酸性液体肥对几种土壤的氨挥发的影响
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(华南农业大学资源环境学院,广东 广州 510642)

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周海锋(2001-),硕士研究生,研究方向为资源利用与植物保护。E-mail:907979453@qq.com。

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Effects of acid liquid fertilizer on ammonia volatilization in several soils
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(School of Resources and Environment,South China Agricultural University,Guangzhou Guangdong 510642)

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    摘要:

    施用酸性物质能够调控土壤碱性从而减少氨挥发。无机酸是液体的,方便添加到液体肥料中,施肥的同时也改良了土壤的碱性。试验在不同pH 的土壤上施用酸性液体肥来探究其氨挥发的差异。共使用了5 种养分相同、pH 不同的酸性液体肥,利用稀硫酸将肥料的pH 调节至6.5、4.7、1.9、1.0 和0。室内氨挥发培养试验以不施肥为对照,分别将5 种不同pH 的肥料(用量0.6 g/kg 土)混施在砂姜黑土、潮土和苏打盐碱土3 种土壤中,每种土壤5 个处理(pH 6.5、pH 4.7、pH 1.9、pH 1.0、pH 0)。在30 d 培养期内在多个时间段对土壤挥发的氨采用静态吸收法收集并测定。砂姜黑土在培养后16 h ~ 1 d,潮土在8 h ~ 1 d,苏打盐碱土在16 h ~ 1 d 氨挥发达到高峰期。培养期内氨挥发总量与液体肥pH 相关,pH 越高,氨挥发越多。砂姜黑土氨挥发总量为31.5 ~ 45.2 mg/kg,占施氮量的19.4% ~ 27.9%,pH 0 比pH 6.5 处理减少30.4%;潮土中氨挥发总量为37.3 ~ 61.2 mg/kg,占施氮量的23.0% ~ 37.8%,pH 0 比pH 4.7 处理减少39.1%;苏打盐碱土氨挥发总量为51.3 ~ 72.8 mg/kg,占施氮量的37.1% ~ 45.0%,pH 0 比pH 6.5 处理减少29.5%。碱性土壤中施用酸性液体肥大部分氨挥发发生在前3 d。在施用相同pH 的液体肥时,氨挥发总量表现为苏打盐碱土> 潮土> 砂姜黑土,表明土壤pH 越高,氨挥发越多。3 种土壤培养30 d 后氨挥发总量最少的为pH 0 处理,表明液体肥的pH 越低,氨挥发总量越少。

    Abstract:

    The application of acidic substances can regulate soil alkalinity and reduce ammonia volatilization. Inorganic liquid acid is convenient to add to liquid fertilizer,which has the functions of both fertilization and the soil alkalinity improvement. In this experiment,acidic liquid fertilizer was applied to soils with different pH to explore the difference of ammonia volatilization. A total of five acidic liquid fertilizers with the same nutrient content but different pH levels were used,with their pH adjusted to 6.5,4.7,1.9,1.0,and 0 using dilute sulfuric acid. In the indoor ammonia volatilization culture experiment,five different pH fertilizers(0.6 g/kg soil)were mixed and applied to black meadow soil,fluvo-aquic soil and soda saline-alkali soil. There were 5 treatments(pH 6.5,pH 4.7,pH 1.9,pH 1.0,pH 0)for each type of soil,with no fertilization as the control. During the 30 d incubation period,the ammonia volatilized from the soil was collected and measured by static absorption method at multiple time periods. The ammonia volatilization of black meadow soil reached the peak at 16 h-1 d after culture,fluvo-aquic soil at 8 h-1 d,and soda saline-alkali soil at 16 h-1 d.The total amount of ammonia volatilization during the culture period was related to the pH of the liquid fertilizer,with higher pH resulting in more ammonia volatilization. The total amount of ammonia volatilization was 31.5–45.2 mg/kg,accounting for 19.4%–27.9% of the nitrogen application rate,and it was 30.4% lower in pH 0 treatment than that in pH 6.5 treatment.The total amount of ammonia volatilization in fluvo-aquic soil was 37.3–61.2 mg/kg,accounting for 23.0%–37.8% of nitrogen application,and it was 39.1% lower in pH 0 treatment than that in pH 4.7 treatment. The total amount of ammonia volatilization in soda saline-alkali soil was 51.3–72.8 mg/kg,accounting for 37.1%–45.0% of the nitrogen application rate,and it was 29.5% lower in pH 0 treatment than that in pH 6.5 treatment. The ammonia volatilization of acidic liquid fertilizer in alkaline soil occurred in the first three days. When the same pH liquid fertilizer was applied,the total amount of ammonia volatilization showed soda saline-alkali soil > fluvo-aquic soil > black meadow soil,indicating that the higher the soil pH,the more ammonia volatilization. The total amount of ammonia volatilization after 30 d of culture in the three soils was at pH 0 treatment,indicating that the lower the pH of the liquid fertilizer,the less the total amount of ammonia volatilization.

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周海锋,张承林.酸性液体肥对几种土壤的氨挥发的影响[J].中国土壤与肥料123,2025,(8):37-42

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  • 收稿日期:2024-11-27
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  • 录用日期:2025-01-24
  • 在线发布日期: 2025-10-11
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