中国矿业
中國礦業
중국광업
CHINA MINING MAGAZINE
2014年
6期
92-95
,共4页
黎琼%张枝焕%欧光习%黄俨然%李文浩
黎瓊%張枝煥%歐光習%黃儼然%李文浩
려경%장지환%구광습%황엄연%리문호
化学动力学%二次生烃%热模拟实验%黄桥地区
化學動力學%二次生烴%熱模擬實驗%黃橋地區
화학동역학%이차생경%열모의실험%황교지구
chemical kinetics%hydrocarbon regeneration%thermal simulation experiments%Huangqiao area
通过对黄桥地区烃源岩进行封闭热模拟实验,获得了不同成熟度的系列样品,对实验的液态产物进行地球化学特征分析,并将未抽提与抽提的样品进行开放热模拟实验,探讨其二次生烃的动力学特征。随着热模拟温度的提高,烃源岩二次生烃活化能的分布逐渐后移,活化能整体增大。未抽提样品中残留有初次生烃的产物,其二次生烃起始温度低于抽提样品。由于未抽提样品中的残留烃在加热过程中进行了二次裂解,未抽提样品的活化能在36~50kcal/moL之间存在一个独立的小峰,而抽提的样品基本没有。溪1井二叠系大隆组烃源岩的生烃史模拟,表明其二次生烃的潜力较大。
通過對黃橋地區烴源巖進行封閉熱模擬實驗,穫得瞭不同成熟度的繫列樣品,對實驗的液態產物進行地毬化學特徵分析,併將未抽提與抽提的樣品進行開放熱模擬實驗,探討其二次生烴的動力學特徵。隨著熱模擬溫度的提高,烴源巖二次生烴活化能的分佈逐漸後移,活化能整體增大。未抽提樣品中殘留有初次生烴的產物,其二次生烴起始溫度低于抽提樣品。由于未抽提樣品中的殘留烴在加熱過程中進行瞭二次裂解,未抽提樣品的活化能在36~50kcal/moL之間存在一箇獨立的小峰,而抽提的樣品基本沒有。溪1井二疊繫大隆組烴源巖的生烴史模擬,錶明其二次生烴的潛力較大。
통과대황교지구경원암진행봉폐열모의실험,획득료불동성숙도적계렬양품,대실험적액태산물진행지구화학특정분석,병장미추제여추제적양품진행개방열모의실험,탐토기이차생경적동역학특정。수착열모의온도적제고,경원암이차생경활화능적분포축점후이,활화능정체증대。미추제양품중잔류유초차생경적산물,기이차생경기시온도저우추제양품。유우미추제양품중적잔류경재가열과정중진행료이차렬해,미추제양품적활화능재36~50kcal/moL지간존재일개독립적소봉,이추제적양품기본몰유。계1정이첩계대륭조경원암적생경사모의,표명기이차생경적잠력교대。
After closed thermal simulation experiments of source rocks in Huangqiao area ,a series of samples with different maturity were obtained ,the geochemical characteristics of liquid products were analyzed .Open thermal simulation experiments were carried out with extracted and no-extracted samples to explore the dynamics characteristics of hydrocarbon regeneration .With the increased temperature of thermal simulation experiments ,the distribution of activation energy of hydrocarbon regeneration gradually moves backward ,and the whole activation energy increase .Because primary products remained in no-extracted samples ,their initial temperatures of hydrocarbon regeneration are below that of the extracted samples .In no-extracted samples residual hydrocarbon cracked again in the heating process ,so they have a small separate peak between 36kcal/moL to 50kcal/moL ,and the extracted samples have not .The simulation of hydrocarbon generation history of Dalong formation in Xi1 well shows that the source rocks have a great potential of hydrocarbon regeneration .