CN104850742A - Method for calculating CO2 salty water layer mineral sequestration potential - Google Patents
Method for calculating CO2 salty water layer mineral sequestration potential Download PDFInfo
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- CN104850742A CN104850742A CN201510235551.0A CN201510235551A CN104850742A CN 104850742 A CN104850742 A CN 104850742A CN 201510235551 A CN201510235551 A CN 201510235551A CN 104850742 A CN104850742 A CN 104850742A
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- feldspar
- albite
- anorthite
- safekeeping
- potentiality
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Abstract
The invention belongs to the technical field of geochemistry, in particular to a method for quantitatively calculating a CO2 salty water layer mineral sequestration potential by using a water-rock-CO2 geochemistry reaction. The CO2 sequestration potential is calculated according to the CO2 quantity consumed in the dissolving process of feldspar-like minerals in rock volume per unit and rock effective volume, contribution of calcite dissolving to the CO2 sequestration quantity is not contained in the calculating process, and only the quantity of CO2 consumed in the geochemistry reaction of the feldspar-like minerals is considered.
Description
Technical field
The invention belongs to geochemical techniques field, be specifically related to one and utilize water-rock-CO
2geochemical reaction quantitatively calculates CO
2salt water layer mineral seal the method for potentiality up for safekeeping.
Background technology
Under the general layout and background of global climate and environmental pollution, energy-saving and emission-reduction are industries that current government organs actively push forward.CO
2salt water layer is sealed up for safekeeping and is considered to reduce CO
2one of most effective method of discharge capacity, existing commercial scale and pilot scale yardstick CO
2seal test up for safekeeping and also prove that it is feasible technically.A large amount of CO
2after being injected into salt water layer, can catch with structure and structure, residual gas is caught, and dissolving is caught the mode of catching with mineral and sealed up for safekeeping; From catching form, be then with free state, solubilised state and mineral state form are sealed up for safekeeping.In other words, total CO
2it is by free state that salt water layer seals potentiality up for safekeeping, solubilised state and mineral state CO
2three part compositions.Accurate calculating CO
2salt water layer seals potentiality up for safekeeping for carrying out commercial size profit pilot scale yardstick CO
2injection project is significant, is one of key factor of addressing.
Current existing CO
2it is all for free state and solubilised state CO that salt water layer seals potentiality method up for safekeeping
2seal up for safekeeping gauge calculate, such as carbon sequestration leader forum and american energy office etc. propose catch for structure and structure, residual gas is caught and CO is caught in dissolving
2seal free state and the solubilised state CO of potentiality computing method and some scholars proposition up for safekeeping
2seal potentiality computing method up for safekeeping.For mineral state CO
2seal potentiality up for safekeeping, some scholars adopts the CO on actual geology model-based plinth
2migration reaction numerical simulation calculates, but inherently there is a lot of uncertainty in numerical model, there is error even mistake in the inaccurate result of calculation that also can cause of the assignment of parameter, and this geochemical model all cannot correct in most cases, and the confidence level providing result is worth discussion.There are some researches show, on-Wan annual time scale in thousand, mineral are sealed up for safekeeping CO
2the contribution proportion sealing potentiality up for safekeeping is 5%-40%, and the actual amount of sealing up for safekeeping depends on salt water layer formation water geochemistry and Reservoir Minerals component.Structure compared and structure are sealed up for safekeeping and residual gas seals (free state) up for safekeeping and dissolving is sealed up for safekeeping (solubilised state), and the security that mineral are sealed up for safekeeping (mineral state) is best, so need to propose a kind of calculating CO
2mineral seal the computing method of potentiality up for safekeeping.
In fact, a large amount of CO
2can local water be dissolved in after being injected into salt water layer, and promote water rock chemical reaction, namely cause a series of geochemical reaction.These courses of reaction can consume a certain amount of CO
2, generate new secondary mineral, reach the object that mineral are sealed up for safekeeping.So this method is for CO main in current world wide
2rock type-the sandstone reservoir of reservoir and typical mineral component characteristics thereof, according to these mineral and CO
2chemical equation interactional with local water, sets up CO in unit rock volume
2consumption, obtain total mineral and seal potentiality up for safekeeping, for carrying out CO
2the site addressing that injection test or scale are sealed up for safekeeping and later stage planning provide reference frame.
