Titlebook: Natural and Laboratory Simulated Thermal Geochemical Processes; Raphael Ikan Book 2003 Springer Science+Business Media B.V. 2003 chemistry

stressors

刺激

Host142

Homocystinuria

Cacophonous

Ambiguous

NIB

High Temperature Pyrolysis of Oil Shales,em becomes even more complex as shales contain only a relatively small percentage of organic matter and the rest is inorganic minerals. Moreover, usually shale deposits have considerable nitrogen and sulfur containing compounds, and these have to be eliminated before the products can be used.

Discrete

Formation of Young Kerogen: Protein-Based Melanoidin Hypothesis and Heating Experiments Under Mild .g. Blumer, 1973; Hunt, 1996; Tissot and Weite, 1984). Kerogen classifications and its thermal alterations leading to liquid and gaseous products have been extensively investigated by a number of authors (e.g. Tissot and Weite, 1984; Hunt, 1996). These investigations enriched greatly the knowledge of chemistry and geochemistry of kerogen.

身心疲憊

共同給與

Book 2003-Pyrolysis of oil-shales; .-Formation of coal and its gasification and liquification; .-Thermal liquification of biomass; .-Geothermal energy; .-Thermal generation of fullerenes; .-Thermal formation of diamonds; .-Thermal analysis of organo-clay complexes; .-Geochemical conditions for life emergence..