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Energy exchange and evapotranspiration over irrigated seed maize agroecosystems in a desert-oasis region, northwest China

机译:西北荒漠绿洲地区灌溉种子玉米农业生态系统的能量交换和蒸散

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Investigating the dynamics of energy and water vapor exchange in oasis agroecosystems is important to improve scientific understanding of land surface processes in desert-oasis regions. In this study, water vapor and energy fluxes were obtained by using an eddy covariance technique for two similar irrigated seed maize fields at Yingke and Pingchuan, in northwest China. Seasonal variabilities of evapotranspiration (ET) and relevant environmental and biophysical factors were explored. Results showed that the energy balance closures were reasonable, with energy balance ratio of 0.99 and 0.79 for a half-hourly time scale at Yingke and Pingchuan, respectively. The seasonal changes in net radiation (RQ), latent heat flux (LE), and sensible heat flux (H) of Yingke and Pingchuan were similar. Net radiation was 11.27 MJ m(-1) day(-1) during the growing season. Latent heat flux accounted for 67.5% of net radiation, sensible heat flux was 25.0%, and soil heat flux was 7.5%. A reverse" seasonal change was found in partitioning energy flux into LE and H. The seasonal variation in energy flux partitioning was significantly related to the phenology of maize. During the growing season, ET was 467 and 545 mm, and mean daily ET 2.84 and 3.35 mm day(-1) at Pingchuan and Yingke, respectively. "Non-growing" season ET was 15% of the annual ET in the bare field (during October-March) and 85% of the annual ET for maize (during April-September). Daily ET was mainly controlled by net radiation and air temperature, and was significantly affected by leaf area index (3.0 m(2) m(-2)) and canopy conductance (10 mm s(-1)). Furthermore, irrigation promoted daily ET greatly during the growing season. Accurate estimation of seed maize ET and determination the controlling factors helps to develop exact irrigation scheduling and improve water resource use in desert-oasis agroecosystems. (C) 2016 Elsevier B.V. All rights reserved.
机译:研究绿洲农业生态系统中能量和水蒸气交换的动力学,对于增进对沙漠绿洲地区土地表面过程的科学理解至关重要。在这项研究中,水汽和能量通量是通过使用涡度协方差技术获得的,在中国西北地区英科和平川两个相似的灌溉种子玉米田中。探讨了蒸散量(ET)的季节变化以及相关的环境和生物物理因素。结果表明,能量平衡的闭合是合理的,在英科和平川的半小时尺度上,能量平衡比分别为0.99和0.79。英科和平川的净辐射(RQ),潜热通量(LE)和显热通量(H)的季节变化相似。在生长季节中,净辐射为11.27 MJ m(-1)天(-1)。潜热通量占净辐射的67.5%,显热通量为25.0%,土壤热通量为7.5%。在将能量通量分配给LE和H时发现了一个相反的季节性变化。能量通量分配的季节变化与玉米的物候显着相关。在生长季节,ET分别为467和545 mm,平均日ET为2.84和平川和英科分别为3.35毫米日(-1),“非生长”季节ET占裸地(10月至3月)的年度ET的15%,玉米(4月期间)的年度ET的85%。 -9月):每日ET主要受净辐射和气温控制,并受到叶面积指数(<3.0 m(2)m(-2))和冠层导度(<10 mm s(-1))的显着影响。 。此外,灌溉在生长季节极大地促进了每日ET的增长,准确估算种子玉米ET并确定控制因素有助于制定精确的灌溉计划并改善荒漠绿洲农业生态系统的水资源利用(C)2016 Elsevier BV版权所有。

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