有
参扌颉rder isorder缩写为(O )。指物体内部结构中质点在空间排布的两种不同状态。其呈某种有规律性的排布(例如位置呈周期性重复、配位多面体的空间取向一致等等)者是为有序(态)；无规律者则为无序(态)。至于多型中的有序 参扌蛳窒螅 则是指其结构层的堆积顺序是否有一定的重复规律。参见“超结构”。
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contributed at 2011-10-12
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●
Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name |
| Chinese |
|---|
| Name | 有 |
| Description | 参扌颉rder isorder缩写为(O )。指物体内部结构中质点在空间排布的两种不同状态。其呈某种有规律性的排布(例如位置呈周期性重复、配位多面体的空间取向一致等等)者是为有序(态)；无规律者则为无序(态)。至于多型中的有序 参扌蛳窒螅 则是指其结构层的堆积顺序是否有一定的重复规律。参见“超结构”。 |
How to Cite
NNU_Group (2011). 有, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/746e3eed-17aa-429d-b1cf-23a304c9e3b3
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