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91.
The inference of fault geometry from suprajacent fold shape relies on consistent and verified forward models of fault-cored folds, e.g. suites of models with differing fault boundary conditions demonstrate the range of possible folding. Results of kinematic (fault-parallel flow) and mechanical (boundary element method) models are compared to ascertain differences in the way the two methods simulate flexure associated with slip along flat-ramp-flat geometry. These differences are assessed by systematically altering fault parameters in each model and observing subsequent changes in the suprajacent fold shapes. Differences between the kinematic and mechanical fault-fold relationships highlight the differences between the methods. Additionally, a laboratory fold is simulated to determine which method might best predict fault parameters from fold shape. Although kinematic folds do not fully capture the three-dimensional nature of geologic folds, mechanical models have non-unique fold-fault relationships. Predicting fault geometry from fold shape is best accomplished by a combination of the two methods.  相似文献   
92.
SARS疫情控制的模拟分析   总被引:1,自引:0,他引:1  
应用系统动力学模型,定量地分析“早发现、早隔离、早治疗”措施,对于控制SARS疾病扩散与传播的重要性。结果表明,“得病后入院时间”与“隔离措施强度”对于SARS疫情态势发展,具有很大的敏感性与相关性,其中得病后的患者几时去医院治疗,对于疫情的控制具有更重要的意义。同时应用动力学模型,对北京的SARS疫情进行分时间段的模拟与SARS实施控制因素影响分析,结果表明,2003—04—20以后一段时间内实行的各种控制措施,以及5月1日—5月5日的长假对于北京SARS疫情的控制是非常有效的;而4月27日左右北京市社  相似文献   
93.
Several stratospheric chemistry modules from box, 2-D or 3-D models, have been intercompared. The intercomparison was focused on the ozone loss and associated reactive species under the conditions found in the cold, wintertime Arctic and Antarctic vortices. Comparisons of both gas phase and heterogeneous chemistry modules show excellent agreement between the models under constrained conditions for photolysis and the microphysics of polar stratospheric clouds. While the mean integral ozone loss ranges from 4–80% for different 30–50 days long air parcel trajectories, the mean scatter of model results around these values is only about ±1.5%. In a case study, where the models employed their standard photolysis and microphysical schemes, the variation around the mean percentage ozone loss increases to about ±7%. This increased scatter of model results is mainly due to the different treatment of the PSC microphysics and heterogeneous chemistry in the models, whereby the most unrealistic assumptions about PSC processes consequently lead to the least representative ozone chemistry. Furthermore, for this case study the model results for the ozone mixing ratios at different altitudes were compared with a measured ozone profile to investigate the extent to which models reproduce the stratospheric ozone losses. It was found that mainly in the height range of strong ozone depletion all models underestimate the ozone loss by about a factor of two. This finding corroborates earlier studies and implies a general deficiency in our understanding of the stratospheric ozone loss chemistry rather than a specific problem related to a particular model simulation.  相似文献   
94.
森林和林地的图象二向性反射函数是一个统计函数,较之小尺度的树冠,它更多地用于大尺度的均匀覆盖的地块。用航空象片和高空间分辨率扫描仪数据作的图象热点影响研究在小尺度下显示出很大方差,而且,太阳和观测角度的交互变化进一步增加了这种反射各向异性变化的方差并有规律地继续呈现在分辨率低的图象中,这被称作BRVF或二向性反射方差函数。近年来,作为一种解释结构的手段,高分辨率图象的方向性方差和直方图结构越来越受到重视,这方面的数据也越来越多。这项工作是利用图象方差来解释结构问题(Strahler和李小文倡导)的一种延伸,并在过去15年中由众多人员作了大量工作。在树冠尺度下,森林的直方图和二向反射方差函数可以计算出来,这里利用了近似迭代函数来处理这些数据并和数值积分模拟进行了对比,结果显示可对二向性反射方差函数的测量和引入直方图的各向异性进行准确建模。  相似文献   
95.