Summary of the invention
Technical matters to be solved by this invention calculates CO exactly
2salt water layer mineral seal potentiality up for safekeeping, promote CO
2the research and development that salt water layer is sealed up for safekeeping.
The present invention proposes a kind of CO based on sandstone reservoir geochemical reaction
2salt water layer mineral seal potentiality computing method up for safekeeping, can determine CO efficiently and accurately
2salt water layer mineral seal potentiality up for safekeeping.According to existing research, CO main at present
2reservoir is sandstone reservoir, and its typical mineral component is potassium feldspar, soda feldspar and lime feldspar and a small amount of carbonate mineral.CO
2after being injected into salt water layer reservoir, the dissolving of feldspar and carbonate mineral can be promoted.So the ultimate principle of this method is according to the used up CO of feldspathoid course of dissolution in unit rock volume
2amount and total rock active volume, set up mineral state CO
2seal potentiality computing method up for safekeeping, obtain CO
2mineral seal potentiality up for safekeeping.
Sandstone reservoir typical case geochemical reaction: sandstone belongs to petroclastic rock, and comprise chip and cementing matter two parts, chip content is greater than 50% usually.The mineral of sandstone reservoir are primarily of quartz, and feldspar and clay mineral form, and its andesine is mainly potassium feldspar, soda feldspar and lime feldspar; The components such as cementing matter comprises calcareous, siliceous and shale, wherein calcareous cement is based on carbonate mineral.A large amount of CO
2after being injected into sandstone reservoir, can there is following geochemical reaction (2-1 ~ 2-5) in carbonate mineral and feldspathoid.
2KAlSi
3o
8(potassium feldspar)+CO
2+ 2H
2o → Al
2(Si
2o
5) (OH)
4(smalite)+4SiO
2+ K
2cO
32-2
2NaAlSi
3o
8(soda feldspar)+2CO
2+ 3H
2o → Al
2(Si
2o
5) (OH)
4(smalite)+4SiO
2+ 2NaHCO
32-3
NaAlSi
3o
8(soda feldspar)+CO
2+ H
2o → NaAlCO
3(OH)
2(dawsonite)+3SiO
22-4
CaAl
2si
2o
8(lime feldspar)+CO
2+ 2H
2o → Al
2(Si
2o
5) (OH)
4(smalite)+CaCO
32-5
Because kalzit belongs to least stable mineral, so it is to CO
2the mineral amount of sealing up for safekeeping produced belongs to temporary and seals up for safekeeping; On the contrary, the course of dissolution of feldspathoid is to CO
2consumption be permanent sealing up for safekeeping.So, at calculating CO
2salt water layer mineral are sealed up for safekeeping in potentiality and are not comprised Calcite Dissolution to CO
2the contribution of the amount of sealing up for safekeeping, only considers that feldspathoid geochemical reaction consumes CO
2amount.
CO
2salt water layer mineral seal potentiality computing method up for safekeeping: according to chemical equation 2-2 ~ 2-5, and the dissolving of every 1mol potassium feldspar can consume the CO of 0.5mol
2, the dissolving of every 1mol soda feldspar can consume the CO of 1mol
2, the dissolving of every 1mol lime feldspar can consume the CO of 1mol
2.So, CO
2salt water layer mineral are sealed potentiality computing method up for safekeeping and can be calculated by through type 2-6, wherein m
cO2cO
2salt water layer mineral seal total potentiality up for safekeeping,
with
be that the mineral that the dissolving of potassium feldspar, soda feldspar and lime feldspar produces seal potentiality up for safekeeping respectively, unit is Mt; ρ
k-feldspar, ρ
albiteand ρ
anorthitebe potassium feldspar, soda feldspar and anorthitic density respectively, unit is kg/m
3; V
k-feldspar, V
albiteand V
anothitebe the cumulative volume of potassium feldspar, soda feldspar and lime feldspar mineral respectively, unit is km
3; M
cO2, M
k-feldspar, M
albiteand M
anorthitecO respectively
2, potassium feldspar, soda feldspar and lime feldspar mineral molal weight, CO
2molal weight be 44g/mol; A is CO
2store coefficient of efficiency, dimensionless.
The present invention is based on CO
2be injected into the geochemical reaction that sandstone salt water layer promotes afterwards, utilize unit rock volume spectra to dissolve used up CO
2amount and reservoir rock volume, establish CO
2salt water layer mineral seal potentiality computing method up for safekeeping, can obtain CO exactly
2salt water layer mineral seal potentiality up for safekeeping.
