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21.
H.?Liu W. A.?Caldwell L. R.?Benedetti W.?Panero R.?JeanlozEmail author 《Physics and Chemistry of Minerals》2003,30(9):582-588
The high-pressure behavior of x8tf9p4/xxlarge945.gif" alt="agr" align="BASELINE" BORDER="0">-Fe2O3 has been studied under static compression up to 60 GPa, using a laser-heated diamond anvil cell. Synchrotron-based angular-dispersive X-ray diffraction shows that the sample remains in the corundum structure up to 50 GPa, but with the appearance of coexisting diffraction lines from a high-pressure phase at pressures above 45 GPa. A least-squares fit of low-pressure phase data to an Eulerian finite-strain equation of state yields linear incompressibilities of K
a
0=749.5 (± 18.4) GPa and K
c
0= 455.7 (± 21.4) GPa, differing by a factor of 1.6 along the two directions. The enhanced compressibility of the c axis may lead to breaking of vertex- or edge-sharing bonds between octahedra, inducing the high-pressure phase transformation at 50 GPa. Analysis of linear compressibilities suggests that the high-pressure phase above 50 GPa is of the Rh2O3 (II) structure. Continuous laser heating reveals a new structural phase transformation of x8tf9p4/xxlarge945.gif" alt="agr" align="BASELINE" BORDER="0">-Fe2O3 at 22 GPa, to an orthorhombic structure with a=7.305(3) Å, b=7.850(3) Å, and c=12.877(14) Å, different from the Rh2O3 (II) structure. 相似文献
22.
龙凤山大气近地层O3浓度变化及与其它因素的关系 总被引:16,自引:0,他引:16
研究首次在龙凤山区域大气本底站测得的地面O3浓度及其变化的资料表明,中国东北农村地面大气O3浓度总体水平不很高,但在少数特殊的天气条件下,时均浓度可超过国家二级标准。O3浓度存在明显的季节和日变化,其月平均浓度1995年1月最低(27.5ppb),1994年11月最高(43.2ppb)。O3日变化幅度夏季的晴天最大(28ppb),冬季的阴天最小(8ppb)。气象要素(尤其是风速、气温和相对湿度等)和NOx与地面O3浓度有较密切的关系。用多变量分析法探讨了地面O3各指标随气象因子和NOx共同变化的规律,并拟合了寒冷和温暖期里与地面O3日最高浓度、日最低浓度及日变化幅度有关的方程。 相似文献
23.
在大气环境影响评价工作中,对于多源问题通常采用逐个计算叠加的方法。本文介绍了在大型水泥厂大气环境影响预测中,对数量众多的粉尘排放源进行简化处理的一种方法。在瑞昌水泥厂的环境影响评价中,我们采用了这种方法,并对这种方法得到的结果进行了比较验证,讨论了这种方法的合理性和可行性。通过这种简化处理,可以使大气预测工作更简单化,更省时。 相似文献
24.
本文运用Maslov渐近理论编写的二维横向非均匀介质中的理论地震图程序,与其它类型算法作了精确对比,结果表明,在层状介质模型中,本程序的结果无论振幅还是波形对比都与反射率法基本相同。对于二维横向非均匀模型,在射线理论的非奇点处,本算法与射线方法基本一致,在射线理论的奇异点处,Maslov方法消除了射线理论所固有奇点,提高了计算精度。 相似文献
25.
Seismic imaging is an important step for imaging the subsurface structures of the Earth. One of the attractive domains for seismic imaging is explicit frequency–space (f – x) prestack depth migration. So far, this domain focused on migrating seismic data in acoustic media, but very little work assumed visco‐acoustic media. In reality, seismic exploration data amplitudes suffer from attenuation. To tackle the problem of attenuation, new operators are required, which compensates for it. We propose the weighted L 1 ‐error minimisation technique to design visco‐acoustic f – x wavefield extrapolators. The L 1 ‐error wavenumber responses provide superior extrapolator designs as compared with the previously designed equiripple L 4 ‐norm and L∞‐norm extrapolation wavenumber responses. To verify the new compensating designs, prestack depth migration is performed on the challenging Marmousi model dataset. A reference migrated section is obtained using non‐compensating f – x extrapolators on an acoustic dataset. Then, both compensating and non‐compensating extrapolators are applied to a visco‐acoustic dataset, and both migrated sections are then compared. The final images show that the proposed weighted L 1 ‐error method enhances the resolution and results in practically stable images. 相似文献
26.
Efi Meletlidou 《Celestial Mechanics and Dynamical Astronomy》2000,78(1-4):161-166
We consider a one-dimensional non-degenerate Hamiltonian system perturbed by a periodically time dependent non-Hamiltonian vector field and show that the non-vanishing of the Melx17051258586732r/xxlarge8217.gif" alt="rsquo" align="BASELINE" BORDER="0">nikov subharmonic function is strongly related to the non-existence of an analytic integral in the perturbed system. 相似文献
27.
28.
《International Journal of Digital Earth》2013,6(5):483-503
Abstract 3D geo spatial data have become the normal. However, to view the data, usually expert software is required, which have up to now hindered the wide spread use of 3D scenes for the display of geological data. The internet real time 3D rendering framework X3D is assessed regarding its suitability for building a geological GIS on the internet. Especially important for geological data, 3D rendering enhances the intuitive grasp of the data and enables the user to interactively explore it. It is often necessary to find a solution to distribute this data to a wide range of interested parties, experts and non-experts alike. According to the nature of 3D data, the best technique to display geo-data, the modeling of objects and unresolved issues have to be taken into consideration. The internet is the apparent tool for the public distribution and visualization of 3D data and it was found that through the open ISO-standardized format X3D it offers a multitude of possibilities. A 3D geological interactive map was created with these prerequisites to identify challenges and possibilities through this process. It was found that the use of lead to satisfactory results, that could probably not have been achieved with another technology. 相似文献
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