Soil surface-atmosphere interaction in a monitored embankment constructed with two compacted lime-treated soils

Katia Bicalho, Thiago Poleto, Yu-Jun Cui, Yasmina Boussafir
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Abstract

This study was carried out in an instrumented and monitored embankment divided into two symetrical sections and constructed with compacted treated soils (i.e., a silty soil and a clayey soil) exposed to the same atmospheric conditions in a continental climate, with oceanic influences. It aimed to investigate changes of bare soil surface moisture (w) and corresponding suction (s) as result of soil water evaporation processes on a monthly time scale. Seasonal variations in the w (and s) measurement in both soil surfaces show overall consistency with the meteorological measurement within the study area. The paper also examines the ability of four air temperature-based potential evaporation (PET) formulations to capture the process of evaporation at the site. Results indicated that soil water evaporation is controlled by both atmospheric and soil conditions. And, during the most significant drying time period, the measured s consistently increased and the corresponding w decreased suggesting a relatively significant water evaporation effect. However, the monthly predicted PET data varied from a maximum of over 120 mm/month to less than 50 mm/month during the drying time, depending on the used method. The continuously monitored soil surface suctions are used for discussing the variations of evaporation according to the predicted PET method and time period at the site.
用两种经石灰处理的压实土建造的监测堤坝中的土表-大气相互作用
这项研究是在受海洋影响的大陆性气候中,在相同的大气条件下,用仪器对堤坝进行监测,堤坝分为两个对称部分,并用压实处理过的土壤(即淤泥质土壤和粘性土壤)建造。其目的是研究裸土表面湿度(w)和相应吸力(s)的变化,这是土壤水分蒸发过程的月度结果。两种土壤表面水分(和吸力)测量值的季节性变化与研究区域内的气象测量值基本一致。本文还研究了四种基于气温的潜在蒸发(PET)公式捕捉现场蒸发过程的能力。结果表明,土壤水分蒸发受大气和土壤条件的控制。在最干燥的时期,测量到的 s 持续增加,而相应的 w 则减少,这表明水分蒸发效应相对显著。然而,在干燥期间,月预测 PET 数据从最大超过 120 毫米/月到不足 50 毫米/月不等,这取决于所使用的方法。连续监测的土壤表面吸力可用于讨论根据预测 PET 方法和时间段在该地点的蒸发变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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