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CN111291497A - Improved digital core modeling method - Google Patents

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CN111291497A
CN111291497A CN202010128527.8A CN202010128527A CN111291497A CN 111291497 A CN111291497 A CN 111291497A CN 202010128527 A CN202010128527 A CN 202010128527A CN 111291497 A CN111291497 A CN 111291497A
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particle
digital core
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杨莎莎
傅少君
谢明
权娟娟
习羽
刘恺德
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Xijing University
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Abstract

本发明公开了一种改进的数字岩心建模方法,包含以下步骤:A、获取岩石颗粒特征;B、模拟岩石颗粒;C、沉积、压实、成岩作用模拟;D、构建数字岩心模型。本发明应用EDEM不仅能模拟压实作用中颗粒的平移、变形、转动、重新排列及破碎等变化,还能结合前期沉积作用和后期成岩作用的模拟,使整个岩石的形成过程可视化,并能随时进行颗粒与孔隙变化的监测与分析。保证整个过程法构建数字岩心更加准确。

Figure 202010128527

The invention discloses an improved digital core modeling method, comprising the following steps: A. acquiring rock particle characteristics; B. simulating rock particles; C. simulating deposition, compaction and diagenesis; D. building a digital core model. The application of EDEM in the invention can not only simulate the changes such as the translation, deformation, rotation, rearrangement and fragmentation of particles in the compaction, but also combine the simulation of the early sedimentation and the later diagenesis, so that the entire rock formation process can be visualized and can be used at any time. Monitoring and analysis of particle and pore changes. To ensure that the whole process method to construct digital core is more accurate.

Figure 202010128527

Description

一种改进的数字岩心建模方法An Improved Digital Core Modeling Method

技术领域technical field

本发明涉及岩土技术领域,具体是一种改进的数字岩心建模方法。The invention relates to the field of geotechnical technology, in particular to an improved digital core modeling method.

背景技术Background technique

数字岩心技术是近年兴起的岩心分析的有效方法,在地球科学、岩土工程和环境工程等领域应用广泛,获得了极大的成功。基本原理是基于二维或三维的岩心扫描图像,运用计算机图像处理技术,通过一定的算法完成数字岩心重构。Digital core technology is an effective method for core analysis that has emerged in recent years. It has been widely used in earth science, geotechnical engineering and environmental engineering and has achieved great success. The basic principle is based on two-dimensional or three-dimensional core scanning images, using computer image processing technology, and completing digital core reconstruction through certain algorithms.

岩心是由自然界中的岩石颗粒经过沉积作用、压实作用和成岩作用形成的。而过程法正是通过模拟以上岩石形成过程来构建数字岩心的一种技术。因过程法的约束条件是从岩石薄片或其他途径获得的岩石颗粒信息数据,建模灵活性更强,且因过程法的模拟加入了地质因素,考虑了岩石的形成过程及其各向异性,构建的数字岩心更加精准。得到了国内外学者的广泛关注。Cores are formed from natural rock particles through sedimentation, compaction and diagenesis. The process method is a technology for constructing digital cores by simulating the above rock formation process. Because the constraint condition of the process method is the rock particle information data obtained from rock slices or other methods, the modeling flexibility is stronger, and the simulation of the process method adds geological factors, and considers the formation process and anisotropy of the rock. The constructed digital core is more accurate. It has received extensive attention from scholars at home and abroad.

