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    • 4. 发明授权
    • Method of evaluating the capillary pressure curve of an underground deposit rocks based on rock cuttings measurements
    • 基于岩石测量的地下沉积岩的毛细管压力曲线评估方法
    • US07092822B2
    • 2006-08-15
    • US10514414
    • 2003-05-14
    • Roland LenormandPatrick EgermannDaniel Longeron
    • Roland LenormandPatrick EgermannDaniel Longeron
    • G01N15/08G01N33/24
    • G01N13/02G01N15/08G01N15/0826G01N33/24G01N2015/0873
    • A method of evaluating the capillary pressure curve of rocks of an underground reservoir from measurements on rock debris or fragments such as cuttings from the reservoir, over the total saturation range of these rocks, within a short period and at a low cost, from these measurements is disclosed. The method comprises measuring the permeability k of the debris, measuring the capillary pressure curve Pc as a function of the saturation of these fragments initially saturated with a fluid (brine for example) by subjecting them to centrifugation, and parametrizing a capillary pressure curve Pc satisfying empirical relations depending on adjustable parameters, constrained to adjust to an asymptotic part of the capillary curve measured by centrifugation, and to the value of permeability k measured on the cuttings, so as to obtain the whole of the capillary pressure curve. Applications include hydrocarbon reservoir evaluation.
    • 从这些测量结果可以看出,在这些岩石的总饱和度范围内,在这些岩石的总饱和度范围内,对来自储层的岩石碎屑或碎片,如岩石碎屑或碎屑的测量值,在短时间内和低成本下,对地下水库岩石的毛细管压力曲线进行评估。 被披露。 该方法包括测量碎片的渗透性k,测量毛细管压力曲线Pc作为最初饱和的流体(例如盐水)的这些碎片的饱和度的函数,通过使它们离心,并且对毛细管压力曲线Pc进行参数化,满足 经验关系取决于可调参数,受限于通过离心法测量的毛细管曲线的渐近部分,以及在切屑上测量的渗透率k值,以获得毛细管压力曲线的整体。 应用包括油气藏评估。
    • 6. 发明授权
    • Device for petrophysical measurement and implementation method
    • 岩石物理测量与实施方法
    • US5610524A
    • 1997-03-11
    • US526229
    • 1995-09-11
    • Daniel LongeronMarc Fleury
    • Daniel LongeronMarc Fleury
    • G01N15/08G01N27/04G01N33/24G01V3/02
    • G01N27/041G01N15/082G01N33/241
    • The device includes a cell for a sample, delimited lengthwise by two end pieces (7, 8) and laterally by a deformable sheath (17). The end pieces are traversed by channels (14) which place their grooved inside faces in communication respectively with two sources (14, 15) at an adjustable pressure delivering respectively a first and a second fluid. Between the inside faces of the end pieces and the sample, two semipermeable membranes (12, 13) are disposed, which are permeable respectively to the first and to the second fluid. Electrodes (18, 19) are placed inside sheath (17) in contact with the sample and connected to a system (24) for measuring the electrical conductivity of the sample. The cell is placed in a body (1) associated with pressure means (28) for applying a confinement pressure to sheath (17) and membranes (12, 13). The device is designed to operate at relatively high temperatures.
