CN112129801A - A fast measurement method for layer-selective T2 relaxation spectrum of porous media - Google Patents
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Abstract
本发明公布了一种多孔介质的选层T2弛豫谱快速测试方法,通过设计具有选层功能的T2弛豫谱测试脉冲序列,在恒定选层梯度下,用CPMG脉冲序列同时对空间位置点进行选层编码,实现多孔介质中不同选层位置的核磁共振T2弛豫谱的测试分析,能够获取多孔介质不同位置的物性参数特征。
The invention discloses a fast measurement method for layer-selective T2 relaxation spectrum of porous media. By designing a T2 relaxation spectrum test pulse sequence with layer-selective function, under a constant layer-selective gradient, the CPMG pulse sequence is used to simultaneously measure spatial position points. The layer selection coding is performed to realize the test and analysis of the nuclear magnetic resonance T2 relaxation spectrum of different layer selection positions in the porous medium, and the physical parameter characteristics of different positions of the porous medium can be obtained.
Description
技术领域technical field
本发明属于核磁共振技术领域,涉及一种多孔介质的选层T2弛豫谱快速测试方法。The invention belongs to the technical field of nuclear magnetic resonance, and relates to a method for rapidly testing a layer-selective T2 relaxation spectrum of a porous medium.
背景技术Background technique
核磁共振T2弛豫谱技术具有快速、无损、无污染、一样多测试参数等优点,目前,其作为多孔介质的主要测试手段被广泛应用于石油勘探开发、煤层气赋存运移、水泥建筑材料分析、岩土冻土测试等方面,在核磁共振测试过程中,利用 CPMG核磁共振脉冲序列测试样品中流体产生的回波串信号,并对回波串信号进行数学反演运算得到T2弛豫谱,分析时样品被作为一个整体进行激发,同时根据核磁共振T2弛豫谱测试结果分析被测样品的孔隙度、渗透率、含油饱和度、含水饱和度、含气饱和度、可动流体分布以及动态驱替过程的分析等。Nuclear magnetic resonance T2 relaxation spectroscopy has the advantages of fast, non-destructive, pollution-free, and the same number of test parameters. At present, it is widely used as the main test method for porous media in petroleum exploration and development, coalbed methane occurrence and migration, and cement building materials. In the NMR test process, the CPMG NMR pulse sequence is used to test the echo train signal generated by the fluid in the sample, and the T2 relaxation spectrum is obtained by mathematical inversion of the echo train signal. , the sample is excited as a whole during the analysis, and the porosity, permeability, oil saturation, water saturation, gas saturation, movable fluid distribution, and Analysis of dynamic displacement process, etc.
多孔介质常常具有一定的非均质性,尤其是低孔隙度、低渗隙度的样品,其结构混乱复杂、层理叠加严重,在核磁共振T2弛豫谱的测试中,由于T2弛豫谱不具有空间信息,整块岩心的不均匀性常常被忽略,无法反映岩心内部巨大的差异性,难以精准描述岩心信息,因此,利用现有方法很难获得岩心不同位置的物性参数变化规律。Porous media often have a certain degree of heterogeneity, especially for samples with low porosity and low porosity, which have a chaotic and complex structure and serious bedding stacking. Without spatial information, the inhomogeneity of the entire core is often ignored, which cannot reflect the huge differences inside the core, and it is difficult to accurately describe the core information. Therefore, it is difficult to obtain the variation law of physical parameters at different positions of the core using the existing methods.
