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bulk susceptibility
相关语句
  磁化率
     BULK SUSCEPTIBILITY STUDY OF RARE EARTH IONS BY NMR TWO-SPECTROMETER METHOD
     用NMR双谱仪方法研究稀土离子的磁化率
短句来源
     In the present paper, the bulk susceptibility of rare earth iona in aqueous solutiona has been tmdied by NMR two-spectrometer method. The experimental relults are in good agreement with that predicted by Curie's law.
     用NMR双谱仪方法对0.1M氯化稀土水溶液的顺磁磁化率进行了研究,实验结果完全符合Cmrle定律。
短句来源
     The criteria for the reliable average orientaion of a principal axis of magnetic susceptibility have been made in reference to repeated measurement of the weak bulk susceptibility (<250× 10~(-6) SI) and weak AMS in a sample,i. c.
     对于磁化率和各向异度较低的样品(<250×10~(-6)SI),规定了重复测量数据可靠平均值的判定标准:(1)发散度系数Ci 小于20°;
短句来源
     Based on the properties of the four magnetic parameters of bulk susceptibility,saturation isothermal remanent magnetism,coercivity remanent and anhysteretic remanent mag-netism,this paper discusses the roles of these parameters and the problems they have solved in environmental investigation,and their applications abroad in recent years.
     根据体积磁化率、饱和等温剩磁、剩磁矫顽力、非磁滞剩磁四种主要磁性参数的特征,分别阐述了它们在环境研究中的作用及所解决的问题,并介绍了近年来国外在这方面的实际应用结果。
短句来源
  相似匹配句对
     The susceptibility of C.
     海南苏铁C.
短句来源
     Magnetic Susceptibility
     稀磁合金的磁化率
短句来源
     BULK SUSCEPTIBILITY STUDY OF RARE EARTH IONS BY NMR TWO-SPECTROMETER METHOD
     用NMR双谱仪方法研究稀土离子的磁化率
短句来源
     Bulk Amorphous Alloys
     大体积非晶态合金材料
短句来源
     Bulk Translation for scaffold
     脚手架整体平移技术
短句来源
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  bulk susceptibility
Both nucleation rates and bulk susceptibility measurements seem to support the prediction of the Ginzburg-Landau theories.
      
Corrections for bulk susceptibility give fairly good agreement with earlier values but make clear that existing susceptibility data are inadequate for making these corrections precisely.
      
The muonic Knight shift in CeRhSb exhibits similar features as the bulk susceptibility in the temperature range between 20 and 2 K.
      
It is confirmed that the temperature dependence of the Knight shift does not scale with the bulk susceptibility.
      
μ+ Knight shift measurements in the normal state of UPt3 show a temperature dependent shift Kμ which tracks the bulk susceptibility X.
      
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In the present paper, the bulk susceptibility of rare earth iona in aqueous solutiona has been tmdied by NMR two-spectrometer method. The experimental relults are in good agreement with that predicted by Curie's law.

用NMR双谱仪方法对0.1M氯化稀土水溶液的顺磁磁化率进行了研究,实验结果完全符合Cmrle定律。

Mylonites as products of ductile deformation, as well as the process of deformation and its genesis mechanism, have been studied intensively in recent years. The study of anisotropy of magnetic susceptibility(AMS)in rocks which was initiated in the 1960's has offered a new technique to research on the microstructures of rocks, especially on thosc of metamorphic rocks. A measurement has been made of the AMS in 54 specimens of mylonites, gneisses, and metagraywackes from the ductile deformation belts in an early...

Mylonites as products of ductile deformation, as well as the process of deformation and its genesis mechanism, have been studied intensively in recent years. The study of anisotropy of magnetic susceptibility(AMS)in rocks which was initiated in the 1960's has offered a new technique to research on the microstructures of rocks, especially on thosc of metamorphic rocks. A measurement has been made of the AMS in 54 specimens of mylonites, gneisses, and metagraywackes from the ductile deformation belts in an early Paleozoic collision zone between the NW. Fujian and SE. Zhejiang terrancs. The criteria for the reliable average orientaion of a principal axis of magnetic susceptibility have been made in reference to repeated measurement of the weak bulk susceptibility(<250×10~(-6)SI)and weak AMS in a sample, i.e.(1)the scattering parameter Ci<20°,(2)the quanta of magnetic lincation or foliation, i.e. the difference between K_1 and K_2 or bctween K_2 and K_3 should be five times higher than background noisc the instrument, It was thus found that the magnetic foliation is well developed but the magnetic lineation is weakly developed in mylonitic rocks, forming an oblate susceptibility amplitude ellipsoid. The converge orientations of minimum principal axes, which are poles of magnetic foliations(gently dipping toward SE with the stikes of NE), coincide basically with the normals to the schistocities of the rocks measured in the field, showing a feature of the NW-ward compressive stress. The strain of the rocks is characterized by the transformation of a simple shcar component to a pure shear strain in the ductile deformation belts as the depth of the belt increased. The schistocity structures in the rocks studied have devel. oped continuously with increase of deformation. Consequently, it is shown that the measurement on magnetic fabric in rocks provides some quick and precise informationabout the features of dynamics in the genesis process of rrylonites, including the techonis stress, strain mechanism and other techonic factors, which were associated with the collisional orogenic belt.