Embodiment
About CO in reference summary of the invention
2salt water layer mineral seal potentiality computing method up for safekeeping, based on molecular weight and the data such as density and calculating site sandstone reservoir mineral content of typical spectra, determine the calculating parameter in formula 2-6, can calculate CO
2salt water layer mineral seal potentiality up for safekeeping.The wherein density p of spectra
k-feldspar, ρ
albiteand ρ
anorthitewith molal weight M
k-feldspar, M
albiteand M
anorthitecan be obtained by inspection information; Spectra cumulative volume V
k-feldspar, V
albiteand V
anorthitecan be determined by the reservoir landwaste of site and various spectra content parameter; Store the value that coefficient of efficiency a can utilize monte carlo method to draw for North America geologic condition with reference to the USDOE extensively adopted in the world at present.Concrete mode is as described below.
The density p of spectra
k-feldspar, ρ
albiteand ρ
anorthite
By By consulting literatures data, potassium feldspar, soda feldspar and anorthitic density are ρ respectively
k-feldspar=2.55-2.67 × 10
3kg/m
3, ρ
albite=2.55-2.60 × 10
3kg/m
3and ρ
anorthite=2.75-2.76 × 10
3kg/m
3.
the molal weight M of spectra
k-feldspar, M
albiteand M
anorthite
Potassium feldspar, soda feldspar and anorthitic molal weight are M respectively
k-feldspar=279.07g/mol, M
albite=262.96g/mol profit M
albite=278.94g/mol.
The volume V of spectra
k-feldspar, V
albiteand V
anorthite
Potassium feldspar, soda feldspar and anorthitic concrete account form are such as formula shown in 2-7.Wherein φ is the average pore of sandstone reservoir, dimensionless; V is the volume of sandstone reservoir, and can be obtained by geologic examination and well-log information, unit is km
3; C
debristhe content ratio of chip in sandstone reservoir, dimensionless; C
feldsparthe content ratio of chip andesine mineral, dimensionless; X
k-feldsapr, X
albiteand X
anorthitebe potassium feldspar, soda feldspar and the lime feldspar content ratio at spectra respectively, dimensionless, these parameters can be analyzed by the mineral constituent of actual sandstone reservoir and obtain measured value.
V
K-feldspar=V·(1-φ)·C
debris·C
feldspar·X
K-feldspar
V
albite=V·(1-φ)·C
debris·C
feldspar·X
albite2-7
V
anorthite=V·(1-φ)·C
debris·C
feldspar·X
anorthite
CO
2store coefficient of efficiency a
CO
2store coefficient of efficiency a to control by the dissolution precipitation dynamic process of the nonuniformity of reservoir and anisotropy, mineral and local water contact area and mineral.Widely use at present the parameter value that USDOE obtains according to the Monte Carlo simulation that North America geologic condition carries out in the world, namely 15%, 50% and 85% confidence level condition under, store coefficient of efficiency and be respectively 1%, 2.4% and 4%.
First embodiment
Utilize above-mentioned CO
2salt water layer mineral seal potentiality computing method up for safekeeping, carried out mineral seal potentiality calculating up for safekeeping to upper Cretaceous series Qingshankou group to the Nenjiang group salt water layer reservoir of the Baokang sedimentary system growth of central depression, Jilin Oil Field south Changling Sag.Reservoir lithology feature shows to be suitable for CO
2the salt water layer sealed up for safekeeping is Qingshankou group one section, two sections, three sections and Yao Jia group one section, and corresponding cap rock is the thick-layer shape mud stone of Nenjiang group and Yao Jia group two sections and three sections.Qingshankou group one section, two sections, three sections are respectively 430km with Yao Jia group one section of sandstone cumulative volume V
3, 980km
3, 1500km
3profit 80kmn
3; Average pore φ is respectively 14.1%, 18.7%, 18.7% and 9.2%, i.e. CO
2sealing the total active volume of sand body up for safekeeping is 2459.2km
3.According to the microscopic of actual reservoir core sample, this sandstone, based on landwaste arkosic arenite and feldspar rock-fragment sandstone, forms primarily of quartz, feldspar, landwaste and a small amount of heavy mineral.Chip content is 40 ~ 85%, and chip andesine content is 15 ~ 52%, and in spectra, potassium feldspar, the anorthitic content of soda feldspar profit are respectively 5 ~ 10%, 50 ~ 70% and 20 ~ 35%.Store coefficient of efficiency and be assumed to be 1%.Result shows, based on the CO that the present invention proposes
2salt water layer mineral seal potentiality computing method up for safekeeping, draw Baokang sedimentary system CO
2salt water layer mineral are sealed potentiality minimum value profit maximal value up for safekeeping and are respectively 457.5Mt and 5114.4Mt, and wherein soda feldspar and lime feldspar dissolve the CO produced
2the mineral amount of sealing up for safekeeping is the main contributions that mineral are sealed up for safekeeping, and account for respectively and always seal 60% and 30% of potentiality up for safekeeping, this is relevant with the content characteristics of this area spectra.
