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CN110132818B - Method and system for obtaining permeability of sediments containing natural gas hydrate - Google Patents

Method and system for obtaining permeability of sediments containing natural gas hydrate Download PDF

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CN110132818B
CN110132818B CN201910454469.5A CN201910454469A CN110132818B CN 110132818 B CN110132818 B CN 110132818B CN 201910454469 A CN201910454469 A CN 201910454469A CN 110132818 B CN110132818 B CN 110132818B
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王磊
卢海龙
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Abstract

The invention discloses a method and a system for obtaining the permeability of sediments containing natural gas hydrates. The system comprises: a pore network model building module; a pore-filling hydrate model addition module; a permeability conduction equation establishing module; a permeability calculation module; the method can be made by secondary development on the basis of an open source computing tool OpenPNM of a pore network model. The invention can calculate the permeability when the pore network model contains the hydrate and the hydrate does not completely block the pore throat, provides the selection of the positions of various hydrates and solves the problem that the permeability of the deposit containing the hydrate changes along with the change of the saturation of the hydrate.

Description

一种含天然气水合物沉积物渗透率的获取方法及系统A method and system for obtaining permeability of natural gas hydrate-bearing sediments

技术领域technical field

本发明属于水合物储层成藏和开发技术领域,涉及水合物沉积物渗透率的求取方法,具体涉及一种基于孔隙网络模型数值模拟算法获取含天然气水合物沉积物渗透率的方法及系统。The invention belongs to the technical field of accumulation and development of hydrate reservoirs, relates to a method for obtaining the permeability of hydrate sediments, and in particular relates to a method and system for obtaining the permeability of gas hydrate-bearing sediments based on a pore network model numerical simulation algorithm .

背景技术Background technique

天然气水合物是水分子以氢键连接包络小气体分子形成的一类笼形化合物[Sloan E D,Koh C A.Clathrate hydrates of natural gas[M].Third Edition ed.BocaRaton:CRC Press,2007],当气体组分为甲烷为主的天然气时,因其可燃也称“可燃冰”。由于它储量大,是一种很有前景的能源,因此在过去的几十年里,主要的能源消耗国在水合物勘查和开发技术研究上投入巨大[Li J F,Ye J L,Qin X W,et al.The first offshorenatural gas hydrate production test in South China Sea[J].China Geology,2018,1(1):5–16.],开发过程中,水合物沉积物的物理性质,包括渗透率,孔隙度,饱和度,是建立适当生产策略的先决条件[Waite W F,Santamarina J C,Cortes D D,et al.Physicalproperties of hydrate-bearing sediments[J].Reviews of Geophysics,2009,47(4):465–84.]。在上述性质中,含水合物沉积物的渗透性是研究生产过程中水和气体行为的关键参数[Konno Y,Yoneda J,Egawa K,et al.Permeability of sediment cores frommethane hydrate deposit in the eastern nankai trough[J].Marine and PetroleumGeology,2015,66:487–95.]。Natural gas hydrates are a class of clathrate compounds formed by water molecules connected by hydrogen bonds to envelop small gas molecules [Sloan E D, Koh C A. Clathrate hydrates of natural gas[M].Third Edition ed.BocaRaton:CRC Press,2007] , when the gas component is methane-based natural gas, it is also called "flammable ice" because it is flammable. Because of its large reserves, it is a promising energy source, so in the past few decades, major energy consuming countries have invested heavily in hydrate exploration and development technology research [Li J F, Ye J L, Qin X W, et al. al.The first offshorenatural gas hydrate production test in South China Sea[J].China Geology,2018,1(1):5–16.], during development, physical properties of hydrate sediments, including permeability, porosity Degree, saturation, is a prerequisite for establishing an appropriate production strategy [Waite WF, Santamarina J C, Cortes D D, et al.Physical properties of hydrate-bearing sediments[J].Reviews of Geophysics,2009,47(4):465–84 .]. Among the above properties, the permeability of sediment cores from methane hydrate deposits in the eastern nankai trough is a key parameter for studying water and gas behavior during production [Konno Y, Yoneda J, Egawa K, et al. [J]. Marine and Petroleum Geology, 2015, 66: 487–95.].

水合物在沉积物孔隙中形成时占据了孔隙与喉道空间,降低了沉积物的渗透率;水合物分解时,孔隙空间得以释放使沉积物的渗透性增加。因此,含水合物储层的渗透率会随水合物饱和度(沉积物孔隙中水合物体积占沉积物孔隙总体积的比)变化,准确预测含水合物沉积物渗透率变化是水合物成功开发的关键因素。由于开展水合物热力学稳定域条件下的室内实验较为困难,因此数值模拟是水合物产生与分解对沉积物渗透性影响较为可行的研究方法。When hydrates are formed in sediment pores, they occupy the space of pores and throats, reducing the permeability of sediments; when hydrates are decomposed, the pore space is released to increase the permeability of sediments. Therefore, the permeability of hydrate-bearing reservoirs will change with the hydrate saturation (the ratio of the hydrate volume in the sediment pores to the total sediment pore volume). Accurately predicting the permeability change of the hydrate-bearing sediments is the key to the successful development of hydrates. key factor. Since it is difficult to carry out laboratory experiments under the condition of hydrate thermodynamic stability, numerical simulation is a more feasible method to study the effect of hydrate formation and decomposition on sediment permeability.