糜棱岩是韧性变形的产物,对其形成过程和机理近年来进行了多方面的研究。岩石磁化率各向异性研究。为岩石特别是变质岩的显微构造研究提供了更为有效的新兴工作方法。作者对在闽西北和浙东南地体碰撞带内的庆元济下和龙泉查田韧性剪切带中采集的54个下古生界糜棱岩及与其共生的片麻岩和变质硬砂岩样品进行了磁性组构——磁化率各向异性的实验测定。对于磁化率和各向异度较低的样品(<250×10~(-6)SI),规定了重复测量数据可靠平均值的判定标准:(1)发散度系数Ci小于20°;(2)磁性线理量或面理量应在仪器噪音水平(仪器空转时的信号)的五倍以上。测量结果发现这些糜棱岩的磁面理非常发育,而磁线理发育较弱,其磁化率量值椭球为压偏型,与磁性面理相垂直的最小磁化率主轴的分布收敛,并与野外实地测量岩石的片理(走向NE,向SE缓倾)所得到的片理法线产状基本吻合,显示了向NW方向的挤压应力场特征。剪切带中岩石的应变随着深度的增加,表现为由简单剪切作用向纯剪作用转化,因而其面状构造的发育不断增强。这些结果说明,岩石磁性组构的测定可为研究糜棱岩形成的构造应力作用和应变机制以及与糜棱岩形成有关的构造因素——碰撞造山带的动力学特征提供更为迅速而精确的...

糜棱岩是韧性变形的产物,对其形成过程和机理近年来进行了多方面的研究。岩石磁化率各向异性研究。为岩石特别是变质岩的显微构造研究提供了更为有效的新兴工作方法。作者对在闽西北和浙东南地体碰撞带内的庆元济下和龙泉查田韧性剪切带中采集的54个下古生界糜棱岩及与其共生的片麻岩和变质硬砂岩样品进行了磁性组构——磁化率各向异性的实验测定。对于磁化率和各向异度较低的样品(<250×10~(-6)SI),规定了重复测量数据可靠平均值的判定标准:(1)发散度系数Ci小于20°;(2)磁性线理量或面理量应在仪器噪音水平(仪器空转时的信号)的五倍以上。测量结果发现这些糜棱岩的磁面理非常发育,而磁线理发育较弱,其磁化率量值椭球为压偏型,与磁性面理相垂直的最小磁化率主轴的分布收敛,并与野外实地测量岩石的片理(走向NE,向SE缓倾)所得到的片理法线产状基本吻合,显示了向NW方向的挤压应力场特征。剪切带中岩石的应变随着深度的增加,表现为由简单剪切作用向纯剪作用转化,因而其面状构造的发育不断增强。这些结果说明,岩石磁性组构的测定可为研究糜棱岩形成的构造应力作用和应变机制以及与糜棱岩形成有关的构造因素——碰撞造山带的动力学特征提供更为迅速而精确的信息。

Mylonites as products of ductile deformation,as well as the process of deformation and its genesis mechanism,have been studied intensively in recent years.The study of anisotropy of magnetic susceptibility (AMS) in rocks which was initiated in the 1960's has offered a new technique to research on the microstructures of rocks,especially on those of metamorphic rocks.A measurement has been made of the AMS in 54 specimens of mylonites,gneisses,and metagraywackes from the ductile deformation belts in an early Paleozoic...

