1) dissolution-crystallization
溶解-结晶作用
2) dissolution-precipitation
溶解-结晶
1.
According to the results of TEM, XRD, Ba/Ti (molar ratio) and specific surface area, the crystallization process of barium titanate followed the “dissolution-precipitation” mechanism in the hydrothermal synthesis with single water medium that contained a aggregation-growth.
TEM、XRD、钡/钛摩尔比(Ba/Ti)和比表面积的测试结果表明,在单一水介质中水热合成钛酸钡晶体的结晶过程遵循“溶解-结晶”机制,存在第II类聚集长大过程。
3) solubility and crystallization
溶解结晶
4) dissolution
[英][,dɪsə'lu:ʃn] [美]['dɪsə'luʃən]
溶解作用
1.
A study of the secondary dissolution pores in the volcanic reservoirs of Xingcheng development area can provide a basis for future exploration and development of the Xushen gas field.
结果发现,次生溶蚀孔隙是该类储层中最重要的储集空间类型之一,主要由晚埋藏成岩阶段有机酸性水与地层中易溶组分(长石)发生溶解作用而形成。
2.
Dissolution is the most important constructive diagenesis, and many oil geology scientist pay many attention for it.
溶解作用作为最为重要的建设性成岩作用是石油地质学家和沉积学家多年来长期研究的重要课题之一。
3.
Based on core description and microscope analysis, it is held that the main diagenesis types in the area are cementation, metasomasis and dissolution.
为了认清柴北缘第三系有利储层的分布规律 ,在岩心观察、微观照片及分析化验的基础上 ,认为本区主要的成岩作用类型有胶结作用、交代作用及溶解作用 ,其中早期及中期的碳酸盐胶结物的溶解作用对本区第三系储层形成次生孔隙起着重要的促进作用 ,在碳酸盐质量分数小于 2 0 %的情况下 ,易产生有利的次生孔隙 。
5) solution
[英][sə'lu:ʃn] [美][sə'luʃən]
溶解作用
1.
Diagenesis types include compaction,cementation,solution and metasomasis.
成岩作用类型主要包括压实作用、胶结作用、溶解作用和交代作用,其中胶结作用使储层原生孔隙迅速变差,而溶解作用是次生空隙发育的主要因素。
6) dissolve-repreparation
溶解-重结晶
1.
At higher pH environment,amorphous precipitation may tend to dissolve-repreparation reaction,and make boehmite grains,and the crysta-llite state can improve by prolong aging time.
无定形沉淀在较高的pH条件下,能促使溶解-重结晶反应发生,生成勃姆石颗粒,颗粒的结晶度随着老化时间的延长而有所提高。
补充资料：二次再结晶(见再结晶晶粒长大)
二次再结晶(见再结晶晶粒长大)
secondary recrystallization
erCI 201」le」Ing二次再结晶(seeondary reerystallization) 见再结晶晶杠长大。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条