现有技术中,文献[1](Blunt M J.Flow in porous media–pore-network modelsand multiphase flow[J].Current Opinion in Colloid&Interface Science,2001,6(3):197–207.)记载的孔隙网络模型(Pore Network Model,PNM)是一种成熟的多孔介质多相流渗透性模拟方法,也广泛应用于水合物饱和度与渗透率性质的数值模拟研究中,文献[2](Dai S,Seol Y.Water permeability in hydrate-bearing sediments:A pore-scalestudy[J].Geophysical Research Letters,2014,41(12):4176–84.)、文献[3](Jang J,Santamarina J C.Recoverable gas from hydrate-bearing sediments:Pore networkmodel simulation and macroscale analyses[J].Journal of Geophysical Research:Solid Earth,2011,116(B8))、文献[4](Mahabadi N,Jang J.Relative water and gaspermeability for gas production from hydrate-bearing sediments[J].Geochemistry,Geophysics,Geosystems,2014,15(6):2346–53.)、文献[5](Mahabadi N,Dai S,Seol Y,et al.The water retention curve and relative permeability forgas production from hydrate-bearing sediments:Pore–network model simulation[J].Geochemistry,Geophysics,Geosystems,2016,17(8):3099–110.)均有记载孔隙网络模型的相关应用。目前应用PNM进行水合物饱和度-渗透率关系的数值模拟研究中,均假设水合物一旦形成即完全堵塞该孔隙(孔隙仅存在完全不含水合物与被水合物完全堵死两种状态),通过被堵死的孔隙数量逐渐增多来模拟饱和度增加的状况。然而,水合物在孔隙中生长的实际过程是一个渐进过程(水合物逐渐堵塞孔隙),现有方法在模拟过程中难以体现该渐进过程,难以准确描述水合物在孔隙中的合成和分解。因此,现有技术应用于水合物饱和度与渗透率的数值模拟,准确性较低,难以解决解决含水合物沉积物渗透率随水合物饱和度变化而变化的问题。In the prior art, the pores described in the literature [1] (Blunt M J. Flow in porous media–pore-network models and multiphase flow [J]. Current Opinion in Colloid & Interface Science, 2001, 6(3): 197–207.) The Pore Network Model (PNM) is a mature method for simulating the permeability of multiphase flow in porous media, and it is also widely used in the numerical simulation of hydrate saturation and permeability properties. Seol Y. Water permeability in hydrate-bearing sediments: A pore-scale study [J]. Geophysical Research Letters, 2014, 41(12): 4176–84.), literature [3] (Jang J, Santamarina J C. Recoverable gas from hydrate-bearing sediments:Pore networkmodel simulation and macroscale analyses[J].Journal of Geophysical Research:Solid Earth,2011,116(B8)), literature[4](Mahabadi N,Jang J.Relative water and gaspermeability for gas production from hydrate-bearing sediments[J].Geochemistry,Geophysics,Geosystems,2014,15(6):2346–53.), literature[5](Mahabadi N,Dai S,Seol Y,et al.The water retention curve and Relative permeability forgas production from hydrate-bearing sediments: Pore–network model simulation [J]. Geochemistry, Geophysics, Geosystems, 2016, 17(8): 3099–110.) have documented the related applications of pore network models. At present, in the numerical simulation study of the relationship between hydrate saturation and permeability using PNM, it is assumed that once the hydrate is formed, the pore will be completely blocked (the pores only have two states of being completely free of hydrate and completely blocked by hydrate). The increased saturation is simulated by increasing the number of blocked pores. However, the actual process of hydrate growth in the pores is a gradual process (the hydrate gradually plugs the pores), and the existing methods are difficult to reflect this gradual process in the simulation process, and it is difficult to accurately describe the synthesis and decomposition of hydrates in the pores. Therefore, the existing technology applied to the numerical simulation of hydrate saturation and permeability has low accuracy, and it is difficult to solve the problem that the permeability of hydrate-containing sediments changes with the change of hydrate saturation.

发明内容SUMMARY OF THE INVENTION

为了克服上述现有技术的不足,本发明提供一种含天然气水合物沉积物渗透率的获取方法及系统,通过在孔隙网络模型计算方法中添加孔隙填充型水合物模型,并给出孔隙被水合物充填下的渗透性传导方程,可以计算含天然气水合物的渗透率,用以解决含水合物沉积物渗透率随水合物饱和度变化而变化的问题。In order to overcome the above-mentioned deficiencies of the prior art, the present invention provides a method and system for obtaining the permeability of natural gas hydrate-containing sediments. By adding a pore-filling hydrate model to the calculation method of the pore network model, and giving the hydrated pores of the pores According to the permeability conduction equation under gas filling, the permeability of natural gas hydrates can be calculated to solve the problem that the permeability of hydrate-containing sediments changes with the change of hydrate saturation.

为了便于说明,本文约定:For the convenience of explanation, this article agrees:

水合物饱和度:沉积物孔隙中水合物体积占沉积物孔隙总体积的比,无量纲。Hydrate saturation: the ratio of hydrate volume in sediment pores to the total volume of sediment pores, dimensionless.

水合物:天然气水合物的简称。是水分子以氢键连接包络小气体分子形成的一类笼形化合物,当气体组分为甲烷为主的天然气时,因其可燃也称“可燃冰”。Hydrate: Abbreviation for natural gas hydrate. It is a type of clathrate compound formed by water molecules connecting and enveloping small gas molecules by hydrogen bonds. When the gas component is natural gas mainly composed of methane, it is also called "flammable ice" because of its flammability.

孔隙空间:沉积物中的非固体部分。Pore space: The non-solid portion of a sediment.

孔隙:孔隙空间中较大的独立空间。Pore: The larger independent space in the pore space.

