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Effects of elevated atmospheric CO2 and soil water availability on root biomass, root length, and N, P and K uptake by wheat

Published online by Cambridge University Press:  01 March 1997

MARGRET M. I. VAN VUUREN
Affiliation:
Department of Biological Sciences, University of Dundee, Dundee DD1 4HN, UK Cellular and Environmental Physiology Department, Scottish Crop Research Institute, Invergowrie, Dundee DD2 5DA, UK
DAVID ROBINSON
Affiliation:
Cellular and Environmental Physiology Department, Scottish Crop Research Institute, Invergowrie, Dundee DD2 5DA, UK
ALASTAIR H. FITTER
Affiliation:
Department of Biology, University of York, P.O. Box 373, York YO1 5YW, UK
SCOTT D. CHASALOW
Affiliation:
Biomathematics and Statistics Scotland, Scottish Crop Research Institute, Invergowrie, Dundee DD2 5DA, UK
LISA WILLIAMSON
Affiliation:
Department of Biology, University of York, P.O. Box 373, York YO1 5YW, UK
JOHN A. RAVEN
Affiliation:
Department of Biological Sciences, University of Dundee, Dundee DD1 4HN, UK
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Abstract

We investigated interactions between the effects of elevated atmospheric carbon dioxide concentrations ([CO2]) and soil water availability on root biomass, root length and nutrient uptake by spring wheat (Triticum aestivum cv. Tonic). We grew plants at 350 and 700 µmol mol−1 CO2 and with frequent and infrequent watering (‘wet’ and ‘dry’ treatments, respectively). Water use per plant was 1·25 times greater at 350 than at 700 µmol CO2 mol−1, and 1·4 times greater in the ‘wet’ than in the ‘dry’ treatment. Root biomass increased with [CO2] and with watering frequency. Elevated [CO2] changed the vertical distribution of the roots, with a greater stimulation of root growth in the top layers of the soil. These data were confirmed by the video data of root lengths in the ‘dry’ treatment, which showed a delayed root development at depth under elevated [CO2]. The apparent amount of N mineralized appeared to be equal for all treatments. Nutrient uptake was affected by [CO2] and by watering frequency, and there were interactions between these treatments. These interactions were different for N, K and P, which appeared to be related to differences in nutrient availability and mobility in the soil. Moreover, these interactions changed with time as the root system became larger with [CO2] and with watering frequency, and as fluctuations in soil moisture contents increased. Elevated [CO2] affected nutrient uptake in contrasting ways. Potassium uptake appeared to be reduced by the smaller mass flow of water reaching the root surface. However, this might be countered with time by the greater root biomass at elevated [CO2], by the greater soil moisture contents at elevated [CO2], enabling faster diffusion, or both. Phosphorus uptake appeared to be increased by the greater root biomass at elevated [CO2]. We conclude that plant nutrient uptake at elevated [CO2] is affected by interactions with water availability, though differences between nutrients preclude generalizations of the response.

Type
Research Article
Copyright
© Trustees of The New Phytologist 1997

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