首页> 外文期刊>Soil Biology & Biochemistry >Carbon uptake by a microbial community during 30-day treatment with 13C-glucose of a sandy loam soil fertilized for 20 years with NPK or compost as determined by a GC-C-IRMS analysis of phospholipid fatty acids.
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Carbon uptake by a microbial community during 30-day treatment with 13C-glucose of a sandy loam soil fertilized for 20 years with NPK or compost as determined by a GC-C-IRMS analysis of phospholipid fatty acids.

机译:微生物群落在 13 C-葡萄糖处理30天的含氮磷钾或堆肥的沙质壤土上处理30天的碳吸收量,方法是通过GC-C-IRMS分析磷脂脂肪酸。

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摘要

To investigate the uptake by the microbial community of easily decomposable exogenous organic C and the proportion of this organic C remaining in soils under long-term fertilization schemes, 13C-glucose was supplied to arable soils (aquic inceptisol) following a 20-year (1989-2009) application of compost (CM) or inorganic NPK (NPK), along with a control (no fertilizer). Phospholipid fatty acids (PLFAs) were used as biomarkers for actinobacteria, bacteria and fungi. Gas chromatography-combustion-stable isotope ratio mass spectrometry (GC-C-IRMS) was used to determine the incorporation of 13C into individual PLFAs. The concentrations of soil microbial PLFAs significantly (P<0.05) increased in all three soils after the addition of 13C-glucose. Over a 30-day incubation period, the highest PLFA concentrations were on day 7 (control) or day 15 (NPK and CM) for bacteria, and on day 30 for both fungi and actinobacteria. The added 13C-glucose was incorporated into bacterial PLFAs first, whilst an increase of 13C in fungal and actinobacterial PLFAs was measured on day 7 and 15, respectively. The mean amounts of 13C in bacterial, actinobacterial and fungal PLFAs in CM-treated soil during the 30-day incubation period were 0.589, 0.030 and 0.056 micro g g-1 soil, respectively, which were significantly (P<0.05) higher than levels measured in the NPK and control soils. Among the bacterial groups, the amount of 13C in Gram-positive (G+) bacteria over the entire incubation ranged from 0.326 to 0.440 micro g g-1 soil in the CM scheme, which was significantly (P<0.05) higher than levels detected in the NPK and control regimes. In contrast, 13C concentrations in monounsaturated PLFAs (aerobic microorganisms) in the CM-treated soil were 0.030-0.045 micro g g-1 soil, which was significantly (P<0.05) lower than in the NPK schemes. The proportion of glucose-derived 13C remaining in soils was ranked as follows: CM (53%) > NPK (41%) > control (28%) after 30 days of incubation. Easily decomposable exogenous organic C was thus more effectively maintained under the CM regime, primarily because, after 20 years, CM had altered the microbial community by reducing the ratio of aerobic to anaerobic microorganisms whilst increasing levels of G+ bacteria in soil compared to the control and NPK soils. This study aids our understanding of the transformation and maintenance of easily decomposable organic C in soil over long-term fertilization regimes.
机译:为了研究长期施肥方案下微生物群落对易分解的外源有机碳的吸收以及该有机碳在土壤中残留的比例,向耕地提供了 13 C-葡萄糖)施用了20年(1989-2009)的堆肥(CM)或无机NPK(NPK),以及对照(无肥料)。磷脂脂肪酸(PLFA)被用作放线菌,细菌和真菌的生物标记。气相色谱-燃烧稳定同位素比质谱法(GC-C-IRMS)用于确定 13 C掺入单个PLFA中的情况。添加 13 C-葡萄糖后,三种土壤中的土壤微生物PLFAs浓度均显着增加(P <0.05)。在30天的潜伏期中,细菌的最高PLFA浓度在第7天(对照)或第15天(NPK和CM),在真菌和放线菌的第30天。首先将添加的 13 C-葡萄糖掺入细菌PLFA中,而分别在第7天和第15天测量到真菌和放线菌PLFA中 13 C的增加。在30天的培养期内,CM处理过的土壤中细菌,放线菌和真菌PLFA中 13 C的平均量分别为0.589、0.030和0.056 micro gg -1 土壤分别比NPK和对照土壤中的水平显着(P <0.05)高。在细菌组中,整个培养过程中革兰氏阳性(G + )细菌中 13 C的量在0.326至0.440 micro gg -1 < CM方案中的土壤,显着(P <0.05)高于NPK和对照方案中检测到的水平。相比之下,经CM处理的土壤中单不饱和PLFA(好氧微生物)中的 13 C浓度为0.030-0.045 micro gg -1 土壤,这是显着的(P <0.05 )低于NPK计划中的价格。孵育30天后,土壤中残留的葡萄糖衍生的 13 C的比例排名为:CM(53%)>​​ NPK(41%)>对照(28%)。因此,在CM模式下可以更容易地保持易分解的外源有机碳,这主要是因为20年后,CM通过降低需氧微生物与厌氧微生物的比例同时增加G + 的水平改变了微生物群落。与对照和NPK土壤相比,土壤中的细菌更容易。这项研究有助于我们了解长期施肥制度下土壤中易分解的有机碳的转化和维持。

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