Alain Mollier

A knowledge of plant interactions above and below ground with respect to water is essential to understand the performance of intercrop systems. In this study, a physically based framework is proposed to analyse the competition for soil water in the case of intercropped plants. A radiative transfer model, associated with a transpiration-partitioning model based on a modified form of the Penman-Monteith equation, was used to estimate the evaporative demand of maize (Zea mays L.) and sorghum ( Sorghum vulgare R.) intercrops. In order to model soil–root water transport, the root water potential of each species was calculated so as to minimise the difference between the evaporative demand and the amount of water taken up by each species. A characterisation of the micrometeorological conditions (net radiation, photosynthetically active radiation, air temperature and humidity, rain), plant water relations (leaf area index, leaf water potential, stomatal conductance, sap flow measurements), as well as the two-component root systems and water balance (soil–root impacts, soil evaporation) was carried out during a 7-day experiment with densities of about 4.2 plant m-2 for both maize and sorghum. Comparison of the measured and calculated transpiration values shows that the slopes of the measured versus predicted regression lines for hourly transpiration were 0.823 and 0.778 for maize and sorghum, respectively. Overall trends in the variation of volumetric water content profiles are also reasonably well described. This model could be useful for analysing competition where several root systems are present under various environmental conditions.

In simulation models for water movement and nutrient transport, uptake of water and nutrients by roots forms an essential part. As roots are spatially distributed, prediction of root growth and root distribution is crucial for modelling water and nutrient uptake. In a preceding paper, De Willigen et al. (2002; Plant and Soil 240, 225–234) presented an analytical solution for describing root length density distribution as a diffusion-type process. In the current paper, we present a numerical model that does the same, but which is more flexible with respect to where root input can occur. We show that the diffusion-type root growth model can describe well observed rooting patterns. We used rooting patterns for different types of crops: maize, gladiolus, eastern white cedar, and tomato. For maize, we used data for two different types of fertiliser application: broadcast and row application. In case of row application, roots extend more vertically than horizontally with respect to the broadcast application situation. This is reflected in a larger ratio of diffusion coefficients in vertical versus horizontal direction. For tomato, we considered tomatoes grown on an artificial rooting medium, i.e. rockwool. We have shown that, in principle, the model can be extended by including reduction functions on the diffusion coefficient in order to account for environmental conditions.

For functioning of a root system, the temporal development of distribution of roots in the soil is important. For example, for computing uptake of water and nutrients the root length density distribution might be required. A way to describe root proliferation is to consider it as a diffusion process with a first-order sink term accounting for decay. In this paper, analytical solutions are derived for two-dimensional diffusion of roots both in a rectangular area, and in a cylindrical volume. The source of root dry matter is located at the surface. Root dry matter enters the soil domain through a part of the soil surface. It is shown that different distribution patterns are obtained, with different ratios of the diffusion coefficients in horizontal and vertical direction. From the solutions obtained it can be shown that for the situation where the dry matter enters through the complete surface eventually a steady-state occurs where root length density decreases exponentially with depth, as often is found in experiments.

A knowledge of above and below ground plant interactions for water is essential to understand the performance of intercropped systems. In this work, root water potential dynamics and water uptake partitioning were compared between single crops and intercrops, using a simulation model. Four root maps having 498, 364, 431 and 431 soil-root contacts were used. In the first and second cases, single crops with ‘deep’ and ‘surface’ roots were considered, whereas in the third and fourth cases, roots of two mixed crops were simultaneously considered with different row spacing (40 cm and 60 cm). Two soils corresponding to a clay and a silty clay loam were used in the calculations. A total maximum evapotranspiration of 6 mm d-1 for both single or mixed crops was considered, for the mixed crops however, two transpiration distributions between the crops were analyzed (3:3 mm d-1, or 4:2 mm d-1 for each crop, respectively). The model was based on a previous theoretical framework applied to singl...

The aim of this study is to analyze the effects of early growth behaviors under conditions of P deficiency on further performances at the end of the vegetative phase of different Zea mays L. genotypes. The effects of soil P availability on biomass and P allocation during early growth and its effects on further performances were investigated on six maize genotypes which were chosen for their growth and development traits in response to P availability. Plants were grown under two contrasting P supplies and collected at 393°Cd and 780°Cd after emergence. Shoot and root growth, root:shoot allometric indicators and efficiencies related to P uptake and utilization, carbon (C) assimilation and allocation were determined. The results showed that the behavior of the six–leave-stage plants was a determining indicator of plant performance at the pre-anthesis phase. Total dry weight of the different maize genotypes ranged from 8.3 to 19.2 g/plant under low P supply at 780°Cd. At 393°Cd, extreme...