在地球表面到湍流层顶以下的区域，由于大气的湍流、对流等活动比较强盛，使得各物理化学成分能够比较均匀的混合，各种物质、能量被均均的耗散到背景大气中去，称之为“均质层”（homosphere）。均质层的高度在100km以内，属低层大气，包括对流层、平流层和中层。
n. homosphere
... homogeneous isotropic medium 均质各向同性介质 homogeneous layer 均质层 homogeneous light 单色光 ...
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... uniform asymptotic formula 均匀渐近公式 uniform bed 均质层 uniform circular motion 匀速圆周运动 ...
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均质层顶 [地物] homopause
非均质层 [地物] heterosphere
非均质层理 nonuniform stratification
不均质储层 heterogeneous reservoir
均质地层 uniform formation ; homogeneous formation ; isotropic formation
均质储层 homogeneous reservoir
非均质油层 [油气] non-homogeneous pay
储层非均质性 reservoir heterogeneity ; reservoir inhomogeneity ; areal heterogeneity ; vertical heterogeneity
均质产层 homogeneous pay zone
低层大气由均质的混合气体组成，所以也叫均质层。
The lower atmosphere is referred to as the homosphere because it has a uniform mixture of gases.
高层大气包括气体成分不同的几个层，所以也叫非均质层。
The upper layer of the atmosphere is referred to as the heterosphere because it has several layers of different gases.
外壁由几层组成：上部均质层，具不平的外、内表面，中间均质层，穴状层和下部均质层。
It consists of the following layers: the upper homogenous layer, with uneven external and internal surfaces, the intermediate homogenous layer, the alveolate layer, and the lower homogenous one.
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