Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments
Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolys...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhu, Xiaojun [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022transfer abstract |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Iterated Gilbert mosaics - Baccelli, Francois ELSEVIER, 2019, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:219 ; year:2022 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.petrol.2022.111072 |
|---|
| Katalog-ID: |
ELV059409754 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | ELV059409754 | ||
| 003 | DE-627 | ||
| 005 | 20230626052832.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 221219s2022 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1016/j.petrol.2022.111072 |2 doi | |
| 028 | 5 | 2 | |a /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001953.pica |
| 035 | |a (DE-627)ELV059409754 | ||
| 035 | |a (ELSEVIER)S0920-4105(22)00924-X | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 510 |q VZ |
| 084 | |a 31.70 |2 bkl | ||
| 100 | 1 | |a Zhu, Xiaojun |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments |
| 264 | 1 | |c 2022transfer abstract | |
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. | ||
| 520 | |a Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. | ||
| 650 | 7 | |a Source rocks |2 Elsevier | |
| 650 | 7 | |a Organic-mineral interactions |2 Elsevier | |
| 650 | 7 | |a Light and heavy hydrocarbons |2 Elsevier | |
| 650 | 7 | |a Hydrocarbon generation |2 Elsevier | |
| 700 | 1 | |a Guo, Min |4 oth | |
| 700 | 1 | |a Cai, Jingong |4 oth | |
| 700 | 1 | |a Song, Mingshui |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Baccelli, Francois ELSEVIER |t Iterated Gilbert mosaics |d 2019 |g Amsterdam [u.a.] |w (DE-627)ELV008094314 |
| 773 | 1 | 8 | |g volume:219 |g year:2022 |g pages:0 |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.petrol.2022.111072 |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a GBV_ELV | ||
| 912 | |a SYSFLAG_U | ||
| 912 | |a SSG-OPC-MAT | ||
| 936 | b | k | |a 31.70 |j Wahrscheinlichkeitsrechnung |q VZ |
| 951 | |a AR | ||
| 952 | |d 219 |j 2022 |h 0 | ||
| author_variant |
x z xz |
|---|---|
| matchkey_str |
zhuxiaojunguomincaijingongsongmingshui:2022----:rcintoohdoabneeainnuebogncieaitrci |
| hierarchy_sort_str |
2022transfer abstract |
| bklnumber |
31.70 |
| publishDate |
2022 |
| allfields |
10.1016/j.petrol.2022.111072 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001953.pica (DE-627)ELV059409754 (ELSEVIER)S0920-4105(22)00924-X DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Zhu, Xiaojun verfasserin aut Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation Elsevier Guo, Min oth Cai, Jingong oth Song, Mingshui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:219 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2022.111072 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 219 2022 0 |
| spelling |
10.1016/j.petrol.2022.111072 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001953.pica (DE-627)ELV059409754 (ELSEVIER)S0920-4105(22)00924-X DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Zhu, Xiaojun verfasserin aut Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation Elsevier Guo, Min oth Cai, Jingong oth Song, Mingshui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:219 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2022.111072 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 219 2022 0 |
| allfields_unstemmed |
10.1016/j.petrol.2022.111072 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001953.pica (DE-627)ELV059409754 (ELSEVIER)S0920-4105(22)00924-X DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Zhu, Xiaojun verfasserin aut Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation Elsevier Guo, Min oth Cai, Jingong oth Song, Mingshui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:219 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2022.111072 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 219 2022 0 |
| allfieldsGer |
10.1016/j.petrol.2022.111072 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001953.pica (DE-627)ELV059409754 (ELSEVIER)S0920-4105(22)00924-X DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Zhu, Xiaojun verfasserin aut Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation Elsevier Guo, Min oth Cai, Jingong oth Song, Mingshui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:219 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2022.111072 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 219 2022 0 |
| allfieldsSound |
10.1016/j.petrol.2022.111072 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001953.pica (DE-627)ELV059409754 (ELSEVIER)S0920-4105(22)00924-X DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Zhu, Xiaojun verfasserin aut Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation Elsevier Guo, Min oth Cai, Jingong oth Song, Mingshui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:219 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2022.111072 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 219 2022 0 |
| language |
English |
| source |
Enthalten in Iterated Gilbert mosaics Amsterdam [u.a.] volume:219 year:2022 pages:0 |
| sourceStr |
Enthalten in Iterated Gilbert mosaics Amsterdam [u.a.] volume:219 year:2022 pages:0 |
| format_phy_str_mv |
Article |
| bklname |
Wahrscheinlichkeitsrechnung |
| institution |
findex.gbv.de |
| topic_facet |
Source rocks Organic-mineral interactions Light and heavy hydrocarbons Hydrocarbon generation |
| dewey-raw |
510 |
| isfreeaccess_bool |
false |
| container_title |
Iterated Gilbert mosaics |
| authorswithroles_txt_mv |
Zhu, Xiaojun @@aut@@ Guo, Min @@oth@@ Cai, Jingong @@oth@@ Song, Mingshui @@oth@@ |
| publishDateDaySort_date |
2022-01-01T00:00:00Z |
| hierarchy_top_id |
ELV008094314 |
| dewey-sort |
3510 |
| id |
ELV059409754 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV059409754</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626052832.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">221219s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.petrol.2022.111072</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001953.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV059409754</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0920-4105(22)00924-X</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">510</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">31.70</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhu, Xiaojun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022transfer abstract</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Source rocks</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Organic-mineral interactions</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Light and heavy hydrocarbons</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Hydrocarbon generation</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Guo, Min</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cai, Jingong</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Song, Mingshui</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Baccelli, Francois ELSEVIER</subfield><subfield code="t">Iterated Gilbert mosaics</subfield><subfield code="d">2019</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV008094314</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:219</subfield><subfield code="g">year:2022</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.petrol.2022.111072</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">31.70</subfield><subfield code="j">Wahrscheinlichkeitsrechnung</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">219</subfield><subfield code="j">2022</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| author |