发明内容SUMMARY OF THE INVENTION
为了克服上述现有核磁共振T2弛豫谱测试技术不具有空间信息、难以获得岩心不同位置的物性参数变化特征的技术问题,本发明提供一种多孔介质(如岩心测试样品)选层的核磁共振T2弛豫谱快速测试方法,通过设计沿样品轴向的频率编码梯度,实现多孔介质不同空间位置选层的核磁共振T2弛豫谱分析,获得多孔介质不同位置的物性参数变化特征。本发明的技术方案是:In order to overcome the above-mentioned technical problems that the existing nuclear magnetic resonance T2 relaxation spectrum testing technology has no spatial information and is difficult to obtain the physical property parameter variation characteristics of different positions of the core, the present invention provides a nuclear magnetic resonance method for layer selection of porous media (such as core test samples). The rapid T2 relaxation spectrum measurement method realizes the NMR T2 relaxation spectrum analysis of the selected layers in different spatial positions of the porous medium by designing the frequency encoding gradient along the sample axis, and obtains the variation characteristics of physical parameters in different positions of the porous medium. The technical scheme of the present invention is:
一种多孔介质选层T2弛豫谱快速测试方法,通过在一个恒定选层梯度下,用CPMG(Carr-Purcell-Meiboom-Gill)脉冲序列同时对空间位置点进行选层编码来减少扫描时间。A fast measurement method for layer-selective T2 relaxation spectrum of porous media, which reduces scanning time by simultaneously performing layer-selective coding on spatial position points with CPMG (Carr-Purcell-Meiboom-Gill) pulse sequence under a constant layer-selective gradient.
本发明提供的快速选层T2谱的测试方法用于测试多孔介质测试样品不同选层位置的T2弛豫谱,包括如下步骤:The method for testing the T2 spectrum of rapid layer selection provided by the present invention is used to test the T2 relaxation spectrum of different layer selection positions of a porous medium test sample, and includes the following steps:
1)获取多孔介质测试样品选层T2脉冲序列;1) Obtain the layer selection T2 pulse sequence of the porous medium test sample;
多孔介质的选层T2脉冲序列如图1所示,包括RF(Radio Frequency,射频)通道、GREAD(Gradient in Read,读取梯度)梯度通道、READ采集通道的核磁共振波形图。具体实施时,多孔介质的选层为岩心测试样品的不同位置切片。The layer-selective T2 pulse sequence of the porous medium is shown in FIG. 1 , which includes an NMR waveform diagram of an RF (Radio Frequency, radio frequency) channel, a GREAD (Gradient in Read, gradient in read) gradient channel, and a READ acquisition channel. In specific implementation, the layer selection of the porous medium is sliced at different positions of the core test sample.
2)执行选层T2脉冲序列,单次扫描开始,单次扫描包括步骤2)-7)。在 GREAD梯度通道上,向多孔介质测试样品施加一个恒定幅度的频率编码梯度,通过该梯度沿测试样品长度方向进行一维选层编码。2) Execute the layer-selecting T2 pulse sequence, and start a single scan, which includes steps 2)-7). On the GREAD gradient channel, a constant-amplitude frequency-encoding gradient is applied to the porous medium test sample, through which one-dimensional layer-selective encoding is performed along the length of the test sample.
a)通常,梯度是一个三维向量,但在本发明中,我们只需要沿测试样本轴向(长度方向)的一维选层结果,所以本发明中GREAD梯度选取的是测试样本的轴向。a) Usually, the gradient is a three-dimensional vector, but in the present invention, we only need the one-dimensional layer selection result along the axial (length direction) of the test sample, so the GREAD gradient in the present invention selects the axial direction of the test sample.
b)为了避免梯度产生涡流干扰测试样品产生的核磁共振信号,本发明采用斜坡上升形状的梯度,梯度爬升至预设幅度G(G取值范围为 10-300mT/m,如预设G=60mT/m)后恒定保持不变,该梯度将一直持续,直到单次扫描结束。b) In order to avoid the eddy current generated by the gradient from interfering with the nuclear magnetic resonance signal generated by the test sample, the present invention adopts a gradient with a ramp-up shape, and the gradient climbs to a preset amplitude G (the value range of G is 10-300mT/m, such as the preset G=60mT /m), the gradient will continue until the end of a single sweep.
3)在RF射频通道上,向测试样品施加90°射频脉冲。3) On the RF radio frequency channel, apply a 90° radio frequency pulse to the test sample.
a)90°射频脉冲为无形状的硬脉冲,持续时间为t90,取值11us。a) The 90° radio frequency pulse is a shapeless hard pulse, the duration is t 90 , and the value is 11us.
b)90°射频脉冲将宏观磁化强度矢量M0扳转90°,使得宏观磁化强度矢量M0处于横向平面。b) The 90° radio frequency pulse rotates the macroscopic magnetization vector M 0 by 90°, so that the macroscopic magnetization vector M 0 is in the transverse plane.