喉道:孔隙空间中连接两个孔隙的细窄部分。Throat: A narrow section of pore space that connects two pores.

节点:孔隙的几何中心点。Node: The geometric center point of the pore.

导管:孔隙相邻两个节点之间的联通部分,包括:左边节点半孔隙、两节点间喉道、右边节点半孔隙。Conduit: the connecting part between two adjacent nodes of a pore, including: a half-pore at the left node, a throat between two nodes, and a half-pore at the right node.

孔隙网络模型法(PNM)计算沉积物渗透率的步骤如下:The steps of calculating sediment permeability by pore network model method (PNM) are as follows:

1、建立孔隙网络几何模型。1. Establish a geometric model of the pore network.

2、计算网络模型中孔隙和喉道的渗透性传导率。2. Calculate the permeability conductivity of pores and throats in the network model.

3、网络模型的所有节点体积守恒。3. The volume of all nodes of the network model is conserved.

4、对进出口压力进行赋值。4. Assign value to import and export pressure.

5、计算每个节点的压力。5. Calculate the pressure at each node.

6、计算入口流量和出口流量。6. Calculate the inlet flow and outlet flow.

7、应用达西(Darcy)定律计算渗透率。7. Apply Darcy's law to calculate permeability.

本发明在孔隙网络模型法基础上,通过在建立孔隙网络几何模型中添加孔隙水合物模型,并给出含水合物情况下孔隙网络模型中孔隙和喉道的渗透性传导率计算方法,从而使孔隙网络模型法适用于含水合物沉积物的渗透率计算。本发明实现过程中,孔隙网络模型法采用孔隙网络模型开源计算工具—OpenPNM作为底层,在其基础上进行二次开发。Based on the pore network model method, the invention adds a pore hydrate model to the pore network geometric model, and provides a calculation method for the permeability and conductivity of the pores and throats in the pore network model under the condition of hydrate, so as to make the Pore network model method is suitable for permeability calculation of hydrate-bearing sediments. In the implementation process of the present invention, the pore network model method adopts the open source calculation tool of pore network model—OpenPNM as the bottom layer, and performs secondary development on the basis.

本发明提供的技术方案如下:The technical scheme provided by the present invention is as follows:

(一)一种含天然气水合物沉积物渗透率的获取方法,在沉积物的孔隙被含天然气水合物充填状态下,通过在已经建立完成的孔隙网络模型的孔喉空间中添加孔隙填充型水合物模型,并建立该状态下的渗透性传导方程,计算获得含天然气水合物孔隙网络模型的渗透率;包括如下步骤:(1) A method for obtaining the permeability of gas hydrate-containing sediments. In the state where the pores of the sediment are filled with gas hydrates, the pore-filling hydration type is added to the pore-throat space of the pore network model that has been established and completed. The gas hydrate-bearing pore network model is obtained by calculating the permeability of the gas hydrate-containing pore network model, and the permeability conduction equation is established in this state. The following steps are included:

A.建立孔隙网络模型,在孔隙网络模型的孔喉空间中添加孔隙填充型水合物模型;A. Establish a pore network model, and add a pore-filled hydrate model to the pore throat space of the pore network model;

建立的孔隙网络模型中的节点代表沉积物中孔隙的中心点;孔隙网络几何模型中的导管代表沉积物中相邻两个孔隙中心点之间的联通部分。导管包括:相邻两个孔隙节点中左节点半孔隙、两节点间喉道、右节点半孔隙。The nodes in the established pore network model represent the center points of pores in the sediment; the conduits in the pore network geometric model represent the connection between two adjacent pore center points in the sediment. The conduit includes: a left node half-pore in two adjacent pore nodes, a throat between the two nodes, and a right node half-pore.

具体实施时,在孔隙网络模型的孔喉空间中添加孔隙填充型水合物模型是在OpenPNM中的几何类中,添加孔隙水合物几何特征表征数组参数,包括:In specific implementation, adding a pore-filled hydrate model to the pore-throat space of the pore network model is to add the pore-hydrate geometric feature representation array parameters in the geometry class in OpenPNM, including:

A1.添加的孔隙水合物几何特征表征数组参数包括:水合物生成在孔隙中心的直径数组hi、水合物生成在孔隙表面厚度数组hp、水合物生成在喉道表面的厚度数组htA1. The added pore hydrate geometric characteristic characterization array parameters include: the diameter array h i of the hydrate generated in the center of the pore, the thickness array h p of the hydrate generated on the pore surface, and the thickness array h t of the hydrate generated on the throat surface;

A2.设孔隙网络模型中的孔隙直径数组为D,喉道长度数组为L,喉道直径数组为T。当水合物生长在孔隙表面时,孔隙直径数组为:D-hp,当水合物生长在喉道表面时,喉道直径记录为数组T-htA2. Set the pore diameter array in the pore network model as D, the throat length array as L, and the throat diameter array as T. When the hydrate grows on the surface of the pore, the pore diameter array is: Dh p , and when the hydrate grows on the throat surface, the throat diameter is recorded as the array Th t .

