CN107560994A - Aperture location mode in one kind evaluation mud shale organic matter, clay and other mineral - Google Patents

Aperture location mode in one kind evaluation mud shale organic matter, clay and other mineral Download PDF

Info

Publication number
CN107560994A
CN107560994A CN201710788441.6A CN201710788441A CN107560994A CN 107560994 A CN107560994 A CN 107560994A CN 201710788441 A CN201710788441 A CN 201710788441A CN 107560994 A CN107560994 A CN 107560994A
Authority
CN
China
Prior art keywords
organic matter
mineral
clay
shale reservoir
shale
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Granted
Application number
CN201710788441.6A
Other languages
Chinese (zh)
Other versions
CN107560994B (en
Inventor
陈方文
卢双舫
薛海涛
李吉君
王民
王伟明
黄文彪
肖佃师
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
China University of Petroleum East China
Original Assignee
China University of Petroleum East China
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by China University of Petroleum East China filed Critical China University of Petroleum East China
Priority to CN201710788441.6A priority Critical patent/CN107560994B/en
Publication of CN107560994A publication Critical patent/CN107560994A/en
Application granted granted Critical
Publication of CN107560994B publication Critical patent/CN107560994B/en
Active legal-status Critical Current
Anticipated expiration legal-status Critical

Links

Landscapes

  • Solid-Sorbent Or Filter-Aiding Compositions (AREA)
  • Analysing Materials By The Use Of Radiation (AREA)

Abstract

Aperture location mode in one kind evaluation mud shale organic matter, clay and other mineral, belongs to natural gas exploration field.This method can evaluate the pore volume distribution feature of nanometer range in shale reservoir organic matter, clay mineral and other mineral.Steps of the method are:1. TOC, cheese root element composition, total rock analysis and low temperature nitrogen adsorption and desorption experiment are carried out to same set of more than 3 samples of shale reservoir;2. calculate each sample content of organic matter using each shale reservoir sample TOC and kerogen Elemental Composition analysis result;3. according to shale reservoir sample organic matter, clay mineral, other mineral contents and adsorption isotherm experiment result, the pore volume evaluation model of each pore diameter range in organic matter, clay mineral and other mineral is established;4. calculate the pore volume of each pore diameter range in shale reservoir organic matter, clay mineral, other mineral.

