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CN107271346A - The measuring method of oil-containing tight sand pore-size distribution feature - Google Patents

The measuring method of oil-containing tight sand pore-size distribution feature Download PDF

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CN107271346A
CN107271346A CN201710485773.7A CN201710485773A CN107271346A CN 107271346 A CN107271346 A CN 107271346A CN 201710485773 A CN201710485773 A CN 201710485773A CN 107271346 A CN107271346 A CN 107271346A
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tight sand
size distribution
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姚素平
刘标
胡文瑄
曹剑
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Nanjing University
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Abstract

The invention provides a kind of measuring method of oil-containing tight sand pore-size distribution feature, belong to geology field, more particularly to tight sand field, probe liquid is used as using octamethylcy-clotetrasiloxane, oil-containing tight sand nanoscale hole completely can be quantitatively portrayed, the accuracy of oil-containing tight sand pore-size distribution numerical representation method is improved.The measuring method of the oil-containing tight sand pore-size distribution feature, comprises the following steps:Oil-containing tight sand sample is pre-processed;Using nuclear magnetic resonance freeze-thaw method test oil-containing tight sand as former state;To oil-containing tight sand former state saturation octamethylcy-clotetrasiloxane, saturated sample is tested using nuclear magnetic resonance freeze-thaw method;Data by above-mentioned oil-containing tight sand as former state with oil-containing tight sand saturated sample calculate the pore-size distribution of oil-containing tight sand.

Description

含油致密砂岩孔径分布特征的测量方法Measuring method of pore size distribution characteristics of oil-bearing tight sandstone

技术领域technical field

本发明涉及地质领域,尤其涉及致密砂岩领域,具体涉及一种含油致密砂岩孔径分布特征的测量方法。The invention relates to the field of geology, in particular to the field of tight sandstone, and in particular to a method for measuring the pore size distribution characteristics of oil-bearing tight sandstone.

背景技术Background technique

近年来,随着油气勘探开发的不断深入发展,国内外油气资源研究的重点逐渐由浅层转向深层,由常规油气藏转向非常规油气藏,致密气、页岩气、煤层气、致密油等非常规油气在现有经济技术条件下展示了巨大的潜力,中国常规油气资源相对贫乏,但非常规油气资源量丰富,尤其是致密油气开发利用潜力巨大。因此致密砂岩油气对于我们国家具有重要的意义。致密砂岩油气勘探开发的快速发展,已经突破了传统意义上常规储层物性下限,发现了致密砂岩的纳米孔也可储集丰富的油气资源。因此,对致密砂岩的纳米孔隙结构的研究对致密油气勘探开发至关重要。In recent years, with the continuous in-depth development of oil and gas exploration and development, the focus of oil and gas resources research at home and abroad has gradually shifted from shallow layers to deep layers, from conventional oil and gas reservoirs to unconventional oil and gas reservoirs, tight gas, shale gas, coalbed methane, tight oil, etc. Unconventional oil and gas have shown great potential under the current economic and technological conditions. China's conventional oil and gas resources are relatively poor, but unconventional oil and gas resources are abundant, especially tight oil and gas development and utilization potential is huge. Therefore, tight sandstone oil and gas are of great significance to our country. The rapid development of tight sandstone oil and gas exploration and development has broken through the lower limit of physical properties of conventional reservoirs in the traditional sense, and it has been discovered that nanopores in tight sandstone can also store rich oil and gas resources. Therefore, the research on the nano-pore structure of tight sandstone is very important for the exploration and development of tight oil and gas.

常规储层的孔隙一般在毫米-微米级,而致密砂岩的孔隙是以纳米级孔隙为主体。纳米级孔隙的物理性质明显不同于微米级以上孔隙,使得常规储层孔隙的表征技术方法对非常规储层适用性低。对致密砂岩储层纳米孔隙特征表征的技术手段很多,包括压汞法、气体等温吸附以及核磁共振T2谱等技术方法。其中以压汞法和气体吸附法应用的最为广泛。但是压汞法和气体吸附法在对于致密砂岩的表征中还是存在很多局限。压汞法使用的Washburn公式对大于50nm孔隙的分析比较准确,但是对小于50nm的孔隙分析就存在较大误差。同时压汞法测量纳米级孔隙时因所需压力过大可能对致密砂岩孔隙有破坏作用。气体吸附对于材料孔径的表征,依赖于计算模型。同一样品,利用不同计算模型,所得的孔径分布特征相差较大。同时气体吸附测试时间较长,精确表征的主要是0.4-100nm范围内的孔隙。这些方法都不能完整地刻画致密砂岩纳米级孔隙结构特征。因此,如何准确定量分析致密砂岩纳米级孔隙成为致密砂岩储层评价的难点。The pores of conventional reservoirs are generally on the millimeter-micron scale, while the pores of tight sandstone are mainly nano-scale pores. The physical properties of nanoscale pores are obviously different from pores above micron scale, which makes the characterization techniques and methods of conventional reservoir pores less applicable to unconventional reservoirs. There are many technical means to characterize the nanopore characteristics of tight sandstone reservoirs, including mercury porosimetry, gas isothermal adsorption, and nuclear magnetic resonance T 2 spectrum and other technical methods. Among them, mercury porosimetry and gas adsorption method are the most widely used. However, there are still many limitations in the characterization of tight sandstone by mercury porosimetry and gas adsorption. The Washburn formula used by mercury intrusion porosimetry is more accurate in the analysis of pores larger than 50nm, but there is a large error in the analysis of pores smaller than 50nm. At the same time, when the mercury porosimetry is used to measure nano-scale pores, the excessive pressure required may damage the pores of tight sandstone. The characterization of gas adsorption for material pore size depends on computational models. For the same sample, using different calculation models, the obtained pore size distribution characteristics are quite different. At the same time, the gas adsorption test takes a long time, and the pores in the range of 0.4-100nm are mainly accurately characterized. None of these methods can completely characterize the nanoscale pore structure characteristics of tight sandstone. Therefore, how to accurately and quantitatively analyze the nanoscale pores of tight sandstone has become a difficult point in the evaluation of tight sandstone reservoirs.