自然界中岩石的形成包括沉积、压实和成岩三个阶段,过程复杂。尤其是压实作用,发生时,岩石颗粒常受到上方及四周岩石的压力、水流产生的摩擦力、水中静压力以及其他摩擦力作用,造成颗粒平移、变形、转动、重新排列甚至破碎等变化,使得岩石颗粒之间的原始孔隙大幅度减小。例如,致密砂岩中的压实作用会使原始孔隙损失率高达60%左右。因压实作用在岩石成岩过程中是自始至终存在的,其对岩石性质的影响巨大,用过程法模拟数字岩心时,压实作用的准确模拟尤为重要。The formation of rocks in nature includes three stages of deposition, compaction and diagenesis, and the process is complex. Especially when compaction occurs, the rock particles are often subjected to the pressure of the rocks above and around them, the friction force generated by the water flow, the static pressure in the water and other friction forces, resulting in changes such as translation, deformation, rotation, rearrangement and even fragmentation of the particles. The original pores between the rock particles are greatly reduced. For example, compaction in tight sandstones can lead to loss of original porosity as high as about 60%. Because compaction exists throughout the rock diagenesis process, it has a huge impact on rock properties. When using the process method to simulate digital cores, the accurate simulation of compaction is particularly important.

为解决此问题,国内外学者在进行压实作用模拟时设定了假设条件。Bakke和Φren(1997)在模拟压实作用过程中,假设颗粒的几何形状不发生变化,无侧向位移,颗粒不发生转动,颗粒无弹性变形,只通过改变各个颗粒的垂直坐标来实现岩石的压实过程。Zhu(2012)假设颗粒在压实过程中只发生平移,认为颗粒的压实包括垂直(Z轴)和水平(X轴、Y轴)两个方向上的压实,对两个方向上都进行了模拟。屈乐(2014)为了达到压实后颗粒重排和孔隙减小的效果,将所有沉积物颗粒或小球的Z轴坐标减小(向下移动)来实现,在整个过程通过压实因子(一般取[0,1])和颗粒重排因子(一般取[-0.02,0.02])来控制压实程度和颗粒排列状态。In order to solve this problem, scholars at home and abroad have set up assumptions when simulating compaction. In the process of simulating compaction, Bakke and Φren (1997) assumed that the geometry of the particles did not change, there was no lateral displacement, the particles did not rotate, and the particles were inelastically deformed. compaction process. Zhu (2012) assumed that the particles only translate during the compaction process, and considered that the compaction of particles includes compaction in both vertical (Z-axis) and horizontal (X-axis, Y-axis) directions. simulation. Culler (2014) in order to achieve the effect of particle rearrangement and porosity reduction after compaction, the Z-axis coordinate of all sediment particles or spheres is reduced (moved down) to achieve, through the compaction factor ( Generally take [0,1]) and particle rearrangement factor (generally take [-0.02,0.02]) to control the degree of compaction and the state of particle arrangement.

综上所述,前人都是假设颗粒不发生变形、转动及破碎的情况下,通过颗粒的平移来进行压实过程的模拟。为了保证数字岩心的准确性,常常需要改变压实因子和颗粒重排因子进行多次模拟,才能达到满意的效果。此尝试过程缓慢,模拟结果随机性太强,极大地降低了数字岩心建模的效率。To sum up, the predecessors simulated the compaction process through the translation of the particles under the assumption that the particles do not deform, rotate and break. In order to ensure the accuracy of digital cores, it is often necessary to change the compaction factor and particle rearrangement factor for multiple simulations to achieve satisfactory results. This attempt is slow, and the simulation results are too random, which greatly reduces the efficiency of digital core modeling.

发明内容SUMMARY OF THE INVENTION

本发明的目的在于提供一种改进的数字岩心建模方法,以解决上述背景技术中提出的问题。The purpose of the present invention is to provide an improved digital core modeling method to solve the problems raised in the above background art.

为实现上述目的,本发明提供如下技术方案:To achieve the above object, the present invention provides the following technical solutions:

一种改进的数字岩心建模方法,包含以下步骤:An improved approach to digital core modeling comprising the following steps:

A、获取岩石颗粒特征;A. Obtain rock particle characteristics;

B、模拟岩石颗粒;B. Simulated rock particles;

C、沉积、压实、成岩作用模拟;C. Sedimentation, compaction, and diagenesis simulation;

D、构建数字岩心模型。D. Build a digital core model.