Claims (5)
1. one kind calculates CO
2salt water layer mineral seal the method for potentiality up for safekeeping, it is characterized in that: according to the used up CO of feldspathoid course of dissolution in unit rock volume
2amount and rock active volume, calculate CO
2seal potentiality up for safekeeping, in computation process, do not comprise Calcite Dissolution to CO
2the contribution of the amount of sealing up for safekeeping, only considers that feldspathoid geochemical reaction consumes CO
2amount.
2. calculate CO as claimed in claim 1
2salt water layer mineral seal the method for potentiality up for safekeeping, wherein CO
2salt water layer mineral seal potentiality up for safekeeping by following formulae discovery:
Wherein M
cO2cO
2salt water layer mineral seal total potentiality up for safekeeping,
with
be that the mineral that the dissolving of potassium feldspar, soda feldspar and lime feldspar produces seal potentiality up for safekeeping respectively, unit is Mt; ρ
k-feldspar, ρ
albiteand ρ
anorthitebe potassium feldspar, soda feldspar and anorthitic density respectively, unit is kg/m
3; V
k-feldspar, V
albiteand V
anorthitebe the cumulative volume of potassium feldspar, soda feldspar and lime feldspar mineral respectively, unit is km
3; M
cO2, M
k-feldspar, M
albiteand M
anorthitecO respectively
2, potassium feldspar, soda feldspar and lime feldspar mineral molal weight, CO
2molal weight be 44g/mol; A is CO
2store coefficient of efficiency, dimensionless.
3. calculate CO as claimed in claim 2
2salt water layer mineral seal the method for potentiality up for safekeeping, wherein the density p of spectra
k-feldspar, ρ
albiteand ρ
anorthitewith molal weight M
k-feldspar, M
albiteand M
anorthiteobtained by inspection information; Spectra cumulative volume V
k-feldspar, V
albiteand V
anorthitedetermined by the reservoir landwaste of site and various spectra content parameter; CO
2store the value that coefficient of efficiency a adopts USDOE to utilize monte carlo method to draw for North America geologic condition.
4. calculate CO as claimed in claim 3
2salt water layer mineral seal the method for potentiality up for safekeeping, spectra cumulative volume V
k-feldspar, V
albiteand V
anorthitespecific formula for calculation as follows:
V
K-feldspar=V·(1-φ)·C
debris·C
feldspar·X
K-feldspar
V
albite=V·(1-φ)·C
debris·C
feldspar·X
albite
V
anorthite=V·(1-φ)·C
debris·C
feldspar·X
anorthite
Wherein φ is the average pore of sandstone reservoir, dimensionless; V is the volume of sandstone reservoir, and can be obtained by geologic examination and well-log information, unit is km
3; C
debristhe content ratio of chip in sandstone reservoir, dimensionless; C
feldsparthe content ratio of chip andesine mineral, dimensionless; X
k-feldsapr, X
albiteand X
anorthitebe potassium feldspar, soda feldspar and the lime feldspar content ratio at spectra respectively, dimensionless, these parameters can be analyzed by the mineral constituent of actual sandstone reservoir and obtain measured value.
5. calculate CO as claimed in claim 4
2salt water layer mineral seal the method for potentiality up for safekeeping, CO
2store the parameter value that coefficient of efficiency a uses USDOE to obtain according to the Monte Carlo simulation that North America geologic condition carries out, namely 15%, 50% and 85% confidence level condition under, store coefficient of efficiency and be respectively 1%, 2.4% and 4%.
