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971.
A. J. Cross D. J. Purdy D. C. Champion D. D. Brown C. Siégel R. A. Armstrong 《Australian Journal of Earth Sciences》2013,60(7-8):987-1008
AbstractZircon U–Pb ages, εHf(t), and δ18O isotopic data together with geochemistry and limited Sm–Nd results from magmatic rocks sampled in deep-basement drill cores from undercover parts of the Thomson Orogen provide strong temporal links with outcropping regions of the orogen and important clues to its evolution and relationship with the Lachlan Orogen. SHRIMP U–Pb zircon ages show that magmatism of Early Ordovician age is widespread across the central, undercover regions of the Thomson Orogen and occurred in a narrow time-window between 480 and 470?Ma. These rocks have evolved εHf(t)zrn (?12.18 to ?6.26) and εNd (?11.3 to ?7.1), and supracrustal δ18Ozrn (7.01–8.50‰), which is in stark contrast to Early Ordovician magmatic rocks in the Lachlan Orogen that are isotopically juvenile. Two samples have late Silurian ages (425–420?Ma), and four have Devonian ages (408–382?Ma). The late Silurian rocks have evolved εHf(t)zrn (?6.42 to ?4.62) and supracrustal δ18Ozrn (9.26–10.29‰) values, while the younger Devonian rocks show a shift toward more juvenile εHf(t)zrn, a trend that is also seen in rocks of this age in the Lachlan Orogen. Interestingly, two early Late Devonian samples have juvenile εHf(t)zrn (0.01–1.92) but supracrustal δ18Ozrn (7.45–8.77‰) indicating rapid recycling of juvenile material. Two distinct Hf–O isotopic mixing trends are observed for magmatic rocks of the Thomson Orogen. One trend appears to have incorporated a more evolved supracrustal component and is defined by samples from the northern two-thirds of the Thomson Orogen, while the other trend is generally less evolved and from samples in the southern third of the Thomson Orogen and matches the isotopic character of rocks from the Lachlan Orogen. The spatial association of the Early Ordovician magmatism with the more evolved metasedimentary signature suggests that at least the northern part of the Thomson Orogen is underlain by older pre-Delamerian metasedimentary rocks. 相似文献
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973.
974.
针对某高架桥工程采用旋挖钻机在软土层钻进中发生的孔口坍塌、缩径、钻头打滑、孔底沉渣厚度大等情况,进行了原因分析,并采取了加长护筒、改进钻头结构、优化钻进工艺、气举反循环清孔、泥浆净化等针对性措施,取得了良好的效果,确保了工程质量,提高了施工效率,施工经验可供类似工程参考。 相似文献
975.
976.
One of the main construction problems in permafrost regions is protecting permafrost thermal stability. Although ventilating ducts and crushed-rock layers were successfully used in railway embankment construction, their effects might not meet large-width expressway requirements. The convection-intensifying composite embankment composed of perforated ventilation ducts and crushed-rock layers was numerically studied to investigate its cooling effects. Adopting a numerical model, the temperature fields for two kinds of composite embankment with and without air doors were analyzed considering air flow and heat transfer characteristics in porous media. The results show that wind velocity in the crushed-rock zone is intensified by the perforated ventilation duct. The underlying permafrost temperature obviously decreases, and the 0 °C isotherm position rises significantly due to composite embankment. The composite embankment with air doors is more effective than that without air doors. Therefore, the new convection-intensifying composite embankment is potentially a highly efficient cooling measure for construction in permafrost regions. 相似文献
977.
本文根据火山灰粒子的辐射光学特性,计算了火山灰粒子和平流层本底的辐射光学参数。另外,采用大气多次散射的辐射传输方程,计算了火山喷发对大气辐射变温的影响效果。结果表明,与平流层本底相比,火山灰粒子具有很强的吸收性。火山喷发使平流层吸收太阳辐射增温,并使到达对流层和地面的太阳辐射减少;同时,对大气长波冷却率的影响甚微。 相似文献
978.
Jing Yang Qing Bao Duoying Ji Daoyi Gong Rui Mao Ziyin Zhang Seong-Joong Kim 《大气科学进展》2014,31(5):1147-1156
Two parallel sets of numerical experiments (an ozone-hole simulation and a non-ozone-hole simulation) were performed to investigate the effect of ozone depletion on surface temperature change using the second spectral version of the Flexible Global Ocean-Atmosphere-Land System model (FGOALS-s2), focusing on the eastern Antarctica (EA) continent in austral summer. First, we evaluated the ability of the model to simulate the EA surface cooling, and found the model can successfully reproduce the cooling trend of the EA surface, as well as the circulation change circling the South Pole in the past 30 years. Second, we compared the two experiments and discovered that the ozone depletion causes the cooling trend and strengthens the circumpolar westerly flow. We further investigated the causes of the EA surface cooling associated with the ozone hole and found two major contributors. The first is the ozone-hole direct radiation effect (DRE) upon the surface that happens because the decrease of the downward longwave (LW) radiation overcomes the increase of the downward shortwave (SW) radiation under clear sky. The second is the cloud radiation effect (CRE) induced by ozone depletion, which happens because the decreased downward SW radiation overcomes the increased downward LW radiation in the case of increased cloud. Although the CRE is theoretically opposite to the DRE, their final net effect makes comparable contributions to the EA surface cooling. Compared with the surface radiation budget, the surface heat flux budgets have a much smaller contribution. We additionally note that the CRE is basically ascribed to the circulation change. 相似文献
979.
既有管道由于自身弯曲和多处沉降导致其三维模型十分复杂,常用的三维管道设计软件不可用,若以测量的纵断面图为依据进行平面层次的设计则存在极大的不可靠性,因而只能利用计算机三维图形技术解决。这里研究采用三维技术辅助既有地下给排水管道内套新管的设计,用三维碰撞检测算法来趋近获取最大管径,并采用基于四元数的球面线性插值法进行三维圆弧的拟合,从而实现对复杂管道的三维建模。采用基于三角形单元的碰撞检测方法,具有简便、适用的特点。基于高效三维引擎Open Scene Graph开发了三维建模及碰撞检测演示软件并对某设计项目进行察看、验证,证实了此方法的正确性。 相似文献
980.
在skyline平台进行地下管线的自动建模时,接头处的弯管skyline没有合适的方案实现。鉴于此,通过数学方法,自动进行弯管接头的建模,使在skyline中进行管线系统开发时,弯管接头有了一种可选的建模方案。 相似文献