三维冻结应力条纹经切片加工后，往往发生条纹歪曲的现象。
Distortion often takes place in streaks when the three dimensional frozen stress streaks are sectioned.
法向冻胀力则是在冻结锋面上冻胀应力沿基础影响范围之内的积分。
The normal frost heave force is an integral of soil frost heave stress at the freezing front along the range effected by a foundation.
这在应用应力冻结法解决三维问题时尤为重要。
It is especially important when three-dimensional problem must be solved with frozen stress method.
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