Description

Aperture location mode in one kind evaluation mud shale organic matter, clay and other mineral
Technical field
The present invention relates to aperture location mode in one kind evaluation mud shale organic matter, clay and other mineral, belong to natural Gas exploration technical field.
Background technology
Shale gas is main body to adsorb with free state preservation in the stratum such as the mud stone with hydrocarbon generation capacity and shale Gas accumulation, free gas and adsorbed gas are two kinds of main preservation modes of shale gas in shale reservoir.Free gas is mainly deposited It is crack, macropore and the small hole center space of shale reservoir, adsorbed gas is primarily present in the pore wall week of nanoscale hole Enclose.The hole contrast surface area contribution of Nano grade protrudes in shale reservoir, has weight to preservation ADSORPTION STATE shale Gas content Want control action.Especially organic hole of Nano grade, clay mineral intercrystalline pore have weight to preservation ADSORPTION STATE shale gas Contribute.At present, measuring the method for shale Nano grade hole has the experiment of low temperature nitrogen absorption-desorption, electron microscopic imaging, pressure Mercury method and Three Dimensional Reconfiguration.But these methods can not evaluate organic matter in shale reservoir, clay mineral and other ore deposits respectively The pore volume of different pore size in thing.Low temperature nitrogen absorption-desorption tests the hole that can obtain different pore size in mud shale sample Gap volume, but it can not be evaluated the pore volume of different pore size in organic matter, clay mineral and other mineral respectively.Electricity Sub- micro-imaging technique can effectively observe shale microstructure among pores, type, but only obtain the qualitative of two dimensional surface and retouch State, lack 3-D quantitative evaluation.Mercury injection method measurement is the pore volume being connected with the throat of different pore size, and cannot be distinguished by The pore volume of different pore size in machine matter, clay mineral and other mineral.Three Dimensional Reconfiguration is ground to shale microstructure Study carefully, it may be determined that micron-sized shale cube mesoporous character and pore volume, but the sample diameter of the technical Analysis is got over Small resolution ratio is higher.The shale granular size of its quantitative assessment is 1 ~ 5um, if can overcome the anisotropism of shale reservoir And result is representative query be present.
Therefore, the present invention is made up of cheese root element, total rock is analyzed and low temperature nitrogen absorption-desorption experimental result, build The pore volume evaluation model of each pore diameter range, quantitative assessment shale reservoir in vertical organic matter, clay mineral and other mineral The pore volume of each pore diameter range in organic matter, clay mineral, other mineral.
The content of the invention
The purpose of the present invention is:Aperture location mode in a kind of evaluation mud shale organic matter of offer, clay and other mineral, Realize the quantitative assessment to each pore diameter range pore volume in shale reservoir organic matter, clay mineral, other mineral.Overcome existing There are technology, method not to open each pore diameter range pore volume in shale reservoir organic matter, clay mineral, other mineral effectively The shortcomings that evaluating by exhibit valency.
The technical solution adopted by the present invention is:Aperture location mode in evaluation mud shale organic matter, clay and other mineral, It is characterized in that:
Step 1:More than 3 samples of same set of shale reservoir are carried out TOC contents, cheese root element composition, total rock analysis and Low temperature nitrogen absorption-desorption is tested, and the mass percent for obtaining TOC in each shale reservoir sample is respectively wTOC1、wTOC2、… And wTOCn, carbon mass percent is respectively w in kerogenC1、wC2... and wCn, protium mass percent point in kerogen Wei not wH1、wH2... and wHn, oxygen element mass percent is respectively w in kerogenO1、wO2... and wOn, nitrogen in kerogen Mass percent is respectively wN1、wN2... and wNn, element sulphur mass percent is respectively w in kerogenS1、wS2... and wSn, glue The mass percent of native mineral is respectively wClay 1、wClay 2... and wClay n, the mass percent of other mineral is respectively wOther 1、 wOther 2... and wOther n, pore diameter range is respectively in each shale reservoir sample<2nm、2-5 nm、5-10nm、10-20nm、20- 50nm, 50-100nm and 100-200nm pore volume are Vij, wherein i=1,2 ..., n, be shale reservoir sample numbering, J=1,2 ..., 7, be pore diameter range numbering, TOC, clay mineral and other mineral quality percentages in shale reservoir sample Unit be %, carbon, hydrogen, oxygen, nitrogen and element sulphur mass percent unit are % in kerogen, each hole of shale reservoir sample The pore volume unit of footpath scope is cm3/g;
Step 2:Utilize each shale reservoir sample TOC mass percents wTOC1、wTOC2... and wTOCn, carbon matter in kerogen Measure percentage wC1、wC2... and wCn, quality of organic matter percentage in each shale reservoir sample is calculated according to the following formula wOrganic matter 1、wOrganic matter 2... and wOrganic matter n
wOrganic matter i=wTOCi/ wCi×100%
In formula, i=1,2 ..., n, be shale reservoir sample numbering, shale reservoir sample TOC mass percents, kerogen The unit of quality of organic matter percentage is % in middle carbon mass percent and shale reservoir sample;
Step 3:According to the mass percent w that each mud shale sample clay mineral is obtained in step 1Clay 1、wClay 2... and wClay n, its The mass percent w of its mineralOther 1、wOther 2... and wOther n, and pore diameter range is respectively in each mud shale sample of unit mass< 2nm, 2-5 nm, 5-10nm, 10-20nm, 20-50nm, 50-100nm and 100-200nm pore volume Vij, and obtained in step 2 The mass percent w of each shale reservoir sample organic matter obtainedOrganic matter 1、wOrganic matter 2... and wOrganic matter n, establish equation below group and mesh Scalar functions, as object function f (VOrganic matter-j, VClay-j, VOther-j) value minimum when, you can obtain unit mass organic matter, clay pit The pore volume V for the pore diameter range that numbering is j in thing and other mineralOrganic matter j、VClay jAnd VOther j,
