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首页> 外文期刊>European Journal of Soil Biology >Abundance and community structure of ammonia-oxidizing bacteria and archaea in purple soil under long-term fertilization.
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Abundance and community structure of ammonia-oxidizing bacteria and archaea in purple soil under long-term fertilization.

机译:长期施肥下紫色土壤氨氧化细菌和古细菌的丰度和群落结构。

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Ammonia-oxidizing microorganisms, which drive the first and rate-limiting step in the process of nitrification, play an important role in soil N-cycling processes. However, little is known about the ammonia-oxidizing bacteria (AOB) and archaea (AOA) in purple soils, which are characterized as lithologic soils without distinct pedogenic horizons and are mainly distributed in the Sichuan basin of Southwestern China. Here, the abundance and community structure of AOB and AOA in a 21-year fertilization experiment were investigated by real-time PCR and terminal restriction fragment-length polymorphism (T-RFLP), respectively. In the present study, nine different fertilization treatments were examined: NPK fertilization plus pig manure (NPK+M), NPK fertilization (NPK), without fertilization (CK), pig manure fertilization (M), P with NH4Cl and KCl plus pig manure (Cl+M), PK fertilization (PK), NK fertilization (NK), NP fertilization (NP), and N fertilization (N). Our results indicate that N-fertilized treatments have higher AOB abundances than the control (CK) and treatments without N amendment. The lowest AOA abundance and AOA/AOB ratios were observed in the treatment (Cl+M) with long-term application of NH4Cl plus KCl. The AOB community structure under combined addition of N and P differed from that under other treatments. The Cl+M treatment had a distinct AOA community structure and higher diversity compared with other treatments. Moreover, higher potential nitrification rates (PNR) were found in the combined N and P addition treatment groups than that in the other treatment groups, and the lowest PNR and pH (<6) were detected in the Cl+M treatment. These results highlight that not only nitrogen but also phosphorus may be a crucial factor affecting soil ammonia-oxidizing activity and triggering changes of AOB community composition. Moreover, soil pH might have an essential role in controlling the AOA community structure and ammonia-oxidizing activity in purple soil.
机译:在硝化过程中驱动第一步和限速步骤的氨氧化微生物在土壤氮循环过程中起着重要作用。然而,对于紫色土壤中的氨氧化细菌(AOB)和古生菌(AOA)知之甚少,这些土壤的特征是没有明显成岩作用层的岩性土壤,主要分布在中国西南部的四川盆地。在这里,分别通过实时PCR和末端限制性片段长度多态性(T-RFLP)研究了21年的施肥实验中AOB和AOA的丰度和群落结构。在本研究中,研究了9种不同的施肥方法:NPK施肥加猪粪(NPK + M),NPK施肥(NPK),不施肥(CK),猪粪施肥(M),NH 4 Cl和KCl加猪粪(Cl + M),PK肥(PK),NK肥(NK),NP肥(NP)和N肥(N)。我们的结果表明,与对照(CK)和未经N修饰的处理相比,N结合的处理具有更高的AOB丰度。长期施用NH 4 Cl + KCl处理(Cl + M)时,AOA丰度和AOA / AOB比最低。氮和磷联合添加下的AOB群落结构与其他处理下的不同。与其他处理相比,Cl + M处理具有独特的AOA群落结构和更高的多样性。此外,在氮和磷联合添加处理组中发现的潜在硝化速率(PNR)比其他处理组更高,并且在Cl + M处理中检测到最低的PNR和pH(<6)。这些结果表明,不仅氮,而且磷可能是影响土壤氨氧化活性并触发AOB群落组成变化的关键因素。此外,土壤pH可能在控制紫色土壤中的AOA群落结构和氨氧化活性方面起着至关重要的作用。

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