通过对塔里木盆地满加尔凹陷侏罗系演化程度较低的(RO=0.40%)煤岩和煤岩加水进行了从250～550℃(50℃为一温阶,恒温72h)的热模拟实验,用氯仿抽提获得了赋存在固体残余物中的可溶液态有机物,即饱和烃、芳烃和非烃。实验结果表明:煤岩在各演化阶段的液态物产率均低于煤岩原样;饱和烃随演化程度升高逐步增加,而芳烃减少,反映出非烃沥青质,甚至不溶有机质向相对稳定的饱和烃转化以及芳烃随演化程度升高的高聚合作用;沥青质随演化程度升高亦有增大的趋势,而非烃比例变化不大,反映出高温下非烃向饱和烃和沥青质转化的两极分化作用;烷/芳值随着演化程度的升高而增加,反映出高演化期芳烃的聚合作用。在煤岩加水热模拟实验中,液态烃产率随温度升高而逐步增加且芳烃是主体产物。在实验的低温阶段,水的加入使得煤岩样中可溶有机质向气态和不溶有机质转化,从而使得可溶有机质组分呈降低趋势,而在高温阶段时煤岩加水后可溶有机质有所增加。在煤岩加水热模拟实验中,烷/芳值均小于1,再一次说明了水对芳烃缩聚的抑制作用及对烷烃形成的促进作用。

Low-mature coal and the coal added water (R_O=0.40%, from Manjia’er depression, Tarim basin, China) were subjected to closed system pyrolysis, in sealed gold tubes, under isothermal temperature conditions, ranging from 250 to 550℃ at temperature intervals of 50℃ (pyrolysis time 72 hours). The soluble organic matters in the pyrolysis remainders were obtained by the chloroform extraction, including saturated hydrocarbon, aromatics and non-hydrocarbons. The result shows that the liquid products for pyrolysis.