作为本发明的进一步技术方案:所述步骤A具体是:获取岩石颗粒特征。选取岩心进行样品制备,利用铸体薄片、粒度分析和CT扫描的方式获取样品中岩石颗粒的大小、形状、组分及分布特征。As a further technical solution of the present invention: the step A is specifically: acquiring rock particle characteristics. The cores were selected for sample preparation, and the size, shape, composition and distribution characteristics of rock particles in the samples were obtained by casting thin sections, particle size analysis and CT scanning.

作为本发明的进一步技术方案:所述步骤B分两步进行:一、用三维软件模拟真实岩石颗粒的形状;二、用Creator将三维软件模拟好的颗粒几何形状导入到EDEM中,并加入颗粒组分及大小信息,完成颗粒模型的建立。As a further technical solution of the present invention: the step B is carried out in two steps: 1. simulating the shape of real rock particles with 3D software; 2. importing the particle geometry simulated by the 3D software into EDEM with Creator, and adding particles Composition and size information, complete the establishment of particle model.

作为本发明的进一步技术方案:所述步骤C的沉积过程中,岩石颗粒会经历下降、滚动,直至达到初始稳定状态后进入压实阶段,颗粒发生平移、变形、转动、重新排列和破碎等变化,再进入成岩阶段,颗粒发生胶结、溶蚀或自生加大作用,导致岩石颗粒形态会进一步发生变化,最终形成目前的岩石。As a further technical solution of the present invention: during the deposition process of the step C, the rock particles will experience falling and rolling, and then enter the compaction stage after reaching the initial stable state, and the particles will undergo changes such as translation, deformation, rotation, rearrangement and fragmentation. , and then enter the diagenetic stage, the particles will undergo cementation, dissolution or autogenous increase, resulting in further changes in the shape of rock particles, and finally the formation of the current rock.

作为本发明的进一步技术方案:所述步骤C用Simulator进行沉积、压实、成岩作用过程中颗粒一系列变化的模拟。As a further technical solution of the present invention: in the step C, a Simulator is used to simulate a series of changes of particles in the process of deposition, compaction and diagenesis.

作为本发明的进一步技术方案:所述步骤D具体是:将一系列岩石形成过程模拟完成之后,用Analyst生成数字岩心模型。As a further technical solution of the present invention: the step D is specifically: after a series of rock formation processes are simulated, use Analyst to generate a digital core model.

作为本发明的进一步技术方案:所述三维软件为CAD。As a further technical solution of the present invention: the three-dimensional software is CAD.

与现有技术相比,本发明的有益效果是:本发明应用EDEM不仅能模拟压实作用中颗粒的平移、变形、转动、重新排列及破碎等变化,还能结合前期沉积作用和后期成岩作用的模拟,使整个岩石的形成过程可视化,并能随时进行颗粒与孔隙变化的监测与分析。保证整个过程法构建数字岩心更加准确。Compared with the prior art, the beneficial effects of the present invention are: the application of EDEM in the present invention can not only simulate changes such as translation, deformation, rotation, rearrangement and fragmentation of particles in the compaction, but also can combine the early sedimentation and the later diagenesis. The simulation of the whole rock can visualize the formation process of the whole rock, and can monitor and analyze the changes of particles and pores at any time. To ensure that the entire process method to construct digital cores is more accurate.

附图说明Description of drawings

图1 是本发明的识别流程图。Fig. 1 is the identification flow chart of the present invention.

具体实施方式Detailed ways

下面将结合本发明实施例中的附图,对本发明实施例中的技术方案进行清楚、完整地描述,显然,所描述的实施例仅仅是本发明一部分实施例,而不是全部的实施例。基于本发明中的实施例,本领域普通技术人员在没有做出创造性劳动前提下所获得的所有其他实施例,都属于本发明保护的范围。The technical solutions in the embodiments of the present invention will be clearly and completely described below with reference to the accompanying drawings in the embodiments of the present invention. Obviously, the described embodiments are only a part of the embodiments of the present invention, but not all of the embodiments. Based on the embodiments of the present invention, all other embodiments obtained by those of ordinary skill in the art without creative efforts shall fall within the protection scope of the present invention.

