Generalized analytical solution to steady-state temperature field of double-circle-piped freezing

Temperature field distribution is the basis theory of artificial ground freezing, which is essential for mastering the temperature development of frozen soil wall. In practice, the double-circle-piped arrangements of freezing pipes are mostly applied. Concerning to all analytical solutions to the st...

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Veröffentlicht in:Cold regions science and technology 2020-07, Vol.175, p.103076, Article 103076
Hauptverfasser: Shao, Zhi-li, Hu, Xiang-dong, Han, Yan-guang, Fang, Tao
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Sprache:eng
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Zusammenfassung:Temperature field distribution is the basis theory of artificial ground freezing, which is essential for mastering the temperature development of frozen soil wall. In practice, the double-circle-piped arrangements of freezing pipes are mostly applied. Concerning to all analytical solutions to the steady-state temperature field, there is no result of the double-circle-piped freezing. This paper establishes a model for the steady-state temperature field of double-circle-piped freezing. Then, according to conformal mapping and the boundary separation method, this model of the double-row-piped freezing is transformed into two special single-row-piped freezing models. Thereby, the solution to double-circle-piped freezing model is obtained by solving the single-row-piped freezing problem. And the analytical results for some typical double-circle-piped problems show good consistent with the numerical thermal results. Furthermore, the applications for calculating the thickness and average temperature under double-circle-piped condition are derived. •Boundary separation method is used to solve steady-state temperature field.•The analytical solution to double-circle-piped freezing is derived.•The analytical solution shows the consistency with the computational results.•The solutions for single-row- and double-row-piped freezing are improved.•The applications of analytical solution satisfy the requirements of projects.
ISSN:0165-232X
1872-7441
DOI:10.1016/j.coldregions.2020.103076