Mylonites as products of ductile deformation,as well as the process of deformation and its genesis mechanism,have been studied intensively in recent years.The study of anisotropy of magnetic susceptibility (AMS) in rocks which was initiated in the 1960's has offered a new technique to research on the microstructures of rocks,especially on those of metamorphic rocks.A measurement has been made of the AMS in 54 specimens of mylonites,gneisses,and metagraywackes from the ductile deformation belts in an early Paleozoic collision zone between the NW,Fujian and SE.Zhejiang terranes.The criteria for the reliable average orientaion of a principal axis of magnetic susceptibility have been made in reference to repeated measurement of the weak bulk susceptibility (<250× 10~(-6) SI) and weak AMS in a sample,i.c.(1) the scattering parameter Ci<20°,(2) the quanta of magnetic lineation or foliation,i.e.the difference between K_1 and K_2 or be- tween K_2 and K_3 should be five times higher than background noise the instrument,It was thus found that the magnetic foliation is well developed but the magnetic lincation is weakly developed in mylonitic rocks,forming an oblate susceptibility amplitude ellipsoid. The converge orientations of minimum principal axes,which are poles of magnetic foliations (gently dipping toward SE with the stikes of NE),coincide basically with the normals to the schistocitics of the rocks measured in the field,showing a feature of the NW-ward compressive stress.The strain of the rocks is characterized by the transforma- tion of a simple shear component to a pure shear strain in the ductile deformation belts as the depth of the belt increased.The schistocity structures in the rocks studied have devel- oped continuously with increase of deformation.Consequently,it is Shown that the measurement on magnetic fabric in rocks provides some quick and precise information about the features of dynamics in the genesis process of mylonites,including the techonis stress,strain mechanism and other techonic factors which were associated with the eollisional orogenic belt.

糜棱岩是韧性变形的产物,对其形成过程和机理近年来进行了多方面的研究.岩石磁化率各向异性研究,为岩石特别是变质岩的显微构造研究提供了更为有效的新兴工作方法.作者对在闽西北和浙东南地体碰撞带内的庆元济下和龙泉查田韧性剪切带中采集的54个下古生界糜棱岩及与其共生的片麻岩和变质硬砂岩样品进行了磁性组构——磁化率各向异性的实验测定.对于磁化率和各向异度较低的样品(<250×10~(-6)SI),规定了重复测量数据可靠平均值的判定标准:(1)发散度系数Ci 小于20°;(2)磁性线理量或面理量应在仪器噪音水平(仪器空转时的信号)的五倍以上.测量结果发现这些糜棱岩的磁面理非常发育,而磁线理发育较弱,其磁化率量值椭球为压偏型,与磁性面理相垂直的最小磁化率主轴的分布收敛,并与野外实地测量岩石的片理(走向 NE,向 SE 缓倾)所得到的片理法线产状基本吻合,显示了向 NW 方向的挤压应力场特征.剪切带中岩石的应变随着深度的增加,表现为由简单剪切作用向纯剪作用转化,因而其面状构造的发育不断增强.这些结果说明,岩石磁性组构的测定可为研究糜棱岩形成的构造应力作用和应变机制以及与糜棱岩形成有关的构造因素——碰撞造山带的动力学特征提供更为...

糜棱岩是韧性变形的产物,对其形成过程和机理近年来进行了多方面的研究.岩石磁化率各向异性研究,为岩石特别是变质岩的显微构造研究提供了更为有效的新兴工作方法.作者对在闽西北和浙东南地体碰撞带内的庆元济下和龙泉查田韧性剪切带中采集的54个下古生界糜棱岩及与其共生的片麻岩和变质硬砂岩样品进行了磁性组构——磁化率各向异性的实验测定.对于磁化率和各向异度较低的样品(<250×10~(-6)SI),规定了重复测量数据可靠平均值的判定标准:(1)发散度系数Ci 小于20°;(2)磁性线理量或面理量应在仪器噪音水平(仪器空转时的信号)的五倍以上.测量结果发现这些糜棱岩的磁面理非常发育,而磁线理发育较弱,其磁化率量值椭球为压偏型,与磁性面理相垂直的最小磁化率主轴的分布收敛,并与野外实地测量岩石的片理(走向 NE,向 SE 缓倾)所得到的片理法线产状基本吻合,显示了向 NW 方向的挤压应力场特征.剪切带中岩石的应变随着深度的增加,表现为由简单剪切作用向纯剪作用转化,因而其面状构造的发育不断增强.这些结果说明,岩石磁性组构的测定可为研究糜棱岩形成的构造应力作用和应变机制以及与糜棱岩形成有关的构造因素——碰撞造山带的动力学特征提供更为迅速而精确的信息.

 
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