    • 该装置包括用于样品的细胞,纵向由两个端部片(7,8)限定,并且由可变形的护套(17)侧向限定。 端部件被通道(14)穿过,通道(14)将沟槽的内表面分别与两个源(14,15)连通,分别以可调节的压力输送第一和第二流体。 在端片和样品的内表面之间设置有分别可渗透到第一和第二流体的两个半透膜(12,13)。 将电极(18,19)放置在与样品接触的护套(17)内,并连接到用于测量样品的电导率的系统(24)。 将电池放置在与压力装置(28)相关联的主体(1)中,用于向护套(17)和膜(12,13)施加约束压力。 该器件设计为在较高温度下工作。
    • 7. 发明授权
    • Method and device for evaluating physical parameters of an underground deposit from rock cuttings sampled therein
    • 用于评估其中采样的岩屑的地下沉积物的物理参数的方法和装置
    • US07131317B2
    • 2006-11-07
    • US10505006
    • 2003-02-19
    • Roland LenormandPatrick EgermannDaniel Longeron
    • Roland LenormandPatrick EgermannDaniel Longeron
    • G01N15/08
    • G01N15/0826G01N15/088G01N2015/0833G01N2015/0873
    • A method and device evaluate simultaneously, with the same equipment, physical parameters such as the absolute permeability and the porosity of fragments taken from a fragmented natural or artificial porous medium. The porosity of the fragments is measured by means of helium pressure tests according to a protocol known in the art. The chamber (1) containing the fragments is communicated with a tank (11) whose volume is also known and containing helium at a known pressure. At pressure balance, the value of the solid volume can be deduced. The rock envelope volume and the fragments mass are also measured. Combining these measurements allows to determine the porosity of the samples and the density of the rock. Their permeability is then measured by immersing them in a viscous fluid and by communicating the chamber with viscous fluid at a determined pressure contained in a vessel (9) so as to compress the gas trapped in the pores of the rock, according to two different protocols. The values of the physical parameters are determined by modelling the evolution of the pressure or of the volume in the chamber and by means of an iterative adjustment.
    • 一种方法和装置用相同的设备同时评价物理参数,例如从碎片天然或人造多孔介质中获取的碎片的绝对渗透性和孔隙率。 通过根据本领域已知的方案的氦压力测试来测量碎片的孔隙率。 含有碎片的室(1)与体积已知的罐(11)连通,并且在已知压力下含有氦。 在压力平衡下,可以推导出固体体积的值。 还测量了岩石体积和碎片质量。 结合这些测量可以确定样品的孔隙度和岩石的密度。 然后通过将它们浸入粘性流体中并通过将容器与包含在容器(9)中的确定压力的粘性流体连通来测量其渗透性,以便根据两种不同的方案压缩被捕获在岩石孔中的气体 。 物理参数的值通过对室中的压力或体积的演变进行建模并通过迭代调整来确定。
    • 9. 发明申请
    • Method and device for evaluating physical parameters of an underground deposit from rock cuttings sampled therein
    • 用于评估其中采样的岩屑的地下沉积物的物理参数的方法和装置
    • US20050178189A1
    • 2005-08-18
    • US10505006
    • 2003-02-19
    • Roland LenormandPatrick EgermannDaniel Longeron
    • Roland LenormandPatrick EgermannDaniel Longeron
    • G01N15/08
    • G01N15/0826G01N15/088G01N2015/0833G01N2015/0873
    • Method and device for evaluating simultaneously, with the same equipment, physical parameters such as the absolute permeability and the porosity of fragments taken from a fragmented natural or artificial porous medium The porosity of the fragments is measured by means of helium pressure tests according to a protocol known in the art. The chamber (1) containing the fragments is communicated with a tank (11) whose volume is also known and containing helium at a known pressure. At pressure balance, the value of the solid volume can be deduced. The rock envelope volume and the fragments mass are also measured. Combining these measurements allows to determine the porosity of the samples and the density of the rock. Their permeability is then measured by immersing them in a viscous fluid and by communicating the chamber with viscous fluid at a determined pressure contained in a vessel (9) so as to compress the gas trapped in the pores of the rock, according to two different protocols. The values of the physical parameters are determined by modelling the evolution of the pressure or of the volume in the chamber and by means of an iterative adjustment. Applications: petrophysical measurements from drilling cuttings or crushed cores for example.
    • 用相同设备同时评估从碎片天然或人造多孔介质中获取的碎片的绝对渗透性和孔隙度的物理参数的方法和装置通过根据方案的氦气压力测试来测量碎片的孔隙率 本领域已知 含有碎片的室(1)与体积已知的罐(11)连通,并且在已知压力下含有氦。 在压力平衡下,可以推导出固体体积的值。 还测量了岩石体积和碎片质量。 结合这些测量可以确定样品的孔隙度和岩石的密度。 然后通过将它们浸入粘性流体中并通过将容器与包含在容器(9)中的确定压力的粘性流体连通来测量其渗透性,以便根据两种不同的方案压缩被捕获在岩石孔中的气体 。 物理参数的值通过对室中的压力或体积的演变进行建模并通过迭代调整来确定。 应用范围:例如来自钻屑或碎芯的岩石物理测量。