R. Subedi, C. Kammann, S. Pelissetti, N. Taupe, C. Bertora, S. Monaco, C. Grignani
{"title":"Does soil amended with biochar and hydrochar reduce ammonia emissions following the application of pig slurry?","authors":"R. Subedi, C. Kammann, S. Pelissetti, N. Taupe, C. Bertora, S. Monaco, C. Grignani","doi":"10.1111/ejss.12302","DOIUrl":null,"url":null,"abstract":"<div>\n \n <p>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 (NH<sub>3</sub>) emissions from slurry similarly, and potentially reduce volatilization of NH<sub>3</sub>. This study measured the potential emissions of NH<sub>3</sub> following application of pig slurry to the surface of silt-loam and loam soils amended with biochar and hydrochar (both derived from <i>Miscanthus</i> × <i>giganteus</i> (Greef et Deu)) at a rate of 3% soil dry weight (16 t ha<sup>−1</sup> 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°C) for 48 hours. Statistically significant differences (<i>P</i> < 0.05) in total emissions were observed between both treatment and soil types. Surprisingly, both amendments increased emissions of NH<sub>3</sub> compared with the control; cumulative NH<sub>3</sub> 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 NH<sub>4</sub><sup>+</sup> associated with greater hydrophobicity and strong pH buffering of the slurry. Furthermore, final soil analyses with deionised water extracts showed significant differences (<i>P</i> < 0.05) in mineral N concentration between treatments. The smaller ammonium concentrations in biochar-amended soil suggest that some NH<sub>4</sub><sup>+</sup>-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 NH<sub>3</sub> 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.</p>\n </div>","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"66 6","pages":"1044-1053"},"PeriodicalIF":4.0000,"publicationDate":"2015-10-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1111/ejss.12302","citationCount":"44","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"European Journal of Soil Science","FirstCategoryId":"97","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/ejss.12302","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 44
Abstract
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 × 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°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.
生物炭或碳氢化合物对土壤的修正与氮肥的结合可以改变土壤氮的动态和有效性。这样的反应表明,这些修正将同样影响浆料中的氨(NH3)排放,并可能减少NH3的挥发。本研究以3%土壤干重(平均16 t ha - 1土壤面积)和60%充水孔隙空间(WFPS)的速率,在粉质壤土和经生物炭和氢炭(均来自芒草)改性的壤土表面施用猪浆后,测量了NH3的潜在排放。实验在一个连接光声痕量气体分析仪的动态室中进行,在受控气候(20°C)下进行48小时。统计学差异显著(P <处理与土壤类型间总排放量差异均达0.05)。令人惊讶的是,与对照相比,这两项修正案都增加了NH3的排放量;氢炭和生物炭的累积NH3排放量平均分别占施用总铵态氮(TAN)的38.7%和23.5%,而对照为18.2%。加氢土壤的排放物较大,归因于浆料对NH4+的吸收能力降低,且浆料的疏水性和强pH缓冲作用增强。此外,去离子水提取物的最终土壤分析显示出显著差异(P <处理间矿质氮含量差异0.05)。经生物炭处理的土壤中铵离子浓度较低,说明部分NH4+-N通过吸附在生物炭表面而被固定化。本研究发现,生物炭和碳氢化合物的性质以及土壤特征在控制地表泥浆的NH3排放中起重要作用。所获得的结果确定了这些修正甚至加剧挥发的情况,这就提供了关于生物炭和碳氢化合物在减少排放方面的潜力的程度和局限性的新信息和见解。
期刊介绍:
The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.