Due
to biochar’s excellent physical and chemical properties,
such as rich void ration and large specific surface area, it could
improve soil by conserving water and fertilizer and providing breeding
grounds for soil microorganisms. Therefore, it has been attracting
researchers’ interests for its potential as a soil amendment.
In this work, elemental analysis-stable isotope ratio mass spectrometry
(EA-IRMS) and X-ray photoelectron spectroscopy (XPS) were conjointly
employed to investigate the migration and transformation mechanism
of biochar nitrogenous compounds in the “preparation–returning”
process. EA-IRMS data indicated that during the preparation process
the nitrogen retention rate in biochar first dropped sharply (300–400
°C), then became stable (400–500 °C), and finally
decreased slowly (500–800 °C) with increasing pyrolysis
temperature. After returning biochar to soil, the measurable total
nitrogen in biochar that migrated to soil and plants displayed a nitrogen
mass distribution rate in the order of biochar after returning (88.40–90.42%)
> soil (8.81–10.07%) > plants (0.77–1.53%). In
addition,
the pyrolysis temperature was negatively related to the nitrogen mass
distribution rate in biochar, soil, and wheat. On the other hand,
the pyrolysis atmosphere had little effect on the nitrogen retention
rate in biochar before returning and the nitrogen mass distribution
rate in biochar after returning to the field. XPS results suggested
that alkaloid-N, free amino acid-N, protein-N, and NH4
+-N in wheat straw were gradually transformed into pyridine-N,
amino-N, pyrrole-N, quaternary-N, NH4
+-N, NO2
–-N, and NO3
–-N in biochar during the biomass pyrolysis process. Biochar produced
at 300 °C was in a transition stage that included all nitrogenous
compounds present in wheat straw as well as biochar produced at the
lower temperatures (≤500 °C). At higher temperatures,
inorganic nitrogen species were more abundant and displayed higher
contents. For pyrolysis temperatures ≤500 °C, biochars
prepared under both N2 and CO2 atmospheres comprised
similar nitrogenous compounds and contents. Moreover, the changes
in nitrogenous compounds and nitrogen release patterns during the
process of returning biochar to the field were not significantly different.