Surface-modified Ag@Ru-P25 for photocatalytic CO_(2) conversion with high selectivity over CH_(4) formation at the solid–gas interface

Systematic optimization of the photocatalyst and investigation of the role of each component is important to maximizing catalytic activity and comprehending the photocatalytic conversion of CO_(2) reduction to solar fuels.A surface-modified Ag@Ru-P25 photocatalyst with H_(2)O_(2) treatment was designed in this study to convert CO_(2) and H_(2)O vapor into highly selective CH4.Ru doping followed by Ag nanoparticles(NPs)cocatalyst deposition on P25(TiO_(2))enhances visible light absorption and charge separation,whereas H_(2)O_(2) treatment modifies the surface of the photocatalyst with hydroxyl(–OH)groups and promotes CO_(2) adsorption.High-resonance transmission electron microscopy,X-ray photoelectron spectroscopy,X-ray absorption near-edge structure,and extended X-ray absorption fine structure techniques were used to analyze the surface and chemical composition of the photocatalyst,while thermogravimetric analysis,CO_(2) adsorption isotherm,and temperature programmed desorption study were performed to examine the significance of H_(2)O_(2) treatment in increasing CO_(2) reduction activity.The optimized Ag1.0@Ru1.0-P25 photocatalyst performed excellent CO_(2) reduction activity into CO,CH4,and C2H6 with a~95%selectivity of CH4,where the activity was~135 times higher than that of pristine TiO_(2)(P25).For the first time,this work explored the effect of H_(2)O_(2) treatment on the photocatalyst that dramatically increases CO_(2) reduction activity.

Formation Characteristics of CO_(2) Hydrates in the Presence of Porous Media and NaCl

Hydrate-based CO_(2) sequestration is an effective method for reducing the greenhouse effect,and the presence of porous media and NaCl can impact the formation characteristics of hydrates.This study uses the constant volume temperature search method to investigate the effects of quartz sand particle size(0.006‒0.03 mm),water saturation(30%–90%),and NaCl concentration(1%‒9%)on the phase equilibrium and kinetics of CO_(2) hydrates within a temperature range of 273‒285 K and pressure range of 1.0‒3.5 MPa.The results indicate that a decrease in quartz sand particle size or an increase in NaCl concentration shifts the hydrate phase equilibrium curve towards lower temperatures and higher pressures,making hydrate generation conditions more demanding.In different particle size systems,there are no significant changes in the rate of CO_(2) hydrate formation or conversion rate.The highest hydrate conversion rate of 71.1%is observed in a 0.015 mm particle size system.With increasing water saturation,both the generation rate and conversion rate of CO_(2) hydrates show a trend of first increasing and then decreasing.Meanwhile,low concentrations of NaCl(1%–3%)are found to enhance the formation and conversion rates of CO_(2) hydrates.However,as NaCl concentration increases,the rate of CO_(2) hydrate formation and conversion rate decrease.

Application and prospects of spatial information technology in CO_(2)sequestration monitoring

This paper systematically reviews the current applications of various spatial information technologies in CO_(2)sequestration monitoring,analyzes the challenges faced by spatial information technologies in CO_(2)sequestration monitoring,and prospects the development of spatial information technologies in CO_(2)sequestration monitoring.Currently,the spatial information technologies applied in CO_(2)sequestration monitoring mainly include five categories:eddy covariance method,remote sensing technology,geographic information system,Internet of Things technology,and global navigation satellite system.These technologies are involved in three aspects:monitoring data acquisition,positioning and data transmission,and data management and decision support.Challenges faced by the spatial information technologies in CO_(2)sequestration monitoring include:selecting spatial information technologies that match different monitoring purposes,different platforms,and different monitoring sites;establishing effective data storage and computing capabilities to cope with the broad sources and large volumes of monitoring data;and promoting collaborative operations by interacting and validating spatial information technologies with mature monitoring technologies.In the future,it is necessary to establish methods and standards for designing spatial information technology monitoring schemes,develop collaborative application methods for cross-scale monitoring technologies,integrate spatial information technologies with artificial intelligence and high-performance computing technologies,and accelerate the application of spatial information technologies in carbon sequestration projects in China.