4)在RF射频通道上,向测试样品施加180°射频脉冲,将处于横向平面的宏观磁化强度矢量M0重聚相。4) On the RF radio frequency channel, apply a 180° radio frequency pulse to the test sample to rephase the macroscopic magnetization vector M 0 in the transverse plane.
a)180°射频脉冲为无形状的硬脉冲,持续时间为t180,取值22us。a) The 180° radio frequency pulse is a shapeless hard pulse with a duration of t 180 and a value of 22us.
b)从步骤3)中“在RF射频通道上施加的90°射频脉冲”的中心开始,至步骤4中“在RF射频通道上施加的180°射频脉冲”的中心为止,持续时间为tau,tau可取值500us;b) from the center of the "90° radio frequency pulse applied on the RF channel" in step 3) to the center of the "180° radio frequency pulse applied on the RF channel" in
5)在READ采集通道,采集到一串离散的自旋回波信号。5) In the READ collection channel, a series of discrete spin echo signals are collected.
a)该信号为测试样品的核磁共振自旋回波信号,是由于90°射频脉冲与180°射频脉冲作用在测试样品的含氢质子自旋系统上产生的,自旋回波信号的幅度值有由弱变强再变弱的特点。a) This signal is the NMR spin echo signal of the test sample, which is generated by the action of the 90° radio frequency pulse and the 180° radio frequency pulse on the hydrogen-containing proton spin system of the test sample. The amplitude of the spin echo signal is determined by Weakness becomes stronger and weaker again.
b)该信号的采集过程是离散采集,采集间隔为DW,采集点数为SI,整个采集过程持续时间为DW*SI。DW范围为1-40us;SI范围为16- 256。b) The acquisition process of the signal is discrete acquisition, the acquisition interval is DW, the number of acquisition points is SI, and the duration of the entire acquisition process is DW*SI. DW range is 1-40us; SI range is 16-256.
c)从步骤4中“在RF射频通道上施加的180°射频脉冲”的中心开始,至步骤5中“在READ采集通道上的信号采集”的中心为止,整个时序持续时间为tau;c) Starting from the center of "180° radio frequency pulse applied on the RF radio frequency channel" in
6)重复步骤4)、5),重复循环N次,循环的时间间隔为2*tau。N取值范围为256-25600。6) Repeat steps 4) and 5), repeat the cycle N times, and the time interval of the cycle is 2*tau. The value range of N is 256-25600.
a)在步骤6)的N次重复循环中,在RF射频通道上循环施加的180°射频脉冲的循环时间间隔为2*tau。a) In the N repeated cycles of step 6), the cycle time interval of the 180° radio frequency pulses cyclically applied on the RF radio frequency channel is 2*tau.
b)在步骤6)的N次重复循环中,在READ采集通道上循环采集到一串离散的自旋回波信号的循环时间间隔为2*taub) In the N repeated cycles of step 6), the cycle time interval of cyclically collecting a series of discrete spin echo signals on the READ acquisition channel is 2*tau
7)关闭GREAD梯度通道,单次扫描结束。7) Close the GREAD gradient channel, and the single scan ends.
a)在READ采集通道上依次将采集得到N串离散的自旋回波信号,每串离散信号的时间间隔为2*tau,每串离散信号的点数为SI;a) On the READ acquisition channel, sequentially acquire N series of discrete spin echo signals, the time interval of each series of discrete signals is 2*tau, and the number of points of each series of discrete signals is SI;
b)在READ采集通道中,最终将采集得到SI*N个信号幅度值,得到一组回波串信号S_1(n,tau),其中1≤n≤N。b) In the READ acquisition channel, SI*N signal amplitude values are finally acquired, and a set of echo train signals S_1(n, tau) is obtained, where 1≤n≤N.
8)循环重复步骤2)-7)M次,重复执行单次扫描。M取值范围为1-32。8) Repeat steps 2)-7) M times cyclically, and perform a single scan repeatedly. The value range of M is 1-32.
a)在READ采集通道中,得到M组回波串信号S_m(n,tau),其中1≤ m≤M。a) In the READ acquisition channel, M groups of echo train signals S_m(n, tau) are obtained, where 1≤m≤M.
b)对M组回波串信号S_m(n,tau)进行信号累加,得到累加回波串信号S(n,tau)。b) Perform signal accumulation on M groups of echo train signals S_m(n, tau) to obtain accumulated echo train signals S(n, tau).
