1941
DOI: 10.1002/j.1537-2197.1941.tb07987.x
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Control of Water Transport in Local Root Regions of Attached and Isolated Roots by Means of the Osmotic Pressure of the External Solution

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Cited by 35 publications
(4 citation statements)
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References 11 publications
(12 reference statements)
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“…Transpiration is a rough measure of water absorption and its reduction by 50% indicates that salinity reduces the transpiration rate. For other plant species, water uptake has been reported to stop at much lower salt concentration levels (Rosene, 1941).…”
Section: Effect Of Naci Concentration On Water Absorptionmentioning
confidence: 99%
“…Transpiration is a rough measure of water absorption and its reduction by 50% indicates that salinity reduces the transpiration rate. For other plant species, water uptake has been reported to stop at much lower salt concentration levels (Rosene, 1941).…”
Section: Effect Of Naci Concentration On Water Absorptionmentioning
confidence: 99%
“…Effects of axial polarity and axial differentiation of roots arose in experiments with excised segments from roots. Exudation from root segments without a root apex and with xylem vessels cut at both ends was demonstrated for onion roots in a saturated atmosphere with several potometers attached along the roots [10,11]. The 25 mm long onion root segments absorbed water from three attached potometers along the axis and then exuded at the basal end (distal to the original apex), while the direction of fluid flow (uptake or efflux) at the apical end depended on the length of removed apical tissue (Figure 4A).…”
Section: Exudation Of Root Segments Without Root Apex and Stem Exudationmentioning
confidence: 99%
“…There was good evidence that intact and excised roots of corresponding age and length showed similar behavior with respect to absolute rates and axial gradients of water uptake (Rosene, 1941a). Rosene (1941b) determined the driving force for water uptake by applying osmotic solutions to different root zones at concentrations just sufficient to stop the water flow. Taking into account a reflection coefficient of about 0.65 for the solute used (KNO,; our unpublished result), the driving force in the absorption experiment could be calculated to be about 0.4 MPa.…”
Section: Lprmentioning
confidence: 99%
“…However, it is doubtful whether RH really was 100% as stated by Rosene (1941b), so that even at near water saturation, transpiration (pressure)-driven water uptake could have substantially contributed to total water absorption. Therefore, the driving force in the experiments of Rosene (1937) may have been a mixed hydrostatic and osmotic gradient and the absolute value of Lp, would be, thus, understandable.…”
Section: Lprmentioning
confidence: 99%