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水层厚度变化对稻田能量分配的影响

刘斌1,2,胡继超1,2**,於琍3   

  1. 1南京信息工程大学生态气象环境研究中心, 南京 210044; 2江苏省农业气象重点实验室, 南京 210044; 3中国气象局国家气候中心, 北京 100081)
  • 出版日期:2015-03-10 发布日期:2015-03-10

Effects of water depth change on energy distribution in paddy rice field.

LIU Bin1,2, HU Ji-chao1,2**, YU Li3   

  1. (1International Center for Ecology, Meteorology and Environment, Nanjing University of Information Science & Technology, Nanjing 210044, China; 2Key Laboratory of Agricultural Meteorology of Jiangsu Province, Nanjing University of Information Science & Technology, Nanjing 210044, China; 3National Climate Centre, China Meteorological Administration, Beijing 100081, China)
  • Online:2015-03-10 Published:2015-03-10

摘要:

稻田土表因存在水层厚度变化和干湿交替,导致垂直方向的能量收支状况发生改变。本文采用逐时多元回归方法,分析了水层、叶面积及气象因子对各能量贡献,并选取典型相似天气以规避能量输入差异、按叶面积划分以规避植冠层结构差异,定量研究了稻田水层厚度变化对稻田能量分配的影响。结果表明:白天,随稻田水层厚度增加,水层储热量也增大,导致水面热通量增大,从而降低了稻田潜热通量,这种作用在水稻冠层稀疏时期尤其明显;在冠层密集时,到达水面的净辐射能量被削弱,水层厚度对潜热通量的调节作用降低;由于稻田感热通量总体较低,水层厚度的变化对其影响小,调节作用不明显;双源蒸散模型模拟揭示,水面潜热随水层深度增加而减少是导致总潜热降低的主要原因,且在水稻冠层稀疏时期表现明显。
 

关键词: 黄土高原, 长期施肥, 氮肥当季利用率, 黄绵土, 氮肥累积利用率

Abstract: The variations of water depth and wetdry alternation in paddy field lead to the energy budget changing vertically. In this paper, an investigation was made to quantify the contribution of water depth, leaf area index and meteorological factors on energy distribution by using multiple regressions. Similar meteorological conditions and leaf area index, which can reduce the differences of energy input and canopy structure respectively, were chosen to quantify the effects of water depth on energy partitioning in a paddy field. The results showed that, with the increase of water depth, both water heat storage and water heat flux above soil layer increased, leading to a decrease in the latent heat during the daytime, especially in the period with sparse canopy. However, due to the decrease in net radiation of water surface in the period with dense canopy, the effects of water depth on the latent heat flux became small. The effect of water depth on sensible heat was not obvious, and could be ignored. The simulated results of the dualsource evapotranspiration model showed that the decrease of water latent heat with the increase of water depth was a major cause reducing the total latent heat, and this phenomenon was more obvious in the period with sparse canopy.

Key words: loessial soil, annual nitrogen fertilizer use efficiency, accumulated nitrogen fertilizer use efficiency, long-term fertilization, Loess Plateau