Abstract
A new pressure-perfusion technique was used to measure hydraulic and osmotic properties of the outer part of roots (OPR) of 30-day-old rice plants (lowland cultivar: IR64, and upland cultivar: Azucena). The OPR comprised rhizodermis, exodermis, sclerenchyma and one cortical cell layer. The technique involved perfusion of aerenchyma of segments from two different root zones (20–50 mm and 50–100 mm from the tip) at precise rates using aerated nutrient solution. The hydraulic conductivity of the OPR (LpOPR=1.2×10−6 m s−1 MPa−1) was larger by a factor of 30 than the overall hydraulic conductivity (Lpr=4×10−8 m s−1 MPa−1) as measured by pressure chamber and root pressure probe. Low reflection coefficients were obtained for mannitol and NaCl for the OPR (σsOPR=0.14 and 0.09, respectively). The diffusional water permeability (P dOPR) estimated from isobaric flow of heavy water was smaller by three orders of magnitude than the hydraulic conductivity (LpOPR/P fOPR). Although detailed root anatomy showed well-defined Casparian bands and suberin lamellae in the exodermis, the findings strongly indicate a predominantly apoplastic water flow in the OPR. The LpOPR of heat-killed root segments increased by a factor of only 2, which is in line with the conclusion of a dominating apoplastic water flow. The hydraulic resistance of the OPR was not limiting the passage of water across the root cylinder. Estimations of the hydraulic properties of aerenchyma suggested that the endodermis was rate-limiting the water flow, although the aerenchyma may contribute to the overall resistance. The resistance of the aerenchyma was relatively low, because mono-layered cortical septa crossing the aerenchyma ('spokes') short-circuited the air space between the stele and the OPR. Spokes form hydraulic bridges that act like wicks. Low diffusional water permeabilities of the OPR suggest that radial oxygen losses from aerenchyma to medium are also low. It is concluded that in rice roots, water uptake and oxygen retention are optimized in such a way that hydraulic water flow can be kept high in the presence of a low efflux of oxygen which is diffusional in nature.
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Abbreviations
- A r :
-
surface area of root
- C i :
-
osmotic concentration of xylem sap
- C o :
-
osmotic concentration of medium
- δ:
-
unstirred layer
- Δπ:
-
osmotic pressure difference
- ΔP r :
-
change of root pressure
- ΔV s :
-
change of volume
- D s :
-
diffusion coefficient of solutes
- J Vr :
-
water flow
- k rw :
-
rate constant for water
- k sr :
-
rate constant for solutes
- Lp:
-
hydraulic conductivity
- LpAER :
-
hydraulic conductivity of aerenchyma
- LpOPR :
-
hydraulic conductivity of outer part of the root
- Lpr :
-
hydraulic conductivity of the root
- LpSPK :
-
hydraulic conductivity of spokes
- OPR:
-
outer part of roots
- P :
-
steady-state pressure
- P d :
-
diffusional water permeability
- P dOPR :
-
diffusional water permeability of outer part of the root
- P fOPR :
-
hydraulic water permeability of outer part of the root
- P gas :
-
pneumatic pressure
- P ro :
-
original root pressure
- P rmin :
-
minimum root pressure
- P sr :
-
permeability coefficient of solutes
- PTS:
-
trisodium 3-hydroxy-5,8,10-pyrenetrisulfonate
- Q V :
-
pump rate
- σsOPR :
-
reflection coefficient of outer part of root
- σsr :
-
reflection coefficient of root
- T 1/2 s :
-
half-time of solute exchange across roots
- T 1/2 w :
-
half-time of water exchange across roots
- t min :
-
required time for minimum root pressure
- V :
-
exuded volume of the xylem sap
- V w :
-
molar volume of water
- V x :
-
volume of xylem
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Acknowledgments
The authors thank Prof. D.T. Clarkson (University of Bristol, UK), Dr. T.D. Colmer (University of Western Australia, Perth), and Prof. C.A. Peterson (University of Waterloo, Ontario, Canada) for carefully reading and discussing the manuscript. The excellent technical support of Burkhard Stumpf (Lehrstuhl Pflanzenökologie, University of Bayreuth) is gratefully acknowledged. This work was supported by a grant from the Deutsche Forschungsgemeinschaft, Schwerpunktprogramm 'Apoplast' to E.S., and by BMZ project No. 2000.7860.0-001.00 "Trait and Gene Discovery to Stabilize Rice Yields in Drought Prone Environments" (R.L.)
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Ranathunge, K., Steudle, E. & Lafitte, R. Control of water uptake by rice (Oryza sativa L.): role of the outer part of the root. Planta 217, 193–205 (2003). https://doi.org/10.1007/s00425-003-0984-9
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DOI: https://doi.org/10.1007/s00425-003-0984-9