Wherein, VOrganic matter j、VClay jAnd VOther jIt is the unit mass organic matter, clay mineral and other ore deposits of the set shale reservoir respectively In thing numbering be j pore diameter range pore volume, j=1,2 ..., 7, be pore diameter range numbering, i=1,2 ..., n, be mud page The numbering of rock reservoir samples, the mass percent unit of organic matter, clay mineral and other mineral is equal in shale reservoir sample For %, the pore volume unit of each pore diameter range is cm in unit mass mud shale sample3/ g, unit mass organic matter, clay The pore volume unit of each pore diameter range is cm in mineral and other mineral3/g;
Step 4:According to the equation group and object function in step 3, shale reservoir unit mass organic matter, clay pit are calculated Pore diameter range is respectively in thing, other mineral<2nm, 2-5nm, 5-10nm, 10-20nm, 20-50nm, 50-100nm and 100- 200nm pore volume Vij, wherein i=1,2 ..., n, be shale reservoir sample numbering, j=1,2 ..., 7, be aperture model The numbering enclosed, the pore volume unit of each pore diameter range is cm3/g.Beneficial effects of the present invention:Present invention evaluation mud shale Aperture location mode in organic matter, clay and other mineral, realize to shale reservoir organic matter, clay mineral and other ore deposits The quantitative assessment of each pore diameter range pore volume in thing, and the evaluation method is easily operated, low-cost, the mud page evaluated Each pore diameter range pore volume is necessary important in shale gas exploration in rock reservoir organic matter, clay mineral and other mineral Parameter.
Brief description of the drawings
Fig. 1 is the flow chart of the present invention.
Embodiment:
Embodiment 1:As described in Figure 1, aperture location mode in a kind of evaluation mud shale organic matter, clay and other mineral, contains Following steps;
Step 1:TOC contents, cheese root element composition, total rock analysis and low temperature are carried out to same set of 5 samples of shale reservoir Nitrogen adsorption-desorption experiment, the mass percent for obtaining TOC in 5 shale reservoir samples is respectively 3.35%, 2.84%, 1.93%th, 1.43% and 0.97%, carbon mass percent is respectively 87.98%, 85.57%, 87.01%, 86.19% in kerogen With 86.72%, protium mass percent is respectively 2.69%, 1.96%, 2.66%, 1.54% and 1.91% in kerogen, kerogen Middle oxygen element mass percent is respectively 4.93%, 6.39%, 6.26%, 7.24% and 6.84%, nitrogen quality percentage in kerogen Than being respectively 1.89%, 2.42%, 2.40%, 2.30% and 2.10%, in kerogen element sulphur mass percent be respectively 2.51%, 3.66%th, 1.67%, 2.73% and 2.43%, the mass percent of clay mineral is respectively 30.30%, 25.70%, 45.45% and 41.60%, the mass percent of other mineral is respectively 66.36%, 71.71%, 52.75% and 56.91%, low temperature nitrogen absorption-solution Inhaling pore diameter range in experiment 5 samples of acquisition is respectively<2nm、2-5 nm、5-10nm、10-20nm、20-50nm、50-100nm 1 is shown in Table with the data of 100-200nm pore volume.
Table 1
Step 2:Using 5 shale reservoir sample TOC mass percents 3.35%, 2.84%, 1.93%, 1.43% and 0.97%, do Carbon mass percent 87.98%, 85.57%, 87.01%, 86.19% and 86.72% in junket root, 5 are calculated according to the following formula Shale reservoir sample quality of organic matter percentage is respectively 3.81%, 3.32%, 2.22%, 1.66% and 1.12%,
wOrganic matter i=wTOCi/ wCi×100%
In formula, i=1,2 ..., 5, be shale reservoir sample numbering.
Step 3:According in step 1 obtain 5 mud shale sample clay minerals mass percent 30.30%, 25.70%, 45.45% and 41.60%, the mass percent 66.36%, 71.71%, 52.75% and 56.91% of other mineral, 5 of unit mass Pore diameter range is respectively in mud shale sample<2nm, 2-5 nm, 5-10nm, 10-20nm, 20-50nm, 50-100nm and 100- 200nm pore volume, and in step 2 obtain 5 shale reservoir sample quality of organic matter percentages 3.81%, 3.32%, 2.22%th, 1.66% and 1.12%, equation below group and object function are established, as object function f (VOrganic matter-j, VClay-j, VOther-j) value When minimum, you can obtain the pore volume of the pore diameter range that numbering is j in unit mass organic matter, clay mineral and other mineral VOrganic matter j、VClay jAnd VOther j,
Wherein, VOrganic matter j、VClay jAnd VOther jIt is the unit mass organic matter, clay mineral and other ore deposits of the set shale reservoir respectively In thing numbering be j pore diameter range pore volume, j=1,2 ..., 7, be pore diameter range numbering, i=1,2,3,4,5 are mud pages Rock sample number into spectrum, wOrganic matter 1、wOrganic matter 2、wOrganic matter 3、wOrganic matter 4And wOrganic matter 5It is the quality of organic matter percentage of 5 mud shale samples respectively, wClay 1、wClay 2、wClay 3、wClay 4... and wClay 5It is the clay mineral quality percentage of 5 mud shale samples respectively, wOther 1、wOther 2、 wOther 3、wOther 4And wOther 5It is the mass percent of other mineral of 5 mud shale samples respectively, it is organic in shale reservoir sample The mass percent unit of matter, clay mineral and other mineral is %, the hole of each pore diameter range in unit mass mud shale sample Gap volume unit is cm3/ g, the pore volume list of each pore diameter range in unit mass organic matter, clay mineral and other mineral Position is cm3/g。
Step 4:According to the equation group and object function in step 3, shale reservoir unit mass organic matter, clay are calculated Pore diameter range is respectively in mineral, other mineral<2nm, 2-5nm, 5-10nm, 10-20nm, 20-50nm, 50-100nm and 100- 200nm pore volume, the results are shown in Table 2.
Table 2