9)对步骤8)得到的回波串信号S(n,tau)进行核磁共振数据处理。9) Perform nuclear magnetic resonance data processing on the echo train signal S(n, tau) obtained in step 8).
a)首先得到不同选层的回波串信号ρ(z,n*tau)。其中z为选层方向坐标。a) First, the echo train signals ρ(z, n*tau) of different selected layers are obtained. Where z is the direction coordinate of the selected layer.
b)最后得到选层T2弛豫谱P(z,T2)。b) Finally, the layer-selected T2 relaxation spectrum P(z, T 2 ) is obtained.
通过上述步骤,即实现多孔介质选层的核磁共振T2弛豫谱快速测试。Through the above steps, the rapid test of the nuclear magnetic resonance T2 relaxation spectrum of the layer selection of the porous medium is realized.
与现有技术相比,本发明的有益效果是:Compared with the prior art, the beneficial effects of the present invention are:
针对现有技术仅能分析多孔介质统计T2弛豫谱,无法分析各个异性、非均匀性对多孔介质样品不同位置的物性参数分析的功能,本发明方法通过设计具有选层功能的T2弛豫谱测试脉冲序列,实现了多孔介质中不同位置的核磁共振T2 弛豫谱的测试分析,能够获取多孔介质不同位置的物性参数特征。In view of the fact that the prior art can only analyze the statistical T2 relaxation spectrum of porous media, but cannot analyze the physical property parameters of different positions of the porous media sample by anisotropy and non-uniformity, the method of the present invention designs a T2 relaxation spectrum with layer selection function. The test pulse sequence realizes the test and analysis of the nuclear magnetic resonance T2 relaxation spectrum at different positions in the porous medium, and can obtain the physical property parameters of the different positions of the porous medium.
附图说明Description of drawings
图1是本发明设计的选层T2脉冲序列。Fig. 1 is the layer-selective T2 pulse sequence designed by the present invention.
图2是本发明实施例中待测样品的选层示意图。FIG. 2 is a schematic diagram of layer selection of a sample to be tested in an embodiment of the present invention.
图3是本发明实施例中在READ采集通道得到的回波串信号。FIG. 3 is an echo train signal obtained from a READ acquisition channel in an embodiment of the present invention.
图4是本发明实施例中数据处理后得到的不同选层的回波串信号。FIG. 4 shows echo train signals of different selected layers obtained after data processing in an embodiment of the present invention.
图5是本发明实施例中数据处理后得到的不同选层的T2弛豫谱。FIG. 5 is the T2 relaxation spectrum of different selected layers obtained after data processing in the embodiment 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.
本发明通过设计具有选层功能的T2弛豫谱测试脉冲序列,在恒定选层梯度下,用CPMG脉冲序列同时对空间位置点进行选层编码,实现了多孔介质中不同位置的核磁共振T2弛豫谱的测试分析,能够获取多孔介质不同位置的物性参数特征,用于多孔介质测试样品不同选层位置的T2弛豫谱。The invention realizes the nuclear magnetic resonance T2 relaxation of different positions in the porous medium by designing the T2 relaxation spectrum test pulse sequence with the function of layer selection, and using the CPMG pulse sequence to simultaneously perform layer selection coding on the spatial position points under the constant layer selection gradient. The test and analysis of the relaxation spectrum can obtain the physical parameter characteristics of different positions of the porous medium, which can be used for the T2 relaxation spectrum of the different layer selection positions of the porous medium test sample.
实施例选用了一块砂岩岩心作为多孔介质测试样品,孔隙度为15.8%,渗透率为8毫达西,岩心为直径25mm*50mm圆柱体形状。In the embodiment, a sandstone core is selected as the porous medium test sample, the porosity is 15.8%, the permeability is 8 millidarcy, and the core is in the shape of a cylinder with a diameter of 25mm*50mm.
