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Titlebook: Belowground Responses to Rising Atmospheric CO2: Implications for Plants, Soil Biota, and Ecosystem ; Proceedings of a wor Peter S. Curtis,

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https://doi.org/10.1007/978-3-031-57804-5 root responses as a component of the overall response of the terrestrial biosphere to increasing atmospheric CO. are suggested: (1) roots as a platform for nutrient acquisition and a mediator of whole-plant response to CO.; (2) carbon storage in roots as a component of whole-plant carbon storage; a
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Worker Resistance — Historical Development stage (1990 only); the positive effects of extra CO. were more evident at interrow positions (0.25 and 0.5 m). A CO. × depth × position interaction at the vegetative phase (1990) indicated that FACE increased root dry weight densities for the top soil depth increment at all positions and at the mid
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Management — Preliminary Argument completion of N addition. Following the N addition, leaf N content increased in both CO. treatments, but net assimilation showed a sustained increase only in elevated CO. grown plants. Root relative extension rate was greater at elevated CO., both before and after the N addition. Although final roo
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Management — Preliminary Argumentannual precipitation decreased colonization in both species. Simulated climate change conditions of elevated CO., elevated temperature and lowered precipitation decreased colonization in . but had less effect on .. After four growth cycles in ., trends of treatments remained similar, but overall col
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https://doi.org/10.1007/978-1-349-26361-5s stress decreased root starch concentrations, increased root sugar concentrations and did not significantly affect TNC concentrations. However, despite significant effects on root carbohydrate levels, there were generally no significant treatment effects on mycorrhizal colonization. Additionally, a
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Industry, Innovation and Infrastructureaf litter. However, there was a large difference in characteristics of leaf litter decomposition among the species. . leaf litter had a different initial chemistry and decayed more rapidly than C. grasses. We conclude that an indirect effect of CO. on decomposition and nutrient cycling could occur i
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https://doi.org/10.1007/978-3-319-95873-6ited greater leaf water potentials and higher plant water use efficiencies. Plant N uptake was reduced by CO. enrichment, while P uptake appeared little influenced by CO. regime. Under the conditions of the experiment, CO. enrichment increased root biomass and VAM infection via stimulated growth and
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