CN105004746B - A visual evaluation method for the plugging performance of gel in rock microchannels - Google Patents
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Abstract
本发明涉及一种凝胶在岩石微通道中的封堵性的可视化评价方法,属于石油工程提高采收率技术和实验流体力学领域。本发明采用低场核磁共振成像技术研究凝胶在微孔道中分布,可通过核磁共振成像技术和T2谱分析技术,直接观察岩心驱替实验中凝胶在多孔介质微孔道内的分布。然后根据核磁共振图像提取凝胶图像,获得凝胶面积、凝胶前缘、凝胶后缘和凝胶中心等参数。最后通过对凝胶封堵面积比和封堵高度比的计算,定量表征凝胶在岩心中的封堵性。本发明方法使凝胶在多孔介质中的封堵特征得到比较直观的描述。
The invention relates to a visual evaluation method for the plugging performance of gel in rock microchannels, and belongs to the fields of petroleum engineering enhanced oil recovery technology and experimental fluid mechanics. The invention adopts the low-field nuclear magnetic resonance imaging technology to study the distribution of the gel in the micropore, and can directly observe the distribution of the gel in the porous medium microchannel in the core displacement experiment through the nuclear magnetic resonance imaging technology and the T2 spectrum analysis technology. Gel images were then extracted from the MRI images to obtain parameters such as gel area, gel leading edge, gel trailing edge, and gel center. Finally, through the calculation of the gel plugging area ratio and plugging height ratio, the plugging performance of the gel in the core is quantitatively characterized. The method of the invention enables the plugging characteristics of the gel in the porous medium to be described intuitively.
Description
技术领域technical field
本发明涉及一种凝胶在岩石微通道中的封堵性的可视化评价方法,属于石油工程提高采收率技术和实验流体力学领域。The invention relates to a visual evaluation method for the plugging performance of gel in rock microchannels, and belongs to the fields of petroleum engineering enhanced oil recovery technology and experimental fluid mechanics.
背景技术Background technique
实验室内岩心驱替实验是一种公认的研究岩心内部流体流动的方法,被广泛应用于石油开发及环境科学等领域,但由于岩心具有不可视特征,流体在岩心内的流动只能用压力和流量两个指标来间接表达,或是根据压力——流量关系,利用数值模拟方法进行间接表征。低场核磁共振是一项近年来发展迅速的高新技术,已经在医疗以及食品行业有了很好的应用。如何使实验室内岩心驱替过程更加直接甚至可视,成为石油工程技术领域努力追求的目标和开展的重要工作。在石油工程中常常采用注入凝胶封堵多孔介质中的大孔道,调节注入液体的流动通道,提高波及面积和驱油效率。但是目前传统的岩心流动实验通常只能用端部或者边界的宏观参数(例如出口压力、入口压力、流速等)来描述或者推演流体在岩心内部的流动状况以及驱替效果。岩心对于研究者来说就相当于一个黑匣子,无法准确了解其内部的流体运动情况。The core displacement experiment in the laboratory is a recognized method for studying the fluid flow inside the core, and is widely used in petroleum development and environmental science. However, due to the invisible characteristics of the core, the fluid flow in the core can only be controlled by pressure It can be expressed indirectly by the two indexes of flow rate and pressure, or it can be represented indirectly by numerical simulation method according to the relationship between pressure and flow rate. Low-field nuclear magnetic resonance is a high-tech that has developed rapidly in recent years, and has been well applied in the medical and food industries. How to make the core displacement process in the laboratory more direct and even visible has become a goal pursued and an important work carried out in the field of petroleum engineering technology. In petroleum engineering, gel injection is often used to block the large pores in porous media, adjust the flow channel of the injected liquid, and improve the swept area and oil displacement efficiency. However, the current traditional core flow experiments can only use the macroscopic parameters of the end or boundary (such as outlet pressure, inlet pressure, flow velocity, etc.) to describe or deduce the flow status and displacement effect of the fluid inside the core. For researchers, the rock core is equivalent to a black box, and it is impossible to accurately understand the fluid movement inside it.
