permeabilities of IMDVR measured by in vivo microperfusion may have been underestimated (Table 2). Given the low permeabilities measured in some OMDVR (Fig. 5A) when perfused at slow rates, it seems likely that their properties vary as a function of medullary depth. This might be verified if DVR could be isolated from various medullary locations in a species other than the rat.
Countercurrent exchange in the inner medulla and in vascular bundles of the outer medulla has been best characterized through mathematical models and measurements. Exchange within the interbundle region remains the subject of speculation. There have been no studies of the properties of the interbundle capillary plexus. It stands to reason that a highly interconnected plexus (Fig. 2) could not support efficient countercurrent exchange. Lateral solute gradients extending across the inner stripe from vascular bundles to the interbundle region might exist. There have been no attempts to simulate this feature of medullary microvascular exchange, either alone or as part of a larger model of the concentrating mechanism.
Many other issues remain unresolved. One that has received insufficient attention is the possibility that vasa recta transport properties are regulated to optimize urinary concentration. There is evidence that a reduction of inner medullary blood flow accompanies hydropenia (27, 28, 91, 93, 154); however, the extent to which this is due to vasoconstriction of juxtamedullary resistance vessels or shunting of water from DVR to AVR via AQP1 is unknown. Hypothetically, a reduction of DVR permeability to NaCl in the hydropenic state would favor the latter, but this is untested. The large variation of permeability measurements obtained by in vitro microperfusion implies that subtle differences between animals maintained in different states of hydropenia or volume depletion would be difficult to resolve.
The flow rate dependence of DVR permeability measurements (Fig. 7) raises two possibilities. One is that, owing to artifacts induced by vessel isolation and perfusion, all in vitro measurements of DVR permeability to hydrophilic solutes have been overestimated (80, 87, 90, 95, 97). If DVR NaCl permeability in vivo is, in fact, generally low, then DVR in vascular bundles equilibrate largely by AQP1-mediated water abstraction (NaCl) and UTB-mediated facilitated diffusion (urea). Variation of permeability with in vitro perfusion rate might not be an artifact. Such flow rate dependence of microvessel permeability has been observed in other microvascular beds and is often nitric oxide dependent (20, 71). If flow rate dependence of DVR NaCl permeability exists in vivo, it would imply that reduction of medullary blood flow during hydropenia is accompanied by a shift of DVR NaCl equilibration from diffusion to AQP1-mediated water abstraction. Given the prediction that the latter favors enhancement of interstitial solute concentrations by reducing blood flow (Fig. 11), it is theoretically enticing that enhancement of DVR permeability with perfusion rate is a true physiological effect.
UTB null mice have a mild urinary concentrating defect, a finding that is consistent with a role for UTB to enhance urea trapping and countercurrent exchange (149). It is known that UTA urea transporter splice variants undergo both short- and long-term regulation (8, 110, 133). Evidence that UTB also undergoes long-term regulation is emerging. Upregulation of mRNA for UTB has been identified during gliosis in the central nervous system (12). Within the kidney, lithium-induced diuresis is accompanied by reduced UTB expression in the medulla (48). Interestingly, UTB expression in the renal medulla is downregulated when the vasopressin V2 agonist dDAVP is supplied to vasopressin-deficient Brattleboro rats (104, 105, 132). The latter observation seems counterintuitive, if a role for UTB is to enhance countercurrent exchange and urinary concentration. Functional measurements to confirm variation of DVR urea permeability with antidiuretic state would shed light on this question.
Also, it would be of importance to know whether UTB mediates water efflux across the DVR wall in vivo. When solutes other than NaCl are used to drive water movement, the DVR of AQP1 null mice exhibit a significant osmotic water permeability (Fig. 6), implying that an additional pathway exists. It remains to be tested whether UTB could mediate such small solute driven water movement. Such a hypothesis might be tested using UTB null mice or selective inhibitors of UTB-mediated water transport. Similarly, the reflection coefficient of the non-AQP1 pathway to small solutes should be determined. Even if that pathway conducts water movement in vivo, low reflection coefficients to small solutes would imply that it concentrates the macromolecules but not NaCl or urea in DVR plasma. The existence of an additional solute other than NaCl and urea has been postulated to accumulate in the renal medulla to provide a driving force for urinary concentration (34, 128-130). If such a solute is identified, its ability to drive water flux across the DVR wall of AQP1 null mice should be tested.
AQP1 seems to be constitutively expressed. AQP1 null mice have a severe urinary concentrating defect, reduction of glomerular filtration rate, and general failure to thrive. Those abnormalities are partially restored by gene replacement via an adenovirus (60, 76); however, the importance of AQP1 to provide a dominant pathway that mediates reabsorption of glomerular filtrate in the proximal nephron is more important and probably overshadows the effect of its deletion from DVR. Isolated deletion of AQP1 from DVR or selective replacement of AQP1 into DVR of AQP1 null mice would be needed to resolve that issue. It has been shown that ureteral obstruction is associated with a global reduction of AQP1 expression in the cortex and medulla, an effect that extends to other aquaporins (46). Similarly, gentamicin toxicity is associated with diminished urinary concentration and decreased expression of AQP1 (57). Thus instances of AQP1 downregulation in disease states have been described, but there is little evidence for short- or long-term regulation in nonpathological states.
