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Stimulated activity of the soil nitrifying community accelerates community adaptation to Zn stress

机译:土壤硝化群落的刺激活动加速了群落对锌胁迫的适应

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Field data have shown that soil nitrifying communities gradually adapt to zinc (Zn) after a single contamination event with reported adaptation times exceeding 1 year. It was hypothesized that this relatively slow adaptation relates to the restricted microbial diversity and low growth rate of the soil nitrifying community. This hypothesis was tested experimentally by recording adaptation rates under varying nitrification activities (assumed to affect growth rates) and by monitoring shifts in community composition. Soils were spiked at various Zn concentrations (04000 mg Zn kg1) and two NH4+N doses (N1, N2) were applied to stimulate growth. A control series receiving no extra NH4+N was also included. Soils were incubated in pots under field conditions with free drainage. The pore water Zn concentration at which nitrification was halved (EC50, mg Zn l1) did not change significantly during 12 months in the control series (without NH4+N applications), although nitrification recovered after 12 months at the highest Zn dose only. The EC50 after 12 months incubation increased by more than a factor 10 with increasing NH4+N dose (p < 0.05) illustrating that increased activity accelerates adaptation to Zn. Zinc tolerance tests confirmed the role of Zn exposure, time and NH4+N dose on adaptation. Zinc tolerance development was ascribed to the AOB community since the AOB/AOA ratio (AOB = ammonia oxidizing bacteria; AOA = ammonia oxidizing archaea) increased from 0.4 in the control to 1.4 in the most tolerant community. Moreover, the AOB amoA DGGE profile changed during Zn adaptation whereas the AOA amoA DGGE profile remained unaffected. These data confirm the slow but pronounced adaptation of nitrifiers to Zn contamination. We showed that adaptation to Zn was accelerated at higher activity and was associated with a shift in soil AOB community that gradually dominated the nitrifying community.
机译:现场数据表明,在一次污染事件发生后,土壤硝化群落逐渐适应锌(Zn),据报道适应时间超过一年。据推测,这种相对较慢的适应性与土壤硝化群落的受限微生物多样性和低生长速率有关。通过记录各种硝化作用下的适应率(假设影响生长率)并监测社区组成的变化,对这一假设进行了实验性检验。在各种锌浓度(04000 mg Zn kg1)下掺加土壤,并施用两次NH4 + N剂量(N1,N2)刺激生长。还包括不接收额外NH 4 + N的对照系列。将土壤在田间条件下的盆中自由排水下孵育。对照系列(未使用NH4 + N)中,硝化作用减半的孔隙水Zn浓度(EC50,mg Zn l1)在12个月内没有显着变化,尽管仅在最高Zn剂量下12个月后硝化作用得以恢复。孵育12个月后,随着NH4 + N剂量的增加,EC50增加了10倍以上(p <0.05),这说明活性增加加速了对Zn的适应性。锌耐受性测试证实了锌暴露,时间和NH4 + N剂量对适应的作用。锌耐受性的提高归因于AOB群落,因为AOB / AOA比率(AOB =氨氧化细菌; AOA =氨氧化古细菌)从对照的0.4增加到最耐受的群落的1.4。此外,在锌适应过程中,AOB amoA DGGE谱发生了变化,而AOA amoA DGGE谱未受到影响。这些数据证实硝化剂缓慢但明显地适应锌污染。我们表明,对锌的适应在较高的活性下会加速,并且与土壤AOB群落的变化有关,而土壤AOB群落的变化逐渐主导了硝化群落。

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