B.推导含水合物导管渗透性传导方程,计算获得含天然气水合物孔隙网络模型的导管间渗透性;B. Derive the permeability conduction equation of the hydrate-containing conduit, and calculate the inter-conduit permeability of the gas hydrate-containing pore network model;

具体实施时,在OpenPNM中的计算类中,添加孔隙中含有水合物情况下的节点间渗透性计算方法,包括如下操作:In the specific implementation, in the calculation class in OpenPNM, the calculation method of inter-node permeability when the pores contain hydrates is added, including the following operations:

B1.对于生成在孔隙中心的水合物,节点间导管被分为5段(图2b中编号为④~⑧),通过对导管几何形态的简化(如图2中d所示),每段导管形态变为可以简化计算渗透性的形状。其中图中编号⑤~⑦段为圆柱形,④、⑧段为环柱状,环柱状的环形截面的渗透性(渗透率gloop)的计算公式如式1:B1. For the hydrates generated in the center of the pores, the internode conduits are divided into 5 segments (numbered ④~⑧ in Fig. 2b). By simplifying the geometry of the conduits (as shown in Fig. 2d), each conduit The morphology becomes a shape that simplifies the calculation of permeability. Among them, the sections numbered ⑤~⑦ in the figure are cylindrical, and the sections ④ and are ring-shaped.

Figure BDA0002075088030000041
Figure BDA0002075088030000041

式中,D为环形截面外直径(孔隙直径),hi为环形截面内直径(水合物直径),L为本段长度(=0.5hi),μ为孔隙流体黏度。where D is the outer diameter of the annular section (pore diameter), hi is the inner diameter of the annular section (hydrate diameter), L is the length of the section (=0.5h i ) , and μ is the pore fluid viscosity.

圆柱形截面渗透性(gc)计算公式如式2:The formula for calculating the permeability (g c ) of the cylindrical section is as shown in Equation 2:

Figure BDA0002075088030000042
Figure BDA0002075088030000042

整个导管的渗透性(g)根据Hagen-Poiseuille方程,表示为式3:The permeability (g) of the entire conduit is expressed as Equation 3 according to the Hagen-Poiseuille equation:

Figure BDA0002075088030000051
Figure BDA0002075088030000051

其中,gzone1~gzone5表示节点间导管被分成的5段;Among them, g zone1 to g zone5 represent the 5 segments into which the conduit between nodes is divided;

B2.对于生成在孔隙和喉道表面的水合物,节点间导管被分为3段(图2a中的①~③),通过对导管形态进行简化(图2c),3段导管均简化为圆柱状(图2c中的①~③)。圆柱截面渗透性公式已经由公式2给出,仅需将公式2中的直径D替换为:D-hp(图2c中的①、③)和T-ht(图2c中的②)进行计算,得到导管间渗透性;B2. For the hydrates generated on the surface of pores and throats, the inter-node conduits are divided into three sections (①~③ in Figure 2a). By simplifying the shape of the conduits (Figure 2c), the three sections of conduits are all simplified into cylinders shape (①~③ in Fig. 2c). The permeability formula of the cylindrical section has been given by Equation 2. It is only necessary to replace the diameter D in Equation 2 with: Dh p (①, ③ in Fig. 2c) and Th t (② in Fig. 2c) for calculation to obtain the conduit interpenetration;

C.采用孔隙网络模型法计算样品渗透率。C. Calculate the permeability of the sample using the pore network model method.

假设节点间导管中流体流态为层流。喉道中流体渗流流量Qij具有如下形式:It is assumed that the fluid flow in the conduit between nodes is laminar. The fluid seepage flow Qij in the throat has the following form:

Figure BDA0002075088030000052
Figure BDA0002075088030000052

其中,p为流体的压强,rij和lij分别为喉道的半径和长度,μ为流体的粘度系数,gij为喉道倒流率。Among them, p is the pressure of the fluid, rij and lij are the radius and length of the throat, respectively, μ is the viscosity coefficient of the fluid, and gij is the backflow rate of the throat.

假设地层孔隙中的流体不可压缩,则对于单个孔隙,所有与其连通的喉道的流量之和应为零,即:Assuming that the fluid in the formation pores is incompressible, for a single pore, the sum of the flow rates of all the throats connected to it should be zero, namely:

∑Qij=0 (式5)∑Q ij =0 (Equation 5)

由此可以得到以压强为未知数的线性方程组,求解后可得地层孔隙的压强分布。最后计算地层的入口流量和出口流量,运用达西定律求解地层的绝对渗透率。From this, a linear equation system with the pressure as the unknown can be obtained, and the pressure distribution of the formation pores can be obtained after the solution. Finally, the inlet flow and outlet flow of the formation are calculated, and Darcy's law is used to solve the absolute permeability of the formation.

通过上述步骤,计算得到含天然气水合物的渗透率。Through the above steps, the permeability of natural gas hydrate-containing hydrate is calculated.

具体实施时,上述计算过程可执行工具OpenPNM自带的计算方法,即可得到含天然气水合物的渗透率。In specific implementation, the above calculation process can execute the calculation method provided by the tool OpenPNM, and then the permeability of natural gas hydrates can be obtained.

(二)一种含天然气水合物沉积物渗透率的获取装置,包括存储器和处理器;所述存储器,用于存储计算机程序;所述处理器,用于当执行所述计算机程序时,实现上述含天然气水合物沉积物渗透率的获取方法。(2) A device for obtaining the permeability of natural gas hydrate-containing sediments, comprising a memory and a processor; the memory is used to store a computer program; the processor is used to implement the above-mentioned computer program when executing the computer program Methods for obtaining permeability of gas hydrate-bearing sediments.

(三)一种计算机可读存储介质,所述存储介质上存储有计算机程序,当所述计算机程序被处理器执行时,实现上述含天然气水合物沉积物渗透率的获取方法。(3) A computer-readable storage medium, where a computer program is stored on the storage medium, and when the computer program is executed by a processor, the above-mentioned method for obtaining the permeability of a gas hydrate-containing sediment is realized.

