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91.
Xiao-Hong Zhao Jin-Ming Bai 《中国天文和天体物理学报》2007,7(4):503-508
A Gamma-ray burst (GRB) is generally believed to be a jet with a small opening angle, this opening angle is usually derived with the afterglow light curve break time using an analytical method. Here we show that the method is not accurate. Using the set of equations of hydrodynamic evolution with the sideways expansion at the local sound speed derived by previous authors and the observed light curve break times, we numerically derive the initial opening angles. Then the collimation-corrected energies (Eγ) for a sample of GRBs are calculated. They are found to show a wide spread, suggesting that the previously declared clustering by some authors may not exist. Also, the Epeak -Eγ relation, claimed by some other authors (Epeak is the spectral peak energy), is found still to hold, with a slightly stronger correlation. 相似文献
92.
Yu Bai Yang Chen Xiang-Tao He Jiang-Hua Wu Qing-Kang Li Richard F.Green Wolfgang Voges 《中国天文和天体物理学报》2007,7(3):375-379
This is the third paper in a series connected with our Multiwavelength Quasar Survey. The survey is aimed to provide a quasar sample more complete than any previous survey by using a combined selection technique to reduce selection effects. We present the observational results for the X-ray candidates in field f836. We found 15 X-ray AGNs in this field of which eight are new discoveries. The X-ray data and optical spectra of these AGNs are given. We give the X-ray candidate selection criteria, which proved to be highly efficient in isolating X-ray AGNs. 相似文献
93.
94.
Deep and shallow tectonic data in Shenyang and its relationship with seismic activity shows that the NE trending faults developed on the surface control the formation and development of the fault-uplift and fault-depression.The uplift and depression of the bedrock at a depth of 7km underground are consistent with the surface structure.12 planar listric normal faults have developed above a depth of 18km ~ 20km and two deep faults have developed in the lower crust.Because of the deep incision and new activities,the surface Wanggangpu-Xinchengzi fault and Yongle-Qingshuitai fault,which correspond to the deep F3 fault and F6 fault,might be related to seismic activity in Shenyang. 相似文献
95.
俯冲带的碳循环不仅在维持地球表层和地球深部之间的碳平衡方面起着关键的作用,而且还和许多重要的地球深部动
力学过程密切相关。热动力学数值模拟和高温高压实验的研究结果表明,俯冲大洋板片中的大多数碳酸盐能够在弧前和弧下深
度幸存下来,从而进入更深的地幔中。在地幔过渡带,因为板片滞留所带来的热松弛效应将使幸存下来的碳酸盐以熔体的形式释
放出去,其独特的物理化学性质使这些熔体构成了一种有效的交代组分。考虑到地幔过渡带的氧逸度特别低,那些进入未经交代
地幔中的碳酸盐熔体将变得不稳定而被还原成其他形式。不过在随后地幔对流上升的过程中,这些被还原的表壳碳又会因为氧
逸度在某些临界深度发生突变而氧化熔融,这也许可以解释地幔不同深度所存在的某些高导低速体和地震波各向异性等现象。
作为洋壳俯冲的后续过程,陆壳的深俯冲作用也可以将表壳碳带至地幔深处,例如超高压大理岩和碳酸盐化榴辉岩的广泛产出就
是最好的证明。超高压变质岩中金刚石的产出表明其构成了表壳碳在地幔深处的一种重要赋存形式,研究显示其形成过程和富
碳熔体、流体的活动密切相关。虽然前人针对俯冲带的碳循环已经取得了若干研究进展,然而仍有大量的科学问题亟待解决。最
后就一些关键性的问题进行了列举说明,并对未来的研究方向进行了展望。 相似文献
力学过程密切相关。热动力学数值模拟和高温高压实验的研究结果表明,俯冲大洋板片中的大多数碳酸盐能够在弧前和弧下深
度幸存下来,从而进入更深的地幔中。在地幔过渡带,因为板片滞留所带来的热松弛效应将使幸存下来的碳酸盐以熔体的形式释
放出去,其独特的物理化学性质使这些熔体构成了一种有效的交代组分。考虑到地幔过渡带的氧逸度特别低,那些进入未经交代
地幔中的碳酸盐熔体将变得不稳定而被还原成其他形式。不过在随后地幔对流上升的过程中,这些被还原的表壳碳又会因为氧
逸度在某些临界深度发生突变而氧化熔融,这也许可以解释地幔不同深度所存在的某些高导低速体和地震波各向异性等现象。
作为洋壳俯冲的后续过程,陆壳的深俯冲作用也可以将表壳碳带至地幔深处,例如超高压大理岩和碳酸盐化榴辉岩的广泛产出就
是最好的证明。超高压变质岩中金刚石的产出表明其构成了表壳碳在地幔深处的一种重要赋存形式,研究显示其形成过程和富
碳熔体、流体的活动密切相关。虽然前人针对俯冲带的碳循环已经取得了若干研究进展,然而仍有大量的科学问题亟待解决。最
后就一些关键性的问题进行了列举说明,并对未来的研究方向进行了展望。 相似文献
96.