含油致密砂岩的孔径分布特征的测定,较成熟的方法有两种,第一种,利用有机试剂洗掉致密砂岩中的残余油,然后利用压汞法进行测定,该方法存在的问题是一方面使用简单的有机试剂不能把半开孔,部分开孔中的残余油气彻底清洗干净,使得利用压汞法测定时,会导致测试结果偏小;另一方面压汞法测试致密砂岩纳米孔隙时所需注汞压力过大,会改变部分孔隙结构,从而使得测试结果偏离真实值。第二种,利用有机溶剂萃取掉致密砂岩中的残余油,然后利用气体吸附法测定,该方法同样存在类似于第一种方法的局限性,同时由于受限于气体吸附法的测定范围,导致不能完整的测定含油致密砂岩纳米孔径分布。这两种方法都存在一定的缺陷和应用局限性,且都会导致测定的孔径含量偏小。There are two mature methods for measuring the pore size distribution characteristics of oil-bearing tight sandstone. The first method uses organic reagents to wash off the residual oil in tight sandstone, and then uses mercury porosimetry to measure. The problem with this method is that on the one hand The use of simple organic reagents cannot thoroughly clean the residual oil and gas in the semi-open pores and some open pores, so that the mercury porosimetry will lead to small test results; Excessive mercury injection pressure will change part of the pore structure, thus making the test results deviate from the true value. The second method is to use organic solvents to extract the residual oil in tight sandstone, and then use gas adsorption method to measure it. This method also has limitations similar to the first method. The nanopore size distribution of oil-bearing tight sandstone cannot be completely measured. These two methods have certain defects and application limitations, and both of them will lead to a smaller pore size content determined.

发明内容Contents of the invention

本发明的目的在于提供一种含油致密砂岩孔径分布特征的测量方法,使用八甲基环四硅氧烷作为探针液体,能够完整定量刻画含油致密砂岩纳米级孔隙,提高含油致密砂岩孔径分布数值表征的精确度。The purpose of the present invention is to provide a method for measuring the pore size distribution characteristics of oil-bearing tight sandstone, using octamethylcyclotetrasiloxane as a probe liquid, which can completely and quantitatively describe the nano-scale pores of oil-bearing tight sandstone, and improve the pore size distribution value of oil-bearing tight sandstone Accuracy of representation.

本发明提供了一种含油致密砂岩孔径分布特征的测量方法,包括如下步骤:The invention provides a method for measuring the pore size distribution characteristics of oil-bearing tight sandstone, comprising the following steps:

对含油致密砂岩样品进行预处理;利用核磁共振冻融法测试含油致密砂岩原样;对含油致密砂岩原样饱和八甲基环四硅氧烷,利用核磁共振冻融法测试饱和样品;通过上述含油致密砂岩原样和含油致密砂岩饱和样品的数据计算含油致密砂岩的孔径分布。Pretreatment of oil-bearing tight sandstone samples; use nuclear magnetic resonance freeze-thaw method to test the original oil-bearing tight sandstone; for oil-bearing tight sandstone original saturated octamethylcyclotetrasiloxane, use nuclear magnetic resonance freeze-thaw method to test saturated samples; through the above oil-bearing tight sandstone The pore size distribution of the oil tight sandstone was calculated from the data of the original sandstone and the saturated sample of the oil tight sandstone.

作为优选的技术方案,所述对含油致密砂岩样品进行预处理的步骤包括:对含油致密砂岩样品进行机械粉碎,取过20-35目的样品烘干,称重,记录质量M后将样品装入色谱瓶。As a preferred technical solution, the step of pretreating the oil-bearing tight sandstone sample includes: mechanically pulverizing the oil-bearing tight sandstone sample, taking a sample of 20-35 mesh, drying, weighing, recording the mass M, and loading the sample into Chromatography vials.

作为更优选的技术方案,所述机械粉碎为使用玛瑙研钵粉碎,所述烘干为真空箱中烘干。As a more preferred technical solution, the mechanical pulverization is pulverization using an agate mortar, and the drying is drying in a vacuum box.

作为优选的技术方案,利用核磁共振冻融法测试含油致密砂岩原样的步骤包括:利用核磁信号强的样品确定永磁体的中心频率,矫正射频信号频率,确定射频脉宽;利用核磁共振冻融法测试酒精,确定核磁共振信号强度温度修正系数λ;确定核磁共振信号强度与八甲基环四硅氧烷含量的关系;确定含油致密砂岩的核磁共振实验参数,设定温度计划,利用核磁共振冻融法测定含油致密砂岩原样。As a preferred technical solution, the steps of using NMR freeze-thaw method to test the original sample of oil-bearing tight sandstone include: using a sample with strong NMR signal to determine the center frequency of the permanent magnet, correcting the frequency of the radio frequency signal, and determining the radio frequency pulse width; Test alcohol, determine the temperature correction coefficient λ of the NMR signal intensity; determine the relationship between the NMR signal intensity and the content of octamethylcyclotetrasiloxane; determine the NMR experimental parameters of oil-bearing tight sandstone, set the temperature plan, Determination of oil-bearing tight sandstone samples by fusion method.

作为更优选的技术方案,利用核磁共振冻融法测试酒精,确定核磁共振信号强度温度修正系数λ为测试酒精在-30℃~20℃范围内不同温度下标样的信号强度,根据公式(1),计算得出λ,所述公式(1)为As a more preferred technical scheme, utilize nuclear magnetic resonance freeze-thaw method to test alcohol, determine the temperature correction coefficient λ of nuclear magnetic resonance signal intensity to be the signal intensity of test alcohol standard sample at different temperatures in the range of -30 ℃ ~ 20 ℃, according to the formula (1 ), calculate λ, the formula (1) is

式(1)中SI为核磁共振信号强度,T为温度,α与β为电阻率参数,λ为核磁共振信号强度温度修正系数。In formula (1), SI is the NMR signal intensity, T is the temperature, α and β are the resistivity parameters, and λ is the temperature correction coefficient of the NMR signal intensity.

作为优选的技术方案,对含油致密砂岩原样饱和八甲基环四硅氧烷的步骤为利用真空饱和装置进行处理,将待测样品放置于真空箱内,抽真空12h;向放置有抽真空后含油致密砂岩原样的色谱瓶中加入八甲基环四硅氧烷,平衡6h;将色谱瓶离心2hAs a preferred technical scheme, the step of saturating the oil-bearing tight sandstone with octamethylcyclotetrasiloxane as it is is to use a vacuum saturation device to process, place the sample to be tested in a vacuum box, and vacuumize it for 12 hours; Add octamethylcyclotetrasiloxane to the original chromatographic bottle of oily tight sandstone, and equilibrate for 6 hours; centrifuge the chromatographic bottle for 2 hours

作为优选的技术方案,利用核磁共振冻融法测试饱和样品时设定与测试原样相同的实验参数和相同的温度计划。As a preferred technical solution, the same experimental parameters and the same temperature plan as the test sample are set when using the NMR freeze-thaw method to test the saturated sample.