Hydrocarbon indication in Rio Bonito Formation sandstone:Implication for CO_(2)storage in São Paulo,Brazil

São Paulo State has witnessed CO_(2)storage-based investigations considering the availability of suitable geologic structures and proximity to primary CO_(2)source sinks related to bioenergy and carbon capture and storage(BECCS)activities.The current study presents the hydrocarbon viability evaluations and CO_(2)storage prospects,focusing on the sandstone units of the Rio Bonito Formation.The objective is to apply petrophysical evaluations with geochemical inputs in predicting future hydrocarbon(gas)production to boost CO_(2)storage within the study location.The study used data from eleven wells with associated wireline logs(gamma ray,resistivity,density,neutron,and sonic)to predict potential hydrocarbon accumulation and fluid mobility in the investigated area.Rock samples(shale and carbonate)obtained from depths>200 m within the study location have shown bitumen presence.Organic geochemistry data of the Rio Bonito Formation shale beds suggest they are potential hydrocarbon source rocks and could have contributed to the gas accumulations within the sandstone units.Some drilled well data,e.g.,CB-1-SP and TI-1-SP,show hydrocarbon(gas)presence based on the typical resistivity and the combined neutron-density responses at depths up to 3400 m,indicating the possibility of other hydrocarbon members apart from the heavy oil(bitumen)observed from the near-surface rocks samples.From the three-dimensional(3-D)model,the free fluid indicator(FFI)is more significant towards the southwest and southeast of the area with deeper depths of occurrence,indicating portions with reasonable hydrocarbon recovery rates and good prospects for CO_(2)injection,circulation and permanent storage.However,future studies based on contemporary datasets are required to establish the hydrocarbon viability further,foster gas production events,and enhance CO_(2)storage possibilities within the region.

Assessment of CO_(2)storage prospect based on physical properties of Rio Bonito Formation rock units

The physical properties of the rock units associated with the Rio Bonito Formation are presented in this study with the focus on modelling reservoir quality based on petrophysics-derived parameters to evaluate CO_(2)storage potentials.It involves the modelling of the reservoir depths,thicknesses,flow zone indicators(FZI),and effective permeability(Keff)and presenting the CO_(2)storage efficiency factors peculiar to the rock units of the study location.Research results presented by this study for the stated objectives are not quite common in the region.Keff values range from 200 mD to higher than 2000 mD,and FZI values are generally above 1.0 mm and up to 13.0 mm within the portions covered by the drilled wells.The sandstone units recorded are up to 20 m thick in some cases.The Keff and FZI models indicate the sandstone reservoirs as permeable units to support the injection and circulation of CO_(2)within the potential reservoir units of the Rio Bonio Formation across São Paulo State.Apart from some points in the southeastern part of the study location,where the Rio Bonito are delineated at depths less than 800 m(minimum CO_(2)storage depth based on best practices),other portions are deeper,ranging from 950 m to 3500 m.Thin-bedded layers will affect the integrity of the rocks as CO_(2)storage tanks or reservoir seals/traps/overburden within the region.Sandstone bed thicknesses are up to 20 m in some cases.However,hybrid CO_(2)reservoir units are feasible,especially in portions where thin siltstone layers are sandwiched between sandstone units to provide considerable thicknesses based on CO_(2)storage standards.The current study shows that useable areas considering reservoir thickness,depth,and other physical qualities will significantly control the CO_(2)storage efficiency of the study location.Further studies featuring a detailed geophysical exploration of the site to confirm the availability and saturations of preexisting fluid(hydrocarbon and water)are encouraged to boost CO_(2)storage in the region.The related research-based results,as mentioned above,may be combined with the results of this research to determine the area's potentials for CO_(2)storage or hydrocarbon production with CO_(2)storage options.

海洋CO_(2)地质封存研究进展与发展趋势

CO_(2)捕集、利用和封存是中国实现“双碳”目标的核心技术,也是全球研究的热点。CO_(2)地质封存是其中的关键环节,特别是海洋CO_(2)地质封存是今后的重点发展方向。以国内外海洋CO_(2)地质封存的发展历程为基础,结合典型CO_(2)海洋封存示范项目案例,系统梳理了国内外海洋CO_(2)地质封存理论研究进展,分析了CO_(2)在井筒流动、相变与传热、CO_(2)流体运移与储层物性参数展布规律、海洋地质封存机制及封存潜力、地质封存盖层完整性及安全性评估等方面的研究现状。认识到中国目前对海底地质结构中CO_(2)注入过程的多相态转化、溶解、捕获传质特征及动力学特性认识尚浅,对海洋封存机制及不同封存机制之间的相互作用机理尚不明确,未来应开展海洋CO_(2)动态地质封存空间重构机制研究,解决地质封存相态转化及流体动态迁移机理等关键科学问题,揭示海洋CO_(2)地质封存机制的相互作用机理,形成适用于中国海洋地质封存CO_(2)高效注入和增效封存方法。

