科技英语文稿修改范例中国物理快报 （说明：兰色是应删部分， 红色是增加部分）EPR introduced the common eigenfunction of two particles the relative position of two particles. * It must be pointed out that here the integration measure is two-fold, but not three-fold, this. This is because the state * if we make a further make a mathematical transformation, . * The A similar situation may also happenoccur when the $b$-mode light falls on a beam- splitter. * (named ascalled the operational phase description) * In summary, for the first time, we have introduced the entangled state in the three-mode Fock space, and analysed its Schmidt decomposition and theits generation. * The thermodynamic processes underwentundergone by olivine, * , peopleresearchers have studied numerically the effects of. * According to Ringwood,31 the lithosphere consists of approximate approximately 78% olivine, 22% enstatite, and a trace of garnet.*However, to simplify the analysis, people often assumeit is often assumed that only one transformation occurs in (Mg,Fe) and. * , where $Delta G_rm c$, $Delta G_d$ and $Delta G_rm a$ are the free energy for homogeneous nucleation, the driving potential, and the free energy for growth, respectively, which. These can be expressed as follows:.In the following part, * Suppose that Supposing a material point moves from node A to node B in a time interval $Delta t$, the phase transformation volume of node B at time it t isSmall dimensions of the networks and accurate thermodynamic data of node A at time $t-Delta t$ will it assure ensure a precise calculation on of the phase transformation volume of node B at time it t. I assure you they will be perfectly safe with us. 我向你保证.(牛津字典) assure sb. of sth. assure sb. that-clause * Now we test what a dimension scale of the networks is required by the kinetic computation of phase transformation requires. * Therefore a smaller dimension of networks would have higher a higher precision. Calculated The calculated depths of *the dot-dot-dashed line stands forrepresents the kinetic phase -ransformational boundary of olivine to wadsleyite. * When we do carry out the kinetic computation of the phase transformation. We obtain the temperature distribution at the fine nodal points. * Therefore, when we try to understand the influence of the phase transformation on the Geodynamics geodynamics of the deep Earths deep interior, an accurate determination of these parameters is necessary. * It This shows that the kinetics of phase transformation from ringwoodite to perovskite plus magnesiowustite would influence the dynamic behaviour of the Earths deep interior, and need more laboratory data are needed. *The discovery of has motivated recent researches1-4 on these compounds which were studied as early as in the 1950s by Jonker and van Santen. * Clearly, in order to reveal the true nature of the CMR, it is needednecessary to understand the origin forof the transition to the FM metallic state. * In this Letter, we use the present work we use the cubic lattice, . * In summary, we have done carried out Monte Carlo simulation for the temperature. * T: More Magic Numbers in Titanium-Carbon Anion Clusters: Can Any Structural Growth Pattern Account for? Can This be Explained by Any Structural Growth? * A: We observe new magic numbers, which can be accounted for by none of (which can not be accounted by) the (any) previously proposed structural growth patterns. * The units manifest themselves their important roles in the growth of * T: XPS Analysis of Ytterbium Fulleride Compound Yb3C60 (X-Ray Photoelectron Spectrum Analysis of Yb3C60 Compound) To obtain this informations about the magnetic field and electron acceleration . *A: The nominal composition Yb3C60 compound was characterized by means of x-ray photoelectron spectroscopy (XPS). The evidences (Evidence) of (the) divalent state for (the) Yb cation in the as-grown crystalline Yb3 C60 are (is) obtained in XPS measurements. After exposure to air the Yb3C60 compound transform to an amorphous phase and Yb3C60 compound, in the same time (while) the valence state of (the) Yb cations change(s) from divalent to trivalent. * Since the discovery of the (superconducting) potassium- doped C60 compound(s) with superconductivity, there has been considerable interest in fulleride intercaltion compounds. Ruoff et. al (et al.) caculated * A single-phase Yb2.75C60 compound, which becomes superconductor (superconducting) be 6K,*They suggested that the rare earth elements Sm, Eu, and Yb should be easier to synthesize (prepare) as the fulleride intercalation compounds. * During the experiment the pressure (vacuum) was maintained (to be) better than 710Torr. * However, the C 1s peak position also approaches to 288.4eV, so we cannot exclude the possibility of carboxyl, being present as well. * (Sinc