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首页> 外文期刊>Tunnelling and underground space technology >Evaporation-induced soil water flux to design suction drain for low-carbon ground stabilisation: Experimental investigation and modelling
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Evaporation-induced soil water flux to design suction drain for low-carbon ground stabilisation: Experimental investigation and modelling

机译:蒸发引起的土壤水通量,设计用于低碳地面稳定的吸水管:实验研究和建模

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摘要

The suction drain is a novel concept for low-carbon temporary ground stabilisation in clayey soils alternative to jet grouting and ground freezing. Boreholes are drilled into the ground and air is injected to the borehole end through a delivery pipe. The air flowing through the gap between the pipe and the borehole surface backward towards the borehole entry removes water by evaporation and, hence, increases the undrained shear strength of the soil surrounding the drain. There are no studies that allow quantifying soil water evaporation generated by tangential airflow for the case of 'wind tunnel' only a few centimetres high over an evaporating surface a few meters long. This paper first presents an experimental investigation on water evaporation induced by air flow. A 3 m long wet surface was subjected to tangential air flow into a 40 mm gap. Tests were carried out by considering different air velocities and inlet air relative humidities. A model was then formulated to quantify the water evaporation rate for any length of the wet surface. The model parameters were calibrated against one experimental dataset and the model was then validated against an independent dataset. Finally, an empirical equation is proposed to estimate model parameters without the need of carrying out experimental tests. This is based on the vapour transfer coefficient established empirically for evaporation from open water (external air flow), which was found to remain valid for confined evaporation (internal air flow). The paper therefore provides a tool to estimate airflow-induced evaporation to successfully design the suction drains.
机译:抽水排水道是一种新颖的概念,可用于在粘土质土壤中进行低碳临时地面稳定,以替代喷射灌浆和地面冻结。钻孔被钻入地下,空气通过输送管注入到钻孔端。流过管道和井眼表面之间的缝隙的空气朝井眼入口向后流动,通过蒸发将水除去,因此增加了排水沟周围土壤的不排水剪切强度。对于“风洞”,在几米长的蒸发表面上只有几厘米高的情况,尚没有研究能够量化切向气流产生的土壤水分蒸发。本文首先对气流引起的水蒸发进行了实验研究。使3 m长的湿表面沿切线空气流进入40 mm的间隙中。通过考虑不同的空气速度和进气相对湿度进行测试。然后制定模型以量化湿表面任何长度的水蒸发速率。针对一个实验数据集校准模型参数,然后针对独立数据集验证模型。最后,提出了一个经验公式来估计模型参数,而无需进行实验测试。这是基于凭经验确定的用于从开放水蒸发(外部气流)的蒸汽传递系数,发现该系数对于受限蒸发(内部气流)仍然有效。因此,本文提供了一种工具,用于估计气流引起的蒸发,从而成功设计吸水口。

著录项

  • 来源
    《Tunnelling and underground space technology》 |2020年第5期|103292.1-103292.19|共19页
  • 作者

  • 作者单位

    UNOPS Hlth Safety Social & Environm Management Copenhagen Denmark|Univ Strathclyde Dept Civil & Environm Engn James Weir Bldg Level 5 75 Montrose St Glasgow G1 1XJ Lanark Scotland;

    Univ Strathclyde Dept Civil & Environm Engn James Weir Bldg Level 5 75 Montrose St Glasgow G1 1XJ Lanark Scotland;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Water evaporation; Airflow; Suction drain; Ground-stability;

    机译:水蒸发;空气流动;吸排水地面稳定性;

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