作为优选的技术方案,所述计算含油致密砂岩的孔径分布的具体步骤包括:As a preferred technical solution, the specific steps of calculating the pore size distribution of the oil-bearing tight sandstone include:

利用饱和样品每个温度点的数据减去原样修正后对应温度点的数据;将核磁共振信号强度,利用核磁共振信号强度温度修正系数λ,进行修正;利用饱和样品每个温度点修正后的数据减去原样修正后对应温度点的数据;利用核磁共振信号强度与八甲基环四硅氧烷含量之间的关系,将信号强度换算成八甲基环四硅氧烷的液体体积;利用吉布斯托马斯方程将温度换算孔径大小,得到孔体积与孔径的相互关系;根据孔体积与孔径的关系,计算并绘制样品的微分孔径分布曲线以及对数微分孔径分布曲线。Use the data of each temperature point of the saturated sample to subtract the data of the corresponding temperature point after the original correction; the NMR signal intensity is corrected by using the NMR signal intensity temperature correction coefficient λ; use the corrected data of each temperature point of the saturated sample Subtract the data corresponding to the temperature point after the original correction; use the relationship between the nuclear magnetic resonance signal intensity and the content of octamethylcyclotetrasiloxane to convert the signal intensity into the liquid volume of octamethylcyclotetrasiloxane; The Booth-Thomas equation converts the temperature into the pore size to obtain the relationship between the pore volume and the pore size; according to the relationship between the pore volume and the pore size, the differential pore size distribution curve and the logarithmic differential pore size distribution curve of the sample are calculated and drawn.

作为更优选的技术方案,所述微分孔径分布和对数微分孔径分布的计算公式为:As a more preferred technical solution, the calculation formulas of the differential pore size distribution and the logarithmic differential pore size distribution are:

式(2)-(3)中V为孔隙体积;D为孔径;T为温度;KGT为吉布斯托马斯常数,与探针液体的热力学性质相关的常数。In formulas (2)-(3), V is the pore volume; D is the pore diameter; T is the temperature; K GT is the Gibbs-Thomas constant, a constant related to the thermodynamic properties of the probe liquid.

与现有技术相比,本发明的有益效果在于:Compared with prior art, the beneficial effect of the present invention is:

1、本发明的测量方法采用核磁共振冻融法具有以下的优势:1, the measuring method of the present invention adopts nuclear magnetic resonance freeze-thaw method to have following advantage:

①核磁共振冻融法法的理论基础为Gibbs-Thomson方程,可以直接揭示了熔点与孔体积之间的关系,含油致密砂岩复杂的孔隙结构对其影响不大;① The theoretical basis of NMR freeze-thaw method is Gibbs-Thomson equation, which can directly reveal the relationship between melting point and pore volume, and the complex pore structure of oil-bearing tight sandstone has little influence on it;

②核磁共振冻融法测试得到的孔径分布曲线的信息更加丰富,更加细腻;与常规核磁共振T2法相比,核磁共振冻融法可以对含油致密砂岩纳米孔径实现精确检测,可测试的有效孔径范围可达4-1500nm;②The information of the pore size distribution curve obtained by the NMR freeze-thaw method is richer and more delicate; compared with the conventional NMR T2 method, the NMR freeze-thaw method can accurately detect the nanopore size of oil-bearing tight sandstone, and the effective pore size range that can be tested is Up to 4-1500nm;

③核磁共振冻融法不仅在致密砂岩的“全孔隙”定量识别方面较压汞法拥有独特的技术优势,而且还具有不污染样品,不破坏样品结构,测试方便快速;③ The nuclear magnetic resonance freeze-thaw method not only has unique technical advantages over the mercury intrusion method in the quantitative identification of "full pores" in tight sandstone, but also has the advantages of not polluting the sample, not destroying the sample structure, and the test is convenient and fast;

2、本发明的测量方法采用八甲基环四硅氧烷作为核磁共振探针液体,其具有双亲性,既有利于进入有机质孔隙,也有利于进入无机矿物孔隙,可以溶解残余在孔隙中的油、沥青等有机物,更好的饱和孔隙;有利于核磁共振冻融法实验精度的提高;在测试的过程中不会冻伤待测样品,不会改变样品原有的孔隙结构;相比与常用的探针液体水和环已烷针对含油致密砂岩更有利于测试。2. The measurement method of the present invention adopts octamethylcyclotetrasiloxane as the NMR probe liquid, which has amphiphilicity, which is conducive to entering the pores of organic matter and the pores of inorganic minerals, and can dissolve the residues in the pores. Organic matter such as oil and asphalt can better saturate pores; it is beneficial to improve the experimental accuracy of NMR freeze-thaw method; it will not frostbite the sample to be tested during the test, and will not change the original pore structure of the sample; compared with commonly used The probe liquid water and cyclohexane are more conducive to testing for oil-bearing tight sandstone.

附图说明Description of drawings

图1为本发明的测量方法的流程示意图;Fig. 1 is the schematic flow sheet of measurement method of the present invention;

图2a.温度与信号强度的关系图;b.与-SIKTK的关系图;Figure 2a. The relationship between temperature and signal intensity; b. Relationship diagram with -SI K T K ;

图3为标样质量与信号强度的线性关系图;Fig. 3 is a linear relationship diagram between standard sample quality and signal strength;

图4为原始的核磁共振信号强度以及修正后的信号强度与温度的关系图;Fig. 4 is the original nuclear magnetic resonance signal intensity and the relationship diagram between the signal intensity and temperature after correction;

图5为含油致密砂岩样品累计孔体积与孔径的关系图;Fig. 5 is a graph showing the relationship between cumulative pore volume and pore diameter of oil-bearing tight sandstone samples;

图6为含油致密砂岩样品孔径分布曲线图。Fig. 6 is the pore size distribution curve of oil-bearing tight sandstone samples.

具体实施方式detailed description

下面将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. Obviously, the described embodiments are only some of the embodiments of the present invention, but not all of them. Based on the embodiments of the present invention, all other embodiments obtained by persons of ordinary skill in the art without making creative efforts belong to the protection scope of the present invention.

本发明实施例提供了一种含油致密砂岩孔径分布特征的测量方法,参见图1,图1是本发明的测量方法的流程示意图,该方法包括如下步骤:The embodiment of the present invention provides a method for measuring the pore size distribution characteristics of oil-bearing tight sandstone, referring to Fig. 1, Fig. 1 is a schematic flow chart of the measuring method of the present invention, the method comprises the following steps:

S101、对含油致密砂岩样品的预处理;S101. Pretreatment of oil-bearing tight sandstone samples;

S102、利用核磁共振冻融法测试含油致密砂岩原样;S102, using nuclear magnetic resonance freeze-thaw method to test the original sample of oil-bearing tight sandstone;

S103、对含油致密砂岩原样饱和八甲基环四硅氧烷,利用核磁共振冻融法测试饱和样品;S103. For oily tight sandstone saturated with octamethylcyclotetrasiloxane as it is, the saturated sample is tested by nuclear magnetic resonance freeze-thaw method;

S104、通过上述含油致密砂岩原样和含油致密砂岩饱和样品的数据计算含油致密砂岩的孔径分布。S104. Calculate the pore size distribution of the oil-bearing tight sandstone based on the above data of the oil-bearing tight sandstone original sample and the oil-bearing tight sandstone saturated sample.

