4.7 Article

Model tests of the barrier measures on moisture and salt migration in soils subjected to freeze-thaw cycles

期刊

COLD REGIONS SCIENCE AND TECHNOLOGY
卷 201, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.coldregions.2022.103607

关键词

Chlorine saline soil; Buried pipeline; Cyclic freeze-thaw; Moisture and salt migration; Barrier measures; Model tests

资金

  1. National Key Research and Development Program of China [2018YFC0809605]
  2. National Natural Science Foundation of China [41601074, 42171146, 41825015]
  3. Key Research Program of Frontier Sciences of Chinese Academy of Sciences [QYZDY-SSW-DQC015]
  4. Key Research Program of the Chinese Academy of Sciences [ZDRW-ZS-2020-1]
  5. CAS Light of West China Program for the Belt and Road Research Teams

向作者/读者索取更多资源

This study investigates the impact of moisture and salt migration and accumulation on pipeline corrosion. Three barrier measure models were established and laboratory tests were conducted to analyze the barrier effect of different measures during freeze-thaw cycles. The results show that impermeable geotextile barrier and gravel replacement can effectively prevent moisture and salt migration and corrosion to the pipeline.
The migration and accumulation of chlorine salt in frozen soils will cause corrosion to the buried pipeline and seriously affect its service life. In order to investigate the effect of moisture and salt migration and accumulation on pipeline corrosion, three models of barrier measures were established using similar criteria, namely, nonsaline soil replacement model (M1), non-saline soil replacement with impermeable geotextile barrier model (M2), and gravel replacement model (M3). Laboratory model tests were carried out to study the characteristics of moisture and salt migration and the barrier effect of different measures in response to freeze-thaw (F-T) cycles. The freezing depth is 38.6, 29.7, and 43.5 cm in three models. The volumetric moisture contents and salt concentrations are positively and negatively correlated with temperature, respectively. In M1, the maximum moisture contents decrease and increase obviously inside and outside of the upper boundary, with the variation rate of 11.7% and 11.1%. The maximum salt concentrations decrease by 7.7% and increase by 1.31 times, respectively. The concentration variations of the lower boundary are not obvious. They remain essentially constant in M2, i.e., 0.323 and 0.039 mol kg-1. The salt concentration in M3 has a far less reduction rate of 4.0%. Impermeable geotextile barrier and gravel replacement can prevent moisture and salt migration and corrosion to the pipeline. Concentration variation of M1 is primarily influenced by convection, salt expulsion and diffusion, while that of M2 outside the upper boundary is only influenced by convection, and M3 is caused by convection and salt expulsion. A combination of M3 and M2 measures are required when the buried pipeline is located above the freezing front and the water table is shallow. In other cases, M2 measures are chosen. The results can provide theoretical support and technical guidance for more economical and efficient construction and safe operation of the buried pipeline.

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