人民长江 ›› 2021, Vol. 52 ›› Issue (3): 172-178.doi: 10.16232/j.cnki.1001-4179.2021.03.030

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灌水量对涌泉根灌湿润体水氮运移特性的影响

何振嘉   

  • 出版日期:2021-03-28 发布日期:2021-04-23

Effect of irrigation volume on water and nitrogen migration characteristics of wetting body in bubbled-root irrigation

HE Zhenjia   

  • Online:2021-03-28 Published:2021-04-23

摘要: 为研究不同灌水量条件下涌泉根灌肥液入渗湿润体特征值的变化规律及水氮运移特性,在陕北米脂县远志山矮化密植山地枣树试验基地原状土上进行了涌泉根灌肥液入渗试验。结果表明:(1)灌水量对湿润锋运移、湿润体体积、含水量及氮素分布运移都有显著的影响。在水平剖面上,水平方向和竖直方向上的湿润锋运移距离均随灌水量减小而增大;在垂直剖面上,灌水量与水平方向的湿润锋运移距离成正比,与竖直方向的运移距离成反比。(2)各剖面上湿润锋运移距离均可由幂函数进行拟合。灌水量越大,湿润体体积也越大,且湿润体显得越宽、越深,灌水结束时湿润体相同位置处的含水率也越高。(3)在水分再分布过程中,湿润体内的含水率逐步趋于稳定,湿润体会继续扩大,但湿润体内含水率较灌水结束时明显降低。(4)不同灌水量下的湿润体在相同土层深度处的氮素含量会随灌水量的增大而升高,硝态氮运移与水分运动规律较为相似,再分布过程中各土层硝态氮含量随分布时间的延长而降低,并在湿润体土壤含水率达到田间持水量时基本趋于稳定。水分运动对铵态氮含量分布及运移的影响并不显著,在水分再分布过程中,不同土层深度处铵态氮含量随灌水量的增大呈现先增大后减小的趋势,再分布时间越长,湿润体内的肥液分布越均匀,但土壤中铵态氮含量总体呈减少趋势。

关键词: 涌泉根灌; 灌水量; 肥液入渗; 湿润体; 水氮分布;

Abstract: To study the characteristics of water and nitrogen migration and the variation of the characteristic values of the infiltration wetting body in bubbled-root irrigation, the infiltration experiment of fertilizer solution was carried out in the undisturbed soil of the jujube test base of the Yuanzhi Mountain dwarf dense planting area in Mizhi County, northern Shaanxi Province.The results showed that:(1) The irrigation volume had significant effects on the wetting front migration, wetting body volume, water content and nitrogen distribution and migration.In the horizontal profile, the wetting front migration distance in the horizontal direction and the vertical direction increased with the decrease of the irrigation volume.In the vertical profile, the irrigation volume was proportional to the wetting front migration distance in horizontal direction, and it was inversely proportional to the wetting front migration distance in vertical direction.(2) The wet front migration distance on horizontal and vertical profiles can be fitted by power functions.The larger the irrigation volume was, the larger the wetting body volume was, the wider and deeper the wetting body appeared, and the higher the water content at the same position of the wetting body at the end of the irrigation was.(3) In the process of water redistribution, the water content in the wetting body gradually stabilized, and the wetting body continued to expand, but the water content in the wetting body was significantly lower than that at the end of the irrigation.(4) The nitrogen content of the wetting body at different soil depths increased with the increase of irrigation volume.The nitrate nitrogen migration law and water movement law were similar.In the process of redistribution, the content of the nitrate nitrogen in different soil layers decreased with the increase of distribution time, and tended to be stable when the water content of the wetting body reached the field water holding capacity.The effect of water movement on the distribution and migration of ammonium nitrogen was not significant.In the process of water redistribution, the content of ammonium nitrogen in different soil depths increased first and then decreased with the increase of irrigation volume.The longer the redistribution time was, the more uniform the distribution of fertilizer solution in the wetting body was, but the ammonium nitrogen content in the soil generally decreased.

Key words: bubbled-root irrigation; irrigation volume; fertilizer solution infiltration; wetting body; water and nitrogen distribution;