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TEST OF A MICROLYSIMETER FOR MEASUREMENT OF SOIL EVAPORATION

机译:测试用于测量土壤蒸发的微分尺

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摘要

Quantifying soil evaporation is required on studies of soil water balance and applications aiming to improve water use efficiency by crops. The performance of a microlysimeter (ML) to measure soil evaporation under irrigation and non-irrigation was evaluated. The MLs were constructed using PVC tubes, with dimensions of 100 mm inner diameter, 150 mm depth and 2.5 mm wall thickness. Four MLs were uniformly distributed on the soil surface of two weighing lysimeters conducted under bare soil, previously installed at Iapar, in Londrina, PR, Brazil. The lysimeters had 1.4 m width, 1.9 m length and 1.3 m depth and were conducted with and without irrigation. Evaporation measurements by MLs (E-ML) were compared with measurements by lysimeters (E-L) during four different periods in the year. Differences between E-ML and E-L were small either for low or high atmospheric demand and also for either irrigated or non-irrigated conditions, which indicates that the ML tested here is suitable for measurement of soil evaporation.
机译:在土壤水分平衡和旨在提高作物水分利用效率的应用研究中,需要量化土壤蒸发。评估了微分仪(ML)在灌溉和非灌溉条件下测量土壤蒸发的性能。ML使用PVC管制成,内径为100毫米,深度为150毫米,壁厚为2.5毫米。四个ML均匀分布在两个称重溶解仪的土壤表面,这些溶解仪是在裸露的土壤下进行的,以前安装在巴西PR州Londrina的Iapar。溶度计宽1.4米,长1.9米,深1.3米,在有和没有灌溉的情况下进行。将MLs(E-ML)的蒸发测量值与溶解仪(E-L)的测量值进行了比较。E-ML和E-L之间的差异很小,无论是在低大气需求还是高大气需求下,在灌溉或非灌溉条件下,都表明这里测试的ML适用于土壤蒸发的测量。

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