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721.
A fast algorithm is proposed to integrate the trajectory of a low obiter perturbed by the earth's non-sphericity. The algorithm
uses a separation degree to define the low-degree and the high-degree acceleration components, the former computed rigorously,
and the latter interpolated from gridded accelerations. An FFT method is used to grid the accelerations. An optimal grid type
for the algorithm depends on the trajectory's permissible error, speed, and memory capacity. Using the non-spherical accelerations
computed from EGM96 to harmonic degree 360, orbit integrations were performed for a low orbiter at an altitude of 170 km.
For a separation degree of 50, the new algorithm, together with the predict-pseudo correct method, speeds up the integration
by 145 times compared to the conventional algorithm while keeping the errors in position and velocity below 10−4 m and 10−7 m/s for a 3-day arc.
Received: 28 July 1997 / Accepted: 1 April 1998 相似文献
722.
鄂尔多斯盆地中部气田奥陶系风化壳气藏天然气来源及混源比计算 总被引:19,自引:4,他引:15
对鄂尔多斯盆地中部气田天然气碳同位素资料按不同地区、不同层位进行了分析,认为奥陶系风化壳气藏甲烷碳同位素值与石炭-二叠系气藏的接近,在平面上变化趋势相似,而与风化壳之下奥陶系自生自储的油型气相差较大。奥陶系风化壳气藏的来源是以石炭-二叠系煤成气为主,定量计算表明,在中部气田的大部分地区,石炭-二叠系来源气的比例大于70%。 相似文献
723.
二连盆地侏罗系地层热演化史研究 总被引:5,自引:1,他引:4
本文应用磷灰石裂变径迹,镜质体动力学模型等方法恢复二连盆地侏罗系地层的热演化史,二连盆地图参1井磷灰石退火浓度为1600-2774m,对应的退火温度为64-102.7℃,图参1井现今温度小于最高古地温,这是由于二连盆地地温梯度逐渐降低及地层发生抬升和剥蚀所致。根据磷灰石裂变径迹分析和镜质体动力学模型模拟图参1井的热演化史,在晚侏罗世时其经受的最高地温梯度分别为7℃/hm和6℃/hm。侏罗系地层在晚 相似文献
724.
725.
1994年9月16日台湾海峡7.3级地震震源过程的研究 总被引:1,自引:1,他引:0
采用数字化台网P波波形资料及台湾台网P波初动方向资料,研究了1994年9月16日台湾海峡73级地震及邻近地区(北纬21~26°,东经115~120°)ML≥58级共5次地震的矩张量解及震源参数。结果表明,这次73级地震的矩张量解以双力偶成分为主,是断层面接近NW走向的正断层。断层面的走向与大震前地震的条带分布走向及余震分布显示的破裂图象较相象,震源机制的张应力轴接近水平,近NE走向;压应力轴几乎垂直,近NWW走向,似乎表明这次地震是受菲律海板块向欧亚板块北西向挤压的力源控制。从P轴接近竖直而T轴接近水平来看,发震断层为强烈拉张性正断层,可能还同时存在垂直向上的应力作用。其它4个强震的震源机制解与73级大震的差别较大。这些地震震源机制解的复杂性,表明台湾海峡地震序列的发展过程比较复杂。 相似文献
726.
Applying genetic algorithm to inversion of seismic moment tensor solution and using the data of P waveform from digital network
and initial motion directions of P waves of Taiwan network stations, we studied the moment tensor solutions and focal parameters
of the earthquake of M=7.3 on 16 September of 1994 in Taiwan Strait and other four quakes of M
L≥5.8 in the near region (21°–26°N, 115°–120°E). Among the five earthquakes, the quake of M=7.3 on September 16, 1994 in Taiwan Strait is the strongest one in the southeastern coast area since Nan’ao earthquake of
M=7.3 in 1918. The results show that moment tensor solution of M=7.3 earthquake is mainly double-couple component, and is normal fault whose fault plane is near NW. The strike of the fault
plane resembles that of the distributive bands of earthquakes before the main event and fracture pattern shown by aftershocks.
The tension stress axis of focal mechanism is about horizontal, near in NE strike, the compressive stress axis is approximately
vertical, near in NWW strike. It seems that this quake is controlled by the force of Philippine plate’s pressing Eurasian
plate in NW direction. But from the viewpoint of P axis of near vertical and T axis of near horizontal, it is a normal fault of strong tensibility. There are relatively big difference between focal mechanism
solution of this quake and those of the four other strong quakes. The complexity of source mechanism solution of these quakes
represents the complexity of the process of the strait earthquake sequences.
Contribution No. 98A01001, Institute of Geophysics, State Seismological Bureau, China.