具体地,在实际测试之前,从含油致密砂岩储层中选取若干样品,从这些岩心样品中确定最能代表该含油致密砂岩储层物性的样品为最优样品,从而可以避免含油致密砂岩非均质性造成测试结果不能感应真实储层物性。Specifically, before the actual test, several samples are selected from the oil-bearing tight sandstone reservoir, and the sample that best represents the physical properties of the oil-bearing tight sandstone reservoir is determined from these core samples as the optimal sample, so that the heterogeneity of the oil-bearing tight sandstone can be avoided. Due to the qualitative nature, the test results cannot reflect the real reservoir physical properties.

作为优选的实施例,在步骤S101中,对含油致密砂岩原样进行预处理的步骤包括:对含油致密砂岩样品进行机械粉碎,取过20-35目的样品烘干,利用分析天平进行称重,记录质量M后将样品装入色谱瓶。As a preferred embodiment, in step S101, the step of pretreating the oil-bearing tight sandstone sample includes: mechanically pulverizing the oil-bearing tight sandstone sample, taking a sample of 20-35 mesh and drying it, weighing it with an analytical balance, and recording After mass M, the sample is loaded into the chromatographic vial.

本实施例中,对待测的含油致密砂岩样品进行机械粉碎时,优选的使用玛瑙研钵,不能使用铜钵、不锈钢钵等金属研磨体,避免金属对待测样品的测试结果的影响。样品粉碎后,使用筛子进行分选,选取20-35目的待测样品。一般来说,样品颗粒的大小的选取是根据待测样品的矿物组成以及致密砂岩胶结程度等性质来确定,本发明实施例中使用20-35目的样品。如果样品选择过大,不利于后期饱和探针液体,从而影响测试结果;样品颗粒太小会堆积产生大量微米-纳米颗粒之间的孔隙,也会影响测试结果。In this embodiment, when the oil-bearing tight sandstone sample to be tested is mechanically crushed, it is preferable to use an agate mortar, and metal grinding bodies such as copper bowls and stainless steel bowls cannot be used to avoid the influence of metal on the test results of the sample to be tested. After the sample is pulverized, use a sieve for sorting, and select a 20-35 mesh sample to be tested. Generally speaking, the size of the sample particles is determined according to the mineral composition of the sample to be tested and the cementation degree of the tight sandstone. In the embodiment of the present invention, a sample of 20-35 mesh is used. If the sample is too large, it is not conducive to the later saturation of the probe liquid, which will affect the test results; if the sample particles are too small, they will accumulate a large number of pores between micron-nano particles, which will also affect the test results.

本实施例中,对于烘干的过程,优选的是选取的样品放置于真空箱中,设定温度为100℃,烘干24小时。如果不是真空环境,有可能会出现部分矿物会氧化等现象,从而改变原始样品。烘干后的样品,利用分析天平称重,可以选择0.5-1.5g左右的样品,具体的质量和体积根据色谱平的大小可以调整,记录测试样品的质量M。In this embodiment, for the drying process, it is preferable to place the selected samples in a vacuum box, set the temperature at 100° C., and dry them for 24 hours. If it is not a vacuum environment, some minerals may be oxidized and other phenomena may occur, thereby changing the original sample. The dried sample is weighed with an analytical balance, and a sample of about 0.5-1.5 g can be selected. The specific mass and volume can be adjusted according to the size of the chromatographic plane, and the mass M of the test sample can be recorded.

本实施例中,将称量的待测样品装入色谱瓶为下一步的测试做准备,优选的,核磁共振仪器线圈内径大小为10mm,因而使用2.5ml的玻璃色谱瓶盛装样品,但是可以理解的是,根据使用仪器的不同,可以使用不同的大小或者材质的色谱瓶。In this embodiment, the weighed sample to be tested is packed into a chromatographic bottle to prepare for the next test. Preferably, the inner diameter of the NMR instrument coil is 10mm, so a 2.5ml glass chromatographic bottle is used to hold the sample, but it can be understood What's more, depending on the instrument used, different sizes or materials of chromatographic vials can be used.

作为优选的实施例,在步骤S102中,利用核磁共振冻融法测试含油致密砂岩原样的步骤包括:利用核磁信号强的样品确定永磁体的中心频率,矫正射频信号频率,确定射频脉宽;利用核磁共振冻融法测试酒精,确定核磁共振信号强度温度修正系数λ;确定核磁共振信号强度与八甲基环四硅氧烷含量的关系;确定含油致密砂岩的核磁共振实验参数,设定温度计划,利用核磁共振冻融法测定含油致密砂岩原样。As a preferred embodiment, in step S102, the step of using nuclear magnetic resonance freeze-thaw method to test the original sample of oil-bearing tight sandstone includes: using a sample with a strong nuclear magnetic signal to determine the center frequency of the permanent magnet, correcting the frequency of the radio frequency signal, and determining the pulse width of the radio frequency; Test alcohol by NMR freeze-thaw method, determine the temperature correction coefficient λ of NMR signal intensity; determine the relationship between NMR signal intensity and octamethylcyclotetrasiloxane content; determine the NMR experimental parameters of oil-bearing tight sandstone, and set the temperature plan , Determination of oil-bearing tight sandstone samples by NMR freeze-thaw method.

本实施例中,核磁共振设备使用的磁体是永磁体,具有固有磁场强度B0,根据ω=γB0,对应氢核一个固有频率。只有在射频脉冲频率与永磁体固有频率相同的条件下,放在磁体内的样品才会发生核磁共振现象,该固有频率称为共振频率,也称作中心频率。永磁体对温度等外界环境变化较敏感,磁体固有频率可能会产生微小漂移,所以需要调整射频脉冲频率使其与当前的磁体固有频率一致,也就是寻找中心频率,进行实验测试之前需要调整。本发明利用植物油等核磁信号强的样品,确定永磁体的中心频率,矫正射频信号频率。In this embodiment, the magnet used in the nuclear magnetic resonance equipment is a permanent magnet with a natural magnetic field strength B 0 , which corresponds to a natural frequency of hydrogen nuclei according to ω=γB 0 . Only when the radio frequency pulse frequency is the same as the natural frequency of the permanent magnet, the sample placed in the magnet will undergo nuclear magnetic resonance. The natural frequency is called the resonance frequency, also known as the center frequency. Permanent magnets are sensitive to changes in the external environment such as temperature, and the natural frequency of the magnet may drift slightly, so it is necessary to adjust the RF pulse frequency to make it consistent with the current natural frequency of the magnet, that is, to find the center frequency, which needs to be adjusted before performing experimental tests. The invention uses samples with strong nuclear magnetic signals such as vegetable oil to determine the center frequency of the permanent magnet and correct the frequency of the radio frequency signal.

