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Experimental Investigation on Effects of Water Flow to Freezing Sand around Vertically Buried Freezing Pipe

机译:水流对垂直埋管内冻沙影响的试验研究

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摘要

High groundwater flow velocity is a major challenge in many artificial ground freezing (AGF) projects, especially in groundwater control projects. That condition may be unfavorable for the formation of a frozen body. This study aims to understand the effect of seepage flow on the heat transfer behavior and hydraulic conductivity variation of sand during the freezing process in AGF projects by using a vertically buried freezing pipe. The authors conducted a small-scale laboratory experiment that combined a flow test, freezing process, and infrared thermograph observations of thermal distribution. The authors prepared saturated Toyoura sand and a Toyoura-silica sand layer combination as the heat-transfer medium. The thermal distribution and hydraulic conductivity behavior were investigated by two series of freezing experiments with different sand layers and flow scenarios. Infrared thermograph observation results showed how water affects the thermal distribution characteristic, whereas flow test results showed the relation between hydraulic conductivity and frozen-body development.
机译:在许多人工地面冻结(AGF)项目中,尤其是在地下水控制项目中,高地下水流速是一项重大挑战。该条件可能不利于冷冻体的形成。本研究旨在通过使用垂直埋入的冻结管来了解渗流对AGF项目冻结过程中砂子的传热行为和水力传导率变化的影响。作者进行了一个小型实验室实验,该实验结合了流量测试,冷冻过程和红外热像仪对热分布的观察。作者准备了饱和的Toyoura砂和Toyoura-硅砂层组合作为传热介质。通过两个不同的砂层和流动情况的冷冻实验,研究了热分布和水力传导行为。红外热像仪观察结果表明水如何影响热分布特性,而流动试验结果表明水力传导率与冻结体发育之间的关系。

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