黄铁矿在CO_(2)气氛下非等温氧化转化及动力学分析

针对煤中常见含铁矿物黄铁矿在富氧燃烧典型气氛下转化特性,通过同步热分析结合烟气分析研究了黄铁矿在CO_(2)气氛下的转化行为.结果发现,黄铁矿在CO_(2)气氛下主要经历5个失重阶段且均为吸热过程,首先是黄铁矿颗粒表面硫脱除的起始热解段(相界面反应,n=1/2),活化能低于其在N_(2)气氛下近30 kJ/mol,为220.27 kJ/mol,随后裂解成磁黄铁矿(三维扩散,n=1/2)活化能与其在N_(2)(177.27 kJ/mol)下接近为178.1 kJ/mol;温度高于690℃,随着升温磁黄铁矿缓慢失硫,CO_(2)逐渐参与磁黄铁矿转化且释放SO_(2)和CO;820~1150℃经历双峰失重峰阶段,820~1020℃,氧化气体产物SO_(2)大量生成且在约1000℃达到体积浓度峰值;最后1020~1150℃,坩埚中残留物大量与CO_(2)持续氧化反应失重形成SO_(2)和CO,坩埚中形成复杂物相体系,铁硫化物和铁氧化物共存(或共融).CO_(2)参与黄铁矿产物转化失重阶段活化能分别为180.94 kJ/mol、229.69 kJ/mol和243.46 kJ/mol,动力学机制均为成核与生长(n=1).

纳米SiO_(2)强化CO_(2)地质封存页岩盖层封堵能力机制试验

页岩为CO_(2)盐水层地质封存常见盖层岩石类型,强化盖层封堵能力有利于提高CO_(2)地质埋存量和安全性。为探究随CO_(2)混注纳米SiO_(2)(SNPs)强化盖层封堵能力的有效性和可行性,对CO_(2)地质封存页岩盖层样品开展原地条件下的超临界CO_(2)酸蚀反应试验,基础组为页岩样品-地层水、对照组为页岩样品-地层水+超临界CO_(2)、优化组为页岩样品-地层水+SNPs+超临界CO_(2),并采用核磁共振测试、场发射扫描电镜可视化观测、X射线衍射测试和岩石力学试验,探究CO_(2)酸蚀反应前后的页岩孔隙结构、表面形貌、矿物成分及力学性质特征。结果表明:优化组的大孔孔隙分量及孔隙度和渗透率增大幅度低于对照组;与对照组相比,优化组黏土矿物与碳酸盐岩矿物相对含量损失少,表明随CO_(2)混注SNPs可使岩样内部酸蚀作用减弱;SNPs在岩石端面吸附聚集或进入岩心孔喉,可使优化组页岩样品力学性能损伤程度降低;随CO_(2)混注SNPs有利于强化CO_(2)盐水层地质封存盖层封堵能力。

三河尖关闭煤矿煤层CO_(2)封存潜力研究

关闭煤矿煤层CO_(2)地质封存是CO_(2)封存的重要方式之一,也是短期内实现碳减排指标的有效手段之一。以江苏省徐州市三河尖关闭煤矿为例,分析了已采7号煤和9号煤的煤岩煤质特征,统计了剩余煤炭资源储量,运用模糊综合评价法,选取了稳定系数、上覆岩层性质、地质构造复杂程度、地下水指标、封存煤层压温比、封存煤层深厚比、封存煤层渗透率、采空塌陷程度和其他因素等9个主要影响因素指标对7号煤和9号煤封存CO_(2)稳定性进行评价,建立关闭煤矿煤层CO_(2)封存评价方法并评估CO_(2)封存潜力。结果表明,三河尖关闭煤矿7号煤和9号煤剩余储量较大,CO_(2)封存稳定性综合评价结果分别为86.209和87.698,评价等级均为较稳定,封存潜力较高。根据建立的关闭煤矿煤层CO_(2)封存评价方法,计算获得三河尖关闭煤矿7号和9号煤层CO_(2)理论封存量分别为207.6 Mt和80.9 Mt,并据此划分封存有利区为有利区、较有利区和不利区3个等级。研究可为关闭煤矿煤层CO_(2)封存研究提供基础依据。