此外,要得到核磁信号离不开射频脉冲激励,由于射频线圈的尺寸以及射频功放的功率不同,所以激发样品所需的脉冲能量也不同。脉冲能量由脉冲幅度和脉冲宽度来决定,因此,改变硬脉冲宽度其本质就是在改变硬脉冲能量。在脉冲序列中较为常用的是90度硬脉冲和180度硬脉冲。同样利用核磁共振仪器测试植物油等信号强的物质,可以确定射频脉宽。In addition, to obtain NMR signals is inseparable from radio frequency pulse excitation, because the size of the radio frequency coil and the power of the radio frequency power amplifier are different, so the pulse energy required to excite the sample is also different. The pulse energy is determined by the pulse amplitude and pulse width. Therefore, changing the hard pulse width is essentially changing the hard pulse energy. The more commonly used pulse sequences are 90-degree hard pulses and 180-degree hard pulses. Similarly, the NMR instrument can be used to test substances with strong signals such as vegetable oil, and the radio frequency pulse width can be determined.

核磁共振信号对温度的变化是非常敏感的,在进行核磁信号对液体体积的换算之前,必须对信号强度进行修正。对信号强度的影响主要表现在两个方面:塞曼能级粒子数分布随温度的变化和探头线圈的质量因子随温度的变化。综合考虑温度对粒子占有数分布和探头线圈的质量因子的影响,将某个温度下的信号强度换算成标准温度信号强度的公式为:The NMR signal is very sensitive to temperature changes, and the signal intensity must be corrected before converting the NMR signal to the liquid volume. The impact on the signal strength is mainly manifested in two aspects: the change of Zeeman level particle number distribution with temperature and the change of quality factor of probe coil with temperature. Considering the influence of temperature on the particle occupancy number distribution and the quality factor of the probe coil, the formula for converting the signal intensity at a certain temperature into the standard temperature signal intensity is:

式(1)中SI为核磁共振信号强度,T为温度,α与β为电阻率参数,λ为核磁共振信号强度温度修正系数,在实验之前进行测定。In formula (1), SI is the NMR signal intensity, T is the temperature, α and β are the resistivity parameters, and λ is the temperature correction coefficient of the NMR signal intensity, which is measured before the experiment.

本发明测试的温度范围为-30℃~20℃,采用凝固点低的液体标样进行测定,本发明采用的是酒精,测试酒精在-30℃~20℃范围内不同温度下标样的信号强度。从而根据公式(1),可以计算得出λ。The temperature range of the test in the present invention is -30°C to 20°C, and the liquid standard sample with a low freezing point is used for measurement. The present invention uses alcohol to test the signal strength of the standard sample at different temperatures in the range of -30°C to 20°C. . Thus, according to formula (1), λ can be calculated.

核磁信号强度SI与探针液体的体积V成正比关系。核磁共振冻融法测量样品内不同温度下的探针含量,即八甲基环四硅氧烷的含量。所以首先应当利用标样标定八甲基环四硅氧烷含量和核磁信号之间的关系。在测试样品时,通过拟合的线性方程,可以每个温度点的核磁共振信号强度换算成八甲基环四硅氧烷的含量。The NMR signal intensity SI is proportional to the volume V of the probe liquid. The NMR freeze-thaw method was used to measure the probe content in the sample at different temperatures, that is, the content of octamethylcyclotetrasiloxane. Therefore, the standard sample should be used to calibrate the relationship between the content of octamethylcyclotetrasiloxane and the NMR signal. When testing the sample, the NMR signal intensity at each temperature point can be converted into the content of octamethylcyclotetrasiloxane through the fitted linear equation.

核磁参数设置是进行实验的前提,参数设置的好,实验结果就接近实际情况,参数设置的差,实验结果可能就偏离了测量样品本来的性质,甚至得不到实验结果。因此需要确定含油致密砂岩的核磁共振实验最优的参数。确定好参数后设定温度计划,利用核磁共振冻融法测定含油致密砂岩原样。The NMR parameter setting is the prerequisite for the experiment. If the parameter setting is good, the experimental result will be close to the actual situation. If the parameter setting is poor, the experimental result may deviate from the original nature of the measured sample, and even the experimental result cannot be obtained. Therefore, it is necessary to determine the optimal parameters of the NMR experiment of oil-bearing tight sandstone. After determining the parameters, set the temperature plan, and use the NMR freeze-thaw method to measure the original oil-bearing tight sandstone.

作为优选的实施例,在步骤S103中,对含油致密砂岩原样饱和八甲基环四硅氧烷的步骤为利用真空饱和装置进行处理,将待测样品放置于真空箱内,抽真空12h;向放置有抽真空后含油致密砂岩样品的色谱瓶中加入八甲基环四硅氧烷,平衡6h;将色谱瓶离心2h。As a preferred embodiment, in step S103, the step of saturating the oil-bearing tight sandstone with octamethylcyclotetrasiloxane as it is is to use a vacuum saturation device to process, place the sample to be tested in a vacuum box, and vacuumize it for 12 hours; Add octamethylcyclotetrasiloxane to the chromatographic bottle in which the oil-bearing tight sandstone sample is placed after vacuuming, and equilibrate for 6 hours; centrifuge the chromatographic bottle for 2 hours.

本实施例中,对含油致密砂岩利用真空饱和装置进行处理简单便捷,操作方便,具体的步骤优选为,将待测样品放置于真空箱内,抽真空12h;向放置有抽真空后含油致密砂岩样品的2.5ml色谱瓶中加入八甲基环四硅氧烷液体,平衡6h,可以使得含油致密砂岩原样充分饱和八甲基环四硅氧烷。作为优选的实施例,离心的步骤为将2.5ml色谱瓶利用离心机以5000r/min的速度离心2h,保证充分离心。但是可以理解的是,上述抽真空和平衡以及离心的时间可以根据实际试验的需要进行常规的调整。In this embodiment, the oil-bearing tight sandstone is treated with a vacuum saturation device, which is simple and convenient, and the operation is convenient. The specific steps are preferably as follows: place the sample to be tested in a vacuum box and vacuumize it for 12 hours; Add octamethylcyclotetrasiloxane liquid into the 2.5ml chromatographic bottle of the sample, and equilibrate for 6 hours, so that the oil-bearing tight sandstone can be fully saturated with octamethylcyclotetrasiloxane as it is. As a preferred embodiment, the centrifugation step is to use a centrifuge to centrifuge the 2.5ml chromatographic bottle at a speed of 5000r/min for 2h to ensure sufficient centrifugation. However, it can be understood that the above vacuuming, balancing and centrifuging time can be routinely adjusted according to the needs of actual experiments.

作为优选的实施例,利用核磁共振冻融法测试饱和样品时设定与测试原样相同的实验参数和相同的温度计划。本实施例中,在相同的实验参数和相同的温度计划下得到的数据用于后续分析更具有严谨性和可用性。As a preferred embodiment, the same experimental parameters and the same temperature plan as the test sample are set when using the nuclear magnetic resonance freeze-thaw method to test the saturated sample. In this example, the data obtained under the same experimental parameters and the same temperature plan are more rigorous and usable for subsequent analysis.

