低臭氧剂量率下臭氧处理对土壤养分和酸度的影响

T. Nagatomo, Keisuke Takigawa, Y. Yamasaki, Takamasa Sakai, F. Mitsugi, T. Ikegami, K. Ebihara, K. Nagahama
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引用次数: 2

摘要

研究了臭氧处理对低臭氧剂量率土壤物理性质的影响。臭氧是由氧等离子体通过电介质表面阻挡放电产生的,并通过电机旋转的石英容器注入土壤中。用于处理的土壤量为100克。处理时间为1 min。臭氧剂量率为0.1%,定义为每单位土壤重量的臭氧剂量重量。臭氧气体流量为1.5 L/min。测定了低臭氧剂量下土壤无机养分(NO3-N、NO2-N和NH4-N)含量、pH(H2O)、真菌(亚硝酸盐和硝酸盐细菌)数量、土壤DNA数量和交换碱(Ca、K、Fe和Al)数量等特征。我们测量了3个样品的土壤物理性质,以确认测量的重复性。臭氧处理1 min后,NO3-N和NH4-N含量略有增加,随后随时间保持在恒定值。臭氧处理后,pH(H2O)降低。而pH(H2O)值随着时间的推移,通过缓冲作用逐渐恢复。
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Influence of Ozone Treatment on Soil Nutrient and Acidity with Low Ozone Dose Rate
In this study, the influence of ozone treatment on physical properties of soil with low ozone dose rate was investigated. Ozone was generated by oxygen plasma using a dielectric surface barrier discharge and injected into soil in a quartz container which is rotated by a motor. The amount of soil used for the treatment was 100 g. Treating time was 1 min. The ozone dose rate, which is defined as ozone dose weight per unit weight of soil, was 0.1 %. Flow rate of ozone gas was 1.5 L/min. We measured the characteristics of soil such as inorganic nutrient contents (NO3-N, NO2-N, and NH4-N), pH(H2O), amount of fungi (nitrite and nitrate bacteria), amount of DNA of soil, and amount of exchangeable base (Ca, K, Fe, and Al) with low ozone dose. We measured physical properties of soil among three samples for confirmation of measurement reproducibility. Content of NO3-N and NH4-N increased slightly by ozone treatment for 1 min., and subsequently maintained at a constant value with time. The pH(H2O) decreased just after ozone treatment. However, the pH(H2O) value recovered gradually with time by the buffering function.
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