使用蒸馏水(H2O)配置模拟地层水,然后按照SY/T5336规定的方法对岩心样品进行饱和。Use distilled water (H 2 O) to configure simulated formation water, and then saturate the core samples according to the method specified in SY/T5336.
1.测试样品准备。1. Test sample preparation.
a)使用有机溶剂对岩心进行洗油处理,使岩心荧光级别小于3级。a) Use organic solvent to wash the core with oil, so that the fluorescence level of the core is less than
b)将岩心在116℃条件下烘干至恒重,并放入干燥器中冷却至室温,将岩心样品置于真空条件下保持。b) Dry the core at 116°C to constant weight, put it in a desiccator to cool to room temperature, and keep the core sample under vacuum.
c)根据SY/T5336-2006规定,测试岩心氦气孔隙度为15.8%,渗透率为 8毫达西,岩心直径为25mm,长度为50mm。c) According to SY/T5336-2006, the helium porosity of the test core is 15.8%, the permeability is 8 millidarcy, the core diameter is 25mm, and the length is 50mm.
d)使用蒸馏水(H2O)配置模拟地层水,然后将模拟地层水按照 SY/T5336规定的方法抽真空保持,对岩心样品进行饱和处理。d) Use distilled water (H 2 O) to configure simulated formation water, then vacuum the simulated formation water according to the method specified in SY/T5336, and perform saturation treatment on core samples.
2.步骤3-步骤10采用核磁共振设备运行本发明提供的选层T2弛豫谱测试方法,核磁共振设备为某公司生产的核磁共振成像系统(SPEC系列),磁体为永磁体,场强1.0T。选层T2脉冲序列如图1所示,包括RF(Radio Frequency,射频)通道、GREAD(Gradient in Read,读取梯度)梯度通道、READ采集通道的核磁共振波形图。。2.
3.执行选层T2脉冲序列,单次扫描开始,单次扫描包括步骤3)-8)。在 GREAD梯度通道上,向测试样品施加一个恒定幅度的梯度,该梯度用于沿测试样本长度方向的一维选层编码。3. Execute the layer-selecting T2 pulse sequence, and start a single scan, which includes steps 3)-8). On the GREAD gradient channel, a gradient of constant magnitude is applied to the test sample for 1D layer-selective encoding along the length of the test sample.
a)通常,梯度是一个三维向量,但在本发明中,我们只需要沿测试样本轴向(长度方向)的一维选层结果,所以GREAD梯度选取的是测试样本的轴向。a) Usually, the gradient is a three-dimensional vector, but in the present invention, we only need the one-dimensional layer selection result along the axis (length direction) of the test sample, so the GREAD gradient selects the axis of the test sample.
b)本发明采用斜坡上升形状的梯度,梯度爬升至预设幅度G (G=60mT/m)后恒定保持不变,该梯度将一直持续,直到单次扫描结束。b) The present invention adopts a gradient in the shape of a ramp-up. The gradient climbs to a preset amplitude G (G=60mT/m) and remains constant. The gradient will continue until the end of a single scan.
4.在RF射频通道上,向测试样品施加90°射频脉冲。4. On the RF channel, apply a 90° RF pulse to the test sample.
a)90°射频脉冲为无形状的硬脉冲,持续时间为t90,取值11us。a) The 90° radio frequency pulse is a shapeless hard pulse, the duration is t 90 , and the value is 11us.
b)90°射频脉冲将宏观磁化强度矢量M0扳转90°,使得宏观磁化强度矢量M0处于横向平面。b) The 90° radio frequency pulse rotates the macroscopic magnetization vector M 0 by 90°, so that the macroscopic magnetization vector M 0 is in the transverse plane.