A wind turbine system equipped with a tuned liquid column damper(TLCD) is comprehensively studied via shaking table tests using a 1/13-scaled model. The effects of wind and wave actions are considered by inputting responseequivalent accelerations on the shaking table. The test results show that the control effect of the TLCD system is significant in reducing the responses under both wind-wave equivalent loads and ground motions, but obviously varies for different inputs. Further, a blade-hub-tower integrated numerical model for the wind turbine system is established. The model is capable of considering the rotational effect of blades by combining Kane’s equation with the finite element method. The responses of the wind tower equipped with TLCD devices are numerically obtained and compared to the test results, showing that under both controlled and uncontrolled conditions with and without blades’ rotation, the corresponding responses exhibit good agreement. This demonstrates that the proposed numerical model performs well in capturing the wind-wave coupled response of the offshore wind turbine systems under control. Both numerical and experimental results show that the TLCD system can significantly reduce the structural response and thus improve the safety and serviceability of the offshore wind turbine tower systems. Additional issues that require further study are discussed. 相似文献
97.
Assimilation systems absorb both satellite measurements and Argo observations. This assimilation is essential to diagnose and evaluate the contribution from each type of data to the reconstructed analysis, allowing for better configuration of assimilation parameters. To achieve this, two comparative reconstruction schemes were designed under the optimal interpolation framework. Using a static scheme, an in situ-only field of ocean temperature was derived by correcting climatology with only Argo ... 相似文献
98.
Eclogite is essentially a bi-mineralogic high-grade metamorphic rock consisting of garnet and omphacite and is the product of high-to-ultrahigh pressure metamorphism of basaltic rocks due to the subduction of oceanic crust or the thickening/subduction of … 相似文献
99.
对西藏亚东淡色花岗岩Rb-Sr和Sm-Nd同位素的详细研究表明,亚东淡色花岗岩Rb-Sr和Sm-Nd同位素组成十分不均匀,其初始Sr值和ε-(Nd)(13 Ma)分别介于0.756~0.775和-11.6~-16.3。由于存在着显著的同位素变异,而难以获得其全岩Rb-Sr等时线年龄。但研究获得了12.9±0.95Ma矿物—全岩Rb-Sr等时线年龄,其锶初始值为0.7744±0.0008,该年龄可以与高喜马拉雅带其他淡色花岗岩的年龄对比。Rb-Sr和Sm-Nd同位素组成显示亚东淡色花岗岩的源岩很可能是聂拉木群副变质岩。年龄统计分析表明,喜马拉雅淡色花岗岩是在地壳伸展和快速隆起背景下形成的,因此它的形成年龄是碰撞造山后地壳强烈活动和快速隆起的重要标志。 相似文献
100.
三江平原沼泽湿地时空动态特征 总被引:3,自引:0,他引:3
1IntroductionThe wetland ecosystem is the latest one understood by humans and it is the most seriously damaged ecosystem (Williams, 1991). The Sanjiang Plain, located in northeast China, is the largest concentrated area of freshwater wetland in China. Since the 1950s, large-scale reclamation of the marsh in the Sanjiang Plain has been started. According to statistics, the natural marsh has lost about 80% of its total area. The marsh resources in the Sanjiang Plain decreased greatly and the… 相似文献