发明内容Contents of the invention
针对目前凝胶在岩心中的封堵性很难表征的难题,本发明的目的是提供一种凝胶在岩石微通道中的封堵性的可视化评价方法,将岩心流动实验和核磁共振检测技术有机结合起来,使凝胶在多孔介质中的封堵特征得到比较直观的描述。Aiming at the current problem that the plugging performance of gel in rock core is difficult to characterize, the purpose of this invention is to provide a visual evaluation method for the plugging performance of gel in rock microchannels, which combines core flow experiment and nuclear magnetic resonance detection technology. Combined organically, the plugging characteristics of gels in porous media can be described intuitively.
为达到上述目的,本发明采用如下技术方案:To achieve the above object, the present invention adopts the following technical solutions:
一种凝胶在岩石微通道中的封堵性的可视化评价方法,包括如下步骤:A method for visually evaluating the plugging properties of gel in rock microchannels, comprising the steps of:
(1)开启核磁共振设备,将饱和水的岩心放入磁体后,通过核磁成像确定岩心位置,使其处于磁场中心;对岩心矢状面和横截面的切片厚度、切片间隔和切片位置进行设置,利用低场核磁共振设备获得岩心驱替实验中岩石微通道内流体信号。(1) Turn on the nuclear magnetic resonance equipment, put the water-saturated core into the magnet, and determine the position of the core through nuclear magnetic imaging, so that it is in the center of the magnetic field; set the slice thickness, slice interval and slice position of the sagittal plane and cross section of the core , using low-field nuclear magnetic resonance equipment to obtain fluid signals in rock microchannels in core displacement experiments.
(2)灰度图像提取。灰度图像通过亮暗表征岩心内部不同位置处信号强弱(信号越强越亮,信号越弱越暗)。(2) Grayscale image extraction. The grayscale image represents the strength of the signal at different positions inside the core through light and dark (the stronger the signal, the brighter, and the weaker the signal, the darker).
(3)感兴趣区域(ROI)提取。核磁图像采集信号视窗为100mm×100mm的视窗,岩心矢状面为90mm×25mm的矩形,横截面为直径25mm的圆,所以需要提取灰度图像的有效区域。(3) Region of interest (ROI) extraction. The NMR image acquisition signal window is 100mm×100mm, the sagittal plane of the core is a rectangle of 90mm×25mm, and the cross section is a circle with a diameter of 25mm, so it is necessary to extract the effective area of the grayscale image.
(4)统一映射。每张核磁共振灰度图像按照自身信号强弱显示亮暗,为比较不同图片中的信号强弱,必须把同一切片的核磁共振图片按照统一标准进行亮暗显示。(4) Unified mapping. Each NMR grayscale image is displayed bright and dark according to its own signal strength. In order to compare the signal strength in different images, the MRI images of the same slice must be displayed bright and dark according to a uniform standard.
(5)提取岩心骨架。为确定岩心的骨架结构,对饱和岩心的核磁图像进行二值化处理,分离岩心骨架和流体信息。(5) Extract the core skeleton. In order to determine the skeleton structure of the core, binarize the nuclear magnetic image of the saturated core to separate the skeleton and fluid information of the core.
(6)添加伪彩。对灰度统一后的岩心,添加JET伪彩,使凝胶和水的区分更加明显。(6) Add pseudo-color. For the core with unified gray scale, add JET pseudo-color to make the distinction between gel and water more obvious.
(7)提取凝胶图像。根据核磁共振图像提取凝胶图像,获得凝胶面积、凝胶前缘、凝胶后缘和凝胶中心等参数。(7) Extract the gel image. Gel images were extracted from the NMR images to obtain parameters such as gel area, gel leading edge, gel trailing edge, and gel center.
(8)凝胶封堵高度比表征:驱替一定孔隙体积的水,水驱后凝胶在纵向上封堵高度与候凝后凝胶在纵向上封堵高度的比值作为凝胶封堵高度比,首先计算每一个矢状面的封堵高度比,然后取平均值记为整个岩心中凝胶的封堵高度比:(8) Characterization of gel plugging height ratio: Displacing water with a certain pore volume, the ratio of the vertical plugging height of the gel after water flooding to the vertical plugging height of the gel after waiting to solidify is taken as the gel plugging height ratio, first calculate the plugging height ratio of each sagittal plane, and then take the average value and record it as the plugging height ratio of the gel in the whole core:
式中:r1为岩心的截面高度,mm;r2为凝胶封堵高度,mm;F1为封堵高度比,无量纲。In the formula: r 1 is the section height of the core, mm; r 2 is the gel plugging height, mm; F 1 is the plugging height ratio, dimensionless.
(9)凝胶封堵面积比表征:在步骤(8)中,同时将水驱后凝胶在横向上凝胶面积与孔隙总面积的比作为凝胶封堵面积比;首先计算每一个横断面的封堵面积比,然后取平均值记为整个岩心中凝胶的封堵面积比:(9) Characterization of gel plugging area ratio: In step (8), at the same time, the ratio of the gel area to the total pore area of the gel in the lateral direction after water flooding is used as the gel plugging area ratio; Then take the average value and record it as the plugging area ratio of the gel in the whole core:
式中:S1为岩心的截面面积,mm2;S2为凝胶封堵面积,mm2;F2为封堵面积比,无量纲。In the formula: S 1 is the cross-sectional area of the core, mm 2 ; S 2 is the plugging area of the gel, mm 2 ; F 2 is the plugging area ratio, dimensionless.
(10)通过封堵高度比和封堵面积比衡量凝胶封堵性的变化:封堵高度比和封堵面积比越大,说明凝胶封堵性越强;封堵高度比和封堵面积比越小,说明凝胶封堵性越差。(10) Measure the change of gel plugging performance by plugging height ratio and plugging area ratio: the larger the plugging height ratio and plugging area ratio, the stronger the plugging performance of the gel; the plugging height ratio and plugging area ratio The smaller the area ratio, the worse the gel plugging performance.
所述岩心的尺寸范围直径25mm,长度60mm~180mm。The size range of the rock core is 25 mm in diameter and 60 mm to 180 mm in length.
所述岩心渗透率范围500mD~5000mD。The core permeability ranges from 500mD to 5000mD.
所述步骤8)中驱替的压力范围为0.01MPa~20MPa。The displacement pressure in step 8) ranges from 0.01MPa to 20MPa.
所述步骤8)中驱替的流量变化范围为0.1ml/min~5ml/min。The displacement flow rate in step 8) ranges from 0.1ml/min to 5ml/min.
与现有技术相比,本发明具有如下突出的实质性特点和显著的优点:Compared with the prior art, the present invention has the following prominent substantive features and remarkable advantages:
本发明采用低场核磁共振成像技术研究凝胶在微孔道中封堵性表征,将岩心流动实验和核磁共振检测技术有机结合起来,使凝胶在多孔介质中的封堵特征得到比较直观的描述。The present invention uses low-field nuclear magnetic resonance imaging technology to study the plugging properties of gel in micropores, and combines the core flow experiment and nuclear magnetic resonance detection technology organically, so that the plugging characteristics of gel in porous media can be more intuitively described .
附图说明Description of drawings
图1为凝胶封堵高度比示意图。Figure 1 is a schematic diagram of the plugging height ratio of the gel.
图2为凝胶封堵面积比示意图。Fig. 2 is a schematic diagram of gel plugging area ratio.
图3为凝胶在岩心中矢状面核磁分布图像。Figure 3 is the NMR distribution image of the gel in the sagittal plane in the core.
图4为凝胶在岩心中横截面核磁分布图像。Figure 4 is the cross-sectional NMR image of the gel in the core.
图5为凝胶封堵高度比表征结果。Figure 5 shows the characterization results of gel plugging height ratio.
图6为凝胶封堵面积比表征结果。Fig. 6 is the characterization result of gel plugging area ratio.
图7为凝胶特征参数表。Figure 7 is a table of gel characteristic parameters.
具体实施方式detailed description
现将本发明结合附图的具体实施例叙述于后。Now the specific embodiment of the present invention in conjunction with accompanying drawing is described in the following.
本实施例的一种凝胶在岩石微通道中的封堵性的可视化评价方法,测试步骤为:A kind of visual evaluation method of the plugging property of gel in the rock microchannel of the present embodiment, the test procedure is:
(1)开启核磁共振设备,将饱和水的岩心放入磁体后,通过核磁成像确定岩心位置,使其处于磁场中心;对岩心矢状面和横截面的切片厚度设置为0.7cm、切片间隔设置为0.1cm以及切片位置进行设置,利用低场核磁共振设备获得岩心驱替实验中岩石微通道内流体信号;(1) Turn on the nuclear magnetic resonance equipment, put the water-saturated core into the magnet, and determine the position of the core through nuclear magnetic imaging, so that it is in the center of the magnetic field; set the slice thickness of the sagittal plane and cross section of the core to 0.7cm, and set the slice interval Set for 0.1cm and slice position, and use low-field nuclear magnetic resonance equipment to obtain fluid signals in rock microchannels in core displacement experiments;
(2)灰度图像提取。通过核磁共振提取凝胶在岩心中的灰度图像。(2) Grayscale image extraction. Grayscale images of the gel in the core were extracted by NMR.
(3)感兴趣区域(ROI)提取。提取90mm×25mm的矩形为灰度图像的有效区域。(3) Region of interest (ROI) extraction. Extract a 90mm×25mm rectangle as the effective area of the grayscale image.
(4)统一映射。所有矢状面统一映射的范围为1~100000无因次等效亮度单位。(4) Unified mapping. All sagittal planes are uniformly mapped in the range of 1 to 100,000 dimensionless equivalent luminance units.
(5)提取岩心骨架。对饱和岩心的核磁图像进行二值化处理,定义岩心骨架和流体的分离阀值为15000无因次等效亮度单位。(5) Extract the core skeleton. The nuclear magnetic image of the saturated core is binarized, and the separation threshold of the core skeleton and fluid is defined as 15,000 dimensionless equivalent brightness units.
(6)添加伪彩:对灰度统一后的岩心,添加JET伪彩,使凝胶和水的区分更加明显。(6) Adding false color: For the core with uniform gray scale, add JET false color to make the distinction between gel and water more obvious.
(7)提取凝胶图像。根据核磁共振图像提取凝胶图像,提取结果见图3和图4。获得凝胶面积、凝胶前缘、凝胶后缘和凝胶中心等参数。提取结果见图7。(7) Extract the gel image. The gel images were extracted from the NMR images, and the extraction results are shown in Figures 3 and 4. Parameters such as gel area, gel leading edge, gel trailing edge, and gel center are obtained. The extraction results are shown in Figure 7.
(8)凝胶封堵高度比表征:驱替一定孔隙体积的水,水驱后凝胶在纵向上封堵高度与候凝后凝胶在纵向上封堵高度的比值作为凝胶封堵高度比,如图1所示,首先计算每一个矢状面的封堵高度比,然后取平均值记为整个岩心中凝胶的封堵高度比,并将计算结果绘图,绘图结果见图5:(8) Characterization of gel plugging height ratio: Displacing water with a certain pore volume, the ratio of the vertical plugging height of the gel after water flooding to the vertical plugging height of the gel after waiting to solidify is taken as the gel plugging height As shown in Figure 1, the plugging height ratio of each sagittal plane is first calculated, and then the average value is recorded as the plugging height ratio of the gel in the whole core, and the calculation results are drawn, and the drawing results are shown in Figure 5:
式中:r1为岩心的截面高度,mm;r2为凝胶封堵高度,mm;F1为封堵高度比,无量纲。In the formula: r 1 is the section height of the core, mm; r 2 is the gel plugging height, mm; F 1 is the plugging height ratio, dimensionless.
(9)凝胶封堵面积比表征:在上一步骤中,将水驱后凝胶在横向上凝胶面积与孔隙总面积的比作为凝胶封堵面积比,如图2所示,首先计算每一个横断面的封堵面积比,然后取平均值记为整个岩心中凝胶的封堵面积比,并将计算结果绘图,绘图结果见图6:(9) Characterization of gel plugging area ratio: In the previous step, the ratio of the gel area to the total pore area of the gel in the lateral direction after water flooding was used as the gel plugging area ratio, as shown in Figure 2. First, Calculate the plugging area ratio of each cross-section, then take the average value and record it as the plugging area ratio of the gel in the entire rock, and draw the calculation results. The drawing results are shown in Figure 6:
式中:S1为岩心的截面面积,mm2;S2为凝胶封堵面积,mm2;F2为封堵面积比,无量纲。In the formula: S 1 is the cross-sectional area of the core, mm 2 ; S 2 is the plugging area of the gel, mm 2 ; F 2 is the plugging area ratio, dimensionless.
(10)通过封堵高度比和封堵面积比的表征,可得凝胶在运移过程中封堵高度比变化不大,封堵面积比先不变后逐渐减小。(10) Through the characterization of the plugging height ratio and plugging area ratio, it can be obtained that the plugging height ratio does not change much during the migration process of the gel, and the plugging area ratio first remains unchanged and then gradually decreases.
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