The rhizosphere and hyphosphere differ in their impacts on carbon and nitrogen cycling in forests exposed to elevated CO₂.
about
Microbial control of soil organic matter mineralization responses to labile carbon in subarctic climate change treatments.Desiccation of sediments affects assimilate transport within aquatic plants and carbon transfer to microorganisms.Forest Soil Bacteria: Diversity, Involvement in Ecosystem Processes, and Response to Global Change.Impact of treated wastewater on growth, respiration and hydraulic conductivity of citrus root systems in light and heavy soils.Feedbacks between plant N demand and rhizosphere priming depend on type of mycorrhizal association.The mycorrhizal type governs root exudation and nitrogen uptake of temperate tree species.Changes in root architecture under elevated concentrations of CO₂ and nitrogen reflect alternate soil exploration strategies.
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The rhizosphere and hyphosphere differ in their impacts on carbon and nitrogen cycling in forests exposed to elevated CO₂.
description
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The rhizosphere and hyphospher ...... rests exposed to elevated CO₂.
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The rhizosphere and hyphospher ...... rests exposed to elevated CO₂.
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type
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The rhizosphere and hyphospher ...... rests exposed to elevated CO₂.
@en
The rhizosphere and hyphospher ...... rests exposed to elevated CO₂.
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The rhizosphere and hyphospher ...... rests exposed to elevated CO₂.
@en
The rhizosphere and hyphospher ...... rests exposed to elevated CO₂.
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The rhizosphere and hyphospher ...... rests exposed to elevated CO₂.
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Edward R Brzostek
M Luke McCormack
Richard P Phillips
Seth G Pritchard
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P304
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10.1111/NPH.13122
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P50
P577
2014-10-28T00:00:00Z