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Effects of Restoration Time on Microbial Diversity in Rhizosphere and Non-Rhizosphere Soil of Bothriochloa ischaemum

机译:恢复时间对双川芎根际和非根际土壤微生物多样性的影响

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摘要

There is well-documented evidence that shows phytoremediation and restoration methods affect physical and chemical properties, enzyme activities, and microbial communities of soil. In this study, we investigated the response of soil microbial communities to restoration time. We found that arsenic content decreased gradually as restoration progressed. Total carbon (C) in shoots and total nitrogen (N) in roots of B. ischaemum both exhibited increasing trends with an increase in restoration time. The transfer factor of chromium was negatively correlated to C in shoots and positively correlated to sulfur in roots. Additionally, the transfer factor of lead had a remarkably positive correlation to the C/N ratio of roots. For soil enzymes, total N in soil was positively correlated to catalase and urease but negatively correlated to sucrose. Moreover, bulk soil bacterial composition was positively correlated to catalase, sucrase and phosphatase while fungal diversity was positively correlated to sucrose. This study found that restoration time plays the most significant role in bacterial and fungal composition and bacterial diversity, but it has no effect on fungal diversity in rhizosphere and non-rhizosphere soil. In addition, the driving factors of microbial composition and diversity varied in rhizosphere and non-rhizosphere soil among the different restoration time treatments.
机译:有良好的证据表明植物修复和恢复方法影响物理和化学性质,酶活性和土壤的微生物群落。在这项研究中,我们研究了土壤微生物社区对恢复时间的反应。我们发现砷含量逐渐降低,因为恢复进展。芽中的总碳(c)和B. keoots的缺血(n)中的总氮(n)都表现出增加趋势,随着恢复时间的增加。铬的转移因子与芽中的C负相关,并与根中的硫相关联。另外,铅的转移因子与根的C / N比具有显着的正相关。对于土壤酶,土壤中的总N与过氧化氢酶和脲酶呈正相关,但与蔗糖负相关。此外,散装土壤细菌组合物与过氧化氢酶,蔗糖酶和磷酸酶正相关,而真菌多样性与蔗糖呈正相关。本研究发现,恢复时间在细菌和真菌组合物和细菌多样性中起最大的作用,但它对根际和非根际土壤的真菌多样性没有影响。此外,不同恢复时间治疗中的根际和非根际土壤中微生物组成和多样性的驱动因素。

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