5.在RF射频通道上,向测试样品施加180°射频脉冲,将处于横向平面的宏观磁化强度矢量M0重聚相。5. On the RF radio frequency channel, apply a 180° radio frequency pulse to the test sample to rephase the macroscopic magnetization vector M 0 in the transverse plane.
a)180°射频脉冲为无形状的硬脉冲,持续时间为t180,取值22us。a) The 180° radio frequency pulse is a shapeless hard pulse with a duration of t 180 and a value of 22us.
b)从所述步骤4中“在RF射频通道上施加的90°射频脉冲”的中心开始,至步骤5中“在RF射频通道上施加的180°射频脉冲”的中心为止,整个时序持续时间为tau,tau可取值500us;b) From the center of the "90° RF pulse applied on the RF channel" in the
6.在READ采集通道,采集到一串离散的自旋回波信号。6. In the READ acquisition channel, a series of discrete spin echo signals are acquired.
a)该信号为测试样品的核磁共振自旋回波信号,是由于90°射频脉冲与180°射频脉冲作用在测试样品的含氢质子自旋系统上产生的,自旋回波信号的幅度值有由弱变强再变弱的特点。a) This signal is the NMR spin echo signal of the test sample, which is generated by the action of the 90° radio frequency pulse and the 180° radio frequency pulse on the hydrogen-containing proton spin system of the test sample. The amplitude of the spin echo signal is determined by Weakness becomes stronger and weaker again.
b)该信号的采集过程是离散采集,采集间隔为DW,采集点数为SI,整个采集过程持续时间为DW*SI。DW取值4us;SI取值16。b) The acquisition process of the signal is discrete acquisition, the acquisition interval is DW, the number of acquisition points is SI, and the duration of the entire acquisition process is DW*SI. The value of DW is 4us; the value of SI is 16.
c)从所述步骤5中“在RF射频通道上施加的180°射频脉冲”的中心开始,至步骤6中“在READ采集通道上的信号采集”的中心为止,整个时序持续时间为tauc) From the center of the "180° RF pulse applied on the RF channel" in the
7.重复步骤5、6,重复循环N次,循环的时间间隔为2*tau。N取值12800。7. Repeat steps 5 and 6, repeat the cycle N times, and the time interval of the cycle is 2*tau. The value of N is 12800.
a)在步骤7的N次重复循环中,在RF射频通道上循环施加的180°射频脉冲的循环时间间隔为2*tau。a) In the N repeated cycles of step 7, the cycle time interval of the 180° radio frequency pulses cyclically applied on the RF radio frequency channel is 2*tau.
b)在步骤7的N次重复循环中,在READ采集通道上循环采集到一串离散的自旋回波信号的循环时间间隔为2*taub) In the N repeated cycles of step 7, the cycle time interval of cyclically collecting a series of discrete spin echo signals on the READ acquisition channel is 2*tau
8.关闭GREAD梯度,单次扫描结束。8. Turn off the GREAD gradient and end a single scan.
a)在READ采集通道上依次将采集得到N串离散的自旋回波信号,每串离散信号的时间间隔为2*tau,每串离散信号的点数为SI;a) On the READ acquisition channel, sequentially acquire N series of discrete spin echo signals, the time interval of each series of discrete signals is 2*tau, and the number of points of each series of discrete signals is SI;
b)在READ采集通道中,最终将采集得到SI*N个信号幅度值,得到一组回波串信号S_1(n,tau),其中1≤n≤N。b) In the READ acquisition channel, SI*N signal amplitude values are finally acquired, and a set of echo train signals S_1(n, tau) is obtained, where 1≤n≤N.
9.重复步骤3-8,对所述时序重复循环M次,重复执行单次扫描。M取值 16。9. Repeat steps 3-8, repeat the cycle M times for the timing sequence, and perform a single scan repeatedly. M takes the value 16.
a)在READ采集通道中,得到M组回波串信号S_m(n,tau),其中 1≤m≤M。a) In the READ acquisition channel, M groups of echo train signals S_m(n, tau) are obtained, where 1≤m≤M.
b)对M组回波串信号S_m(n,tau)进行信号累加,得到累加回波串信号S(n,tau),如图3。b) Perform signal accumulation on M groups of echo train signals S_m(n, tau) to obtain the accumulated echo train signals S(n, tau), as shown in FIG. 3 .
10.对步骤9得到到的回波串信号S(n,tau)进行核磁共振数据处理。10. Perform nuclear magnetic resonance data processing on the echo train signal S(n, tau) obtained in step 9.
a)首先到不同选层的回波串信号ρ(z,n*tau),其中z为选层方向坐标。如图4。a) First to the echo train signals ρ(z, n*tau) of different selected slices, where z is the coordinate of the slice selection direction. Figure 4.
b)最后得到选层T2弛豫谱P(z,T2),如图5。b) Finally, the layer-selected T2 relaxation spectrum P(z, T 2 ) is obtained, as shown in Figure 5 .
