Library

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    ISSN: 1432-2013
    Keywords: Renal Microperfusion ; Isotonic Reabsorption ; Tracer Permeability ; Glomerulo Tubular Balance ; Renale Mikroperfusion ; Isotone Resorption ; Tracerpermeabilität ; Glomerulotubuläre Balance
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Summary In the first experimental series proximal convolutions of the rat kidney were perfused with a modified Ringer solution and the isotonic fluid absorption was measured. In a second series the tubule was perfused with equilibrium solution which contained36Cl and the chloride permeability was determined. By the recollection method each individual tubule was perfused twice either at constant luminal diameter but different perfusion rates (10:30 or 6:16 nl/min) or at constant perfusion rates but different luminal diameters (20:30 μ). The perfusate was recollected at two different sites which were at least 500 μ distant from the infusion site. The isotonic fluid absorption as well as the36Cl permeability was unchanged when the tubule was distended from 20–30 μ. Both, however, increased about 20% when the perfusion rate was increased 3-fold. The data led to the following conclusions: 1. It is unlikely that there is a flow reactor type dependence of proximal tubular transport on flow rate. 2. The tubular distension cannot be responsible for the glomerulo-tubular balance. 3. It is more advantageous to relate permeability data of the rat nephron to tubular length. 4. In microperfusion experiments non steady sampling does not affect transepithelial fluxes per unit tubular length, provided that the pump delivery is constant.
    Type of Medium: Electronic Resource
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...