中国农业科学 ›› 2008, Vol. 41 ›› Issue (7): 2025-2032 .doi: 10.3864/j.issn.0578-1752.2008.07.020

• 土壤肥料·节水灌溉·农业生态环境 • 上一篇    下一篇

交替隔沟灌溉和施氮对玉米根区水氮迁移的影响

刘小刚,张富仓,田育丰   

  1. 西北农林科技大学旱区农业水土工程教育部重点实验室
  • 收稿日期:2007-11-22 修回日期:2007-12-06 出版日期:2008-07-10 发布日期:2008-07-10
  • 通讯作者: 张富仓

Effects of alternate furrow Irrigation on transport of water and nitrogen in maize rootzone soil

  

  1. 西北农林科技大学旱区农业水土工程教育部重点实验室
  • Received:2007-11-22 Revised:2007-12-06 Online:2008-07-10 Published:2008-07-10

摘要: 【目的】研究交替隔沟灌溉条件下作物根区土壤水氮迁移和累积。【方法】利用小区试验,对供试玉米采取不同的水分和氮素处理,测定交替隔沟灌溉条件下玉米根区土壤硝态氮、铵态氮和水分的变化。【结果】施氮后沟中硝态氮含量增长很快,大多集中在地表下0~30 cm处。随着时间的推移,上层土壤水分携带氮素养分下渗,造成下层土壤硝态氮含量的上升。收获时低水高氮处理的整个剖面上硝态氮的累积量最大,是高水高氮处理的1.2倍,低水低氮处理的是高水低氮的1.27倍。施氮后表层0~30 cm土壤铵态氮含量和累积量达到高峰,30 cm以下变化不明显。收获时各处理的铵态氮在剖面上的分布和累积基本相同。高水处理的土壤水分累积量明显大于低水处理,氮素水平的高低对土壤水分的累积影响不大。【结论】施氮量和灌水量是影响土壤硝态氮、铵态氮和土壤水分分布和累积的最主要因素。高水处理造成根区硝态氮淋失,降低了氮肥的利用。施氮量与硝态氮在根区剖面上的累积呈正相关。与硝态氮含量相比,铵态氮含量较低并且变化不大。最佳的水氮耦合形式为低水高氮(施氮量240 kgN•ha-1,灌水量1485.71 m3•ha-1)。

关键词: 交替隔沟灌溉, 玉米, 水氮迁移, 水氮累积

Abstract: 【Objection】study the effect of alternative furrow irrigation on transport and acumulation of water and nitrogen in maize rootzone soil.【Method】little section was adopted for this experiment about maize. Treatments included: a. water, b nitrogen. The water and nitrogen treatments included: high level and low level. The mode of irrigation is alternate furrow Irrigation.【Result】NO3--N contents increased quickly after fertilization, most of it was concentrated in the sub-surface of 0-30cm. With the time went on, the upper soil water took the nitrogen contents down, and all this lead to the NO3--N contents of subsoil raised. The maximal accumulated NO3--N of low water and high nitrogen that gained at harvest time in the whole profile was 1.2 times of that of high water and high nitrogen. The accumulation of NO3--N of low water and low nitrogen was 1.27 times of that of low nitrogen and high water. The maximum residual value of NO3--N of per nitrogen fertilized was found in the treatment of low water and low nitrogen, the treatment of low water and high nitrogen was followed and the treatment of high water and high nitrogen was less. The treatment of high water high nitrogen was lest, in which the residual value of NO3--N of per nitrogen fertilized was only half of the treatment of low water and low nitrogen. After fertilizing the NH4+-N contents in the soil of sub-surface of 0-30cm reached a peak, and the contents basically did not change at the same level in the soil of 30cm below surface. The accumulation and distribution of NH4+-N of every treatment were basically the same. The level of water obviously effected accumulation and distribution of soil moisture. The acumulation soil water content of high water was obviously larger than that of low water. The level of nitrogen was not obviously affected of them.【Conclusion】The distribution and accumulation of NO3--N, NH4+-N and soil moisture were commonly affected by the amount of nitrogen application and irrigation. The treatment of high water reduced the accumulation of NO3--N in root zone, which lead to leaching and reduced nitrogen fertilizer use efficiency. The treatment of low water kept high content of NO3--N in root zone, helped the absorption of the crops and raised the efficiency of water and nitrogen. A positive correlation existed in amount of nitrogen application and NO3--N accumulation in root zone. Compared with NO3--N, the content of NH4+-N was lower and basically did not change. The best coupling form was the treatment of low water and high nitrogen.

Key words: Alternate furrow irrigation, Maize, water and nitrogen, Transport, Accumulation