In-situ monitoring the thermal regime of foundation backfill of a power transmission line tower in permafrost regions on the Qinghai-Tibet Plateau
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文摘

Hydrothermal process was monitored continuously in backfill of a tower foundation.

Water infiltration caused a 1 to 2 orders higher heat transfer rate in the backfill.

Air natural convection was potentially occurred in the porously backfill in winter.

Convective heat transfer was not remarkable after the freezing-thawing process.

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