Sub-critical water extraction of bitumen from Huadian oil shale lumps

被引:35
作者
Deng, Sunhua [1 ]
Wang, Zhijun [1 ]
Gao, Yan [1 ]
Gu, Qiang [1 ]
Cui, Xuejun [1 ]
Wang, Hongyan [1 ]
机构
[1] Jilin Univ, Coll Chem, Changchun 130012, Peoples R China
关键词
Oil shale; Large-sized; Sub-critical water; Bitumen; Extract yield; Py-GC-MS; NEAR-CRITICAL WATER; SUPERCRITICAL WATER; CHEMICAL-REACTIONS; ORGANIC-COMPOUNDS; FLASH PYROLYSIS; KEROGEN; REACTIVITY; PRODUCTS;
D O I
10.1016/j.jaap.2012.07.011
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Three sizes of Huadian oil shale lumps from 1 cm to 10cm were extracted by sub-critical water at 350 degrees C and 16 MPa for 2-70h. The oil shale lumps were fractured alone the shale texture in sub-critical water that greatly improved the extraction efficiency of bitumen from the large- and middle-sized sample. The extract yields of bitumen from different sized samples were similar when the extraction time is longer than 20h and stabilized at about 18 wt.% (ad) after 50h duration. With the increase of extraction time, asphaltene and preasphaltene extracts were gradually decomposed to maltene. The gas chromatography-mass spectrometry (GC-MS) analysis of the extracts showed that n-alkanes, n-alk-1-enes, isoprenoids, n-alk-2-ones and n-alkanoic acids were the major components. In contrast, aromatic extracts were rare and most of them were remained in the shale residue. The pyrolysis gas chromatography-mass spectrometry (Py-GC-MS) analysis of the spent shale showed that the final undecomposed organics in kerogen were some macromolecular linear hydrocarbon, n-alk-2-ones and n-alkanoic acids fragments. The comparison of the classical pyrolyzate and the sub-critical water extracts showed that the water extracts contained more long-chain alkanes than anhydrous pyrolysis and the alkene extracts could transform to alkanes in sub-critical water. Moreover, the n-alkanoic acids could be decomposed to short-chain compounds through the cleavage of carbon carbon bonds. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:151 / 158
页数:8
相关论文
共 23 条
  • [1] Influence of particle grain size on the yield and composition of products from the pyrolysis of oil shales
    Ahmad, N
    Williams, PT
    [J]. JOURNAL OF ANALYTICAL AND APPLIED PYROLYSIS, 1998, 46 (01) : 31 - 49
  • [2] Roles of water for chemical reactions in high-temperature water
    Akiya, N
    Savage, PE
    [J]. CHEMICAL REVIEWS, 2002, 102 (08) : 2725 - 2750
  • [3] CO2 supercritical fluid extraction of Jordanian oil shale utilizing different co-solvents
    Allawzi, Mamdouh
    Al-Otoom, Awni
    Allaboun, Hussein
    Ajlouni, Abdulaziz
    Al Nseirat, Fatima
    [J]. FUEL PROCESSING TECHNOLOGY, 2011, 92 (10) : 2016 - 2023
  • [4] Ambles A., 1999, J ANAL APPL PYROLYSI, V50, P163
  • [5] Changes in the molecular structure of a Type II-S kerogen (Monterey Formation, USA) during sequential chemical degradation
    Höld, IM
    Brussee, NJ
    Schouten, S
    Damsté, JSS
    [J]. ORGANIC GEOCHEMISTRY, 1998, 29 (5-7) : 1403 - 1417
  • [6] Extraction of Huadian oil shale with water in sub- and supercritical states
    Hu, HQ
    Zhang, J
    Guo, SC
    Chen, GH
    [J]. FUEL, 1999, 78 (06) : 645 - 651
  • [7] ORGANIC SULFUR-COMPOUNDS PRODUCED BY FLASH PYROLYSIS OF TIMHADIT OIL-SHALE
    ISHIWATARI, M
    SAKASHITA, H
    TATSUMI, T
    TOMINAGA, H
    [J]. JOURNAL OF ANALYTICAL AND APPLIED PYROLYSIS, 1990, 17 (03) : 217 - 225
  • [8] THERMAL-DECOMPOSITION BEHAVIOR OF OIL-SHALE KEROGENS OBSERVED BY STEPWISE PYROLYSIS-GAS CHROMATOGRAPHY
    ISHIWATARI, M
    SAKASHITA, H
    TATSUMI, T
    TOMINAGA, H
    [J]. JOURNAL OF ANALYTICAL AND APPLIED PYROLYSIS, 1993, 24 (03) : 273 - 290
  • [9] Non-isothermal thermogravimetry and decomposition kinetics of two Jordanian oil shales under different processing conditions
    Jaber, JO
    Probert, SD
    [J]. FUEL PROCESSING TECHNOLOGY, 2000, 63 (01) : 57 - 70
  • [10] LONG-CHAIN CARBOXYLIC-ACIDS IN PYROLYSATES OF GREEN RIVER KEROGEN
    KAWAMURA, K
    TANNENBAUM, E
    HUIZINGA, BJ
    KAPLAN, IR
    [J]. ORGANIC GEOCHEMISTRY, 1986, 10 (4-6) : 1059 - 1065