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    • 1. 发明授权
    • Cryogenic thermometer employing molecular luminescence
    • 使用分子发光的低温温度计
    • US4791585A
    • 1988-12-13
    • US706331
    • 1985-02-27
    • August H. MakiMohammad-Reza Taherian
    • August H. MakiMohammad-Reza Taherian
    • G01K11/32G01J5/00G01K11/00
    • G01K11/3213
    • A cryogenic thermometer using molecular luminescence determines temperature. A sensor material is used which is capable of emitting radiant energy from a spin multiplet when excited, the excited state being characterized by a large zero field splitting (ZFS), and in which two of the sublevels split by the ZFS are radiative in the visible or near infrared region and are optically resolvable from each other. Spin-lattice relaxation rates between the sublevels are much larger than the sublevel decay rates to other states in order that their populations remain close to thermal equilibrium during optical pumping. The relative intensity of the two bands of radiation is determined and the temperature calculated therefrom. Xanthione (XS) dissolved in n-hexane may be used as a sensor material in the optimum range of 3 to 10K, with estimated precision varying between 0.4 mK and 3.0 mK within this range. Other disclosed sensor materials should allow extension of the optimal range to about 20K on the high end and somewhat below 2K on the low end.
    • 使用分子发光的低温温度测定温度。 使用传感器材料,其能够在被激发时从自旋多重峰发射辐射能,所述激发态的特征在于大的零场分裂(ZFS),其中由ZFS分裂的两个子级在辐射可见 或近红外区域并且彼此可光学地解析。 子层之间的自旋晶格弛豫速率比其他状态的次级衰减速率大得多,以便在光泵浦期间它们的群体保持接近热平衡。 确定两个辐射带的相对强度,并由此计算温度。 溶解在正己烷中的Xanthione(XS)可以用作3至10K的最佳范围内的传感器材料,估计精度在该范围内在0.4mK和3.0mK之间变化。 其他公开的传感器材料应允许将最佳范围扩展到高端约20K,低端稍微低于2K。
    • 2. 发明授权
    • Method and device for complex permittivity measurements as a function of frequency
    • 作为频率的函数的复介电常数测量的方法和装置
    • US07642785B2
    • 2010-01-05
    • US11241185
    • 2005-09-30
    • Tarek M. HabashyNikita V. SeleznevMohammad-Reza TaherianAustin J. Boyd
    • Tarek M. HabashyNikita V. SeleznevMohammad-Reza TaherianAustin J. Boyd
    • G01V3/00
    • G01R27/2647
    • An apparatus for use in a system that includes a network analyzer for determining a property, such as dielectric permittivity of a sample material as a function of frequency, the apparatus including: a cylindrical chamber for receiving the sample; a coaxial connector having a first relatively small diameter end coupleable with the analyzer and a second relatively large diameter end communicating with a side of the cylindrical chamber, the connector having inner and outer coaxial conductors; the inner conductor of the connector having a diameter that tapers outwardly from the first end to the second end, and the outer conductor of the connector having an inner surface whose diameter tapers outwardly from the first end to the second end. The chamber can accommodate relatively large samples, such as standard earth formation coring samples.
    • 一种用于系统的装置,包括用于确定作为频率的函数的样品材料的介电常数的性质的网络分析仪,所述装置包括:用于接收样品的圆柱形室; 同轴连接器,其具有与分析器相连的第一相对较小直径的端部,以及与圆柱形腔室的一侧连通的第二较大直径端,该连接器具有内部和外部同轴导体; 连接器的内部导体具有从第一端向第二端向外逐渐变细的直径,并且连接器的外部导体具有一个内表面,该内表面的直径从第一端向第二端向外逐渐变细。 该室可以容纳相对大的样品,例如标准的地层取芯样品。
    • 3. 发明申请
    • Method and device for complex permittivity measurements as a function of frequency
    • 作为频率的函数的复介电常数测量的方法和装置
    • US20070090846A1
    • 2007-04-26
    • US11241185
    • 2005-09-30
    • Tarek HabashyNikita SeleznevMohammad-Reza TaherianAustin Boyd
    • Tarek HabashyNikita SeleznevMohammad-Reza TaherianAustin Boyd
    • G01R27/00
    • G01R27/2647
    • An apparatus for use in a system that includes a network analyzer for determining a property, such as dielectric permittivity of a sample material as a function of frequency, the apparatus including: a cylindrical chamber for receiving the sample; a coaxial connector having a first relatively small diameter end coupleable with the analyzer and a second relatively large diameter end communicating with a side of the cylindrical chamber, the connector having inner and outer coaxial conductors; the inner conductor of the connector having a diameter that tapers outwardly from the first end to the second end, and the outer conductor of the connector having an inner surface whose diameter tapers outwardly from the first end to the second end. The chamber can accommodate relatively large samples, such as standard earth formation coring samples.
    • 一种用于系统的装置,包括用于确定作为频率的函数的样品材料的介电常数的性质的网络分析仪,所述装置包括:用于接收样品的圆柱形室; 同轴连接器,其具有与分析器相连的第一相对较小直径的端部,以及与圆柱形腔室的一侧连通的第二较大直径端,该连接器具有内部和外部同轴导体; 连接器的内部导体具有从第一端向第二端向外逐渐变细的直径,并且连接器的外部导体具有一个内表面,该内表面的直径从第一端向第二端向外逐渐变细。 该室可以容纳相对大的样品,例如标准的地层取芯样品。
    • 4. 发明授权
    • Method and apparatus for measuring nuclear magnetic resonance
    • 用于测量核磁共振的方法和装置
    • US6166543A
    • 2000-12-26
    • US936892
    • 1997-09-25
    • Abdurrahman SezginerPabitra N. SenMohammad Reza TaherianBoqin Sun
    • Abdurrahman SezginerPabitra N. SenMohammad Reza TaherianBoqin Sun
    • G01R33/44G01V3/32G01U3/00
    • G01V3/32G01N24/081
    • The present invention relates generally to an apparatus and method for measuring nuclear magnetic resonance properties of an earth formation traversed by a borehole by generating gradient-echoes. The measurement can be made while drilling or using a wireline tool. The apparatus applies a static magnetic field, B.sub.a, in a volume of the formation which polarizes the nuclei of hydrogenous connate fluids within the formation. The apparatus applies a second magnetic field, B.sub.b, in a volume of the formation. The magnetic fields B.sub.a and B.sub.b are substantially orthogonal in the volume of the formation. A change in the polarity of the magnetic field, B.sub.b, reverses the direction of precession of the nuclei thereby generating a train of gradient-echoes. Each gradient-echo signal is transformed into the frequency domain and the signal frequency is mapped to a radial position in the volume of the formation in order to generate an image of the formation. Various properties of the formation, such as the effective diffusion coefficient of the formation fluid, longitudinal relaxation time, spin--spin relaxation time, and porosity can be estimated from the train of gradient-echoes.
    • 本发明一般涉及通过产生梯度回波来测量由钻孔穿过的地层的核磁共振特性的装置和方法。 可以在钻孔或使用有线工具时进行测量。 该装置在地层的体积中施加静磁场Ba,其使地层内的含氢原生液体的核极化。 该装置在地层的体积中施加第二磁场Bb。 磁场Ba和Bb在地层的体积中基本正交。 磁场极性的变化Bb反转核的进动方向,从而产生一系列梯度回波。 每个梯度回波信号被变换成频域,并且信号频率被映射到地层体积中的径向位置,以便产生地层的图像。 可以从梯度回波序列估计地层的各种性质,例如地层流体的有效扩散系数,纵向松弛时间,自旋 - 自旋弛豫时间和孔隙度。