中国农业科学 ›› 2020, Vol. 53 ›› Issue (19): 3996-4009.doi: 10.3864/j.issn.0578-1752.2020.19.013

• 土壤肥料·节水灌溉·农业生态环境 • 上一篇    下一篇

基于不同方法的汉中盆地稻麦轮作土壤供氮能力评价

张方方1,2(),马宁博1,3,岳善超1,2,李世清1,2()   

  1. 1西北农林科技大学资源环境学院,陕西杨凌 712100
    2西北农林科技大学黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西杨凌 712100
    3陕西省汉中市汉台区人民政府,陕西汉中 723000
  • 收稿日期:2020-01-07 接受日期:2020-04-13 出版日期:2020-10-01 发布日期:2020-10-19
  • 通讯作者: 李世清
  • 作者简介:张方方,Tel:18907799055;E-mail: setzhang@126.com
  • 基金资助:
    国家重点研发计划(2017YFD0201807)

Evaluation of Nitrogen Supply Capacity of Paddy and Wheat Rotation Soil in Hanzhong Basin by Different Determination Methods

ZHANG FangFang1,2(),MA NingBo1,3,YUE ShanChao1,2,LI ShiQing1,2()   

  1. 1College of Resources and Environment, Northwest A&F University, Yangling 712100, Shannxi
    2State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Northwest A&F University, Yangling 712100, Shaanxi
    3People's Government of Hantai District in Hanzhong, Hanzhong 723000, Shaanxi
  • Received:2020-01-07 Accepted:2020-04-13 Online:2020-10-01 Published:2020-10-19
  • Contact: ShiQing LI

摘要:

【目的】比较多种指标评价汉中盆地稻麦轮作土壤供氮能力的可靠性,为当地土壤氮素管理提供参考。【方法】以采集于汉中盆地及周边丘陵区的12个农田耕层土壤为供试土样,以盆栽黑麦草地上部累积吸氮量为参比,以土壤理化性质指标以及矿质氮法、KCl冷凝回流法、酸性高锰酸钾法3种化学方法和淹水培养法、通气培养法2种生物培养方法测定土壤氮素矿化量作为土壤供氮能力指标。【结果】土壤类型是影响土壤供氮能力的重要因素;土壤全氮或有机质可以反映土壤潜在供氮能力;土壤质地、pH、有效磷、CEC、碳酸钙、颗粒组成(砂粒、粉粒、黏粒)均不能反映稻麦轮作土壤供氮能力。矿质氮法测定氮素值与作物吸氮量相关系数为 0.963(P<0.01),但由于起始矿质氮不能反映有机氮矿化量,故矿质氮法只能反映当前供氮能力,不宜作为土壤供氮能力评价指标;KCl冷凝回流法测得的总矿质氮量与作物吸氮量相关系数为0.912(P<0.01),而KCl冷凝回流法测得的可矿化氮量与作物吸氮量相关系数为-0.766(P<0.01),由于KCl冷凝回流法浸取土壤可矿化氮过程中会造成铵态氮的挥发,导致在反映土壤潜在供氮能力和总供氮能力上可能不一致,故KCl冷凝回流法不是反映汉中盆地土壤供氮能力的理想指标;酸性高锰酸钾法测得的总矿质氮量和可矿化氮量与作物吸氮量相关系数分别为0.847和0.833(P<0.01),既能够反映土壤潜在供氮能力,又能够反映总供氮能力,是最佳化学方法。通气培养条件下,总矿质氮量和可矿化氮与作物吸氮量均不相关,而在淹水培养条件下,总矿质氮量和可矿化氮与作物吸氮量的相关系数分别为0.921和0.890(P<0.01),表明淹水培养法可以反映汉中盆地稻麦轮作土壤潜在供氮能力和总供氮能力,是良好的生物培养方法。氮素矿化势(N0)和起始矿质氮+N0与前4期黑麦草地上部累积吸氮量相关系数分别为0.834和0.845(P<0.01),与整株累积吸氮量相关系数分别为0.840和0.851(P<0.01)。表明,N0和起始矿质氮+N0均可反映土壤潜在供氮能力,但N0仅能够反映土壤潜在供氮能力,起始矿质氮+N0可反映土壤潜在供氮能力和总供氮能力,因此,起始矿质氮+N0是评价汉中盆地稻麦轮作土壤供氮能力的理想指标。【结论】对于汉中盆地稻麦轮作土壤供氮能力的评价,酸性高锰酸钾法是最佳化学方法;淹水培养法是良好的生物培养方法,起始矿质氮+N0是反映汉中盆地土壤供氮能力的理想指标。