作为优选的实施例,在步骤S104中,所述计算并绘制含油致密砂岩原样的微分孔径分布曲线以及对数微分孔径分布曲线的具体步骤包括:As a preferred embodiment, in step S104, the specific steps of calculating and drawing the original differential pore size distribution curve and logarithmic differential pore size distribution curve of the oil-bearing tight sandstone include:

利用饱和样品每个温度点的数据减去原样修正后对应温度点的数Use the data of each temperature point of the saturated sample to subtract the number of the corresponding temperature point after the original correction

据;将核磁共振信号强度,利用核磁共振信号强度温度修正系数λ,进行修正;利用饱和样品每个温度点修正后的数据减去原样修正后对应温度点的数据;利用核磁共振信号强度与八甲基环四硅氧烷含量之间的关系,将信号强度换算成八甲基环四硅氧烷的液体体积;利用吉布斯托马斯方程将温度换算孔径大小,得到孔体积与孔径的相互关系;根据孔体积与孔径的关系,计算样品的微分孔径分布曲线以及对数微分孔径分布曲线,从而测量含油致密砂岩孔径分布特征。According to the data; the nuclear magnetic resonance signal strength is corrected by the temperature correction coefficient λ of the nuclear magnetic resonance signal strength; the corrected data of each temperature point of the saturated sample is used to subtract the data of the corresponding temperature point after the original correction; the difference between the nuclear magnetic resonance signal strength and eight The relationship between the content of methylcyclotetrasiloxane, the signal intensity is converted into the liquid volume of octamethylcyclotetrasiloxane; the temperature is converted into the pore size by using the Gibbs-Thomas equation, and the relationship between the pore volume and the pore diameter is obtained ; Calculate the differential pore size distribution curve and the logarithmic differential pore size distribution curve of the sample according to the relationship between the pore volume and the pore size, so as to measure the pore size distribution characteristics of the oil-bearing tight sandstone.

本实施例中,实验的直接数据是样品的信号强度对温度的变化,首先利用饱和样品每个温度点的数据减去原样修正后对应温度点的数据;将核磁共振信号强度,利用核磁共振信号强度温度修正系数λ,进行修正;利用核磁共振信号强度与八甲基环四硅氧烷含量之间的关系,将信号强度换算成八甲基环四硅氧烷的液体体积;利用吉布斯托马斯方程将温度换算孔径大小,从而得到了累积孔体积与孔径的相互关系;根据孔体积与孔径的关系,计算并绘制样品的微分孔径分布曲线以及对数微分孔径分布曲线,In this embodiment, the direct data of the experiment is the change of the signal intensity of the sample to the temperature. First, the data of each temperature point of the saturated sample is used to subtract the data of the corresponding temperature point after the original correction; The intensity temperature correction coefficient λ is used for correction; the signal intensity is converted into the liquid volume of octamethylcyclotetrasiloxane by using the relationship between the nuclear magnetic resonance signal intensity and the content of octamethylcyclotetrasiloxane; using Gibbs The Thomas equation converts the temperature into the pore size, thereby obtaining the relationship between the cumulative pore volume and the pore size; according to the relationship between the pore volume and the pore size, calculate and draw the differential pore size distribution curve and the logarithmic differential pore size distribution curve of the sample,

其中,样品的微分孔径分布Pd(D)的计算方式为Among them, the calculation method of the differential pore size distribution P d (D) of the sample is

样品的对数微分孔径分布Plog(D)的计算方式为The logarithmic differential pore size distribution P log (D) of the sample is calculated as

式(2)-(3)中V为孔隙体积;D为孔径;T为温度;KGT为吉布斯托马斯常数,与探针液体的热力学性质相关的常数。In formulas (2)-(3), V is the pore volume; D is the pore diameter; T is the temperature; K GT is the Gibbs-Thomas constant, a constant related to the thermodynamic properties of the probe liquid.

为了更清楚详细地介绍本发明实施例所提供的含油致密砂岩孔径分布特征的测量方法,以下将结合具体实施例进行说明。In order to more clearly and in detail describe the method for measuring the pore size distribution characteristics of oil-bearing tight sandstone provided by the embodiments of the present invention, the following will be described in conjunction with specific examples.

选定一块含油致密砂岩的样品。A sample of oil-bearing tight sandstone is selected.

对含油致密砂岩样品在玛瑙研钵中进行机械粉碎,取过20-35目的样品真空箱中烘干,利用分析天平称重,记录质量M为0.607g;将称量的待测样品装入2.5ml的色谱瓶。The oil-bearing tight sandstone samples were mechanically pulverized in an agate mortar, dried in a vacuum box with 20-35 mesh samples, weighed with an analytical balance, and the recorded mass M was 0.607g; the weighed sample to be tested was loaded into 2.5 ml chromatographic vials.

利用核磁共振冻融法测试含油致密砂岩原样的步骤包括:利用核磁信号强的样品确定永磁体的中心频率,矫正射频信号频率,确定射频脉宽;利用核磁共振冻融法测试酒精,确定核磁共振信号强度温度修正系数λ;确定核磁共振信号强度与八甲基环四硅氧烷含量的关系;确定含油致密砂岩的核磁共振实验参数,设定温度计划,利用核磁共振冻融法测定含油致密砂岩原样。The steps of testing the original sample of oil-bearing tight sandstone by nuclear magnetic resonance freeze-thaw method include: using a sample with a strong nuclear magnetic signal to determine the center frequency of the permanent magnet, correcting the frequency of the radio frequency signal, and determining the pulse width of the radio frequency; Signal intensity temperature correction coefficient λ; Determine the relationship between NMR signal intensity and octamethylcyclotetrasiloxane content; Determine the NMR experimental parameters of oil-bearing tight sandstone, set the temperature plan, and use NMR freeze-thaw method to determine oil-bearing tight sandstone as is.

利用植物油确定永磁体的中心频率,矫正射频信号频率,利用植物油确定射频脉宽,P1为3.2μs,P2为6.6μs;Use vegetable oil to determine the center frequency of the permanent magnet, correct the frequency of the radio frequency signal, and use vegetable oil to determine the pulse width of the radio frequency, P1 is 3.2μs, P2 is 6.6μs;

利用核磁共振冻融法测试酒精,确定核磁共振信号强度温度修正系数λ,设定从253.15K开始,293.15K结束,每隔10K,测试一个CPMG序列,得到信号强度与温度的关系,参见图2a,结合SIK 与-SIKTK的关系,通过线性拟合可以计算出λ为507.38,参见图2b;Use the NMR freeze-thaw method to test alcohol, determine the temperature correction coefficient λ of the NMR signal intensity, set it from 253.15K to 293.15K, and test a CPMG sequence every 10K to obtain the relationship between signal intensity and temperature, see Figure 2a , combined with SI K The relationship with -S IK T K can be calculated as 507.38 through linear fitting, see Figure 2b;

利用标样标定八甲基环四硅氧烷含量和核磁信号之间的关系,参见图3,在测试样品时,通过拟合的线性方程,可以把每个温度点的CPMG信号强度换算成八甲基环四硅氧烷的含量。Use the standard sample to calibrate the relationship between the octamethylcyclotetrasiloxane content and the nuclear magnetic signal, see Figure 3, when testing the sample, the CPMG signal intensity at each temperature point can be converted into eight Methylcyclotetrasiloxane content.

