陕西禾草沟煤矿工业场地主厂房段古滑坡变形破坏特征及稳定性分析

工程建设引发禾草沟煤矿工业场地主厂房段古滑坡复活,通过野外调查和测量、钻探、探槽、变形监测、室内试验和数值计算,分析该古滑坡的复活原因及变形破坏特征;采用改进的数值计算法对古滑坡的稳定性进行分析,古滑坡在天然条件下处于稳定状态;对古滑坡复活采用"削头压脚"措施后,稳定性满足安全要求,这对古滑坡的治理设计提供了理论依据。同时,该措施能节约工程投资,缩短工期,具有良好的经济效益。     

Some considerations on the calculation of the response spectra

This paper is about the calculation of the response spectra. It describes the importance of the three effects which are usually neglected: low quality of accelerograms linear interpolation, the shift of transfer functions which arises in discrete filtering, and the roundoff error.     

利用CAD次开发程序计算超欠挖的研究

应用CAD平台进行二次开发,研究了超欠挖的计算方法,发现利用CAD平台计算超欠挖可实现计算过程自动化、可视化,并介绍了其工作原理、软件组成部分。结果表明,CAD二次开发程序能很好地计算隧道超欠挖。     

重组抗菌肽海藻酸钠微囊制备与体外释放特征研究

对重组表达的海洋生物抗菌肽对虾素3-2进行亲和层析纯化,以海藻酸钠为壁材,采用凝聚法制备了重组抗菌肽海藻酸钠微囊,以微囊的形态和包封率为指标优化制备工艺,对制备的微囊进行体外释放特征的初步研究。结果显示,在氯化钙浓度为1.5%,海藻酸钠浓度为2.0%时,制备的微囊为完整的球形,冷冻干燥后的直径约为1.1 mm,包封率为83.87%。微囊在模拟胃液(pH 2.0)中2 h左右释放量趋于稳定,释放量低于14%;微囊在模拟肠液(pH 7.8)中不断释放,5 h时释放量达98%,表明微囊具有良好的肠溶性而可以抵抗胃液的破坏,可以用作重组抗菌肽缓释/控释制剂,为抗菌肽在水产病害防治过程的口服给药提供实验基础。     

A theoretical investigation of the relative stabilities of Fe-free clinozoisite and orthozoisite

 The relative stabilities of orthozoisite, Ca₂Al₃[O|OH|Si₂O₇|SiO₄], space group Pnma, and the monoclinic polymorph, clinozoisite, space group P2₁/m, have been investigated using calculations based on density functional theory. It is found that orthozoisite is more stable than clinozoisite by about 1 kJ mol⁻¹ at zero pressure in the athermal limit. The bulk moduli of the two polymorphs have been calculated to be B_ortho=117.5(1.7) GPa and B_clino=136(4) GPa. Received: 20 March 2000 / Accepted: 26 February 2001     

The crystal chemistry and Fe<Superscript>II</Superscript>–site properties of aluminosilicate garnet solid solutions as revealed by Mössbauer spectroscopy and electronic structure calculations

The three binary garnet solid solutions Fe^II₃Al₂Si₃O₁₂–X^II₃Al₂Si₃O₁₂ (X^II= Mg^II, Mn^II, Ca^II) have been investigated by ⁵⁷Fe Mössbauer spectroscopy at 298 and 77 K and by electronic structure calculations in the local spin density approximation. The spectra yield isomer shifts and quadrupole splittings that are typical for Fe^II in the dodecahedral X-site of 222 point symmetry and are similar for each of the three binaries recorded. Conversely, electronic structure calculations based on the experimental crystal structure of the different end-member garnets exhibit pronounced variations in some of the electronic properties of Fe^II that are not reflected in the spectroscopic data. These results are interpreted as indicating that the different X–O bonds in garnet solid solutions retain to a large degree the intrinsic lengths that they possess in their respective end members, and that the Fe–O bond does not change greatly as a function of composition. This is evidence for the state of alternating bonds and not for the virtual crystal approximation in describing the X–O bond types or lengths in aluminosilicate garnet solid solutions. The observed degree and behavior of the Fe^II doublet asymmetry in the Mössbauer spectra for the three solid solution series do not indicate major variations in the anisotropic recoil-free fraction of Fe^II. Variations in doublet asymmetry are more likely a result of complex next-nearest X-site neighbor interactions and/or some degree of short-range cation ordering, though doublets representing different local X-site cation configurations cannot be resolved or fitted to the experimental spectra.     

密度计法试验土用量规定的讨论

通过对密度计法颗粒分析用土量的对比试验及各国有关标准的比较，可以认为国标的有关规定有待修改、完善。     

Multipole-refined charge density study of diopside at ambient conditions

The experimental multipole electron density, ρ(r), of diopside was derived from high-resolution single-crystal diffraction at room temperature. Its topological analysis revealed predominantly ionic Si–O bonding, as found in electron density studies of other silicates. In particular, the non-bridging Si–O bonds are slightly less ionic in character than the bridging Si–O bonds. The Ca–O and Mg–O bonds are classified as pure closed-shell ionic interactions. An analysis of –∇²ρ(r) showed the presence of maxima around the oxygen atoms, associated to lone pairs domains that are involved in bonds with the surrounding ions. Calculation of atomic basins gave net charges of –1.56(12), 3.11(17), 1.79(13) and 1.88(18) e for O (averaged), Si, Ca and Mg atoms, respectively. O···O interactions between the O atoms at the vertices of the SiO₄ tetrahedron were also detected from the topological analysis of ρ(r), and indicate a cooperative interaction among the lone pairs of neighbouring oxygen atoms. All these results were also confirmed by periodic restricted Hartree–Fock (RHF) calculations. Electronic Supplementary Material Supplementary material is available for this article at and is accessible for authorized users.