“双碳”目标下火电厂CO_(2)计量技术研究现状与展望

中国电力行业CO_(2)排放量是CO_(2)排放的主要来源,其中火电厂CO_(2)排放量在电力行业中占比最大。在“双碳”目标下,CO_(2)计量技术可以实现对火电厂中CO_(2)排放量的直观判断,为火电厂CO_(2)减排提供重要支撑,促进火电厂参与碳交易,带动区域经济发展。结合国内外政策,讨论了目前通用CO_(2)计量方法的实施进展,总结归纳了以碳核算为主、碳监测为辅的火电厂CO_(2)计量方法存在的问题,并对火电厂CO_(2)计量技术应用的重难点进行了分析。最后,对火电厂CO_(2)计量技术的发展及应用进行了展望。

一种基于“四区”的低渗透油藏CO_(2)埋存量计算方法及应用

CO_(2)驱油和埋存能有效减少温室气体排放量达到碳中和目标,已有的CO_(2)埋存量计算方法主要针对CO_(2)的静态埋存量进行粗略计算,未考虑实际生产过程中CO_(2)埋存量的变化。针对上述问题,运用CO_(2)溶解、CO_(2)波及体积和驱油机理,将CO_(2)驱油与埋存过程分为气相区、两相或近混相区、扩散区和油相区,并基于“四区法”计算CO_(2)埋存量,得到了不同烃类的注入孔隙体积倍数、注入压力、注气速度下的CO_(2)动态埋存量的变化规律。将研究成果应用于W油田低渗储层,结果表明:注入烃类孔隙体积倍数、压力、注气速度与总埋存量呈正相关性,当压力由12 MPa升至30 MPa,CO_(2)埋存总量增加15.53×10^(4)t;当注气速度由5 t/d增加至30 t/d,峰值CO_(2)埋存总量由3.51×10^(4)t提高至12.62×10^(4)t。研究成果可为同类油藏开展CO_(2)驱油与埋存项目提供新的思路。

CO_(2)分注井气嘴节流特性及矿场应用

为了解决CO_(2)分注井节流压差建立困难,气嘴易冲蚀的技术难题,通过构建CO_(2)物性变化的流动-传热耦合模型,揭示2级和3级节流气嘴的流场演化机制,优化设计气嘴结构、建立了绕流气嘴节流图版并开展现场应用。结果表明:流量为10 m3/d时,2级嘴径1.4 mm和3级嘴径1.6 mm的绕流气嘴分别能产生将近6 MPa和8 MPa的节流压差,证明绕流气嘴结构合理、性能可靠、能够达到调整层间压差的技术要求;参照气嘴图版优选的节流气嘴,现场应用20口井,节流压差可达4 MPa左右,调整后注入压力上升2.4 MPa,加强层相对吸气比例由9.7%上升至50.7%,有效调整了层间差异,解决了分注井小层吸气不均的问题。研究结果指导现场测调,为CO_(2)分注规模化应用提供技术支撑。

跨临界CO_(2)循环系统控制优化策略的研究进展

控制策略作为跨临界CO_(2)循环系统的重要组成部分,是保证系统高效节能运行的关键。介绍了系统最优排气压力经验计算和泊金汉π定理的反馈控制、基于梯度追踪和极值寻优的实时在线控制以及基于神经网络的预测控制等,详细分析了系统控制策略的发展历程和未来发展趋势,并总结如下:离线控制建立简单、成本低,但易受到环境因素和系统部件变化的影响而导致控制性能降低;实时在线控制策略可以实时追踪系统最大能源效率对应的排气压力,但由于寻优过程费时较长,导致控制系统的收敛时间过长;模型预测控制系统可以实现实时优化和快速收敛,有着良好的发展前景。结合新能源汽车、建筑供暖、轨道交通、商超冷藏、军工等实际场景对跨临界CO_(2)循环系统控制策略的应用特点和未来发展趋势进行分析,进一步说明了提高控制策略的适用性是未来研究的重要方向,并分析将广义预测控制、强化学习等具有自适应属性的方法应用于跨临界CO_(2)循环系统控制策略的可行性,同时探讨了开发适用于大规模循环系统和储能系统控制策略在我国“双碳”背景下的重要意义。

