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应用生态学报 ›› 2022, Vol. 33 ›› Issue (7): 1919-1926.doi: 10.13287/j.1001-9332.202207.031

• 研究论文 • 上一篇    下一篇

施用南荻生物炭对不同类型土壤氨挥发的影响

胡旺1, 赵杭1, 周旋2, 王艺哲1, 张含丰1, 张玉平1*   

  1. 1湖南农业大学资源环境学院/农田污染控制与农业资源利用湖南省重点实验室, 长沙 410128;
    2湖南省农业科学院土壤肥料研究所, 长沙 410125
  • 收稿日期:2021-10-13 接受日期:2022-06-15 出版日期:2022-07-15 发布日期:2023-01-15
  • 通讯作者: *E-mail: zhyp2003@126.com
  • 作者简介:胡 旺, 男, 1996年生, 硕士研究生。主要从事农业面源污染防控与农业生态治理研究。E-mail:Huwang2021@163.com
  • 基金资助:
    湖南省重点领域研发计划项目(2019NK2021)、湖南省自然科学基金青年基金项目(2019JJ50337)和湖南省农业科技创新资金项目(2019LS03-3)资助。

Effect of reed-biochar application on ammonia volatilization from different types of soils

HU Wang1, ZHAO Hang1, ZHOU Xuan2, WANG Yi-zhe1, ZHANG Han-feng1, ZHANG Yu-ping1*   

  1. 1College of Resources and Environment/Hunan Provincial Key Laboratory of Farmland Pollution Control and Agricultural Resources Use, Hunan Agricultural University, Changsha 410128, China;
    2Institute of Soil and Fertilizer, Hunan Academy of Agricultural Sciences, Changsha 410125, China
  • Received:2021-10-13 Accepted:2022-06-15 Online:2022-07-15 Published:2023-01-15

摘要: 在洞庭湖区农田施用秸秆生物炭不仅能实现秸秆资源化利用,还可降低环境污染压力。本研究于2020年采用水稻盆栽试验,研究了不同南荻秸秆生物炭施用量对土壤氨挥发速率、累积氨挥发量、表面水pH值和NH4+-N浓度的影响。供试土壤为第四纪红土发育的红黄泥和花岗岩发育的麻砂泥水稻土,设置6个南荻秸秆生物炭添加处理,即分别以土柱0~20 cm土壤重量的0%、1%、2%、4%、6%和8%比例添加生物炭,每盆施用复合肥200 kg N·hm-2。结果表明: 施用生物炭导致两种土壤之间或不同生物炭处理之间的氨挥发速率和累积量均存在显著差异。麻砂泥施用生物炭处理在施肥后第2天出现氨挥发峰值,且较不施生物炭处理峰值降低了23.6%~53.4%;红黄泥氨挥发峰值出现在施肥后第7~13天,且其峰值随着生物炭添加量的增加而升高。整体上,麻砂泥土壤的氨挥发速率均高于红黄泥。麻砂泥土壤<4%生物炭添加量能抑制土壤氨挥发速率及累积量,其中以2%处理降幅最大(46.9%),但生物炭添加对水稻生长前期表面水pH值的影响不显著;红黄泥土壤随着南荻生物炭用量的增加,表面水中pH值和NH4+-N浓度增加,导致氨挥发速率及累积量增幅达1.3~10.5倍。回归分析显示,生物炭添加量是影响两种土壤氨挥发的关键因素。Elo-vich方程能较好地拟合两种土壤的氨挥发累积量随时间的变化动态,各施炭处理的相关系数均达极显著水平。总体上,对于偏中性的麻砂泥土壤,施用一定量的南荻生物炭对氨排放有一定的抑制作用,而对于酸性的红黄泥土壤,增施南荻生物炭会通过提高表面水的pH值和NH4+-N浓度促进氨挥发,因此针对不同类型土壤施用南荻秸秆生物炭应注意选择适宜用量,以降低氮素损失。

关键词: 生物炭, 南荻, 水稻, 氨挥发, pH

Abstract: The application of straw biochar in farmland in Dongting Lake area can realize the resource utilization of straw and reduce environmental risk. In 2020, a rice pot experiment was conducted to investigate the effects of different biochar application levels on ammonia volatilization rate, cumulative ammonia volatilization, pH value, and NH4+-N concentration in surface water. Six levels of reed (Miscanthus lutarioriparius) biochar amount, i.e., 0%, 1%, 2%, 4%, 6% and 8% of soil weight of the 0-20 cm column, were applied in two typical paddy soils in sou-thern China, i.e., reddish clayey soil derived from quaternary red soil and granitic sandy soil derived from granite. Compound fertilizer was applied at a rate of 200 kg N·hm-2. The results showed that biochar application resulted in significant differences in the rate and cumulative amount of ammonia volatilization between the two soils and among different biochar treatments. For the granitic sandy soil, peak ammonia volatilization under different biochar treatments appeared at the second day after fertilization, which was decreased by 23.6%-53.4%. For the reddish clayey soil, peak ammonia volatilization appeared between the 7th to 13th day after fertilization, which increased with biochar addition level. The rate of ammonia volatilization from the granitic sandy soil was generally higher than that from the reddish clayey soil. For the granitic sandy soil, addition of <4% biochar could inhibit the ammonia volatilization and cumulative volatilization amount, with the greatest reduction (46.9%) at the treatment with 2% biochar addition. The addition of biochar did not affect the pH value of surface water at the early stage of rice growth. For the reddish clayey soil, the pH value and NH4+-N concentration in the surface water increased with biochar addition level, resulting in the increases of ammonia volatilization rate and cumulative volatilization amount by 1.3-10.5 times. Biochar addition level was the key factor affecting ammonia volatilization from the two soils. Elovich equation could well fit the variation trend of cumulative ammonia volatilization with time for the two soils, with the correlation reaching extremely significant level for each treatment. Overall, the application of reed biochar could suppress ammonia volatilization from the granitic sandy soil which was nearly neutral in acidity, while would promote ammonia volatilization via increasing pH value and NH4+-N concentration of surface water for the acidic reddish clayey soil. Therefore, appropriate dosages of reed biochar should be selected for different types of soil in order to reduce nitrogen loss.

Key words: biochar, reed, rice, ammonia volatilization, pH