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Cited By (2)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN112924648A (en) * | 2021-01-26 | 2021-06-08 | 大连理工大学 | Evaluation geological sequestration CO2Method for mineralizing evolution law and sealing storage quantity |
WO2022187853A1 (en) * | 2021-03-04 | 2022-09-09 | Okeefe Frank | System incentivizing greenhouse gas sequestration |
Citations (7)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN101190743A (en) * | 2007-11-30 | 2008-06-04 | 中国科学院武汉岩土力学研究所 | Carbon dioxide geological sequestration method based on mixed fluid self-detaching |
CN102313790A (en) * | 2011-07-19 | 2012-01-11 | 北京师范大学 | Submarine geologic body carbon dioxide sequestration potential assessment method |
CN103529487A (en) * | 2013-10-29 | 2014-01-22 | 中国石油大学(华东) | Method for judging mantle-derived CO2 charging time |
CN103544361A (en) * | 2013-11-04 | 2014-01-29 | 西北大学 | Evaluation method of CO2 geological sequestration potential in oil-gas field development |
CN103628867A (en) * | 2013-11-26 | 2014-03-12 | 中国石油天然气股份有限公司 | Method and system for simulating and analyzing shale reservoir diagenetic evolution process |
CN103645125A (en) * | 2013-10-28 | 2014-03-19 | 北京大学 | Method and system for evaluating seepage capability of dense oil reservoir bed |
CN104007484A (en) * | 2014-06-06 | 2014-08-27 | 董春梅 | Shale classification method |
-
2015
- 2015-05-08 CN CN201510235551.0A patent/CN104850742B/en not_active Expired - Fee Related
Patent Citations (7)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN101190743A (en) * | 2007-11-30 | 2008-06-04 | 中国科学院武汉岩土力学研究所 | Carbon dioxide geological sequestration method based on mixed fluid self-detaching |
CN102313790A (en) * | 2011-07-19 | 2012-01-11 | 北京师范大学 | Submarine geologic body carbon dioxide sequestration potential assessment method |
CN103645125A (en) * | 2013-10-28 | 2014-03-19 | 北京大学 | Method and system for evaluating seepage capability of dense oil reservoir bed |
CN103529487A (en) * | 2013-10-29 | 2014-01-22 | 中国石油大学(华东) | Method for judging mantle-derived CO2 charging time |
CN103544361A (en) * | 2013-11-04 | 2014-01-29 | 西北大学 | Evaluation method of CO2 geological sequestration potential in oil-gas field development |
CN103628867A (en) * | 2013-11-26 | 2014-03-12 | 中国石油天然气股份有限公司 | Method and system for simulating and analyzing shale reservoir diagenetic evolution process |
CN104007484A (en) * | 2014-06-06 | 2014-08-27 | 董春梅 | Shale classification method |
Non-Patent Citations (7)
Title |
---|
NING WEI等: "Earyly opportunities of CO2 geological storage deployment in coal chemical industry in China", 《ENERGY PROCEDIA》 * |
R.ZENG等: "Zeolite synthesis from a high SI-AL fly ash from east china", 《JOURNAL OF CHEMICAL TECHNOLOGY AND BIOTECHNOLOGY》 * |
RONGSHU ZENG等: "New potential carbon emission reduction enterprises in China:deep geological storage of CO2 emitted through industrial usage of coal in China", 《GREENHOUSE GASES:SCIENCE AND TECHNOLOGY》 * |
曾荣树等: "华北平原CO2地下埋存潜力研究", 《第四纪研究》 * |
李义曼等: "二氧化碳咸水层封存和利用", 《科技导报》 * |
莫绍星等: "咸水层CO2矿物封存数值模拟研究进展", 《地质科技情报》 * |
金超等: "松辽盆地南部保康体系上白垩统CO2埋存条件与潜力", 《地球科学-中国地质大学学报》 * |
Cited By (4)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN112924648A (en) * | 2021-01-26 | 2021-06-08 | 大连理工大学 | Evaluation geological sequestration CO2Method for mineralizing evolution law and sealing storage quantity |
CN112924648B (en) * | 2021-01-26 | 2022-01-04 | 大连理工大学 | Evaluation geological sequestration CO2Method for mineralizing evolution law and sealing storage quantity |
WO2022187853A1 (en) * | 2021-03-04 | 2022-09-09 | Okeefe Frank | System incentivizing greenhouse gas sequestration |
US11783348B2 (en) | 2021-03-04 | 2023-10-10 | Frank T. O'Keefe | System incentivizing green energy usage |
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