适合致密油藏的超临界CO_(2)-气溶性表面活性剂复合吞吐技术

为了进一步提高致密油储层超临界CO_(2)吞吐的开发效果,探索适合致密油藏的超临界CO_(2)-气溶性表面活性剂复合吞吐技术,通过原油黏度实验、油气界面张力实验、最小混相压力实验、原油膨胀系数实验以及超临界CO_(2)-气溶性表面活性剂复合吞吐模拟实验,评价了不同类型气溶性表面活性剂的性能及其对吞吐采收率的影响。结果表明:气溶性表面活性剂GRS⁃1的综合性能更加突出,随着气溶性表面活性剂质量分数的不断增大,原油黏度、油气界面张力和最小混相压力均呈现出逐渐降低的趋势,而原油体积膨胀系数则逐渐增大,并且岩心的吞吐采收率和入口端压力也呈现出逐渐增大的趋势;随着混合流体注入量的增加以及闷井时间的延长,岩心吞吐采收率和入口端压力均逐渐增大,并且岩心的渗透率越大,吞吐采收率就越高;超临界CO_(2)-气溶性表面活性剂复合吞吐的最佳实验参数为气溶性表面活性剂GRS⁃1的质量分数0.6%、混合流体注入量0.5 PV、闷井时间3 h、吞吐轮次3次。该复合吞吐技术能够显著提高致密油藏的采收率,对高效开发致密油藏具有指导意义。

“双碳”愿景下CO_(2)驱强化采油封存技术工程选址指标评价

在国家能源安全和“双碳”战略愿景下,CO_(2)驱强化采油封存技术(CO_(2)-EOR)因能助力油气行业转型发展,成为“低碳化”乃至“负碳化”的首选技术和最现实的选择。无论是实验、数值模拟还是现场实践,目前国内外学者对CO_(2)-EOR研究侧重于CO_(2)作为高效的驱油“催化剂”本身及油藏CO_(2)-EOR适应性认识,对于工程选址评价缺乏统一标准和系统研究。在充分调研国内外文献的基础上,结合中国CO_(2)-EOR应用进展和工程实践,明确了CO_(2)-EOR工程选址可行性评价所需的通用依据,指出了CO_(2)-EOR工程选址遵循“CO_(2)封存与驱油双统一”、安全性、经济性的专属性原则,并从CO_(2)-EOR工程选址的地质、工程、安全、经济4个要素开展了较详尽系统的研究,定性-定量构建了“4+8+27”CO_(2)-EOR工程选址三级指标评价体系(GESE),以期为油藏开展CO_(2)-EOR工程选址提供借鉴,助力中国碳减排技术的应用与发展。

低渗砂岩油田CO_(2)驱化学机理及提高采收率研究

针对低渗砂岩油藏进行了CO_(2)驱开发技术研究,分析了CO_(2)驱油化学机理及主要影响因素。基于目标油藏流体特征进行了PVT拟合,确定其CO_(2)驱最小混相压力,明确了不同压力及注入时机对CO_(2)驱采收率、气油比、含水率及驱动压差等的影响规律,探究了CO_(2)泡沫驱在提高采收率方面的效用。结果表明:24.5 MPa为目标区域CO_(2)驱的最小混相压力,采收率会随着压力的升高而增加,28 MPa时CO_(2)驱提高采收率可达30.57%。气体突破时间、总采收率与CO_(2)注入时机密切相关,CO_(2)注入越早,越有利于采收率的提高,出口含水率为60%时注入可提高采收率39.13%。CO_(2)泡沫驱可以在一定程度上起到提高采收率的效用。

页岩油藏注CO_(2)驱孔隙动用特征研究

CO_(2)在页岩油藏驱油时的孔隙动用特征是评价其应用于提高页岩油藏采收率效果的一项重要指标。因此,开展了超临界CO_(2)驱替页岩岩心室内实验,并以核磁共振(NMR)在线岩心扫描技术为手段对CO_(2)驱页岩油藏的孔隙动用特征和规律进行研究。结果表明,超临界CO_(2)非混相驱油主要动用页岩中孔隙半径在0.1~3.0µm范围内的油,而此过程中小于0.008µm孔隙半径内的油量反而增加,分析原因主要是CO_(2)在页岩层中通过压差和扩散作用将大孔隙内页岩油带入小孔隙中并发生吸附滞留,在驱替时间5 h后,CO_(2)驱替页岩油采收率达到35.7%,驱油效果较好。

