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Hence, in order to predict the net mineralization of nitrogen in animal manures, transformation of nitrogen from organic into inorganic form and immobilization processes need to be understood.
Transformation of nitrogen (N) from different manure sources to available forms to promote food security in context of rising climate change is vital.
Overall, the transformation of nitrogen was low, and the total maximum conversion (<20%) occurred at basic conditions.
Through mass-balance analysis, it was found that CANON (Completely Autotrophic Nitrogen-removal Over Nitrite) was responsible for the transformation of nitrogen into gaseous form, thereby causing the loss of nitrogen mass.
Subsequent thermal annealing of the resultant HTGO introduces a gradual transformation of nitrogen bonding configurations in graphene sheets from amine N to pyridinic and graphitic N with the increase of annealing temperature.
As far as the optimal design, operation, and field application of the Aerobic Anaerobic Landfill Method (AALM) are concerned, it is very important to understand how aeration modes (different combinations of aeration depth and air injection rate) affect the biodegradation of organic carbon and the transformation of nitrogen in landfill solid waste.
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The hydrological conditions encountered are likely to exert large and variable influences on the transport and transformations of nitrogen in this part of the landscape.
However, several forms of N are also pollutants, so soil microbial transformations of nitrogen also affect human and environmental health, sometimes far away from the microbes that performed the transformation.
Pennino et al. (2016) examined the transformations of nitrogen derived from a wastewater treatment facility, based on the nitrogen mass balance and the δ15N and oxygen stable isotope ratios (δ18O) in the tidal Potomac River estuary from Washington, D.C., to the Chesapeake Bay.
Because we are interested in microbial transformations of nitrogen in the CRCM, the majority (1638, 73.6%) of probes corresponded to genes involved in nitrogen metabolism.
The key results described above were consistent across an ensemble of 10 simulations that had different randomly generated phytoplankton communities, and in simulations using different parameter values for the mutation rate, and some biogeochemical transformations of nitrogen (see Text S1).
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