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首页> 外文期刊>Soil Biology & Biochemistry >Litter quantity confers soil functional resilience through mediating soil biophysical habitat and microbial community structure on an eroded bare land restored with mono Pinus massoniana.
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Litter quantity confers soil functional resilience through mediating soil biophysical habitat and microbial community structure on an eroded bare land restored with mono Pinus massoniana.

机译:凋落物数量通过介导由马尾松单胞菌恢复的受侵蚀的裸地上的土壤生物物理生境和微生物群落结构,赋予土壤功能弹性。

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Soils have an intrinsic ability to adapt to environmental perturbations compounded by global warming and soil pollution to continuously deliver soil functions, but little is known about how a severely degraded soil regains its functional stability after restoration of vegetation. Surface soils were sampled along slopes in a long-term trial where mono Pinus massoniana was transplanted since 1987 on an eroded bare land and pine litter was either protected or removed on the slopes. We hypothesized that litter quantity would drive changes in soil properties rather than soil microbial communities, which would be main factors in controlling soil functional stability. The specific objectives of this study were: (1) to evaluate the effects of litter management on soil properties, soil microbial community structure and functional stability and (2) to explore the relative role of soil properties and microbial community structure in controlling soil functional stability. The functional stability (resistance and resilience) was determined by measuring how the short-term decomposition of added barley (Hordeum vulgare) powder changed over 28-days following copper addition and heating. Community-level physiological profiles (CLPP) and phospholipid fatty acid (PLFA) profiles were measured to characterize soil microbial community structure. Litter quantity was significantly (P<0.05) and positively correlated with soil organic carbon (SOC) and microbial biomass carbon (SMB-C) concentration, soil structural properties (porosity and aggregate stability) and the resilience to both perturbations. Soil microbial community structure was significantly separated in two different ways. One was associated with the quantity of litter, SOC concentration and its mediated soil properties (SMB and non-capillary porosity). Another was associated with SOC quality and its mediated soil properties (aggregate stability). These biophysical soil properties (SMB, SOC and capillary porosity) were significantly correlated with the resilience to heating and the resistance and resilience to copper addition. The separations of soil microbial community structure driven by litter quality were significantly correlated with the resistance to heating and the resilience to copper addition. This result suggests that the degraded soil could regain its functional stability after re-vegetation due to the concordant development of soil biophysical habitat and soil microbial community structure through continuous organic inputs. Maintaining litter on floor against anthropogenic collection has an important ecological value.
机译:土壤具有适应环境扰动的内在能力,这种环境扰动加上全球变暖和土壤污染不断地传递土壤功能,但对于严重退化的土壤在恢复植被后如何恢复其功能稳定性方面知之甚少。在一项长期试验中,沿斜坡对表层土壤进行了取样,自1987年以来,马尾松已在受侵蚀的光秃秃的土地上进行了移植,在斜坡上保护或清除了松树凋落物。我们假设凋落物的数量将驱动土壤性质的变化,而不是土壤微生物群落的变化,这将是控制土壤功能稳定性的主要因素。这项研究的具体目标是:(1)评估凋落物管理对土壤特性,土壤微生物群落结构和功能稳定性的影响,以及(2)探索土壤特性和微生物群落结构在控制土壤功能稳定性中的相对作用。 。通过测量添加的大麦(添加大麦)粉末在添加铜和加热后28天内的短期分解如何变化,来确定功能稳定性(电阻和弹性)。测量了群落水平的生理概况(CLPP)和磷脂脂肪酸(PLFA)概况,以表征土壤微生物群落结构。凋落物数量显着(P <0.05),并与土壤有机碳(SOC)和微生物生物量碳(SMB-C)浓度,土壤结构特性(孔隙度和聚集体稳定性)以及对两种扰动的恢复力呈正相关。土壤微生物群落结构以两种不同方式明显分离。一个与垫料的数量,SOC浓度及其介导的土壤特性(SMB和非毛细管孔隙度)有关。另一个与SOC质量及其介导的土壤特性(骨料稳定性)有关。这些生物物理土壤特性(SMB,SOC和毛细管孔隙率)与加热的回弹性以及添加铜的电阻和回弹性显着相关。凋落物质量驱动的土壤微生物群落结构的分离与耐热性和添加铜的适应性显着相关。该结果表明,由于土壤生物物理生境和土壤微生物群落结构通过持续的有机输入而协调发展,退化后的土壤在重新植被后可以恢复其功能稳定性。保持地板上的垃圾免于人为收集具有重要的生态价值。

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