Matches in SemOpenAlex for { <https://semopenalex.org/work/W3160334444> ?p ?o ?g. }
- W3160334444 endingPage "105117" @default.
- W3160334444 startingPage "105117" @default.
- W3160334444 abstract "Oxidizing stimulation of organic-rich shale was proposed to enhance the rate of methane extraction from the matrix. Previous studies lacked attention on the dissolution characteristics of organic matter (OM) during the dissolution process performed using oxidative fluids. In this study, the organic-rich shale samples obtained from the Longmaxi Formation, Niutitang Formation, and Yanchang Formation were used for dissolution experiments. Crushed shale samples were treated with deionized water, hydrogen peroxide (H2O2), or sodium hypochlorite (NaClO) for 240 h, respectively. By using a combination of X-ray Diffraction, rock-eval pyrolysis, total organic carbon analysis, X-ray photoelectron spectroscopy, and Fourier transform infrared spectroscopy, the composition and organic geochemical characteristics of the treated shale samples were determined. The results showed that H2O2 induces the dissolution of both the pyrite and carbonate minerals, and NaClO more readily dissolves pyrite and not carbonate minerals. Higher removal efficiency of OM for all four shale samples occurs when treated with NaClO than with H2O2. The oxidative dissolution of OM in these shale samples occurs as two dominant modes: one is the oxidation cracking of C–C, C–H such as in the Niutitang or Yanchange formations; the other is oxidation cracking of C–O, such as in the Longmaxi Formation samples. Both the Longmaxi Formation samples, which showed higher C–O contents compared to samples from the other two formations, exhibited better oxidizability than others when treated with H2O2 or NaClO. Oxidation products such as Fe2+/Fe3+ and H+ enhance the oxidizing ability of H2O2 and NaClO toward cracking of OM. However, the consumption of H+ due to the carbonate minerals may impair the oxidizing ability of H2O2, but not that of NaClO. Furthermore, the presence of an organo-clay complex has an adverse influence on the removal of OM. The results indicated that the type of OM, the content of the pyrite and carbonated minerals, and the physical protection of the organic carbon by clays should be taken into account, when selecting a shale reservoir suitable for oxidizing stimulation and associated optimization of the oxidant during the fracturing operation design." @default.
- W3160334444 created "2021-05-24" @default.
- W3160334444 creator A5009318195 @default.
- W3160334444 creator A5040587895 @default.
- W3160334444 creator A5050479133 @default.
- W3160334444 creator A5052444797 @default.
- W3160334444 creator A5061838802 @default.
- W3160334444 date "2021-08-01" @default.
- W3160334444 modified "2023-10-14" @default.
- W3160334444 title "An experimental investigation into the oxidative dissolution of typical organic-rich shale from China" @default.
- W3160334444 cites W1035623028 @default.
- W3160334444 cites W1464145918 @default.
- W3160334444 cites W1970964011 @default.
- W3160334444 cites W1971862621 @default.
- W3160334444 cites W1975010088 @default.
- W3160334444 cites W1978231584 @default.
- W3160334444 cites W1979595098 @default.
- W3160334444 cites W1991541725 @default.
- W3160334444 cites W1996117895 @default.
- W3160334444 cites W2001959072 @default.
- W3160334444 cites W2004117683 @default.
- W3160334444 cites W2007963183 @default.
- W3160334444 cites W2018628930 @default.
- W3160334444 cites W2022305155 @default.
- W3160334444 cites W2026253675 @default.
- W3160334444 cites W2034018503 @default.
- W3160334444 cites W2035025414 @default.
- W3160334444 cites W2042629881 @default.
- W3160334444 cites W2045154440 @default.
- W3160334444 cites W2053615901 @default.
- W3160334444 cites W2060941996 @default.
- W3160334444 cites W2069075208 @default.
- W3160334444 cites W2075763471 @default.
- W3160334444 cites W2080267461 @default.
- W3160334444 cites W2082582946 @default.
- W3160334444 cites W2089173561 @default.
- W3160334444 cites W2089973523 @default.
- W3160334444 cites W2098412431 @default.
- W3160334444 cites W2121051499 @default.
- W3160334444 cites W2122545254 @default.
- W3160334444 cites W2150135465 @default.
- W3160334444 cites W2210868848 @default.
- W3160334444 cites W2261233543 @default.
- W3160334444 cites W2317379052 @default.
- W3160334444 cites W2340100393 @default.
- W3160334444 cites W2512684499 @default.
- W3160334444 cites W2585521082 @default.
- W3160334444 cites W2756049388 @default.
- W3160334444 cites W2769587958 @default.
- W3160334444 cites W2792728516 @default.
- W3160334444 cites W2793458647 @default.
- W3160334444 cites W2793662803 @default.
- W3160334444 cites W2889600938 @default.
- W3160334444 cites W2892728764 @default.
- W3160334444 cites W2897232526 @default.
- W3160334444 cites W2901549540 @default.
- W3160334444 cites W2912714529 @default.
- W3160334444 cites W2943614561 @default.
- W3160334444 cites W2963787356 @default.
- W3160334444 cites W2969545500 @default.
- W3160334444 cites W2995433926 @default.
- W3160334444 cites W2999056178 @default.
- W3160334444 cites W3001125821 @default.
- W3160334444 cites W3015034127 @default.
- W3160334444 cites W3015680652 @default.
- W3160334444 cites W4241114923 @default.
- W3160334444 cites W4241889653 @default.
- W3160334444 doi "https://doi.org/10.1016/j.marpetgeo.2021.105117" @default.
- W3160334444 hasPublicationYear "2021" @default.
- W3160334444 type Work @default.
- W3160334444 sameAs 3160334444 @default.
- W3160334444 citedByCount "11" @default.
- W3160334444 countsByYear W31603344442021 @default.
- W3160334444 countsByYear W31603344442022 @default.
- W3160334444 countsByYear W31603344442023 @default.
- W3160334444 crossrefType "journal-article" @default.
- W3160334444 hasAuthorship W3160334444A5009318195 @default.
- W3160334444 hasAuthorship W3160334444A5040587895 @default.
- W3160334444 hasAuthorship W3160334444A5050479133 @default.
- W3160334444 hasAuthorship W3160334444A5052444797 @default.
- W3160334444 hasAuthorship W3160334444A5061838802 @default.
- W3160334444 hasConcept C107872376 @default.
- W3160334444 hasConcept C127313418 @default.
- W3160334444 hasConcept C13965031 @default.
- W3160334444 hasConcept C151730666 @default.
- W3160334444 hasConcept C153127940 @default.
- W3160334444 hasConcept C158787203 @default.
- W3160334444 hasConcept C178790620 @default.
- W3160334444 hasConcept C185592680 @default.
- W3160334444 hasConcept C199289684 @default.
- W3160334444 hasConcept C2776062231 @default.
- W3160334444 hasConcept C2780659211 @default.
- W3160334444 hasConcept C48743137 @default.
- W3160334444 hasConcept C77176794 @default.
- W3160334444 hasConcept C88380143 @default.
- W3160334444 hasConceptScore W3160334444C107872376 @default.
- W3160334444 hasConceptScore W3160334444C127313418 @default.
- W3160334444 hasConceptScore W3160334444C13965031 @default.