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Microbial activity related to N cycling in the rhizosphere of maize stressed by heavy metals

机译:重金属胁迫下玉米根际氮循环的微生物活性

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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 ali 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.
机译:进行了温室试验,以比较重金属胁迫系统中根际和散装土壤中氨化,硝化和反硝化的潜在活性差异。玉米根际中Cd,Cu和Cr的可交换部分比散装土壤中的高。结果表明,低浓度的镉会刺激土壤中氮的矿化。低水平添加镉刺激土壤中的氨化和硝化活性,而高水平显示抑制作用。硝化细菌被证明是最敏感的细菌,而反硝化细菌的作用非常有限。与20 mg / kg土壤中的Cd,Cu和Cr(VI)相比,Cd是最有效的氨化和反硝化抑制剂,而Cr(VI)对硝化活性的抑制作用最强。根系分泌物在根际和非根际之间不同的可交换金属组分和细菌活性中起着重要作用。硝酸盐是土壤中矿质氮的主要形式,也是植物吸收氮的主要形式,但由于高Cd暴露,促进了铵的形成和相对吸收。

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