(四)一种含天然气水合物沉积物渗透率的获取系统,其特征是,所述系统在孔隙网络模型开源计算工具OpenPNM的基础上进行二次开发而成;包括如下模块:(4) A system for acquiring the permeability of natural gas hydrate-bearing sediments, characterized in that the system is developed on the basis of the open source computing tool OpenPNM for pore network model; it includes the following modules:

孔隙网络模型建立模块,用于建立沉积物的孔隙网络模型;The pore network model building module is used to establish the pore network model of sediments;

孔隙填充型水合物模型添加模块,用于在孔隙网络模型的孔喉空间中添加孔隙填充型水合物模型;Pore-filled hydrate model add-on module, used to add a pore-filled hydrate model to the pore throat space of the pore network model;

渗透性传导方程建立模块,所述渗透性包括环柱状的环形截面的渗透性和圆柱形截面渗透性;a permeability conduction equation establishment module, the permeability includes the permeability of the annular columnar annular section and the permeability of the cylindrical section;

含天然气水合物孔隙网络模型的渗透率计算模块,用于利用孔隙中含有水合物情况下的节点间渗透性计算方法计算得到含天然气水合物孔隙网络模型的渗透率。The permeability calculation module of the gas hydrate-containing pore network model is used to calculate the permeability of the gas hydrate-containing pore network model by using the inter-node permeability calculation method when the pores contain hydrate.

本发明的有益效果:Beneficial effects of the present invention:

本发明提供一种含天然气水合物沉积物渗透率的获取方法,通过在孔隙网络模型计算方法中添加孔隙填充型水合物模型,并给出此状态下的渗透性传导方程,可以计算含天然气水合物的渗透率。本发明首次采用改进孔隙网络模型和简化公式来实现含水合物渗透率连续模拟。利用本发明提供的解决方案,可以计算孔隙网络模型中含有水合物且水合物并没有完全堵塞孔喉时的渗透率,并提供了多种水合物存在位置的选择,解决含水合物沉积物渗透率随水合物饱和度变化而变化的问题。The invention provides a method for obtaining the permeability of natural gas hydrate-containing sediments. By adding a pore-filled hydrate model to the calculation method of the pore network model, and giving the permeability conduction equation in this state, the natural gas hydrate can be calculated. permeability of the substance. The present invention adopts the improved pore network model and simplified formula for the first time to realize the continuous simulation of hydrate permeability. Using the solution provided by the present invention, the permeability of the pore network model containing hydrate and the hydrate does not completely block the pore throat can be calculated, and a variety of hydrate location options are provided to solve the problem of hydrate-containing sediment permeation. rate changes with hydrate saturation.

附图说明Description of drawings

图1是本发明在OpenPNM中的几何类中添加自定义的水合物几何参数;包括:水合物生成在孔隙中心的直径数组hi;hp为水合物生成在孔隙表面厚度数组;ht为水合物生成在喉道表面的厚度数组。Figure 1 shows the custom hydrate geometric parameters added to the geometry class in OpenPNM by the present invention; including: the diameter array hi of the hydrate generated in the center of the pore; hp is the thickness array of the hydrate generated on the pore surface; ht is the hydrate generated Array of thicknesses on the throat surface.

图2是本发明建立的节点间导管计算模型;Fig. 2 is the calculation model of the conduit between nodes established by the present invention;

其中,(a)为水合物生长在孔隙表面时的节点间导管模型;(b)为水合物生长在孔隙中心时的节点间导管模型;(c)水合物生长在孔隙表面时的节点间导管渗透性简化计算模型;(d)水合物生长在孔隙中心时的节点间导管渗透性计算模型;①~③分别表示水合物生长在孔隙表面时导管3分段中的左节点半孔隙段、节点间喉道段、右节点半孔隙段,④~⑧分别表示水合物生长在孔隙中心时的节点间导管5分段中的左节点环柱形段、左节点圆柱形段、节点间喉道段、右节点圆柱形段、右节点环柱形段。Among them, (a) is the inter-node conduit model when the hydrate grows on the pore surface; (b) is the inter-node conduit model when the hydrate grows in the center of the pore; (c) The inter-node conduit model when the hydrate grows on the pore surface Simplified calculation model of permeability; (d) Calculation model of conduit permeability between nodes when hydrate grows in the center of the pore; ①~③ represent the left node semi-porous section and node of conduit 3 segment when hydrate grows on the pore surface, respectively The inter-nodal throat segment and the right-node semi-porous segment, ④~⑧ respectively represent the left-nodal ring cylindrical segment, left-nodal cylindrical segment, and inter-nodal throat segment in the 5 segment of the inter-nodal conduit when the hydrate grows in the center of the pore , right node cylindrical segment, right node ring cylindrical segment.

图3是本发明方法的实施流程框图。FIG. 3 is a flow chart of the implementation of the method of the present invention.

具体实施方式Detailed ways

下面结合附图,通过实施例进一步描述本发明,但不以任何方式限制本发明的范围。Below in conjunction with the accompanying drawings, the present invention is further described by means of embodiments, but the scope of the present invention is not limited in any way.

本发明提供一种含天然气水合物沉积物渗透率的获取方法及系统,通过在孔隙网络模型计算方法中添加孔隙填充型水合物模型,并给出此状态下的渗透性传导方程,可以计算含天然气水合物的渗透率。The invention provides a method and system for obtaining the permeability of natural gas hydrate-containing sediments. By adding a pore-filled hydrate model to the calculation method of the pore network model, and giving the permeability conduction equation in this state, the calculation method of Permeability of natural gas hydrates.