Claims (1)

1. aperture location mode in one kind evaluation mud shale organic matter, clay and other mineral, it is characterised in that:
Step 1:More than 3 samples of same set of shale reservoir are carried out TOC contents, cheese root element composition, total rock analysis and Low temperature nitrogen absorption-desorption is tested, and the mass percent for obtaining TOC in each shale reservoir sample is respectively wTOC1、wTOC2、… And wTOCn, carbon mass percent is respectively w in kerogenC1、wC2... and wCn, protium mass percent point in kerogen Wei not wH1、wH2... and wHn, oxygen element mass percent is respectively w in kerogenO1、wO2... and wOn, nitrogen in kerogen Mass percent is respectively wN1、wN2... and wNn, element sulphur mass percent is respectively w in kerogenS1、wS2... and wSn, glue The mass percent of native mineral is respectively wClay 1、wClay 2... and wClay n, the mass percent of other mineral is respectively wOther 1、 wOther 2... and wOther n, pore diameter range is respectively in each shale reservoir sample<2nm、2-5 nm、5-10nm、10-20nm、20- 50nm, 50-100nm and 100-200nm pore volume are Vij, wherein i=1,2 ..., n, be shale reservoir sample numbering, J=1,2 ..., 7, be pore diameter range numbering, TOC, clay mineral and other mineral quality percentages in shale reservoir sample Unit be %, carbon, hydrogen, oxygen, nitrogen and element sulphur mass percent unit are % in kerogen, each hole of shale reservoir sample The pore volume unit of footpath scope is cm3/g;
Step 2:Utilize each shale reservoir sample TOC mass percents wTOC1、wTOC2... and wTOCn, carbon matter in kerogen Measure percentage wC1、wC2... and wCn, quality of organic matter percentage in each shale reservoir sample is calculated according to the following formula wOrganic matter 1、wOrganic matter 2... and wOrganic matter n
wOrganic matter i=wTOCi/ wCi×100%
In formula, i=1,2 ..., n, be shale reservoir sample numbering, shale reservoir sample TOC mass percents, kerogen The unit of quality of organic matter percentage is % in middle carbon mass percent and shale reservoir sample;
Step 3:According to the mass percent w that each mud shale sample clay mineral is obtained in step 1Clay 1、wClay 2... and wClay n, its The mass percent w of its mineralOther 1、wOther 2... and wOther n, and pore diameter range is respectively in each mud shale sample of unit mass< 2nm, 2-5 nm, 5-10nm, 10-20nm, 20-50nm, 50-100nm and 100-200nm pore volume Vij, and obtained in step 2 The mass percent w of each shale reservoir sample organic matter obtainedOrganic matter 1、wOrganic matter 2... and wOrganic matter n, establish equation below group and mesh Scalar functions, as object function f (VOrganic matter-j, VClay-j, VOther-j) value minimum when, you can obtain unit mass organic matter, clay pit The pore volume V for the pore diameter range that numbering is j in thing and other mineralOrganic matter j、VClay jAnd VOther j,
Wherein, VOrganic matter j、VClay jAnd VOther jIt is the unit mass organic matter, clay mineral and other ore deposits of the set shale reservoir respectively In thing numbering be j pore diameter range pore volume, j=1,2 ..., 7, be pore diameter range numbering, i=1,2 ..., n, be mud page The numbering of rock reservoir samples, the mass percent unit of organic matter, clay mineral and other mineral is equal in shale reservoir sample For %, the pore volume unit of each pore diameter range is cm in unit mass mud shale sample3/ g, unit mass organic matter, clay The pore volume unit of each pore diameter range is cm in mineral and other mineral3/g;
Step 4:According to the equation group and object function in step 3, shale reservoir unit mass organic matter, clay pit are calculated Pore diameter range is respectively in thing, other mineral<2nm, 2-5nm, 5-10nm, 10-20nm, 20-50nm, 50-100nm and 100- 200nm pore volume Vij, wherein i=1,2 ..., n, be shale reservoir sample numbering, j=1,2 ..., 7, be aperture model The numbering enclosed, the pore volume unit of each pore diameter range is cm3/g。
CN201710788441.6A 2017-09-05 2017-09-05 Aperture location mode in a kind of evaluation mud shale organic matter, clay and other mineral Active CN107560994B (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN201710788441.6A CN107560994B (en) 2017-09-05 2017-09-05 Aperture location mode in a kind of evaluation mud shale organic matter, clay and other mineral

