GROWTH AND FUNCTIONING OF ROOTS AND OF ROOT SYSTEMS SUBJECTED TO SOIL COMPACTION - TOWARDS A SYSTEM WITH MULTIPLE SIGNALING

被引:92
作者
TARDIEU, F
机构
[1] INRA, Laboratoire d'Ecophysiologie des Plantes sous Stress Environnementaux, F 34060 Montpellier cedex 1, 2, place Viala
关键词
COMPACTION; ELONGATION RATE; SOIL MECHANICAL IMPEDANCE; WATER FLUX; PLANT GROWTH REGULATOR; STOMATAL CONDUCTANCE;
D O I
10.1016/0167-1987(94)90006-X
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The effect of soil mechanical impedance on root growth is discussed on several levels from the apex to the root system. At the individual root level, the balance of pressures on the root apex cannot account for observed reductions in root elongation rate. Furthermore, soil mechanical impedance affects the elongation rate of non-impeded organs, such as leaves or non-impeded roots. A chemical message originating in roots could account for such an effect, probably via changes in cell wall rheological properties in all growing zones of the plant. Changes in carbon allocation could also have a role. At a whole-plant level, indirect effects linked to changes in the plant structure contribute in a major way to the effect of mechanical impedance on root growth. Although only a small proportion of roots of field-grown plants are in contact with compact soil, geometrical characteristics of root systems are considerably affected. In particular, root deepening is delayed and roots tend to have a clumped spatial arrangement. Experimental evidence and modelling suggest that this change in root system architecture could cause water stress, even in relatively wet soil, because of an increase in resistance to the soil-root water flux. As a consequence, root water status and water flux decrease, and stomatal conductance is reduced as a consequence of a chemical message originating in the roots. This secondary message is superimposed onto the direct message linked to mechanical impedance. Under some climatic conditions, whole-plant growth rate, carbon allocation and phenologic development can then be significantly affected by a compaction in the ploughed layer, while only small changes can be expected under more favourable conditions.
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页码:217 / 243
页数:27
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