图2是本发明建立的节点间导管计算模型;其中,(a)为水合物生长在孔隙表面时的节点间导管模型;(b)为水合物生长在孔隙中心时的节点间导管模型;(c)水合物生长在孔隙表面时的节点间导管渗透性简化计算模型;(d)水合物生长在孔隙中心时的节点间导管渗透性计算模型;①~③分别表示水合物生长在孔隙表面时导管3分段中的左节点半孔隙段、节点间喉道段、右节点半孔隙段,④~⑧分别表示水合物生长在孔隙中心时的节点间导管5分段中的左节点环柱形段、左节点圆柱形段、节点间喉道段、右节点圆柱形段、右节点环柱形段。Fig. 2 is the calculation model of the conduit between nodes established by the present invention; wherein, (a) is the conduit model between nodes when hydrates grow on the surface of pores; (b) is conduit model between nodes when hydrates grow in the center of pores; ( c) Simplified calculation model of inter-node conduit permeability when hydrates grow on the pore surface; (d) Calculation model of inter-node conduit permeability when hydrates grow in the center of pores; ①~③ represent when hydrates grow on the pore surface, respectively The left-node semi-porous section, the inter-node throat section, and the right-node semi-porous section in the conduit 3 segment, ④~⑧ respectively represent the left nodal ring column in the inter-node conduit 5 segment when the hydrate grows in the center of the pore. Segment, Left Node Cylindrical Segment, Internode Throat Segment, Right Node Cylindrical Segment, Right Node Ring Cylindrical Segment.

图3所示是本发明方法的实施流程,包括如下步骤:Figure 3 shows the implementation flow of the method of the present invention, comprising the following steps:

A.在孔隙网络模型开源计算工具—OpenPNM中的几何类中,添加孔隙水合物几何特征表征数组,包括:A. In the geometry class in OpenPNM, an open source computing tool for pore network models, add a pore hydrate geometric feature representation array, including:

A1.添加水合物生成在孔隙中心的直径数组hi,添加水合物生成在孔隙表面厚度数组hp,添加水合物生成在喉道表面的厚度数组htA1. The diameter array hi generated by adding hydrate in the center of the pore, the thickness array h p generated by adding hydrate on the pore surface , and the thickness array h t generated by adding hydrate on the throat surface;

A2.设孔隙网络模型中的孔隙直径数组为D,喉道长度数组为L,喉道直径数组为T。当水合物生长在孔隙表面时,孔隙直径数组为:D-hp,当水合物生长在喉道表面时,喉道直径记录为数组T-htA2. Set the pore diameter array in the pore network model as D, the throat length array as L, and the throat diameter array as T. When the hydrate grows on the surface of the pore, the pore diameter array is: Dh p , and when the hydrate grows on the throat surface, the throat diameter is recorded as the array Th t .

B.在孔隙网络模型开源计算工具—OpenPNM中的计算类中,添加孔隙中含有水合物情况下的节点间渗透性计算方法:B. In the calculation class in OpenPNM, an open source calculation tool for the pore network model, the calculation method of inter-node permeability when the pores contain hydrates is added:

B1.对于生成在孔隙中心的水合物,节点间导管被分为5段(见附图2),B1. For hydrates generated in the center of pores, the internode conduit is divided into 5 segments (see Figure 2),

如图2中b所示,其中图中编号⑤~⑦段为圆柱形,④、⑧段为环柱状,环柱状的环形截面的渗透性(渗透率,gloop)的计算公式:As shown in b in Figure 2, the sections numbered ⑤ to ⑦ in the figure are cylindrical, and the sections ④ and ⑧ are annular columns. The formula for calculating the permeability (permeability, g loop ) of the annular section of the annular column is:

Figure BDA0002075088030000081
Figure BDA0002075088030000081

式中,D为环形截面外直径,d为环形截面内直径,L为本段长度,μ为孔隙流体黏度。where D is the outer diameter of the annular section, d is the inner diameter of the annular section, L is the length of the section, and μ is the pore fluid viscosity.

圆柱形截面渗透性(gc)计算公式如式2:The formula for calculating the permeability (g c ) of the cylindrical section is as shown in Equation 2:

Figure BDA0002075088030000082
Figure BDA0002075088030000082

整个导管的渗透性(g)根据Hagen-Poiseuille方程,表示为式3:The permeability (g) of the entire conduit is expressed as Equation 3 according to the Hagen-Poiseuille equation:

Figure BDA0002075088030000083
Figure BDA0002075088030000083

B2.对于生成在孔隙和喉道表面的水合物,导管间渗透性计算公式将孔隙直径和喉道直径替换为D-hp和T-ht,按照工具OpenPNM自带计算方法执行。主要计算方法为;B2. For the hydrates generated on the surface of pores and throats, replace the pore diameter and throat diameter with Dh p and Th t in the calculation formula of inter-conduit permeability, and execute according to the calculation method of the tool OpenPNM. The main calculation method is;

假设节点间导管中流体流态为层流。喉道中流体渗流流量Qij具有如下形式:It is assumed that the fluid flow in the conduit between nodes is laminar. The fluid seepage flow Qij in the throat has the following form:

Figure BDA0002075088030000084
Figure BDA0002075088030000084

其中,p为流体的压强,rij和lij分别为喉道的半径和长度,μ为流体的粘度系数,gij为喉道倒流率。Among them, p is the pressure of the fluid, rij and lij are the radius and length of the throat, respectively, μ is the viscosity coefficient of the fluid, and gij is the backflow rate of the throat.

