中国农业气象 ›› 2017, Vol. 38 ›› Issue (03): 163-171.doi: 10.3969/j.issn.1000-6362.2017.03.004

• 论文 • 上一篇    下一篇

生物炭施用对稻田氮磷肥流失的影响

肖建南,张爱平,刘汝亮,杨正礼   

  1. 1.中国农业科学院农业环境与可持续发展研究所/农业部农业环境重点实验室,北京100081;2.宁夏农林科学院,银川750000
  • 收稿日期:2016-08-08 出版日期:2017-03-20 发布日期:2017-03-13
  • 作者简介:肖建南(1991-),女,硕士生,主要从事生态农业与清洁生产研究。E-mail:xiaojiannan1999@163.com
  • 基金资助:
    国家自然科学基金项目(31601834;31660597);农业清洁流域创新基金;宁夏农林科学院科技创新先导基金

Effects of Biochar Application on the Losses of Nitrogen and Phosphorus in Surface Water of Paddy Field

XIAO Jian-nan, ZHANG Ai-ping, LIU Ru-liang, YANG Zheng-li   

  1. 1.Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences /Key Laboratory of Agricultural Environment, Ministry of Agriculture, Beijing 100081, China; 2.Ningxia Academy of Agriculture and Forestry Sciences, Yinchuan 750000
  • Received:2016-08-08 Online:2017-03-20 Published:2017-03-13

摘要: 针对宁夏引黄灌区稻田过量施肥导致土壤养分利用效率低的问题,通过田间小区试验,在优化施氮条件下(240kg·hm-2),设4个生物炭水平(0、4500、9000、13500kg·hm-2),研究施用外源生物炭对稻田氮磷流失和土壤养分含量的影响。结果表明:生物炭对稻田田面水氮素动态产生影响,表现为田面水中全氮、硝态氮含量随生物炭用量的增加而降低,铵态氮表现则相反;全氮和铵态氮的最大峰值出现在第1次追施氮肥后的第2天,最大值为34.86、8.28mg·L-1;硝态氮最大峰值3.31mg·L-1出现在第2次追施氮肥后的第2天。随后均迅速下降,全氮含量在施氮肥后10d回到第1次追氮前的含量水平,并趋于稳定,铵态氮和硝态氮则在7d后。生物炭对田面水全磷未产生显著影响,全磷含量在第1次施氮肥后3d达到峰值,为3.69mg·L-1,之后迅速下降,6~7d后降至追氮前的含量水平,并趋于稳定。生物炭处理显著降低了稻田全氮流失量8.03%~13.36%,高量炭处理(13500kg·hm-2)显著提高了土壤全氮和有机质含量,提高幅度分别为41.2%和27.5%(P<0.05)。说明生物炭对稻田磷流失、土壤全磷和速效磷含量无显著影响,对降低稻田氮素淋失表现出积极效果。

关键词: 生物炭, 稻田田面水, 氮素, 磷素, 土壤养分

Abstract: Applied high rates of nitrogen (N) fertilizer in rice production may result in lower N use efficiency in a paddy rice field of the Yellow River irrigation region, Ningxia. To reduce N and phosphorus (P) leaching and improve fertilizer use efficiency are important for sustainable and water quality. Thus, a field plot experiment was conducted to study the effect of exogenous biochar application on the loss risk of N and P and soil quality in a paddy field. Four biochar rates, i.e., 0, 4500, 9000, and 13500kg·ha-1 with optimum nitrogen rate (240kg·ha-1) were chosen. From May to October 2014, we determined the contents of NH4+-N, NO3--N, total N (TN) and total P (TP) in the surface water of paddy field during the whole rice growth period. The results showed that biochar amendment decreased the contents of both TN and NO3--N but increased NH4+-N content in the surface water. The contents of TN and NH4+-N reached the peak on the following day of the first top dressing and the maximum values were 34.86 and 8.28mg·L-1 respectively. The content of NO3--N reached the peak on the following day of the second top dressing and the maximum value was 3.31mg·L-1. Then TN leveled off after 10 days, but the NH4+-N and NO3--N contents approached a relatively stable level after a week. There was no significant difference in TP content in the surface water between the biochar addition and the control treatments. The content of TP peaked 3 days after fertilization and decreased rapidly afterwards, then leveled off after another 6-7 days. On the other hand, biochar amendment decreased TN leaching by 8.03%-13.36% relative to control, but the high-level biochar amendments (13500kg·ha-1) significantly (P<0.05) increased the contents of TN and soil organic matter by 41.2% and 27.5% respectively compared with the control. There was no significant difference in TP and available P contents in soil between the biochar addition treatments and the control. Our study has revealed that biochar could positively reduce N leaching in the rice fields, while there has no significant effect on P loss.

Key words: Biochar, Surface water of paddy field, Nitrogen, Phosphorus, Soil nutrients