A study on fractal characteristics of lacustrine shales of Qingshankou Formation in the Songliao Basin, northeast China using nitrogen adsorption and mercury injection methods

被引:42
|
作者
Han, Hui [1 ,2 ,3 ,4 ]
Guo, Chen [1 ]
Zhong, Ning-ning [3 ]
Pang, Peng [1 ]
Gao, Yuan [1 ,5 ]
机构
[1] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Sichuan, Peoples R China
[2] Shandong Univ Sci & Technol, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266590, Shandong, Peoples R China
[3] China Univ Petr, State Key Lab Petr Resource & Prospecting, Beijing 102249, Peoples R China
[4] Southwest Petr Univ, Cooperat Innovat Ctr Shale Gas Resource & Environ, Chengdu 610500, Sichuan, Peoples R China
[5] Beijing Ctr Phys & Chem Anal, Beijing 100089, Peoples R China
基金
美国国家科学基金会;
关键词
Songliao basin; Lacustrine shales; Fractal dimension; Low-pressure N-2 adsorption; Mercury injection; Pore structure; PORE STRUCTURE CHARACTERIZATION; CHANG; 7; MEMBER; GAS-ADSORPTION; ORGANIC-MATTER; SICHUAN BASIN; YANCHANG FORMATION; LONGMAXI SHALE; ORDOS BASIN; ACCUMULATION; AREA;
D O I
10.1016/j.petrol.2020.107378
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
In order to research the fractal characteristics of lacustrine shale, we conducted low-pressure N-2 adsorption and mercury injection measurements on 35 shale samples of Cretaceous Qingshankou Formation in the Songliao Basin, northeast China. The fractal dimensions (D-1, D-2, and D-3) were obtained from N-2 adsorption (P/P-o < 0.5 and P/P-o > 0.5) and mercury injection data, respectively. Accordingly, we analyzed the relationships between fractal dimensions and petmphysical and geochemical parameters. The results show that the fractal dimensions (D-1, D-2, and D-3) are in the ranges of 2.0174-2.5705, 2.5589-2.8425, and 2.1461-2.9728, respectively. There exists a positive relationship between D-1 and D-2, suggesting that micmpores and mesopores have similar surface characteristics. The poor correlations between D-3 and D-1 or D-2 may be related to the different principles of low-pressure N-2 adsorption and mercury injection. The fractal dimensions (D-1 and D-2) correlate positively with pore volumes and surface areas, which indicates that the fractal dimensions can well reflect the pore structure and surface characteristics. The fractal dimensions (D-1 and D-2) decreased with the increasing TOC content, which may be aroused by the low abundance of pores in organic matters. The fractal dimensions (D-1 and D-2) decreased firstly and then increased with the increasing maturity, which is aroused by liquid hydrocarbons generation and cracking. And the fractal dimension D-3 decreased during maturation, which may be induced by compaction. The fractal dimensions (D-1 and D-2) decreased with the increasing Rock-Eval pyrolysis parameters S-1 and S-1/TOC, which suggests that the fractal dimensions can be indicators of oil content of shales.
引用
收藏
页数:14
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