Abstract: A greenhouse experiment was carried out to compare differences in
potential activities of ammonification, nitrification and denitrification in
rhizosphere and bulk soil in a heavy-metal-stressed system. Exchangeable
fractions of Cd, Cu and Cr were all higher in the rhizosphere of maize than in
bulk soil. Results showed that the mineralization of N in soil was stimulated
by low concentration of Cd. Addition of Cd at low levels stimulated the
ammonifying and nitrifying activity in soil, while inhibitory influences were
shown at high levels. Nitrifying bacteria was proved to be the most sensitive
one, whilst the effect on denitrifying bacteria was very limited. Comparing Cd,
Cu and Cr(VI) at 20 mg/kg soil, Cd was the most effective inhibitor
of ammonification and denitrification, while Cr(VI) had the strongest
inhibitory influence on nitrifying activity. Root exudates played important
roles on the different exchangeable metal fractions and bacterial activities
between rhizosphere and non-rhizosphere. Nitrate was the main form of mineral N
in soil, as well as the main form of N absorbed by plants, but the formation
and relative absorption of ammonium were promoted in response to high Cd
exposure.
Keywords: heavy metal, nitrogen cycle, rhizosphere, root exudates