Dai Teng-fei, Xi Ben-ye, Yan Xiao-li, Jia Li-ming
Ying Yong Sheng Tai Xue Bao. 2015 Jun;26(6):1641-8.
A field experiment was conducted to investigate the effects of fertilization methods, i.e., drip (DF) and furrow fertilization (GF), and nitrogen (N) application rates (25, 50, 75 g N · plant(-1) · time(-1)) on the dynamics of soil N vertical migration in a Populus x euramericana cv. 'Guariento' plantation. The results showed that soil NH4(+)-N and NO3(-)-N contents decreased with the increasing soil depth under different fertilization methods and N application rates. In the DF treatment, soil NH4(+)-N and NO3(-)-N were mainly concentrated in the 0-40 cm soil layer, and their contents ascended firstly and then descended, reaching their maximum values at the 5th day (211.1 mg · kg(-1)) and 10th day (128.8 mg · kg(-1)) after fertilization, respectively. In the GF treatment, soil NH4(+)-N and NO3(-)-N were mainly concentrated in the 0-20 cm layer, and the content of soil NO3(-)-N rose gradually and reached its maximum at the 20th day (175.7 mg · kg(-1)) after fertilization, while the NH4(+)-N content did not change significantly after fertilization. Overall, N fertilizer had an effect within 20 days in the DF treatment, and more than 20 days in the GF treatment. In the DF treatment, the content and migration depth of soil NH4(+)-N and NO3(-)-N increased with the N application rate. In the GF treatment, the NO3(-)-N content increased with the N application rate, but the NH4(+)-N content was not influenced. Under the DF treatment, the hydrolysis rate, nitrification rate and migration depth of urea were higher or larger than that under the GF treatment, and more N accumulated in deep soil as the N application rate increased. Considering the distribution characteristics of fine roots and soil N, DF would be a better fertilization method in P. xeuramericana cv. 'Guariento' plantation, since it could supply N to larger distribution area of fine roots. When the N application rate was 50 g · tree(-1) each time, nitrogen mainly distributed in the zone of fine roots and had no risk of deep leaching, consequently improving the fertilizer utilization efficiency.
开展了一项田间试验,以研究施肥方法(即滴灌施肥(DF)和沟施(GF))以及施氮量(25、50、75克氮·株⁻¹·次⁻¹)对欧美杨‘Guariento’人工林中土壤氮素垂直迁移动态的影响。结果表明,在不同施肥方法和施氮量下,土壤铵态氮(NH₄⁺-N)和硝态氮(NO₃⁻-N)含量均随土壤深度增加而降低。在滴灌施肥处理中,土壤铵态氮和硝态氮主要集中在0-40厘米土层,其含量先升后降,分别在施肥后第5天(211.1毫克·千克⁻¹)和第10天(128.8毫克·千克⁻¹)达到最大值。在沟施处理中,土壤铵态氮和硝态氮主要集中在0-20厘米土层,土壤硝态氮含量逐渐上升,在施肥后第20天(175.7毫克·千克⁻¹)达到最大值,而施肥后铵态氮含量变化不显著。总体而言,滴灌施肥处理中氮肥在20天内起作用,沟施处理中则超过20天。在滴灌施肥处理中,土壤铵态氮和硝态氮的含量及迁移深度随施氮量增加而增加。在沟施处理中,硝态氮含量随施氮量增加而增加,但铵态氮含量不受影响。在滴灌施肥处理下,尿素的水解速率、硝化速率和迁移深度均高于沟施处理,且随着施氮量增加,更多的氮积累在深层土壤中。考虑到细根分布特征和土壤氮素情况,滴灌施肥在欧美杨‘Guariento’人工林中是一种更好的施肥方法,因为它能为更大范围的细根分布区域供应氮素。当每次施氮量为50克·株⁻¹时,氮主要分布在细根区域,没有深层淋溶风险,从而提高了肥料利用效率。