. Concentration of solutes in the renal inner medulla: interstitial hyaluronan as a mechano-osmotic transducer. Am J Physiol Renal Physiol 284: F433-F446, 2003; 10.1152/ajprenal.00067.2002Although the concentrating process in the renal outer medulla is well understood, the concentrating mechanism in the renal inner medulla remains an enigma. The purposes of this review are fourfold. 1) We summarize a theoretical basis for classifying all possible steady-state inner medullary countercurrent concentrating mechanisms based on mass balance principles. 2) We review the major hypotheses that have been proposed to explain the axial osmolality gradient in the interstitium of the renal inner medulla. 3) We summarize and expand on the SchmidtNielsen hypothesis that the contractions of the renal pelvocalyceal wall may provide an important energy source for concentration in the inner medulla. 4) We discuss the special properties of hyaluronan, a glycosaminoglycan that is the chief component of a gel-like renal inner medullary interstitial matrix, which may allow it to function as a mechanoosmotic transducer, converting energy from the contractions of the pelvic wall to an axial osmolality gradient in the medulla. These considerations set the stage for renewed experimental investigation of the urinary concentrating process and a new generation of mathematical models of the renal concentrating mechanism, which treat the inner medullary interstitium as a viscoelastic system rather than a purely hydraulic system. glycosaminoglycans; renal pelvis; vasopressin; hyaluronan IN STATES OF FLUID DEPRIVATION or nonrenal water loss, the kidney can conserve water while maintaining excretion of solutes. It does this by concentrating the solutes in the urine to osmolalities that markedly exceed the osmolality of plasma. A large number of studies, exemplified by the data shown in Fig. 1, have demonstrated that the urinary concentrating process is associated with the generation of a corticomedullary osmolality gradient in the medullary tissue, oriented with the maximum osmolality in the deepest part of the inner medulla, i.e., at the papillary tip. The classic micropuncture studies of Gottschalk and Mylle (17) have established that the medullary hypertonicity is due to solute accumulation in all structures in the medulla, including loops of Henle, vasculature, and collecting ducts. The high medullary interstitial osmolality provides a driving force for osmotic water flow across the collecting ducts, which are rendered permeable to water through the action of vasopressin (33). The high water permeability allows osmotic equilibration of urine with the medullary interstitial fluid.In 1959, Kuhn and Ramel (43) proposed a model to explain concentration of solutes in the renal medulla Address for reprint requests and other correspondence: M. A. Knepper,