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Quantification of excess water loss in plant canopies warmed with infrared heating.

机译:量化用红外加热加热的植物冠层中多余水分的流失。

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Here we investigate the extent to which infrared heating used to warm plant canopies in climate manipulation experiments increases transpiration. Concerns regarding the impact of the infrared heater technique on the water balance have been raised before, but a quantification is lacking. We calculate transpiration rates under infrared heaters and compare these with air warming at constant relative humidity. As infrared heating primarily warms the leaves and not the air, this method increases both the gradient and the conductance for water vapour. Stomatal conductance is determined both independently of vapour pressure differences and as a function thereof, while boundary layer conductance is calculated using several approaches. We argue that none of these approaches is fully accurate, and opt to present results as an interval in which the actual water loss is likely to be found. For typical conditions in a temperate climate, our results suggest a 12-15% increase in transpiration under infrared heaters for a 1 degrees C warming. This effect decreases when stomatal conductance is allowed to vary with the vapour pressure difference. Importantly, the artefact is less of a concern when simulating heat waves. The higher atmospheric water demand underneath the heaters reflects naturally occurring increases of potential evapotranspiration during heat waves resulting from atmospheric feedback. While air warming encompasses no increases in transpiration, this fully depends on the ability to keep humidity constant, which in the case of greenhouses requires the presence of an air humidification system. As various artefacts have been associated with chamber experiments, we argue that manipulating climate in the field should be prioritized, while striving to limit confounding factors. The excess water loss underneath infrared heaters reported upon here could be compensated by increasing irrigation or applying newly developed techniques for increasing air humidity in the field.
机译:在这里,我们研究了在气候操纵实验中用于加热植物冠层的红外加热增加蒸腾作用的程度。以前已经提出了关于红外线加热器技术对水平衡的影响的担忧,但是缺乏量化。我们计算红外加热器下的蒸腾速率,并将其与恒定相对湿度下的空气加热进行比较。由于红外加热主要是加热叶子而不是加热空气,因此此方法会增加水蒸气的梯度和电导率。气孔电导率的确定既独立于蒸气压差,又取决于蒸汽压差的函数,而边界层电导率则使用几种方法进行计算。我们认为,这些方法都不是完全准确的,而是选择将结果作为可能发现实际失水的时间间隔进行展示。对于温带气候下的典型条件,我们的结果表明,在1摄氏度的温度下,红外加热器下的蒸腾作用增加12-15%。当允许气孔电导随蒸汽压差而变化时,该效果降低。重要的是,在模拟热波时,假象不再是问题。加热器下方较高的大气需水量反映了由于大气反馈导致的热浪期间自然蒸发蒸腾量的自然增加。空气变暖不包括蒸腾作用的增加,但这完全取决于保持湿度恒定的能力,在温室中,这需要存在空气加湿系统。由于各种文物已与室内实验相关联,我们认为应该优先控制野外气候,同时努力限制混杂因素。此处报道的红外加热器下方的过多失水可以通过增加灌溉量或应用新开发的增加田间空气湿度的技术来弥补。

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