该文用几何光学与辐射传输混合模型研究不连续植被冠层的几何光学反射模型的四分量(承照树冠、承照地面、阴影树冠、阴影地面)的参数化。用一个修正的均匀介质层路径散射(反射与传输)参数的解析算法估计路径散射参数(反射与传输),其中也考虑了冠层间隙的影响。光谱分量特征是不连续植被冠层的传输与反射,背景反照率,以直射光通量与天空漫射光通量比例的函数。光谱分量特征的模型与在美国缅因州Holand采集的针叶林数据吻合。基于LiStrahler几何光学相互遮蔽模型,用参数化的光谱分量特征对老松林和老云杉林的方向反射进行估计,其结果与在不同太阳与观测方向上的PARABOLA测量值匹配得很好。  相似文献   
96.
In this paper, we evaluate the Lagrangian velocity structure function constant, C0, in the inertial subrange by comparing experimental diffusion data and simulation results obtained with applicable Lagrangian stochastic models. We find in several different flows (grid turbulence, laboratory boundary-layer flow and the atmospheric surface layer under neutral stratification) the value for C0 is 3.0 ± 0.5. We also identify the reasons responsible for earlier studies having not reached the present result.  相似文献   
97.
试论陆壳增生的两种基本模式及其对比   总被引:2,自引:0,他引:2  
大陆地壳是地球形成演化的必然产物。大陆地壳由不同时代、不同类型、不同规模地体的拼贴而增生;同时已形成的大陆地壳沿着新的断裂分裂、离散而碱小。因此大陆地壳是地体拼贴增生与分裂离散的综合结果。太古代早期,原始陆壳形成后,主要通过环太平洋型与天山型两种基本模式达到陆壳的增生。环太平洋型陆壳增生模式出现于陆块的边缘,由古大陆向大洋方向单向增生,增生年代由老到新,增生地体一般都有较大距离的移置,其增生与板块的俯冲作用密切有关。天山型陆壳增生模式出现在陆块的内部,其形成与陆块的开台作用密切有关,可以但不一定伴随有俯冲作用。当古大陆沿一定方向断裂带分裂、离散。其间形成新的海槽接受碳酸盐岩和正常陆源碎屑沉积物与来自地壳深部或地幔的火山物质。由于壳下应力条件改变,两侧古陆相向运动,海槽中物质受两侧古陆碰撞挤压,形成褶皱造山带,并把两侧的古大陆“焊接”成新的、范围更大的大陆地壳。  相似文献   
98.
Two distinct phases are commonly observed at the initial part of seismograms of large shallow earthquakes: low-frequency and low-amplitude waves following the onset of a P wave ( P 1) are interrupted by the arrival of the second impulsive phase P2 enriched with high-frequency components. This observation suggests that a large shallow earthquake involves two qualitatively different stages of rupture at its nucleation.
We propose a theoretical model that can naturally explain the above nucleation behaviour. The model is 2-D and the deformation is assumed to be anti-plane. A key clement in our model is the assumption of a zone in which numbers of pre-existing cracks are densely distributed; this cracked zone is a model for the fault zone. Dynamic crack growth nucleated in such a zone is intensely affected by the crack interactions, which exert two conflicting effects: one tends to accelerate the crack growth, and the other tends to decelerate it. The accelerating and decelerating effects are generally ascribable to coplanar and non-coplanar crack interactions, respectively. We rigorously treat the multiple interactions among the cracks, using the boundary integral equation method (BIEM), and assume the critical stress fracture criterion for the analysis of spontaneous crack propagation.
Our analysis shows that a dynamic rupture nucleated in the cracked zone begins to grow slowly due to the relative predominance of non-coplanar interactions. This process radiates the P1 phase. If the crack continues to grow, coalescence with adjacent coplanar cracks occurs after a short time. Then, coplanar interactions suddenly begin to prevail and crack growth is accelerated; the P2 phase is emitted in this process. It is interpreted that the two distinct phases appear in the process of the transition from non-coplanar to coplanar interaction predominance.  相似文献   
99.
腾格里沙漠东南缘降尘粒度特征和沉积速率   总被引:15,自引:9,他引:15  
消洪浪  张继贤 《中国沙漠》1997,17(2):127-132
从多年降尘实测资料入手,分析了粉尘粒度特征、沉积速率和时变过程。提出了气象要素相关估测模型.确定0.25mm为本区粉尘沉积粒径上限。周围沙漠是粉尘沉积细砂部分的尘源,粉砂和粘土部分沉积来自一个较大的时空范围,二者几乎各占降尘量的1/2。研究区年平均粉尘沉积速率4358kg/hm2,每年5月的季风转期具有年内最大沉积速率。  相似文献   
100.
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