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN201710788441.6A CN107560994B (en) 2017-09-05 2017-09-05 Aperture location mode in a kind of evaluation mud shale organic matter, clay and other mineral

Publications (2)

Publication Number Publication Date
CN107560994A true CN107560994A (en) 2018-01-09
CN107560994B CN107560994B (en) 2019-08-02

Family

ID=60979207

Family Applications (1)

Application Number Title Priority Date Filing Date
CN201710788441.6A Active CN107560994B (en) 2017-09-05 2017-09-05 Aperture location mode in a kind of evaluation mud shale organic matter, clay and other mineral

Country Status (1)

Country Link
CN (1) CN107560994B (en)

Cited By (7)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN109540764A (en) * 2018-12-13 2019-03-29 中国石油大学(华东) A method of evaluation shale reservoir organic matter, clay and the contributed hole preservation ADSORPTION STATE methane thickness and density of other mineral
CN110018293A (en) * 2019-05-05 2019-07-16 西安石油大学 It is a kind of to consider the water-sensitive multiphase coupled methane air content calculation method of shale clay
CN110132816A (en) * 2019-05-15 2019-08-16 重庆地质矿产研究院 Method for analyzing pore structure of organic matter in shale of ancient world
CN111537390A (en) * 2020-06-11 2020-08-14 中国石油大学(华东) Method for evaluating increment of organic porosity of reservoir during shale oil thermal upgrading exploitation
CN113049785A (en) * 2021-04-08 2021-06-29 中国石油大学(华东) Method for evaluating methane in various components of shale reservoir in adsorption state
CN113670787A (en) * 2020-05-14 2021-11-19 中国石油天然气股份有限公司 Method for testing pore diameters of micropores and mesopores of organic matters and other minerals in shale
CN113970512A (en) * 2021-01-05 2022-01-25 中国石油天然气股份有限公司 Method for determining enrichment pore size range of free hydrocarbon

Citations (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN104697914A (en) * 2015-03-18 2015-06-10 中国石油大学(华东) Predication method of organic holes of different types of clay shale
CN105334149A (en) * 2015-11-24 2016-02-17 中国石油大学(北京) Micro-pore structure evaluation and reservoir classification method for tight reservoirs
CN106248521A (en) * 2016-07-11 2016-12-21 中国环境科学研究院 The hot authentication method of Organic Matter In Sediments early diagenesis evolution grade
CN106950347A (en) * 2017-03-03 2017-07-14 中国石油大学(华东) A kind of method for evaluating mud shale each group partial volume

Patent Citations (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN104697914A (en) * 2015-03-18 2015-06-10 中国石油大学(华东) Predication method of organic holes of different types of clay shale
CN105334149A (en) * 2015-11-24 2016-02-17 中国石油大学(北京) Micro-pore structure evaluation and reservoir classification method for tight reservoirs
CN106248521A (en) * 2016-07-11 2016-12-21 中国环境科学研究院 The hot authentication method of Organic Matter In Sediments early diagenesis evolution grade
CN106950347A (en) * 2017-03-03 2017-07-14 中国石油大学(华东) A kind of method for evaluating mud shale each group partial volume