用八甲基环四硅氧烷作为探针液体,利用核磁共振冻融法测定含油致密砂岩孔径分布时,CPMG序列参数为等待时间Tw为2500ms,回波时间TE为1ms,回波个数为2000。温度计划为250.55~280.55K以下温度间隔2K;280.55~285.55K温度间隔1K;285.55~288.55K,温度间隔0.5K;288.55~289.55K,温度间隔0.2K;289.55~290.55K,温度间隔0.1K。每个温度点等待时间20分钟后利用CPMG序列采集数据。然后利用核磁共振冻融法测试含油致密砂岩原样。When octamethylcyclotetrasiloxane is used as the probe liquid to measure the pore size distribution of oil-bearing tight sandstone by NMR freeze-thaw method, the CPMG sequence parameters are as follows: waiting time Tw is 2500ms, echo time TE is 1ms, and the number of echoes is 2000. The temperature plan is 250.55-280.55K with a temperature interval of 2K; 280.55-285.55K with a temperature interval of 1K; 285.55-288.55K with a temperature interval of 0.5K; 288.55-289.55K with a temperature interval of 0.2K; Data were collected using CPMG sequences after a waiting time of 20 minutes at each temperature point. The oil-bearing tight sandstone samples were then tested by NMR freeze-thaw method.

利用真空饱和装置,将待测样品放置于真空箱内,抽真空12h;向放置有抽真空后含油致密砂岩样品的色谱瓶中加入八甲基环四硅氧烷,平衡6h;将色谱瓶离心2h。利用核磁共振冻融法测试饱和样品,设定与测试原样相同的实验参数和相同的温度计划。Using a vacuum saturation device, place the sample to be tested in a vacuum box and vacuumize for 12 hours; add octamethylcyclotetrasiloxane to the chromatographic bottle containing the oil-containing dense sandstone sample after vacuuming, and balance for 6 hours; centrifuge the chromatographic bottle 2h. The saturated samples were tested using the NMR freeze-thaw method, setting the same experimental parameters and the same temperature schedule as the original samples.

通过上述含油致密砂岩原样和含油致密砂岩饱和样品的数据计算含油致密砂岩的孔径分布:The pore size distribution of the oil-bearing tight sandstone is calculated from the above data of the oil-bearing tight sandstone original sample and the oil-bearing tight sandstone saturated sample:

利用饱和样品每个温度点的数据减去原样修正后对应温度点的数Use the data of each temperature point of the saturated sample to subtract the number of the corresponding temperature point after the original correction

据;将核磁共振信号强度,利用核磁共振信号强度温度修正系数λ,利用上述公式(1)进行温度修正。将所有温度点的核磁共振信号强度修正到290.15K,修正后的数据见图4。再进行后续的计算。可以发现温度越低,原始信号强度与修正后的信号强度偏差越多。According to; the nuclear magnetic resonance signal intensity, using the temperature correction coefficient λ of the nuclear magnetic resonance signal intensity, using the above formula (1) for temperature correction. The NMR signal intensities at all temperature points were corrected to 290.15K, and the corrected data are shown in Figure 4. Then perform subsequent calculations. It can be found that the lower the temperature, the more the deviation between the original signal strength and the corrected signal strength.

利用核磁共振信号强度与八甲基环四硅氧烷含量之间的关系,将信号强度换算成八甲基环四硅氧烷的液体体积,利用吉布斯托马斯方程将温度换算孔径大小,从而得到了累积孔体积与孔径的相互关系见图5。从累积孔体积与孔径的关系中,根据公式(2)和(3),可以计算和绘制得出样品的对数微分孔径分布曲线见图6。通过图6可以看出含油致密砂岩的孔隙是以纳米级孔隙为主,致密砂岩纳米级孔隙中富含大量原油。因此,本发明的测量方法可以更准确的对含油致密砂岩的孔径分布特征进行测定,更有利于致密砂岩的油气研究。Using the relationship between the NMR signal intensity and the content of octamethylcyclotetrasiloxane, the signal intensity is converted into the liquid volume of octamethylcyclotetrasiloxane, and the temperature is converted into the pore size using the Gibbs-Thomas equation, thereby The relationship between cumulative pore volume and pore diameter is obtained, as shown in Figure 5. From the relationship between cumulative pore volume and pore diameter, according to formulas (2) and (3), the logarithmic differential pore size distribution curve of the sample can be calculated and drawn, as shown in Figure 6. It can be seen from Fig. 6 that the pores of oil-bearing tight sandstone are mainly nano-scale pores, and the nano-scale pores of tight sandstone are rich in a large amount of crude oil. Therefore, the measurement method of the present invention can more accurately measure the pore size distribution characteristics of the oil-bearing tight sandstone, and is more conducive to the oil and gas research of the tight sandstone.

Claims (9)

