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Does soil amended with biochar and hydrochar reduce ammonia emissions following the application of pig slurry?

机译:施用猪粪后,用生物炭和水炭改性的土壤是否会减少氨气排放?

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Combining amendments to the soil made by biochar or hydrochar with nitrogen (N) fertilizer can modify soil N dynamics and availability. Such a response suggests that these amendments would affect ammonia (NH3) emissions from slurry similarly, and potentially reduce volatilization of NH3. This study measured the potential emissions of NH3 following application of pig slurry to the surface of silt-loam and loam soils amended with biochar and hydrochar (both derived from Miscanthus x giganteus (Greef et Deu)) at a rate of 3% soil dry weight (16 t ha(-1) soil area, on average) and 60% water-filled pore space (WFPS). The experiment was carried out in a dynamic chamber connected to a photo-acoustic trace gas analyser in a controlled climate (20 degrees C) for 48 hours. Statistically significant differences (P 0.05) in total emissions were observed between both treatment and soil types. Surprisingly, both amendments increased emissions of NH3 compared with the control; cumulative NH3 emissions averaged 38.7 and 23.5% of applied total ammonium nitrogen (TAN) for hydrochar and biochar, respectively, whereas it was 18.2% for the control. The larger emissions in hydrochar-amended soil were attributed to the reduced ability to absorb NH4+ associated with greater hydrophobicity and strong pH buffering of the slurry. Furthermore, final soil analyses with deionised water extracts showed significant differences (P 0.05) in mineral N concentration between treatments. The smaller ammonium concentrations in biochar-amended soil suggest that some NH4+-N was immobilized by adsorption on to biochar surfaces. This study observed that biochar and hydrochar properties, as well as soil characteristics, play important roles in controlling NH3 emissions from surface slurry applications. The results obtained identified circumstances where these amendments even enhance volatilization, which provides new information on and insight into the extent and limitations of the potential of biochar and hydrochar for the mitigation of emissions.
机译:将生物炭或水炭对土壤的改良剂与氮(N)肥料结合使用,可以改变土壤的氮素动态和有效性。这种反应表明,这些修订将同样影响浆料中的氨(NH3)排放,并有可能减少NH3的挥发。这项研究测量了将猪粪浆施用到粉砂壤土和壤土上​​的生物质和水质炭(均来自Miscanthus x giganteus(Greef et Deu)改良)的速率,其土壤干重为3%时,可能排放NH3。 (平均16 t ha(-1)的土壤面积)和60%的充满水的孔隙空间(WFPS)。在连接到光声痕量气体分析仪的动态室中,在受控气候(20摄氏度)下进行了48小时的实验。处理和土壤类型之间的总排放量在统计学上有显着差异(P <0.05)。出乎意料的是,与对照相比,两项修正案均增加了NH3的排放;水炭和生物炭的平均累积NH3排放量分别平均为施用的总铵氮(TAN)的38.7和23.5%,而对照组则为18.2%。碳氢化合物改良土壤中的大量排放归因于吸收NH4 +的能力降低,这与浆料的更大疏水性和较强的pH缓冲有关。此外,用去离子水提取物进行的最终土壤分析显示,两次处理之间的矿质氮浓度存在显着差异(P <0.05)。在生物炭改良过的土壤中较小的铵浓度表明,某些NH4 + -N通过吸附在生物炭表面而被固定化。这项研究观察到,生物炭和水炭的特性以及土壤特性在控制表面泥浆施用中的NH3排放中起着重要作用。获得的结果确定了这些修正案甚至会加剧挥发的情况,这为生物炭和水炭减轻排放的潜力提供了新的信息和见识。

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