实施例1:请参阅图1,一种改进的数字岩心建模方法,包含以下步骤:Embodiment 1: Please refer to Figure 1, an improved digital core modeling method, comprising the following steps:

A:获取岩石颗粒特征。选取岩心进行样品制备,利用铸体薄片、粒度分析和CT扫描的方式获取样品中岩石颗粒的大小、形状、组分及分布特征。A: Obtain rock grain characteristics. The cores were selected for sample preparation, and the size, shape, composition and distribution characteristics of rock particles in the samples were obtained by casting thin sections, particle size analysis and CT scanning.

B:模拟岩石颗粒。分两步进行:B: Simulated rock particles. Do it in two steps:

1.用CAD(Computer Aided Design)软件模拟真实岩石颗粒的形状。1. Use CAD (Computer Aided Design) software to simulate the shape of real rock particles.

2.用Creator将CAD模拟好的颗粒几何形状导入到EDEM中,并加入颗粒组分及大小信息,完成颗粒模型的建立。2. Import the particle geometry simulated by CAD into EDEM with Creator, and add particle composition and size information to complete the establishment of the particle model.

C:沉积、压实、成岩作用模拟。沉积过程中,岩石颗粒会经历下降、滚动,直至达到初始稳定状态后进入压实阶段,颗粒发生平移、变形、转动、重新排列和破碎等变化,再进入成岩阶段,颗粒发生胶结、溶蚀或自生加大作用,导致岩石颗粒形态会进一步发生变化,最终形成目前的岩石。用Simulator进行沉积、压实、成岩作用过程中颗粒一系列变化的模拟。C: Sedimentation, compaction, diagenesis simulation. During the deposition process, the rock particles will go through descending and rolling until they reach the initial stable state and then enter the compaction stage, where the particles undergo changes such as translation, deformation, rotation, rearrangement and fragmentation, and then enter the diagenetic stage, where the particles are cemented, dissolved or self-generated. Increase the effect, resulting in further changes in the rock particle morphology, and finally the formation of the current rock. Use Simulator to simulate a series of changes in particles during deposition, compaction, and diagenesis.

D:构建数字岩心模型。将一系列岩石形成过程模拟完成之后,用Analyst生成数字岩心模型。D: Build a digital core model. After simulating a series of rock formation processes, Analyst was used to generate a digital core model.

实施例2:在实施例1的基础上,步骤B中所使用的CAD可以用其他的三维软件所替代。Embodiment 2: On the basis of Embodiment 1, the CAD used in step B can be replaced by other three-dimensional software.

对于本领域技术人员而言,显然本发明不限于上述示范性实施例的细节,而且在不背离本发明的精神或基本特征的情况下,能够以其他的具体形式实现本发明。因此,无论从哪一点来看,均应将实施例看作是示范性的,而且是非限制性的,本发明的范围由所附权利要求而不是上述说明限定,因此旨在将落在权利要求的等同要件的含义和范围内的所有变化囊括在本发明内。不应将权利要求中的任何附图标记视为限制所涉及的权利要求。It will be apparent to those skilled in the art that the present invention is not limited to the details of the above-described exemplary embodiments, but that the present invention may be embodied in other specific forms without departing from the spirit or essential characteristics of the invention. Therefore, the embodiments are to be regarded in all respects as illustrative and not restrictive, and the scope of the invention is to be defined by the appended claims rather than the foregoing description, which are therefore intended to fall within the scope of the claims. All changes within the meaning and range of the equivalents of , are included in the present invention. Any reference signs in the claims shall not be construed as limiting the involved claim.

此外,应当理解,虽然本说明书按照实施方式加以描述,但并非每个实施方式仅包含一个独立的技术方案,说明书的这种叙述方式仅仅是为清楚起见,本领域技术人员应当将说明书作为一个整体,各实施例中的技术方案也可以经适当组合,形成本领域技术人员可以理解的其他实施方式。In addition, it should be understood that although this specification is described in terms of embodiments, not each embodiment only includes an independent technical solution, and this description in the specification is only for the sake of clarity, and those skilled in the art should take the specification as a whole , the technical solutions in each embodiment can also be appropriately combined to form other implementations that can be understood by those skilled in the art.

