Sd. Wullschleger et al., MODELING THE BELOWGROUND RESPONSE OF PLANTS AND SOIL BIOTA TO EDAPHICAND CLIMATIC-CHANGE - WHAT CAN WE EXPECT TO GAIN, Plant and soil, 165(1), 1994, pp. 149-160
As atmospheric CO2 concentrations continue to increase, so too will th
e emphasis placed on understanding the belowground response of plants
to edaphic and climatic change. Controlled-exposure studies that addre
ss the significance of an increased supply of carbon to roots and soil
biota, and the consequences of this to nutrient cycling will play a p
rominent role in this process. Models will also contribute to understa
nding the response of plants and ecosystems to changes in the earth's
climate by incorporating experimental results into conceptual or quant
itative frameworks from which potential feedbacks within the plant-soi
l system can be identified. Here we present five examples of how model
s can be used in this analysis and how they can contribute to the deve
lopment of new hypotheses in the areas of root biology, soil biota, an
d ecosystem processes. Two examples illustrate the role of coarse and
fine roots in nitrogen and phosphorus uptake from soils, the respirato
ry costs associated with this acquisition of nutrients, and the signif
icance of root architecture in these relationships. Another example fo
cuses on a conceptual model that has helped raise new ideas about the
effects of elevated CO2 on root and microbial biomass, and on nutrient
dynamics in the rhizosphere. Difficulties associated with modeling th
e contribution of mycorrhizal fungi to whole-plant growth are also dis
cussed. Finally several broad-scale models are used to illustrate the
importance of root turnover, litter decomposition, and nitrogen minera
lization in determining an ecosystem's response to atmospheric CO2 enr
ichment. We conclude that models are appropriate tools for use both in
guiding existing studies and in identifying new hypotheses for future
research. Development of models that address the complexities of belo
wground processes and their role in determining plant and ecosystem fu
nction within the context of rising CO2 concentrations and associated
climate change should be encouraged.