The subject is supported and helped by Academician Yun-Tai CHEN, Profs. Qing-Yao HONG, Zhen-Xing YAO, Tian-Yu ZHENG, Yao-Lin SHI, Ji-An XU, Bo-Shou HUANG and colleague Mei-Jian AN, Xue-Reng DING, Rui-Feng LIU. De-Chong ZHANG and Ming Li provided the digital data warm-heartedly. Lin-Ying WANG offered us the catalogue of earthquakes in southeastern coastal area in China. Xi-Li WANG and Tong-Xia BAI provided us the issued annual reports data. The authors would like to express their gratitude to all of these people.
This paper is sponsored by the National Natural Science Foundation of China and Scientific and Technological Commission of
Shantou, Guangdong Province. 相似文献
727.
地震前兆场的演化和能量非线性聚集的关系 总被引:4,自引:1,他引:3
运用非均匀介质中“非线性振动的局域能量聚集”过程,模拟唐山7.8级和大同6.1级地震的前兆场演化,发现地震孕育过程中出现的诸多前兆特征与地壳内构造能量的非线性聚集有关。 相似文献
728.
You-Kuan Zhang Jie Lin 《Stochastic Environmental Research and Risk Assessment (SERRA)》1998,12(2):117-140
Transport of non-ergodic solute plumes by steady-state groundwater flow with a uniform mean velocity, μ, were simulated with Monte Carlo approach in a two-dimensional heterogeneous and statistically isotropic aquifer whose transmissivity,
T, is log-normally distributed with an exponential covariance. The ensemble averages of the second spatial moments of the plume
about its center of mass, <S
i
i
(t)>, and the plume centroid covariance, R
i
i
(t) (i=1,2), were simulated for the variance of Y=log T, σ
Y
2=0.1, 0.5 and 1.0 and line sources normal or parallel to μ of three dimensionless lengths, 1, 5, and 10. For σ
Y
2=0.1, all simulated <S
i
i
(t)>−S
i
i
(0) and R
i
i
(t) agree well with the first-order theoretical values, where S
i
i
(0) are the initial values of S
i
i
(t). For σ
Y
2=0.5 and 1.0 and the line sources normal to μ, the simulated longitudinal moments, <S
11(t)>−S
11(0) and R
11(t), agree well with the first-order theoretical results but the simulated transverse moments <S
22(t)>−S
22(0) and R
22(t) are significantly larger than the first-order values. For the same two larger values of σ
Y
2 but the line sources parallel to μ, the simulated <S
11(t)>−S
11(0) are larger than but the simulated R
11 are smaller than the first-order values, and both simulated <S
22(t)>−S
22(0) and R
22(t) stay larger than the first-order values. For a fixed value of σ
Y
2, the summations of <S
i
i
(t)>−S
i
i
(0) and R
i
i
, i.e., X
i
i
(i=1,2), remain almost the same no matter what kind of source simulated. The simulated X
11 are in good agreement with the first-order theory but the simulated X
22 are significantly larger than the first-order values. The simulated X
22, however, are in excellent agreement with a previous modeling result and both of them are very close to the values derived
using Corrsin's conjecture. It is found that the transverse moments may be significantly underestimated if less accurate hydraulic
head solutions are used and that the decreasing of <S
22(t)>−S
22(0) with time or a negative effective dispersivity, defined as , may happen in the case of a line source parallel to μ where σ
Y
2 is small. 相似文献
729.
氧化铬柱支撑蒙脱石的制备研究 总被引:4,自引:1,他引:3
以浙江和新疆的膨润土为原料合成了氧化铝柱支撑蒙脱石,成柱溶液以Na2CO3为碱水解铝盐溶液制得。因为制备含有大聚羟基铬阳离子的成柱溶液是获得具有大的基面间距的柱支撑粘土的关键,我们详细研究了CO32-/Cr3+值、水解温度和水解时间对所得柱支撑蒙脱石性质的影响。聚羟基铬阳离子通过阳离子交换引入蒙脱石,所得产物用X射线衍射分析和BET氮比表面等方法研究。所得氧化铝柱支撑蒙脱石(简称Cr-mont)的基面间距为2.55nm,BET氮比表面积为190~230m2/g。 相似文献
730.
前陆盆地类型及其沉积动力学研究综述 总被引:17,自引:2,他引:15
从前陆盆地的特点及类型入手,综述了前陆盆地研究的热点内容,最新方法及其沉积动力学进展状况,揭示了前陆背景下盆地充填序列的构成及内部演化特征,指出了盆地的沉积-地层格架与冲断造山带的幕式活动之间的响应关系。 相似文献