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林业科学 ›› 2016, Vol. 52 ›› Issue (11): 55-62.doi: 10.11707/j.1001-7488.20161107

• 论文与研究报告 • 上一篇    下一篇

肥培毛竹林土壤氨挥发特征

赵建诚1, 苏文会1, 范少辉1, 蔡春菊1, 朱晓武1,2, 刘广路1   

  1. 1. 国际竹藤中心 国家林业局竹藤科学与技术重点实验室 北京 100102;
    2. 西南林业大学 昆明 650224
  • 收稿日期:2015-11-13 修回日期:2016-04-14 出版日期:2016-11-25 发布日期:2016-12-16
  • 通讯作者: 苏文会
  • 基金资助:
    科研事业费项目(1632014011);国家林业局948项目(2014-4-58)。

Characteristics of Soil Ammonia Volatilization in Fertilized Moso Bamboo (Phyllostachys edulis) Forests

Zhao Jiancheng1, Su Wenhui1, Fan Shaohui1, Cai Chunju1, Zhu Xiaowu1,2, Liu Guanglu1   

  1. 1. Key Laboratory of Science and Technology of Bamboo and Rattan of State Forestry Administration International Centre for Bamboo and Rattan Beijing 100102;
    2. Southwest Forestry University Kunming 650224
  • Received:2015-11-13 Revised:2016-04-14 Online:2016-11-25 Published:2016-12-16

摘要: [目的] 通过田间试验研究不同施肥深度毛竹林土壤氨挥发特征,为毛竹林合理施肥提高养分利用率、降低损失提供理论依据。[方法] 以安徽省黄山区毛竹林为对象,设置0,5,10,15,20,25和30 cm 7个施肥深度,分别施入尿素、过磷酸钙和氯化钾,以不施肥作为空白对照。氨挥发的收集采用通气法,用2%硼酸作为氨的吸收液。采用单因素分析(ANOVA)进行显著性检验和最小显著性差异法(LSD)进行多重比较。[结果] 毛竹林施肥后土壤铵态氮含量先升高后降低,最后趋于稳定;氨挥发进程随施肥时间呈现明显的规律性变化,并与施肥深度关系密切。在施肥后第2天即被检测到挥发氨,施肥后毛竹林土壤的氨挥发速率先升高后降低,呈单峰曲线变化;0,5和10 cm深度施肥处理的氨挥发速率在第3天达到最大值,而15,20,25和30 cm深度施肥处理在第6天达到峰值;随后氨挥发速率逐日降低,至第12天时降至未施肥处理水平。氨挥发过程可分为快速和慢速2个阶段:施肥后1~8天为快速上升阶段,8天内挥发量占试验期间氨挥发总量的81.93%~92.38%;第8天后氨挥发速率明显降低,各施肥深度氨挥发累积量(y)与时间(t)符合Elovish动力学方程(y=a+blnt);试验结束后,各施肥处理毛竹林土壤氨挥发损失量为10.12~27.17 kg·h-1。施肥深度对氨挥发影响明显,平均氨挥发速率和挥发损失量随深度增加而逐渐降低,以0和5 cm施肥深度处损失量最大,分别达27.17和25.66 kg·h-1,相当于施氮量的21.05%和19.88%,在施肥深度超过15 cm时,损失率降幅明显减缓。[结论] 集约经营毛竹林,施肥后8天内氨挥发速度快,建议通过环境条件调控降低氮素流失;施肥深度超过15 cm氨挥发损失率较低,但深层施肥可能导致淋溶损失,同时也增加生产成本。综合考虑毛竹根系分布及氮素损失、利用情况,施肥深度应为15~20 cm土层。

关键词: 毛竹, 氮, 氨挥发, 施肥深度, 铵态氮含量

Abstract: [Objective] Nitrogen (N) is the greatest demand element for Moso bamboo (Phyllostachys edulis) growth. Improper fertilization could result in the decrease of nitrogen use efficiency (NUE) and the increase of nitrogen loss. Ammonia (NH3) volatilization is one of the main pathways of nitrogen loss from soil. Improper depth of fertilizer application in the soil could accelerate the loss of NH3 volatilization. However, very little information is available regarding NH3 volatilization and its influence factors in Moso bamboo forests. Thus, in this study the NH3 volatilization characteristics at different fertilization depths in a Moso bamboo forest were investigated by field experiment to provide the scientific guidance for the reasonable fertilization depth in terms of reducing the ammonia volatilization. [Method] In this paper, seven fertilization depths of 0, 5, 10, 15, 20, 25 and 30 cm and a control treatment without fertilizer were set in Huangshan, Anhui Province of China. The NH3 volatilized from each plot was absorbed by 2% H3BO3 with the venting method. One-way ANOVA was conducted to test the significance of the indexes, and the least significant difference (LSD) was applied for multiple comparisons. [Result] The NH4+ content after fertilization increased first and then declined with the extension of time, and finally stabilized. The NH3 volatilization showed obvious regularity changes with time, and it was closely related to fertilization depth. NH3 volatilization was detected on the second day after fertilization. The NH3 volatilization rates of all fertilization treatments increased first and then decreased, showed a single peak curve. NH3 volatilization rates at fertilization depths of 0, 5 and 10 cm peaked on the third day, while rates of NH3 volatilization at fertilization depths of 15, 20, 25 and 30 cm reached a maximum in 6 days after fertilization. Then, the rates decreased gradually. About twelve days later, NH3 volatilization rates dropped to a low level similar to the control. NH3 volatilization of urea could be divided into 2 stages, namely, rapidly and slowly increasing stages. The first eight days were recognized as the rapidly increasing stage. The ratios of NH3 volatilized within the first eight days to the total volatilization loss were ranged from 81.93% to 92.38%. Then it changed to the slowly increasing stage. The relationship between the cumulative NH3 volatilization (y) and the corresponding time (t) accorded with the Elovich equation (y=a + b lnt). By the end of this experiment, the losses of NH3 volatilization from the fertilization treatments were ranged from 10.12 to 27.17 kg·hm-2. Results showed that NH3 volatilization was influenced significantly by fertilization depth. The mean NH3 volatilization flux and total loss decreased with the increase of fertilization depth. NH3 volatilization losses of fertilization placed at 0 and 5 cm depths were larger than that at other depths, up to 27.17 and 25.66 kg·hm-2, equivalent to 21.05% and 19.88% of the applied N, respectively. When fertilization depth exceeded 15 cm, the loss ratio was significantly reduced. [Conclusion] In this study, NH3 volatilization was characterized by a high speed within the first eight days after fertilization in an intensive management bamboo forest. Thus, the regulation of environmental conditions was suggested to reduce N loss. The nitrogen losses through NH3 volatilization of fertilization placed below 15 cm depth were lower, however deep fertilization application could result in leaching loss and also increased the production cost. Comprehensive consideration of the distribution of bamboo root and nitrogen loss and utilization, the reasonable fertilization depth should be 15-20 cm in P.edulis forests.

Key words: Phyllostachys edulis, nitrogen, ammonia volatilization, fertilization depth, ammonium nitrogen content

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