CSIR-Institute of Minerals and Materials Technology, Bhubaneswar, 751013 India.
Indian J Microbiol. 2013 Mar;53(1):92-9. doi: 10.1007/s12088-012-0318-3. Epub 2012 Oct 13.
Soil from a pulse cultivated farmers land of Odisha, India, have been subjected to incubation studies for 40 consecutive days, to establish the impact of various nitrogenous fertilizers and water filled pore space (WFPS) on green house gas emission (N2O & CH4). C2H2 inhibition technique was followed to have a comprehensive understanding about the individual contribution of nitrifiers and denitrifiers towards the emission of N2O. Nevertheless, low concentration of C2H2 (5 ml: flow rate 0.1 kg/cm(2)) is hypothesized to partially impede the metabolic pathways of denitrifying bacterial population, thus reducing the overall N2O emission rate. Different soil parameters of the experimental soil such as moisture, total organic carbon, ammonium content and nitrate-nitrogen contents were measured at regular intervals. Application of external N-sources under different WFPS conditions revealed the diverse role played by the indigenous soil microorganism towards green house gas emission. Isolation of heterotrophic microorganisms (Pseudomonas) from the soil samples, further supported the fact that denitrification might be prevailing during specific conditions thus contributing to N2O emission. Statistical analysis showed that WFPS was the most influential parameter affecting N2O formation in soil in absence of an inhibitor like C2H2.
来自印度奥里萨邦种植豆类作物的农民土地的土壤,已经进行了 40 天的连续孵化研究,以确定各种氮肥和水充满孔隙空间 (WFPS) 对温室气体排放 (N2O 和 CH4) 的影响。采用 C2H2 抑制技术,全面了解硝化菌和反硝化菌对 N2O 排放的个体贡献。然而,低浓度的 C2H2(5 ml:流速 0.1 kg/cm(2))被假设为部分阻碍反硝化细菌种群的代谢途径,从而降低整体 N2O 排放速率。在实验土壤的不同土壤参数,如水分、总有机碳、铵含量和硝酸盐氮含量,在定期间隔进行测量。在不同 WFPS 条件下应用外源 N 源,揭示了土著土壤微生物对温室气体排放的不同作用。从土壤样本中分离出异养微生物(假单胞菌),进一步证实了在特定条件下反硝化作用可能占主导地位,从而导致 N2O 排放。统计分析表明,在没有 C2H2 等抑制剂的情况下,WFPS 是影响土壤中 N2O 形成的最具影响力的参数。