石油与天然气地质 ›› 1987, Vol. 8 ›› Issue (1): 26-37.doi: 10.11743/ogg19870104

• 论文 • 上一篇    下一篇

腐殖煤的热降解机理和生烃率

杨文宽   

  1. 地质矿产部石油地质综合大队
  • 收稿日期:1986-04-29 出版日期:1987-03-25 发布日期:2012-01-16

THERMO-DEGRADATION MECHANISM AND HYDROCARBON PRODUCTIVITY OF HUMIC COAL

Yang Wenkuan   

  1. Comprehensive Research Institute of Petroleum Geology, Ministry of Geology and Mineral Resources
  • Received:1986-04-29 Online:1987-03-25 Published:2012-01-16

摘要:

腐殖煤的化学结构和热降解机理,目前仍是煤成气研究中的薄弱环节。本文根据我国腐殖煤、镜质组、石墨总共154个样品的煤岩学数据和煤化学数据,提出了褐煤结构式、腐殖煤热降解步骤、腐殖煤生烃率的模型,对腐殖煤元素组成的变化规津、镜质体反射率同原子比的关系、生烃门限、气态产物化学组成和δ13C值的变化趋势、煤成烃气藏和二氧化碳气藏的成因,进行了统一讨论,阐述了它们之间的内在联系。

Abstract:

Based on the statistical data of coal chemistry and coal petrology of 154samples of coal, graphite and vitrinite collected in China, this paper proposesa model of structural formula, thermal evolution process and hydrocarbon pro-ductivity of humic coal, and comes to following conclusions: 1.The typical molecular formuia of Chinese lignite with a vitrinite reflec-tance of 0.359% is C102H96O26. 2.Coalification can be divided into five stages. In the second stage, thebreakaway of methoxyl groups raises the curtain on the formation of hydrocarbon. 3.Under geological condition, the hydrocarbon productivity P2 of residualcoal (water- and ash-free basis) conforms to following equation: p2=402e-2.75(Ro-0.10), (0.30≤Ro<4.80) Where vitrinite reflectance Ro is expressed as percentage, and P2 is m3t-1. Under the condition of simulation test, the hydrocarbon potential P3 con-forms to following equation: P3=598(Ro-0.20)0.55e-1.154(Ro-0.20), (Ro≥0.359).