首页> 美国卫生研究院文献>other >Bacterial and fungal communities respond differently to varying tillage depth in agricultural soils
【2h】

Bacterial and fungal communities respond differently to varying tillage depth in agricultural soils

机译:细菌和真菌群落对农业土壤中不同耕作深度的反应不同

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

In arable cropping systems, reduced or conservation tillage practices are linked with improved soil quality, C retention and higher microbial biomass, but most long-term studies rarely focus on depths greater than 15 cm nor allow comparison of microbial community responses to agricultural practices. We investigated microbial community structure in a long-term field trial (12-years, Lincoln, New Zealand) established in a silt-loam soil over four depth ranges down to 30 cm. Our objectives were to investigate the degree of homogenisation of soil biological and chemical properties with depth, and to determine the main drivers of microbial community response to tillage. We hypothesised that soil microbiological responses would depend on tillage depth, observed by a homogenisation of microbial community composition within the tilled zone. Tillage treatments were mouldboard plough and disc harrow, impacting soil to ∼20 and ∼10 cm depth, respectively. These treatments were compared to a no-tillage treatment and two control treatments, both permanent pasture and permanent fallow. Bacterial and fungal communities collected from the site were not impacted by the spatial location of sampling across the study area but were affected by physicochemical changes associated with tillage induced soil homogenisation and plant presence. Tillage treatment effects on both species richness and composition were more evident for bacterial communities than fungal communities, and were greater at depths <15 cm. Homogenisation of soil and changing land management appears to redistribute both microbiota and nutrients deeper in the soil profile while consequences for soil biogeochemical functioning remain poorly understood.
机译:在耕作制度中,减少耕种或进行保护性耕作与改善土壤质量,保持碳和增加微生物的生物量有关,但大多数长期研究很少关注大于15厘米的深度,也无法比较微生物群落对农业作法的反应。在一项长期的田间试验(12年,新西兰林肯)中,我们研究了微生物群落结构,该试验建立在深至30厘米的四个深度范围内的粉壤土上。我们的目标是调查土壤生物学和化学特性随深度的均匀化程度,并确定微生物群落对耕作反应的主要驱动力。我们假设土壤微生物反应将取决于耕种深度,通过耕种区内微生物群落组成的均质化可以观察到。耕作方法是用犁板犁和圆盘耙,分别冲击土壤至20厘米和10厘米深。将这些处理与免耕处理和两种对照处理(永久牧场和永久休耕)进行了比较。从该地点收集的细菌和真菌群落不受研究区域内采样空间位置的影响,但受到与耕作诱导的土壤均质化和植物存在相关的理化变化的影响。对于真菌群落而言,耕作处理对物种丰富度和成分的影响比真菌群落更为明显,并且在<15 cm的深度处更大。土壤的均质化和土地管理的变化似乎在土壤剖面中更深处重新分配了微生物群和养分,而对土壤生物地球化学功能的后果仍然知之甚少。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号