假设地层孔隙中的流体不可压缩,则对于单个孔隙,所有与其连通的喉道的流量之和应为零,即:Assuming that the fluid in the formation pores is incompressible, for a single pore, the sum of the flow rates of all the throats connected to it should be zero, namely:

∑Qij=0 (式5)∑Q ij =0 (Equation 5)

由此可以得到以压强为未知数的线性方程组,求解后可得地层孔隙的压强分布。最后计算地层的入口流量和出口流量,运用达西定律求解地层的绝对渗透率。通过上述步骤,计算得到含天然气水合物的渗透率。From this, a linear equation system with the pressure as the unknown can be obtained, and the pressure distribution of the formation pores can be obtained after the solution. Finally, the inlet flow and outlet flow of the formation are calculated, and Darcy's law is used to solve the absolute permeability of the formation. Through the above steps, the permeability of natural gas hydrate-containing hydrate is calculated.

以下实施例以生成一个笛卡尔坐标下三方向数量为100×100×100规模的立方体网架的孔隙网络为例具体叙述本发明方法的实施。设定孔隙节点间隔为0.63mm,孔隙直径(D)分布为正态分布,分布中值为0.42mm,标准差为0.1mm,通过随机算法生成所有1000000孔隙的直径。喉道直径取相邻较小孔隙直径的0.7倍。以上孔隙网络模型的几何特征以字典的形式记录。The following embodiment specifically describes the implementation of the method of the present invention by taking the generation of a pore network of a cubic grid with a scale of 100×100×100 in three directions under Cartesian coordinates as an example. The pore node interval is set to 0.63mm, the pore diameter (D) distribution is normal distribution, the distribution median is 0.42mm, and the standard deviation is 0.1mm, and the diameters of all 1,000,000 pores are generated by a random algorithm. The throat diameter is 0.7 times the diameter of the adjacent smaller pores. The geometric features of the above pore network model are recorded in the form of a dictionary.

输入水合物模型,这里假设水合物生成在孔隙中心位置,设定水合物生长步数为10步,则每步里水合物直径为[0.1,0.2,0.3,0.4,0.5,0.6,0.7,0.8,0.9]×D(孔隙直径)。Enter the hydrate model, here it is assumed that the hydrate is generated at the center of the pore, and the number of hydrate growth steps is set to 10 steps, then the hydrate diameter in each step is [0.1, 0.2, 0.3, 0.4, 0.5, 0.6, 0.7, 0.8 ,0.9]×D (pore diameter).

计算含水合物的孔隙网络模型的渗透率。利用OpenPNM计算渗透率时调用步骤B中的节点间导管渗透性计算模型。将[0.1,0.2,0.3,0.4,0.5,0.6,0.7,0.8,0.9]×D(孔隙直径)作为水合物直径依次代入计算中,获得不同水合物尺寸下的渗透率,然后可通过以下公式获得水合物饱和度ShCalculate the permeability of the hydrate-containing pore network model. When using OpenPNM to calculate the permeability, call the inter-node conduit permeability calculation model in step B. Substitute [0.1, 0.2, 0.3, 0.4, 0.5, 0.6, 0.7, 0.8, 0.9] × D (pore diameter) as the hydrate diameter into the calculation in turn to obtain the permeability under different hydrate sizes, and then the following formula Obtain the hydrate saturation Sh :

Figure BDA0002075088030000091
Figure BDA0002075088030000091

式中,∑Vhydrate为所有水合物的体积之和,∑Vpore为所有孔隙空间的体积和。In the formula, ΣV hydrate is the volume sum of all hydrates, and ΣV pore is the volume sum of all pore spaces.

需要注意的是,公布实施例的目的在于帮助进一步理解本发明,但是本领域的技术人员可以理解:在不脱离本发明及所附权利要求的精神和范围内,各种替换和修改都是可能的。因此,本发明不应局限于实施例所公开的内容,本发明要求保护的范围以权利要求书界定的范围为准。It should be noted that the purpose of publishing the embodiments is to help further understanding of the present invention, but those skilled in the art can understand that various replacements and modifications are possible without departing from the spirit and scope of the present invention and the appended claims of. Therefore, the present invention should not be limited to the contents disclosed in the embodiments, and the scope of protection of the present invention shall be subject to the scope defined by the claims.

Claims (4)