CuZn/CeO_(2)催化剂在CO_(2)加氢制甲醇中的应用研究

CO_(2)加氢制甲醇反应过程中产生的大量副产物水会加速催化剂中CuZn物种的聚集和烧结,导致催化剂严重失活。而CeO_(2)亲水性较弱,具有较高的水热稳定性,可以增强CuZn物种的分散。因此,通过水热合成法制备了一系列CeO_(2)载体晶面可调控的CuZn基催化剂,并在其中引入了适当浓度的氧空位。采用TEM、XRD和H_(2)-TPR等表征手段研究了合成的CeO_(2)载体及CuZn/CeO_(2)-y催化剂(y为rod、cube或otca)的形貌、结构和还原性能等物理化学性质,并考察了CuZn/CeO_(2)-y催化剂在CO_(2)加氢制甲醇反应中的催化性能。结果表明,暴露(110)晶面的纳米棒结构的CeO_(2)载体(CeO_(2)-rod)更有利于CuZn基物种的分散,并且CeO_(2)-rod与Cu物种形成了Cu—O—Ce界面,增强了催化剂同时吸附和活化CO_(2)和H_(2)的性能。因此,CuZn/CeO_(2)-rod表现出较高的CO_(2)转化率和甲醇选择性,在260℃、3MPa的条件下,甲醇时空收率为433.4g/(kg·h),甲醇选择性高达68.5%。同时,利用原位漫反射傅立叶变换红外光谱对CO_(2)加氢制甲醇的反应路径和重要中间物种的演变进行了详细研究,发现在CuZn/CeO_(2)催化剂的作用下,反应主要遵循甲酸盐路径,载体的晶面效应没有改变反应路径,但是提高了重要中间物种达到平衡的速率。

运移距离对CO_(2)混相驱重力超覆的影响规律及表征分析

CO_(2)驱油技术具有提高原油采收率和资源化利用与封存的双重目的,已在低渗-致密油藏得到广泛应用。为明确运移距离对CO_(2)混相驱油过程中密度差引起的重力超覆程度的影响规律,分别采用室内物理模型和数值模型开展研究。实验结果表明,混相条件下,由于岩心长度减小,重力超覆的扩展空间受限,但油气混相程度的降低,导致重力超覆程度降低幅度较小;当岩心长度继续减小时,混相程度降低对重力超覆的影响大于岩心长度对重力超覆扩展空间限制的影响,从而使重力超覆程度加剧。数模结果表明,随着运移距离的减小,重力超覆程度减弱,混相驱采收率提高。因此,结合油田现场情况,为减缓重力超覆,应适当减小井距,缩短CO_(2)气体运移距离,从而提高CO_(2)驱的波及效率。研究结果对于CO_(2)驱油现场试验方案设计和参数优化具有一定的指导意义。

深部煤层CO_(2)地质封存量化评估及案例研究

地质封存CO_(2)作为理想的减碳技术,有望成为缓解温室效应的重要手段,因此量化评估深部煤层CO_(2)地质封存潜力与研究超临界CO_(2)与深部煤岩之间相互作用成为了“双碳”背景下的研究热点。以焦作矿区九里山煤样为试验研究对象,分析了深部煤层超临界CO_(2)吸附与封存机理,分别开展了35和45℃下煤样的CO_(2)等温吸附试验,解释并校正了CO_(2)吸附等温线高压异常下拐现象,得到了不同温度下煤样的CO_(2)实际吸附量。提出了一种新方法计算CO_(2)地质封存量,能够校正吸附相体积造成的封存量计算误差,并能精确评估不同埋深煤层CO_(2)理论和有效封存量。研究结果表明:①当高压吸附饱和时,煤样表面所有的吸附位被完全占据,此时吸附相体积和密度不再发生改变,吸附量应趋于稳定,但实验室测得的吸附量却在高压饱和阶段随压力增大而减小,这并不符合Langmuir吸附原理,因此必须对实验室测试的吸附等温线进行校正,才能应用于深部煤层CO_(2)封存量评估;②煤中CO_(2)封存量主要由吸附和游离封存量组成,吸附封存量需要采用吸附相密度和Gibbs吸附量进行反算,游离封存量则需要掌握煤中游离相占据的孔隙体积,它只能根据煤中孔隙总体积减去吸附相体积进行计算,因此,吸附相是精确评估吸附和游离封存量的决定性因素;③采用修正的煤层CO_(2)地质封存量化方法,以焦作修武研究区800~2000 m深部煤层为例,得出其单位质量煤中CO_(2)理论封存量为1.52~2.16 mmol/g,CO_(2)有效封存总量为11.19×10^(9)m^(3),换算为封存总质量为21.97 Mt。本研究案例不仅校正了吸附试验数据的物质平衡错误,而且考虑了吸附相占据孔隙空间对游离封存量的影响,这对深部煤层CO_(2)地质封存量精准评估具有重要的应用意义。