山东省禹城市夏玉米生长期水分利用特征分析
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S513

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国家自然科学基金项目(41571504);国家科技支撑计划项目(2013BAC03B04)


The Water-use characteristics of Summer Corn during Growing Period in Yuchen, Shandong Province
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    摘要:

    以山东省禹城地区夏玉米农田为例,利用氢氧稳定同位素技术测定2015年夏玉米生长期茎干水、大气降水以及不同深度土壤水中δD和δ18O组成,利用直接对比法和多元线性混合模型法分析夏玉米对土壤水的利用情况,并分析农田降水-土壤水-作物水之间的转化规律。降水同位素测定结果显示禹城地区大气降水线方程为δD=6.55δ18O-3.03(R2=0.88),斜率和截距均小于全球大气降水线,表明蒸发是导致同位素富集的主要过程。对夏玉米生长期水分来源特征分析表明,出苗期主要利用表层0—15 cm土壤水,贡献率达73.9%;拔节期从土壤不同深处均吸收水分(0—55 cm,81.8%),30—55 cm处土壤水利用相对较多,同时也会利用同时期降雨;抽穗期较多利用深层土壤(30—55 cm,71%),此时期浅层土壤蒸发强烈,含水量快速减少,植物可利用水分较少。而30—100 cm处土壤含水量受温度,土壤蒸发影响较小,为夏玉米生长持续提供稳定水分。灌浆期吸收各层土壤水分的量相近(15—100 cm,72%),此时期无降水,温度下降,蒸发减弱,各层土壤含水量较稳定。成熟期主要吸收30—100 cm处的土壤水分,贡献率达70%,表明降雨较少时,夏玉米吸收土壤水分依赖于较深层土壤。此外,夏玉米生长期水分来源受土壤体积含水量及土壤蒸发蒸腾的影响较大,同时降雨,大气温度及湿度会影响土壤含水量。通过水量平衡模型计算得出2015年夏玉米在出苗期、拔节期、抽穗期、灌浆期、成熟期的农田蒸散量分别为35.62,34.99,32.4,22.31,16.94 mm。研究结果对于夏玉米不同生长期节水灌溉具有指导意义。

    Abstract:

    In this study, we uses hydrogen and oxygen stable isotope tracer technique to determine the water isotopic compositions of precipitation, soil water at different depth and stalks of summer corn during the growing season in 2015 in Yucheng, Shandong Province. On the base of these measurements, using direct comparison and multivariate linear regression methods, we analyzed the sources of summer corn root water uptake and their contributions, and further discussed field water movement and transference laws in the precipitation-soil-crop continuum. The precipitation isotope measurements showed that the atmospheric precipitation equation was δD=6.55δ18O-3.03 (R2=0.88) for Yucheng area. The analyses of water source during the growing period showed that summer corn mainly used surface (0—15 cm) soil water during the seedling stage and the contribution rate was 73.9%; during the jointing stage, it mainly imbibed water from the 0—50 cm soil layer (81.8%), and the water from the 30—55 cm soil layer was used relatively more. In addition, the precipitation was also significantly used during this period. In contrast, the water used was mostly from deeper soil layer during the heading stage (30—55 cm, 71%). During this period, the evaporation was high and soil water content decreased rapidly in the shallow soil layer, and water that could be used by plants was less. Because the water content in the deeper soil layer (30—100 cm) was less affected by air temperature and soil evaporation, it could provide water for summer corn during the heading stage stably. During the filling stage, the amount of soil water absorbed from each layer was similar (15—100 cm, 72%); the precipitation was small, the temperature dropt and the evaporation decreased, and soil water content in each layer was relatively stable. During the mature stage, the summer corn mainly absorbed water from the 30—100 cm soil layer and the contribution rate was 70%, indicating that the absorption of soil water of summer corn mainly relied on deeper soil layers when the precipitation was small. Furthermore, the results showed that the water sources of summer corn were significantly affected by soil water content and soil evapotranspiration, meanwhile, precipitation, air temperature and humidity affected soil water content. The water balance model showed that the evapotranspiration of summer corn during the seedling, jointing, heading and filling stage was 35.62, 34.99, 32.4, 22.31, 16.94 mm, respectively. This study presents guidelines for summer corn water-saving irrigation during different growth stage in Yucheng area.

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王冰洋, 陈报章, 孙少波, 周子渊, 杨志青, 刘禹淇, 张景文.山东省禹城市夏玉米生长期水分利用特征分析[J].水土保持学报,2016,(6):153~161

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  • 在线发布日期: 2016-12-30
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