Models of porous flow for convection of the flanks of a ridge give a satisfactory match to patterns of conduction off-axis, but again point to a strong convective flow at the ridge axis itself.
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释义
渗水流动模型适用于山脊侧部的传导过程,有效的证明了偏轴的传导方式,同时也表明在山脊中轴有强对流传导。
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