1. A method for obtaining the permeability of the sediments containing the natural gas hydrate comprises the steps of establishing a pore network model under the condition that the pores of the sediments are filled with the natural gas hydrate, adding a pore filling type hydrate model into the pore throat space of the pore network model, establishing a permeability conduction equation under the condition, and calculating to obtain the permeability of the pore network model containing the natural gas hydrate;
the method comprises the following steps:
A. establishing a pore network model, and adding a pore filling type hydrate model into a pore throat space of the pore network model; the method comprises the following steps:
A1. the nodes in the established pore network model represent the central points of pores in the sediment; the conduit in the pore network model represents a communication part between the central points of two adjacent pores in the sediment; the catheter comprises: a left node half-pore, a throat between two nodes and a right node half-pore in two adjacent pore nodes;
A2. adding a pore filling type hydrate model in a pore throat space of the pore network model, namely adding geometric characteristic characterization array parameters of the pore hydrate into a geometric class of the model;
A21. the geometric characteristic characterization array parameters of the added pore hydrate comprise: diameter array h of hydrate generated in pore centeriThe thickness array h of the hydrate generated on the surface of the porepThickness array h of hydrate generated on surface of throatt
A22. Setting the pore diameter array in the pore network model as D, the throat length array as L and the throat diameter array as T, and when hydrate grows on the pore surface, setting the pore diameter array as D-hp(ii) a When the hydrate grows on the surface of the throat, the diameter of the throat is recorded as an array T-ht
B. Establishing a permeability conduction equation, and calculating the permeability of a pore network model containing the natural gas hydrate by adopting a calculation method of the permeability between nodes under the condition that the pores contain the hydrate; the following operations are performed:
B1. for the hydrate generated in the center of the pore, dividing the conduit between the nodes into 5 sections, including a cylindrical shape and an annular column shape;
by permeability gloopThe permeability of a ring-shaped section having a ring-column shape is represented and calculated by formula 1:
Figure FDA0002457749310000011
in the formula 1, D is the outer diameter of the annular section, namely the diameter of a pore; h isiThe inner diameter of the annular section is the diameter of the hydrate, L is the length of the section, mu is the viscosity of the pore fluid;
by permeability gcRepresents the cylindrical section permeability, calculated by equation 2:
Figure FDA0002457749310000012
the permeability g of the internodal catheter is expressed as formula 3:
Figure FDA0002457749310000013
wherein, gzone1~gzone55 segments into which the inter-node conduit is divided;
B2. for the hydrate generated on the surfaces of the pore and the throat, the diameter of the pore and the diameter of the throat are respectively taken as D-hpAnd T-htThen calculating to obtain the permeability between the catheters;
assuming that the fluid flow state in the conduit between the nodes is laminar flow; the fluid seepage flow Qij in the throat is expressed by equation 4:
Figure FDA0002457749310000021
wherein p is the pressure of the fluid; rij and lij are the radius and length of the throat, respectively; μ is the viscosity coefficient of the fluid; gij is the throat inverse flow rate;
assuming that the fluid in the formation pores is incompressible, for a single pore, the sum of the flow rates of all throats communicating with it should be zero, expressed as equation 5:
∑Qijeither case 0 (formula 5)
Thereby obtaining a linear equation system with the pressure as an unknown number; solving to obtain the pressure distribution of the formation pores;
calculating the inlet flow and the outlet flow of the stratum, and solving the absolute permeability of the stratum by applying Darcy's law;
and obtaining the permeability of the sediments containing the natural gas hydrate through the steps.
2. The device for acquiring the permeability of the sediments containing the natural gas hydrate comprises a memory and a processor;
the memory for storing a computer program;
the processor, when executing the computer program, is configured to implement the method for obtaining permeability of a gas hydrate-containing deposit according to claim 1.
3. A computer-readable storage medium, characterized in that the storage medium has stored thereon a computer program which, when being executed by a processor, carries out the method for obtaining natural gas hydrate-containing deposit permeability according to claim 1.
4. The system is characterized in that the system is developed for the second time on the basis of a pore network model open source computing tool OpenPNM; the system comprises the following modules:
the pore network model establishing module is used for establishing a pore network model of the sediment;
the pore filling type hydrate model adding module is used for adding a pore filling type hydrate model in the pore throat space of the pore network model;
a permeability conduction equation establishing module, wherein the permeability comprises the permeability of an annular section of an annular column shape and the permeability of a cylindrical section;
and the permeability calculation module is used for calculating the permeability of the natural gas hydrate-containing pore network model by using a calculation method for the permeability between nodes under the condition that the pores contain hydrates.
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CN112151125B (en) * 2020-09-24 2022-04-19 中国石油大学(华东) A classification method of hydrate occurrence form based on pore network model
CN112304988B (en) * 2020-10-29 2022-02-01 中国石油大学(北京) Method, device and equipment for determining occurrence state of natural gas hydrate
CN112816386B (en) * 2020-12-31 2023-08-18 中国石油大学(华东) Method for measuring permeability of hydrate reservoir in hydrate phase change process
CN115760787B (en) * 2022-11-22 2025-08-26 北京工业大学 A method for characterizing the pore structure of hydrate sediments, an electronic processing module, and a storage medium

Citations (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN109632579A (en) * 2018-12-29 2019-04-16 西南石油大学 A kind of shale clay mineral is forced from pipette prediction technique

Family Cites Families (8)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
US6289725B1 (en) * 1998-04-30 2001-09-18 Bechtel Bwxt Idaho, Llc Field matric potential sensor
CN101846605B (en) * 2010-03-19 2012-07-25 中国科学院武汉岩土力学研究所 Device for testing compressibility of soil containing natural gas hydrate and testing method thereof
CN105547964A (en) * 2016-01-15 2016-05-04 中国石油大学(华东) One-way flowing determination method for air-water relative permeability under state of different hydrate saturations
CN106780744B (en) * 2016-12-27 2020-04-10 中国石油天然气集团公司 Method for constructing multi-scale three-dimensional digital core by utilizing CT images with different resolutions
KR101930068B1 (en) * 2017-04-03 2018-12-17 한국기계연구원 Membrane Filter for Detecting Target Particle, Method for Manufacturing the Same, and Method for Detecting Target Particle Using the Same
CN107991212B (en) * 2017-10-26 2020-06-16 青岛海洋地质研究所 Fractal dimension measuring and calculating method for effective pores of hydrate-containing sediments
CN108729908B (en) * 2018-05-21 2021-11-09 中国石油大学(华东) Dense oil flow simulation and permeability prediction method based on pore network model
CN109557253B (en) * 2018-11-02 2019-07-23 广州海洋地质调查局 A comprehensive hydrate simulation system and its experimental method

Patent Citations (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN109632579A (en) * 2018-12-29 2019-04-16 西南石油大学 A kind of shale clay mineral is forced from pipette prediction technique

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