Zhu, Xiaojun |
| spellingShingle |
Zhu, Xiaojun ddc 510 bkl 31.70 Elsevier Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments |
| authorStr |
Zhu, Xiaojun |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV008094314 |
| format |
electronic Article |
| dewey-ones |
510 - Mathematics |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
elsevier |
| remote_str |
true |
| illustrated |
Not Illustrated |
| topic_title |
510 VZ 31.70 bkl Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation Elsevier |
| topic |
ddc 510 bkl 31.70 Elsevier Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation |
| topic_unstemmed |
ddc 510 bkl 31.70 Elsevier Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation |
| topic_browse |
ddc 510 bkl 31.70 Elsevier Source rocks Elsevier Organic-mineral interactions Elsevier Light and heavy hydrocarbons Elsevier Hydrocarbon generation |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| author2_variant |
m g mg j c jc m s ms |
| hierarchy_parent_title |
Iterated Gilbert mosaics |
| hierarchy_parent_id |
ELV008094314 |
| dewey-tens |
510 - Mathematics |
| hierarchy_top_title |
Iterated Gilbert mosaics |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)ELV008094314 |
| title |
Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments |
| ctrlnum |
(DE-627)ELV059409754 (ELSEVIER)S0920-4105(22)00924-X |
| title_full |
Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments |
| author_sort |
Zhu, Xiaojun |
| journal |
Iterated Gilbert mosaics |
| journalStr |
Iterated Gilbert mosaics |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2022 |
| contenttype_str_mv |
zzz |
| container_start_page |
0 |
| author_browse |
Zhu, Xiaojun |
| container_volume |
219 |
| class |
510 VZ 31.70 bkl |
| format_se |
Elektronische Aufsätze |
| author-letter |
Zhu, Xiaojun |
| doi_str_mv |
10.1016/j.petrol.2022.111072 |
| dewey-full |
510 |
| title_sort |
fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments |
| title_auth |
Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments |
| abstract |
Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. |
| abstractGer |
Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. |
| abstract_unstemmed |
Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle. |
| collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT |
| title_short |
Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments |
| url |
https://doi.org/10.1016/j.petrol.2022.111072 |
| remote_bool |
true |
| author2 |
Guo, Min Cai, Jingong Song, Mingshui |
| author2Str |
Guo, Min Cai, Jingong Song, Mingshui |
| ppnlink |
ELV008094314 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth |
| doi_str |
10.1016/j.petrol.2022.111072 |
| up_date |
2024-07-06T21:55:01.251Z |
| _version_ |
1803868334983217152 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV059409754</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626052832.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">221219s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.petrol.2022.111072</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001953.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV059409754</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0920-4105(22)00924-X</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">510</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">31.70</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhu, Xiaojun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Fractionation of hydrocarbon generation induced by organic-mineral interactions in fine-grained sediments</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022transfer abstract</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Hydrocarbon (HC) generation is closely related to the properties of organic matter (OM), however, rare concern has been paid to the exact influence from its contiguous minerals in fine-grained sediments. Here we employed the physical-chemical sequential treatments and Rock-Eval pyrolysis and pyrolysis gas chromatography determination of shale samples to address the issue. Our results show that the OM type, HC generation potential, Tmax, gas-oil ratio, and ratio of light to heavy HCs (∑C14 −/∑C15 +) of shales are regularly successively changed after sequential treatments. These successive changes suggest that OM with strong interaction strength with minerals has poor OM quality and HC generation potential, and the strong strength of organic-mineral interactions (OMIs) can decrease the geothermal requirement for HC generation and move forward the onset timing of HC generation. Light and heavy HCs are mainly generated from the tight and weak mineral-combined OM, respectively, and more light or mobile oil can be found if a source rock has experienced the stronger OMI strength. Our study reveals the important influence of different OMI strengths on the fractionation of HC generation in fine-grained sediments, which is significant to improve the understanding of petroleum resource assessment and the carbon cycle.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Source rocks</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Organic-mineral interactions</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Light and heavy hydrocarbons</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Hydrocarbon generation</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Guo, Min</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cai, Jingong</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Song, Mingshui</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Baccelli, Francois ELSEVIER</subfield><subfield code="t">Iterated Gilbert mosaics</subfield><subfield code="d">2019</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV008094314</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:219</subfield><subfield code="g">year:2022</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.petrol.2022.111072</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">31.70</subfield><subfield code="j">Wahrscheinlichkeitsrechnung</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">219</subfield><subfield code="j">2022</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| score |
7.4009256 |