There is anisotropy with a certain degree for rocks in the earth 's interior.
地球内部的岩层通常都存在着一定程度的各向异性。
Therefore, it was necessary to take the anisotropy of silty slurry into account.
因此考虑粉土泥浆沉淀的不均匀性是必要的。
The variation of effective anisotropy was basically the same as that of coercivity.
有效各向异性与矫顽力的变化规律基本相同。
The region between the separated bubble and the main region shows strong anisotropy.
结果表明：在管道的中心线附近远离分离泡区域的紊流可以看作各向同性的；
The region between the separated bubble and the main region shows strong anisotropy.
结果表明：在管道的中心线附近远离分离泡区域的紊流可以看作各向同性的；
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