The Motion of a Viscous Fluid Under a Surface Load
The Motion of a Viscous Fluid Under a Surface Load
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表面载荷下粘性流体的运动
DOI：
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发表时间：
1935
期刊：
影响因子：
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通讯作者：
N. A. Haskell
中科院分区：
文献类型：
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作者：
N. A. Haskell
本文给出了高粘性流体在表面受对称压力作用时的运动的形式解。这适用于恒定厚度的圆柱体的沉降和去除载荷后流体的恢复。将后一种情况应用于更新世冰盖消失后地球的塑性反冲，发现地质数据意味着运动粘度为3×1021 c.g.s.。单位
A formal solution is given for the motion of a highly viscous fluid when a symmetrical pressure is applied at the surface. This is applied to the subsidence of a cylindrical body of constant thickness and to the recovery of the fluid after removal of a load. Applying the latter case to the plastic recoil of the earth after the disappearance of the Pleistocene ice sheets, it is found that the geological data imply a kinematic viscosity of the order of 3×1021 c.g.s. units.