关键词: 稻麦轮作, 潜在供氮能力, 总供氮能力, 黑麦草地上部吸氮量, 化学测定方法, 生物培养方法, 汉中盆地

Abstract:

【Objective】 The different indexes were compared to evaluate the reliability of nitrogen (N) supply capacity of soil in Hanzhong basin, so as to provide references for local soil N management.【Method】Soil samples were collected from 12 farmlands in Hanzhong basin and the surrounding hilly areas. The cumulative N uptake of potted ryegrass was used as a reference. Soil physical and chemical properties parameters were used as the indexes of soil N supply capacity, which included soil N mineralization amount based on three chemical methods (mineral N method, KCl condensation and reflux acid potassium permanganate method) and two biological methods (aerobic incubation and waterlogged incubation). 【Result】Soil type was an important factor that affected the N supply capacity of soil. Total N or organic matter could reflect the potential N supply capacity. However, soil texture, pH, available phosphorus (Ava.P), cation exchange capacity (CEC), calcium carbonate and particle composition (sand, silt and clay) could not reflect the N supply capacity. The correlation coefficient between aboveground N uptake of ryegrass and N value by mineral N method was 0.963 (P<0.01). However, since the initial mineral N could not reflect the amount of organic N mineralization, the mineral N method could only reflect the current N supply capacity, so it was not suitable as an evaluation index of soil N supply capacity. The correlation coefficient between aboveground N uptake of ryegrass and total mineral N measured by KCl reflux condensation method was 0.912 (P<0.01), while the correlation coefficient between aboveground N uptake of ryegrass and the amount of mineralizable N measured by KCl condensate reflux method was -0.766 (P<0.01). Because the leaching process of soil mineralizable N by KCl refluxing method led to the volatilization of ammonium N, which might result in the inconsistency in reflecting the potential N supply capacity and the total N supply capacity, so KCl refluxing method was not an ideal indicator to reflect the soil N supply capacity of Hanzhong basin. The correlation coefficients of total mineral N and mineralizable N with aboveground N uptake of ryegrass were 0.847 and 0.833 (P<0.01), respectively, which could reflect both the potential N supply capacity and the total N supply capacity, and it was the best chemical method. Under the condition of aerobic incubation, total mineral N and mineralizable N were not correlated with aboveground N uptake of ryegrass. While under the condition of waterlogged incubation, the correlation coefficients of total mineral N and mineralizable N with aboveground N uptake of ryegrass were 0.921 and 0.890 (P<0.01), respectively, indicating that the waterlogged incubation method could reflect the potential N supply capacity and total N supply capacity of paddy and wheat rotation soil in Hanzhong basin, and it was a good biological incubation method. The correlation coefficients of N0 and initial mineral N + N0 with aboveground N uptake of ryegrass in the first four stages were 0.834 and 0.845(P<0.01), respectively. The correlation coefficients with N uptake of the whole ryegrasses were 0.840 and 0.851(P<0.01), respectively. Both N0 and initial mineral N + N0 could reflect the potential N supply capacity. But N0 could only reflect the potential N supply capacity, while initial mineral N + N0 could reflect the potential N supply capacity and total N supply capacity. Therefore, initial mineral N + N0 was an ideal index.【Conclusion】For the evaluation of N supply capacity of rice-wheat rotation soil in Hanzhong basin, the acid potassium permanganate method was the best chemical method, and the waterlogged incubation method was a good biological incubation method. The initial mineral N + N0 was an ideal indicator to reflect the N supply capacity of soil in Hanzhong basin.

Key words: rice and wheat rotation, potential N supply capacity, total N supply capacity, aboveground N uptake of ryegrass, Chemical determination methods, Biological culture methods, Hanzhong Basin