在弯曲变形的前期,载荷和位移曲线都成线性变化,干态试样在载荷达到峰值之前会出现小的波动。
The load and displacement curves is linear at the early stages of the flexural deformation, the dry samples have a little fluctuation before reach the load peak.
波动是地质作用的基本形式之一,地壳的波状运动和变形是客观存在的。
Undulation is one of the fundamental models of the geological effect, the undulation motion and variation in shape of earth crust is an geologic facts.
接头界面有效连接面积和接头上引线横截面变形量的变化分别是造成接头电阻波动性和整体增大趋势的原因。
The real contact area of the bond interface and the cross-sectional deformation of the bond wire were the causations respectively for the fluctuation and wholly increase of the resistance.
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