摘要
在远离平衡状态的情况下,处于开放型复杂系统的烃源岩,通过粘土矿物晶体层间吸附物(包括金属阳离子、水分子和有机质等)之间的物质交换和能量交换,引发"负熵-自组织"的周期振荡与非周期性交替出现的化学湍流效应。从而使有机质"拆分-重新组装"形成一种新的正构烷烃峰群有序递变排列的石油烃。
The effects of the chemical turbulence of the negentropy and self-organization periodic oscillations and aperiodic alternating appearance can be caused by the material exchange and energy exchange among the absorbed substances of clay mineral crystal laminas, such as metal cations, water molecules and organic matters, etc. in the source rocks in open complex systems of nonequilibrium. This brings about splitting and reassembly of organic matter and forms a new hydrocarbon with n-alkane peaks in order series.
出处
《新疆石油地质》
CAS
CSCD
北大核心
2010年第4期434-439,共6页
Xinjiang Petroleum Geology
关键词
正构烷烃峰群
形成
机理
耗散结构
非平衡系统
负熵
自组织
n-alkane peaks
dissipative structure
nonequilibrium system
negentropy
self-organization