下面对步骤10采用的核磁共振数据处理进行详细说明;.The NMR data processing used in step 10 will be described in detail below;
在READ采集通道的信号采集过程中,信号为S(n,tau),表示为式(1):In the signal acquisition process of the READ acquisition channel, the signal is S(n, tau), which is expressed as formula (1):
S(n,tau)=∫ρ(z,n*tau)exp[i2π(k-k0)z]dz (1)S(n,tau)=∫ρ(z,n*tau)exp[i2π(kk 0 )z]dz (1)
其中,in,
公式(1)中,S(n,tau)是采集的信号,z为选层方向坐标;i为复数;k为核磁共振K空间波矢量;k0为梯度导致的附加的波矢量;ρ(z,n*tau)是测试样本H核自旋激发得到的宏观磁化信号,作为选层方向(z)坐标和READ采集通道每次采集时刻(n*tau)的函数。公式(2)、(3)中,γ为旋磁比,G为步骤3梯度爬升至预设幅度后恒定保持不变对应的数值,t为采集时刻,t在READ采集通道每次采集开始时为零,然后增加到步骤6(b)的采集过程持续时间DW*SI, T为t最大值的一半。In formula (1), S(n, tau) is the acquired signal, z is the layer selection direction coordinate; i is a complex number; k is the nuclear magnetic resonance K space wave vector; k 0 is the additional wave vector caused by the gradient; ρ( z, n*tau) is the macroscopic magnetization signal obtained by the excitation of the H nuclear spins of the test sample, as a function of the layer selection direction (z) coordinate and each acquisition time (n*tau) of the READ acquisition channel. In formulas (2) and (3), γ is the gyromagnetic ratio, G is the corresponding value that remains constant after the gradient climbs to the preset amplitude in
在180°射频脉冲之间,波矢量(k-k0)消掉了,核磁共振信号达到了自旋回波的最大信号。在此之后,磁化再次散掉,并由180°射频脉冲开始产生下一个自旋回波的新过程。Between 180° RF pulses, the wave vector (kk 0 ) is eliminated, and the NMR signal reaches the maximum signal of the spin echo. After this, the magnetization dissipates again and a new process of generating the next spin echo is started by the 180° radio frequency pulse.
通过公式(1)的傅里叶反变换,即公式(4),可以得到ρ(z,n*tau)。Through the inverse Fourier transform of formula (1), namely formula (4), ρ(z, n*tau) can be obtained.
ρ(z,n*tau)=∫S(n,tau)exp[-i2π(k-k0)z]dk (4)ρ(z, n*tau)=∫S(n,tau)exp[-i2π(kk 0 )z]dk (4)
公式(1)与公式(4)为傅里叶变化对。Equation (1) and Equation (4) are pairs of Fourier transforms.
在实际应用中,如步骤6(b),信号S(n,tau)的采集过程是离散采集,所以公式(4)中的傅里叶反变换用快速傅里叶变换(FFT)算法来求解。In practical applications, as in step 6(b), the acquisition process of the signal S(n, tau) is discrete acquisition, so the inverse Fourier transform in formula (4) is solved by the fast Fourier transform (FFT) algorithm .
随后,将FFT求得的ρ(z,n*tau)作为选层方向(z)坐标的函数,对应的多个选层如图2所示(包括1选层~7选层)。我们可以分析ρ(z,n*tau)每个选层随时间(n*tau)的衰减,结果如图4所示。用一个指数函数拟合选层上每个点的衰减,如公式(5)。Subsequently, ρ(z, n*tau) obtained by FFT is used as a function of the layer selection direction (z) coordinate, and the corresponding multiple layers are shown in FIG. 2 (including
其中,P(z,T2)称为选层T2弛豫谱,1选层~7选层的T2弛豫谱如图5所示。Among them, P(z, T 2 ) is called the layer-selected T2 relaxation spectrum, and the T2 relaxation spectra of the 1-selected layer to the 7-selected layer are shown in FIG. 5 .
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.
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