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The soil root zone, especially the rhizosphere, is the active zone of microbial and root activity (Lagos et al. 2015).
Vegetation type, landscape position, and site history can influence soil properties and therefore drive the microbial and root production of soil CO2.
In soils, water saturation and microbial and root respiration limit available O2 as a terminal electron acceptor.
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Carbon dioxide measurements from soil surface may indicate the potential for soil respiration and carbon consumption according to microbial biomass and root activity.
SSCE was used as an indicator of ecological processes as it integrates microbial decomposition and root respiration [ 31].
Such a different response of arable and forest soils to the repeated freezing-thawing events is governed by the differences in substrate availability, the size of microbial pool and root mass in soils.
However, knowledge of the relationship between rhizosphere microbial community and root-rot disease is limited.
Furthermore, because pristine CNTs are lipophilic, there is concern that they might be taken up by microbial communities and roots (Oberdörster et al. 2006) and, consequently, accumulate in plant tissues.
Moreover, the main microbial groups present in the product were characterized and the microbial profile of sand and root samples was investigated by PCR-DGGE.
Moreover, to minimize microbial nitrification, a highly concentrated toxic NH4 + solution was used to create a stable persisting NH4 +- depot in which microbial-growth, root growth, and root N uptake is initially limited to the outer boarder areas with less toxic NH4 + levels [26].
Although these traits differentially impact the release of 20 to 80% of total photosynthates as root exudates, their role in influencing microbial communities in the rhizosphere and root environments is not clear.
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