1. the measuring method of oil-containing tight sand pore-size distribution feature, it is characterised in that comprise the following steps:
Oil-containing tight sand sample is pre-processed;Using nuclear magnetic resonance freeze-thaw method test oil-containing tight sand as former state;To containing Oily tight sand former state saturation octamethylcy-clotetrasiloxane, saturated sample is tested using nuclear magnetic resonance freeze-thaw method;Contained by above-mentioned Oily tight sand calculates the pore-size distribution of oil-containing tight sand with the data of oil-containing tight sand saturated sample as former state.
2. the measuring method of oil-containing tight sand pore-size distribution feature according to claim 1, it is characterised in that described right The step of oil-containing tight sand sample is pre-processed includes:Mechanical crushing is carried out to oil-containing tight sand sample, 20-35 was taken Purpose sample is dried, and is weighed, and sample is loaded into chromatogram bottle after record mass M.
3. the measuring method of oil-containing tight sand pore-size distribution feature according to claim 2, it is characterised in that the machine Tool is crushed to crush using agate mortar, and the drying is drying in vacuum tank.
4. the measuring method of oil-containing tight sand pore-size distribution feature according to claim 1, it is characterised in that utilize core The step of magnetic resonance freeze-thaw method tests oil-containing tight sand former state includes:Determined using the strong sample of nuclear magnetic signal in permanent magnet Frequency of heart, corrects radio frequency signal frequency, determines radio frequency pulsewidth;Alcohol is tested using nuclear magnetic resonance freeze-thaw method, nuclear magnetic resonance is determined Signal intensity temperature correction coefficient λ;Determine the relation of NMR signal intensity and octamethylcy-clotetrasiloxane content;It is determined that containing The nuclear magnetic resonance experiment parameter of oily tight sand, design temperature plan determines oil-containing tight sand using nuclear magnetic resonance freeze-thaw method As former state.
5. the measuring method of oil-containing tight sand pore-size distribution feature according to claim 4, it is characterised in that utilize core Magnetic resonance freeze-thaw method tests alcohol, determines NMR signal strength temperature correction factor λ to test alcohol at -30 DEG C~20 DEG C In the range of under different temperatures standard specimen signal intensity, according to formula (1), calculate λ, the formula (1) is
<mrow> <msub> <mi>SI</mi> <mi>S</mi> </msub> <mo>=</mo> <msub> <mi>SI</mi> <mi>K</mi> </msub> <mfrac> <mrow> <msub> <mi>T</mi> <mi>K</mi> </msub> <mrow> <mo>(</mo> <mi>&amp;alpha;</mi> <mo>+</mo> <mi>&amp;beta;</mi> <mo>&amp;CenterDot;</mo> <msub> <mi>T</mi> <mi>K</mi> </msub> <mo>)</mo> </mrow> </mrow> <mrow> <msub> <mi>T</mi> <mi>S</mi> </msub> <mrow> <mo>(</mo> <mi>&amp;alpha;</mi> <mo>+</mo> <mi>&amp;beta;</mi> <mo>&amp;CenterDot;</mo> <msub> <mi>T</mi> <mi>S</mi> </msub> <mo>)</mo> </mrow> </mrow> </mfrac> <mo>=</mo> <msub> <mi>SI</mi> <mi>K</mi> </msub> <mfrac> <mrow> <msub> <mi>T</mi> <mi>K</mi> </msub> <mrow> <mo>(</mo> <mi>&amp;lambda;</mi> <mo>+</mo> <msub> <mi>T</mi> <mi>K</mi> </msub> <mo>)</mo> </mrow> </mrow> <mrow> <msub> <mi>T</mi> <mi>S</mi> </msub> <mrow> <mo>(</mo> <mi>&amp;lambda;</mi> <mo>+</mo> <msub> <mi>T</mi> <mi>S</mi> </msub> <mo>)</mo> </mrow> </mrow> </mfrac> <mo>-</mo> <mo>-</mo> <mo>-</mo> <mrow> <mo>(</mo> <mn>1</mn> <mo>)</mo> </mrow> <mo>,</mo> </mrow>
SI is NMR signal intensity in formula (1), and T is temperature, and α and β is resistance parameter, and λ is NMR signal intensity Temperature correction coefficient.
6. the measuring method of oil-containing tight sand pore-size distribution feature according to claim 1, it is characterised in that to oil-containing The step of tight sand former state saturation octamethylcy-clotetrasiloxane, to be handled using vacuum saturation device, testing sample is put It is placed in vacuum tank, vacuumizes 12h;Prestox ring is added in the chromatogram bottle for vacuumizing rear oil-containing tight sand former state to being placed with Tetrasiloxane, balances 6h;Chromatogram bottle is centrifuged into 2h.
7. the measuring method of oil-containing tight sand pore-size distribution feature according to claim 6, it is characterised in that utilize core Setting and test former state identical experiment parameter and identical temperature plan when magnetic resonance freeze-thaw method tests saturated sample.
8. the measuring method of oil-containing tight sand pore-size distribution feature according to claim 1, it is characterised in that the meter Calculating the specific steps of the pore-size distribution of oil-containing tight sand includes:
The data of corresponding temperature point after correcting as former state are subtracted using the data of each temperature spot of saturated sample;By NMR signal Intensity, using NMR signal strength temperature correction factor λ, is modified;After each temperature spot amendment of saturated sample Data subtract as former state correct after corresponding temperature point data;Contained using NMR signal intensity and octamethylcy-clotetrasiloxane Relation between amount, signal intensity is converted into the liquid volume of octamethylcy-clotetrasiloxane;Utilize gibbs Thomas's equation By temperature conversion pore size, the correlation in pore volume and aperture is obtained;According to pore volume and the relation in aperture, calculate and paint The differential pore size distribution curve and logarithmic differentiation pore size distribution curve of sample preparation product.
9. the measuring method of oil-containing tight sand pore-size distribution feature according to claim 8, it is characterised in that described micro- The calculation formula of point pore-size distribution and logarithmic differentiation pore-size distribution is:
<mrow> <msub> <mi>P</mi> <mi>d</mi> </msub> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> <mo>=</mo> <mfrac> <mrow> <mi>d</mi> <mi>V</mi> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> </mrow> <mrow> <mi>d</mi> <mi>D</mi> </mrow> </mfrac> <mo>=</mo> <mfrac> <mrow> <mi>d</mi> <mi>V</mi> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> </mrow> <mrow> <mi>d</mi> <mi>T</mi> </mrow> </mfrac> <mo>&amp;CenterDot;</mo> <mfrac> <mrow> <mi>d</mi> <mi>T</mi> </mrow> <mrow> <mi>d</mi> <mi>D</mi> </mrow> </mfrac> <mo>=</mo> <mfrac> <mrow> <mi>d</mi> <mi>V</mi> <mrow> <mo>(</mo> <mi>T</mi> <mo>)</mo> </mrow> </mrow> <mrow> <mi>d</mi> <mi>T</mi> </mrow> </mfrac> <mo>&amp;CenterDot;</mo> <mfrac> <msub> <mi>K</mi> <mrow> <mi>G</mi> <mi>T</mi> </mrow> </msub> <msup> <mi>D</mi> <mn>2</mn> </msup> </mfrac> <mo>-</mo> <mo>-</mo> <mo>-</mo> <mrow> <mo>(</mo> <mn>2</mn> <mo>)</mo> </mrow> </mrow>
<mrow> <msub> <mi>P</mi> <mi>log</mi> </msub> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> <mo>=</mo> <mfrac> <mrow> <mi>d</mi> <mi>V</mi> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> </mrow> <mrow> <mi>d</mi> <mi>log</mi> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> </mrow> </mfrac> <mo>=</mo> <mfrac> <mrow> <mi>d</mi> <mi>V</mi> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> </mrow> <mrow> <mi>d</mi> <mi>D</mi> </mrow> </mfrac> <mo>&amp;CenterDot;</mo> <mfrac> <mrow> <mi>d</mi> <mi>D</mi> </mrow> <mrow> <mi>d</mi> <mi>log</mi> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> </mrow> </mfrac> <mo>=</mo> <msub> <mi>P</mi> <mi>d</mi> </msub> <mrow> <mo>(</mo> <mi>D</mi> <mo>)</mo> </mrow> <mo>&amp;CenterDot;</mo> <mi>D</mi> <mo>&amp;CenterDot;</mo> <mi>l</mi> <mi>n</mi> <mrow> <mo>(</mo> <mn>10</mn> <mo>)</mo> </mrow> <mo>-</mo> <mo>-</mo> <mo>-</mo> <mrow> <mo>(</mo> <mn>3</mn> <mo>)</mo> </mrow> <mo>,</mo> </mrow>
V is pore volume in formula (2)-(3);D is aperture;T is temperature;KGTFor gibbs Thomas's constant.
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