黄土高原旱地夏闲期残留肥料氮淋溶特性研究
作者:
作者单位:

1.秦岭国家植物园/西北农林科技大学资源环境学院;2.中国市政工程西北设计研究院有限公司/西北农林科技大学资源环境学院;3.西北农林科技大学资源环境学院/农业农村部西北植物营养与农业环境重点实验室;4.西北农林科技大学资源环境学院/农业部西北植物营养与农业环境重点实验室;5.西北农林科技大学水土保持科学与工程学院(水土保持研究所)

作者简介:

通讯作者:

中图分类号:

基金项目:

国家自然科学基金项目(42277343,31372137)资助


Leaching Characteristics of Residual Fertilizer Nitrogen in the Dryland of Loess Plateau During the Summer Fallow Period
Author:
Affiliation:

1.Qingling National Botanical Garden/College of Resources and Environment, Northwest A&F University;2.CSCEC AECOM Consultants Co., Ltd./College of Resources and Environment, Northwest A&F University;3.College of Resources and Environment, Northwest A&F University/Northwest Key Laboratory of Plant Nutrition and Agricultural Environment, Ministry of Agriculture and Rural Affairs;4.College of Natural Resources and Environmental,Northwest A&F University,Key Laboratory of Plant Nutrition and the Agri-environment in Northwest China,Ministry of Agriculture;5.College of Soil and Waster Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University

Fund Project:

Supported by the National Natural Science Foundation of China (Nos. 42277343 and 31372137)

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    冬小麦-夏休闲是黄土高原旱地典型的种植模式,夏闲期间为该地区雨季,加上土壤表面裸露,一季作物收获后土壤残留肥料氮的淋失特性是值得关注的问题。在大型渗漏池(3 m×2.2 m×3 m)上采用15N示踪技术于第一季(2014年)小麦播种前基施15N肥料(150 kg•hm-2),测定小麦收获后15N肥料被小麦吸收和土壤残留的量,之后连续3年(2015—2017年)夏季休闲期间测定第一季小麦收获后土壤中残留的15N肥料在0~200 cm土壤剖面中的15N丰度及含量变化,旨在研究残留肥料氮连续多年在夏季休闲期间的淋溶特性。结果表明,小麦对当季15N肥料的利用率(吸收量/施氮量)为53.9%,一季小麦收获后残留于0~100 cm土壤中的肥料氮平均为施氮量的36.3%。第一年夏季休闲前残留肥料氮主要累积在0~40 cm土层,15NO3--N多累积在80 cm以上土层;而休闲后60~100 cm土层残留肥料氮显著增加,80~100 cm土层15NO3--N累积量显著增加。随着年限增加,残留肥料氮及15NO3--N持续向土壤深层迁移;在正常降水条件下,一个夏季休闲期间残留肥料氮向下迁移的速度平均为20 cm。夏季休闲期间0~100 cm土壤中残留肥料氮减少,100~200 cm土壤中增加,同一年休闲前后0~200 cm土壤剖面残留肥料氮累积总量损失小,说明残留肥料氮在土壤剖面的再分配是其迁移的主要机制。

    Abstract:

    【Objective】Summer fallow after winter wheat harvest in dryland is a common practice on the Loess Plateau. However, due to bare land and intensive rainfall during summer fallow, the leaching characteristics of residual fertilizer nitrogen (N) after crop harvest deserve attention. This study aimed to reveal that the destination of applied N fertilizer after wheat season and the leaching characteristics of residual N fertilizer during summer fallow in dryland of the Loess Plateau. 【Method】This study was carried out in large lysimeters (3 m×2.2 m×3 m) by the 15N labeled method. 15N labeled urea was applied at the beginning as basal fertilizer with the rate of 150 kg•hm-2. Firstly, the absorption of 15N labeled fertilizer by wheat and the residual N in the soil after wheat harvest were investigated, and subsequently the 15N abundance and content changes of residual 15N labeled fertilizer in the soil profile were measured during the summer fallow of three years (2015—2017). 【Result】The results showed that the average absorption of nitrogen fertilizer by wheat was 53.9% while the amount of 15N fertilizer distributed in the soil (0-100 cm) after wheat harvest was 36.3% of the N application rate, with an average of 40.1% being in nitrate form. In the first year, the residual 15N fertilizer which accumulated in the 0-40 cm soil layer moved downward and accumulated in the 60-80 cm soil layer during the following summer fallow. The 15NO3--N mainly accumulated in the above 80 cm soil layer before summer fallow, but the accumulation peak of 15NO3--N was in the 80-100 cm soil layer at the end of fallow. In the second and third years, the residual 15N fertilizer and 15NO3--N moved downward about 20 cm, respectively, during summer fallow. After the summer fallow, the amount of residual 15N fertilizer in the 0-100 cm soil layer decreased, but the amount of residual 15N fertilizer and 15NO3--N in the 100-200 cm soil layer both increased. Specifically, the amount of residual N in the 100-200 cm soil layer increased by 1.9 and 7.0 kg•hm-2 during the summer fallow of the second and third years, respectively. Also, the amount of 15NO3--N in the 100-200 cm soil layer increased by 2.7 and 7.0 kg•hm-2 during the summer fallow of the second and third years, respectively. 【Conclusion】During the summer fallow, residual N fertilizer leached significantly. Under normal precipitation conditions, the average downward migration rate of residual N fertilizer during a summer fallow was 20 cm. As the age increased, the residual N fertilizer in the 0-100 cm soil decreased; while it increased in the 100-200 cm soil layer, with nitrate as the main leached form. However, the cumulative total loss of residual N fertilizer in the 0-200 cm soil profile during summer fallow was small, indicating that the redistribution of residual N fertilizer nitrogen in the soil profile was the main mechanism.

    参考文献
    相似文献
    引证文献
引用本文

夏梦洁,王辉民,雷霜,赵梦真,冯浩,周建斌.黄土高原旱地夏闲期残留肥料氮淋溶特性研究[J].土壤学报,DOI:10.11766/trxb202308250340,[待发表]
XIA Mengjie, WANG Huimin, LEI Shuang, ZHAO Mengzhen, FENG Hao, ZHOU Jianbin. Leaching Characteristics of Residual Fertilizer Nitrogen in the Dryland of Loess Plateau During the Summer Fallow Period[J]. Acta Pedologica Sinica, DOI:10.11766/trxb202308250340,[In Press]

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2023-08-25
  • 最后修改日期:2023-11-10
  • 录用日期:2023-12-05
  • 在线发布日期: 2023-12-07
  • 出版日期: