Open AccessCharacteristics of coal-measure source rock and its controlling effect on gas-water distribution of tight sandstone of He8 Member in Sulige Gas Province, Ordos Basin
Author(s) -
Wenzhuo Wu,
Mengna Chen,
Ning Li,
Yi Wang,
Junping Zhao,
Xinshan Wei
Publication year - 2021
Publication title -
energy exploration and exploitation
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.435
H-Index - 30
eISSN - 2048-4054
pISSN - 0144-5987
DOI - 10.1177/01445987211022440
Subject(s) - lithology , source rock , geology , kerogen , tight gas , coal , coal measures , coal mining , sichuan basin , natural gas field , petroleum engineering , mineralogy , natural gas , geochemistry , structural basin , petrology , geomorphology , hydraulic fracturing , chemistry , organic chemistry
Characteristics of complex gas-water distribution affect the efficient exploration of tight gas. The paper aims at tight sandstone gas-water distribution characteristics of He8 Member in Sulige Gas Province (SGP), describes thickness and TOC of source rocks from Benxi Formation in Carboniferous to the Second Member of Shanxi Formation in Permain, evaluates its hydrocarbon generation potential, discusses its controlling effect on tight sandstone gas-water distribution, and determines the threshold values of R o and HGI of commercial gas flow wells. Research shows that the coal-measure source rock has the characteristics of extensive and superimposition. The coal seam and dark mudstone is the lithology of source rock, and its R o is chiefly distributed 1.2% ∼ 2.1% in the stage of high mature thermal evolution, which is mainly type III kerogen. Among them, the thickness of coal seam is mainly ranged from 5 ∼ 15 m with an average of 9.32 m, and its average TOC is 64.08% and the distribution of HGI is (1∼36) ×10 8 m 3 /km 2 . No.8 and No.5 coal seams are relatively stable. The extent of thickness of dark mudstone is mainly between 10m and 30m with an average of 21.2m, and its average TOC is 2.11%, HGI is between (0.2∼10)×10 8 m 3 /km 2 . Gas reservoir of He8 Member is tight sandstone lenticular reservoirs with the large-area quasi-continuous distribution. When the gas testing production is less than 1 × 10 4 m 3 /d, the controlling effect of R o and HGI are relatively obvious, and its controlling effect is obviously weakened with the increase of gas production. When R o is more than 1.6%-1.7%, or HGI is larger than 15 × 10 8 m 3 /km 2 , the decreasing trend of water/gas ratio is evident, especially in commercial gas flow wells (including high producing gas flow wells). In comparison, the controlling effect of HGI is stronger than R o . 1.33% and 8 × 10 8 m 3 /km 2 are the threshold values of R o and HGI for commercial gas flow wells, respectively.