Cited By (10)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN109540764A (en) * 2018-12-13 2019-03-29 中国石油大学(华东) A method of evaluation shale reservoir organic matter, clay and the contributed hole preservation ADSORPTION STATE methane thickness and density of other mineral
WO2020119021A1 (en) * 2018-12-13 2020-06-18 中国石油大学(华东) Method for evaluating thickness and density of adsorbed methane occurring in pores contributed by organic matter, clay and other minerals in shale reservoir
CN110018293A (en) * 2019-05-05 2019-07-16 西安石油大学 It is a kind of to consider the water-sensitive multiphase coupled methane air content calculation method of shale clay
CN110018293B (en) * 2019-05-05 2021-09-21 西安石油大学 Shale clay multiphase coupling methane gas content calculation method considering water sensitivity
CN110132816A (en) * 2019-05-15 2019-08-16 重庆地质矿产研究院 Method for analyzing pore structure of organic matter in shale of ancient world
CN113670787A (en) * 2020-05-14 2021-11-19 中国石油天然气股份有限公司 Method for testing pore diameters of micropores and mesopores of organic matters and other minerals in shale
CN111537390A (en) * 2020-06-11 2020-08-14 中国石油大学(华东) Method for evaluating increment of organic porosity of reservoir during shale oil thermal upgrading exploitation
CN113970512A (en) * 2021-01-05 2022-01-25 中国石油天然气股份有限公司 Method for determining enrichment pore size range of free hydrocarbon
CN113970512B (en) * 2021-01-05 2024-05-28 中国石油天然气股份有限公司 Method for determining free hydrocarbon enrichment pore size range
CN113049785A (en) * 2021-04-08 2021-06-29 中国石油大学(华东) Method for evaluating methane in various components of shale reservoir in adsorption state

Also Published As

Publication number Publication date
CN107560994B (en) 2019-08-02

Similar Documents

Publication Publication Date Title
CN107560994B (en) Aperture location mode in a kind of evaluation mud shale organic matter, clay and other mineral
Zhu et al. Microcosmic gas adsorption mechanism on clay-organic nanocomposites in a marine shale
Wang et al. Experimental study of pore structure and fractal characteristics of pulverized intact coal and tectonic coal by low temperature nitrogen adsorption
Xiong et al. Adsorption of methane in organic-rich shale nanopores: An experimental and molecular simulation study
Ji et al. Pore characterization of isolated organic matter from high matured gas shale reservoir
Yang et al. Pore characterization and methane sorption capacity of over-mature organic-rich Wufeng and Longmaxi shales in the southeast Sichuan Basin, China
Wang et al. Methane adsorption measurements and modeling for organic-rich marine shale samples
Yang et al. Measurement of the surface diffusion coefficient for adsorbed gas in the fine mesopores and micropores of shale organic matter
Gu et al. Influences of the composition and pore structure of a shale on its selective adsorption of CO2 over CH4
Wei et al. The effect of sample particle size on the determination of pore structure parameters in shales
Zhang et al. Research on the organic geochemical and mineral composition properties and its influence on pore structure of coal-measure shales in Yushe-Wuxiang Block, South Central Qinshui Basin, China
Wang et al. Experimental study of water vapor adsorption behaviors on shale
Boruah et al. Specific surface area and pore size distribution in gas shales of Raniganj Basin, India
CN103512838A (en) Method for determining contribution of pores with different apertures in shale reservoir stratum to porosity
Zhang et al. Monte Carlo simulations of methane adsorption on kaolinite as a function of pore size
Sun et al. Pore connectivity and water accessibility in Upper Permian transitional shales, southern China
Huang et al. Discussion on the rising segment of the mercury extrusion curve in the high pressure mercury intrusion experiment on shales
Hamza et al. Impact of clays on CO2 adsorption and enhanced gas recovery in sandstone reservoirs
Han et al. The pore characteristics and gas potential of the Jurassic continental shales in the middle-small basins, northwest China
Fu et al. Pore structure and multi-scale fractal characteristics of adsorbed pores in marine shale: a case study of the Lower Silurian Longmaxi shale in the Sichuan Basin, China
Hu et al. Mechanisms of shale gas adsorption: Insights from a comparative study on a thermodynamic investigation of microfossil-rich shale and non-microfossil shale
Rani et al. CO2 sorption and rate characteristics in micropores of shales
Mendhe et al. Evaluation of gas resource potentiality, geochemical and mineralogical characteristics of Permian shale beds of Latehar-Auranga Coalfield, India
Weishauptová et al. Effect of the properties of Silurian shales from the Barrandian Basin on their methane sorption potential
Yu et al. Structure characteristics and evolution mechanism of nanopore in transitional coal-bearing shale

Legal Events

Date Code Title Description
PB01 Publication
PB01 Publication
SE01 Entry into force of request for substantive examination
SE01 Entry into force of request for substantive examination
GR01 Patent grant
GR01 Patent grant