In addition to transport-related functions, DVR are vasoactive. In vitro, on abluminal exposure to agents such as angiotensin II, endothelins, vasopressin, and norepinephrine, DVR constrict at various foci along their length (84, 92-94, 99, 123). This might modulate corticomedullary gradients in at least two ways. First, an increase in vascular resistance might reduce blood flow to the inner medulla. Second, alteration of permeability to NaCl and urea or reduction of surface area for exchange might occur. If permeability falls during vasoconstriction, exchanger efficiency would be expected to decline, but that effect might be offset because a secondary increase in the magnitude of transmural gradients that drive water efflux across the DVR wall would result. As discussed above, this would favor increased shunting of water from DVR to AVR via AQP1, an effect that has been predicted to reduce blood flow to the deep medulla and enhance interstitial osmolality (87).
Like that of plasma proteins, trafficking of intermediate molecular weight solutes is unexplored but potentially of great interest. Paracrine agents such as angiotensin II, bradykinin, endothelins, and prostaglandins are generated within the medulla. In the presence of a countercurrent exchanger, their release into the interstitium would result in trapping and establishment of a corticomedullary concentration gradient. The concentration of the paracrine hormone present at any level in the medulla is expected to be a complex function of the rate of generation, the rate of degradation, and the permeability of DVR and AVR walls to the solute in question.
Renomedullary interstitial cells are stacked like "rungs of a ladder" and tethered to inner medullary structures. That arrangement might augment concentrating ability by preventing dissipation of axial NaCl and urea gradients within the interstitium (58). Renomedullary interstitial cells are contractile (37) and the possibility that contraction and relaxation of these cells could alter transport properties or vascular resistance cannot be ruled out. Even if they do not modulate transport functions, it is possible that their stacking isolates slitlike regions of interstitium through which the parallel structures present in the inner medulla must exchange (58, 59, 74, 125-127).
Finally, there is a large literature that points to the importance of contractions of the ureter and renal pelvis in the optimization of urinary concentration (15, 18, 22a, 32, 49a, 79, 88, 107, 116, 117). When the ureter is excised to expose the papilla for micropuncture, urinary concentrating ability falls dramatically. Whether this is due to interruption of urea recycling across the pelvic epithelium, hemodynamic effects on inner medullary blood flow, or release of vasoactive agents (18, 32) has not been resolved. When one observes the papilla through the translucent ureter before ureteral excision, blood flow in individual vasa recta seems pulsatile and, on average, much slower than it appears after excision (personal observations). The latter has not been quantified but an increase in inner medullary blood flow after ureteral excision might conceivably contribute to alteration of exchanger efficiency and reduction of concentrating ability.
| |
APPENDIX |
|---|
GENERAL...
GENERAL...
|
|---|
In simplest form, volume flux (Jv) across
a membrane, driven by transmural difference of hydraulic pressure and
osmotic pressure of a single solute (
) is given by
|
(A1) |
d is the osmotic reflection coefficient of
the membrane to the solute. Note that this is a special case of
Equation 3 in which only one solute exerts osmotic pressure.
When Jv is zero, then solute flux
(Js) is given by applying Fick's first law of
diffusion to a membrane (120)
|
(A2) |
is the partition coefficient (the equilibrium
ratio of solute concentration in the membrane to that in bulk
solution), and
x is membrane thickness.
When Jv is more than zero,
Js can be described by (19, 69,
102)
|
(A3) |
|
(A4) |
0 and diffusive flux
dominates, it is readily shown that Js
Ps
C. Conversely, when Pe is very large, so that
convective solute flux (solvent drag) dominates over diffusion,
Js
Jv(1
f)C1.
The volume flux of water (Jw) through a
porous membrane approximates Jv only in the case
of dilute solutions. Jw can be described by
(26)
|
(A5) |
Jv, either because
Js is zero or as an approximation for dilute
solutions, then Pf can be calculated from Lp
(4, 26, 144)
|
(A6) |
| |
ACKNOWLEDGEMENTS |
|---|
We are grateful to Professor C. C. Michel for helpful criticisms. Figure 3 of this article, reproduced from Scientific American, was provided to P. F. Scholander by the late C. Lloyd Claff. We are grateful to Mark Claff and Chester Claff for permission to reproduce it.
| |
FOOTNOTES |
|---|
This work was supported by National Institutes of Health Grants DK-42495, DK-53775, HL-68686, and HL-62220. M. R. Turner is grateful to the British Heart Foundation for research support.
Address for reprint requests and other correspondence: T. L. Pallone, Division of Nephrology, N3W143, Univ. of Maryland at Baltimore, Baltimore, MD 21201-1595 (E-mail: tpallone{at}medicine.umaryland.edu).
The costs of publication of this article were defrayed in part by the payment of page charges. The article must therefore be hereby marked "advertisement" in accordance with 18 U.S.C. Section 1734 solely to indicate this fact.
10.1152/ajpregu.00657.2002
| |
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