Claims (7)

1.一种改进的数字岩心建模方法,其特征在于,包含以下步骤:1. an improved digital rock core modeling method, is characterized in that, comprises the following steps: A、获取岩石颗粒特征;A. Obtain rock particle characteristics; B、模拟岩石颗粒;B. Simulated rock particles; C、沉积、压实、成岩作用模拟;C. Sedimentation, compaction, and diagenesis simulation; D、构建数字岩心模型。D. Build a digital core model. 2.根据权利要求1所述的一种改进的数字岩心建模方法,其特征在于,所述步骤A具体是:获取岩石颗粒特征。选取岩心进行样品制备,利用铸体薄片、粒度分析和CT扫描的方式获取样品中岩石颗粒的大小、形状、组分及分布特征。2 . An improved digital core modeling method according to claim 1 , wherein the step A is specifically: acquiring rock particle characteristics. 3 . The cores were selected for sample preparation, and the size, shape, composition and distribution characteristics of rock particles in the samples were obtained by casting thin sections, particle size analysis and CT scanning. 3.根据权利要求1所述的一种改进的数字岩心建模方法,其特征在于,所述步骤B分两步进行:一、用三维软件模拟真实岩石颗粒的形状;二、用Creator将三维软件模拟好的颗粒几何形状导入到EDEM中,并加入颗粒组分及大小信息,完成颗粒模型的建立。3. a kind of improved digital rock core modeling method according to claim 1, is characterized in that, described step B is carried out in two steps: 1, simulate the shape of real rock particles with three-dimensional software; The particle geometry simulated by the software is imported into EDEM, and the particle composition and size information are added to complete the establishment of the particle model. 4.根据权利要求1所述的一种改进的数字岩心建模方法,其特征在于,所述步骤C的沉积过程中,岩石颗粒会经历下降、滚动,直至达到初始稳定状态后进入压实阶段,颗粒发生平移、变形、转动、重新排列和破碎等变化,再进入成岩阶段,颗粒发生胶结、溶蚀或自生加大作用,导致岩石颗粒形态会进一步发生变化,最终形成目前的岩石。4. a kind of improved digital core modeling method according to claim 1, is characterized in that, in the deposition process of described step C, rock particle can experience descending, rolling, enter compaction stage after reaching initial steady state , the grains undergo changes such as translation, deformation, rotation, rearrangement and fragmentation, and then enter the diagenetic stage, the grains undergo cementation, dissolution or autogenous enlargement, resulting in further changes in the shape of rock grains, and finally the formation of the current rock. 5.根据权利要求1所述的一种改进的数字岩心建模方法,其特征在于,所述步骤C用Simulator进行沉积、压实、成岩作用过程中颗粒一系列变化的模拟。5 . An improved digital core modeling method according to claim 1 , wherein in the step C, a Simulator is used to simulate a series of changes in particles during deposition, compaction, and diagenesis. 6 . 6.根据权利要求1所述的一种改进的数字岩心建模方法,其特征在于,所述步骤D具体是:将一系列岩石形成过程模拟完成之后,用Analyst生成数字岩心模型。6. An improved digital core modeling method according to claim 1, wherein the step D is specifically: after a series of rock formation processes are simulated, use Analyst to generate a digital core model. 7.根据权利要求3所述的一种改进的数字岩心建模方法,其特征在于,所述三维软件为CAD。7. An improved digital core modeling method according to claim 3, wherein the three-dimensional software is CAD.
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Publication number Priority date Publication date Assignee Title
CN112146957A (en) * 2020-09-25 2020-12-29 东北石油大学 A method for quantitative production of artificial cores based on digital cores
CN116465798A (en) * 2023-03-29 2023-07-21 晋江市福大科教园区发展中心 Method for measuring surface contact coefficient of hard concrete based on EDEM simulation

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Application publication date: 20200616