Quantitative evaluation model of shale oil adsorption: A case study of the first member of Cretaceous Qingshankou Formation in northern Songliao Basin, NE China

IF 7 Q1 ENERGY & FUELS
Jinbu LI , Min WANG , Shuangfang LU , Liang LIU , Ming LI , Yuchen ZHANG , Xin WANG , Xinbin ZHAO , Jinyou ZHANG , Ying ZHAO
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Abstract

A quantitative evaluation model that integrates kerogen adsorption and clay pore adsorption of shale oil was proposed, and the evaluation charts of adsorption-swelling capacity of kerogen (Mk) and adsorbed oil capacity of clay minerals (Mc) were established, taking the 1st member of Cretaceous Qingshankou Formation in the northern Songliao Basin as an example. The model and charts were derived from swelling oil experiments performed on naturally evolved kerogens and adsorbed oil experiments on clays (separated from shale core samples). They were constructed on the basis of clarifying the control law of kerogen maturity evolution on its adsorption-swelling capacity, and considering the effect of both the clay pore surface area that occupied by adsorbed oil and formation temperature. The results are obtained in four aspects: (1) For the Qing 1 Member shale, with the increase of maturity, Mk decreases. Given Ro of 0.83%–1.65%, Mk is about 50–250 mg/g. (2) The clay in shale adsorbs asphaltene. Mc is 0.63 mg/m2, and about 15% of the clay pore surface is occupied by adsorbed oil. (3) In the low to medium maturity stages, the shale oil adsorption is controlled by organic matter. When Ro>1.3%, the shale oil adsorption capacity is contributed by clay pores. (4) The oil adsorption capacity evaluated on the surface at room temperature is 8%–22% (avg. 15%) higher than that is held in the formations. The proposed evaluation model reveals the occurrence mechanisms of shale oils with different maturities, and provides a new insight for estimating the reserves of shale oil under formation temperature conditions.

页岩油吸附定量评价模型——以松辽盆地北部白垩系青山口组一段为例
以松辽盆地北部白垩系青山口组一段为例,提出了一个集干酪根吸附和粘土孔隙吸附于一体的页岩油定量评价模型,建立了干酪根吸附膨胀能力(Mk)和粘土矿物吸附油能力(Mc)评价图。该模型和图表来源于对自然演化的干酪根进行的膨胀油实验和对粘土(从页岩岩心样品中分离)进行的吸附油实验。它们是在阐明干酪根成熟度演化对其吸附溶胀能力的控制规律的基础上构建的,并考虑了吸附油所占粘土孔隙表面积和地层温度的影响。研究结果主要体现在四个方面:(1)对于青一段页岩,随着成熟度的增加,Mk减小。假设Ro为0.83%–1.65%,Mk约为50–250 mg/g。(2) 页岩中的粘土吸附沥青质。Mc为0.63mg/m2,约15%的粘土孔隙表面被吸附的油占据。(3) 在中低成熟度阶段,页岩油的吸附受有机质的控制。当Ro>;1.3%,粘土孔隙对页岩油的吸附能力有贡献。(4) 在室温下,表面上评估的石油吸附能力比地层中的吸附能力高8%-22%(平均15%)。该评价模型揭示了不同成熟度页岩油的赋存机制,为在地层温度条件下估算页岩油储量提供了新的思路。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
11.50
自引率
0.00%
发文量
473
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