给定参数条件下海温脉动随机模式的混沌行为

从Ｓａｌｔｚｍａｎ海气随机气候模式出发，得到了海温脉动θ＇的Ｌａｎｇｅｖｉｎ方程以及对应的Ｆｏｋｋｅｒ－ｐｌａｎｋ方程。在给定参数条件下求数值解，得到的概率密度曲线ｐ（ｘ，ｔ）具有多个极大值，并在ｐ（ｘ，ｔ）－ｐ（ｘ，ｔ＋τ）相空间中呈现Ｃａｎｔｏｒ集合图象，表明该随机系统在上述参数条件下出现了混沌行为。     

CHAOTIC OUTPUT OF SST FLUCTUATION STOCHASTIC MODEL WITH GIVEN PARAMETERS

Starting from the Saltzman's air-sea stochastic climatic model, we have derived a langevin-type equation describing SST fluctuation and the related pokker-Plank expression, which were then numerically solved with parameters given, yielding the probability density curve P(x, t) of multiple bifurcations, with the Cantor set of images given in phase space of P(x, t) and P(x, t+τ), thereby indicating that chaotic output comes from the random system under the conditions of the above parameters.     

乌鳢的消化器官与其机能适应性的讨论

本文从乌鳢消化器官的形态学与组织学方面,就各消化器官与其机能的适应性作了初步探讨。各器官均与其食性和捕食方式相适应。     

Sedimentation Rates, Observation Span, and the Problem of Spurious Correlation

Plots of sedimentation rates vs. time span of observation are routinely used to demonstrate that sedimentation rates decrease if one averages over longer time spans. However, these plots are suspect because they plot a variable, time, against its inverse. It has been shown that even random numbers may yield correlation coefficients of 0.7 or higher under these circumstances. We have circumvented this problem by splitting observed sedimentation rates into time classes and performing regression on the primary variables, thickness and time, separately in each class. An alternative is weighted regression that corrects for the effect of spurious correlation. Regression on the primary variables has been performed on real data from siliciclastic and carbonate rocks. Data were sorted into time classes of 10 ^–1–10 ² yr, 10 ²–10 ⁵ yr, and 10 ⁵–10 ⁸ yr. Sedimentation rates decrease systematically as the time windows increase. The experiment indicates that the decrease of sedimentation rates with increase of time is not simply an effect of the mathematical transformation. It is a physical phenomenon, probably related to the fact that sedimentation is an episodic process and that the sediment record is riddled with hiatuses on all scales.     

黄喉拟水龟含肉率及肌肉营养成分分析

分析了黄喉拟水龟成龟的含肉率及肌肉营养成分。结果表明:成龟的含肉率平均为23.4%,内脏平均占体重的14.0%,骨骼平均占体重的39.4%,血液和体液平均占体重的18.4%,脂肪块变动较大,平均占体重的5.0%;肌肉中各物质质量分数平均为:水分79.7%,灰分1.0%,粗脂肪0.3%,蛋白质18.2%;在肌肉16种氨基酸中,必需氨基酸质量分数平均为6.69%,氨基酸总量平均为14.9%;在测出的18种脂肪酸中,不饱和脂肪酸含量平均占64.77%,高度不饱和脂肪酸平均占22.91%。在分析的基础上,本文讨论和评价了黄喉拟水龟的食用价值,为其配合饲料的研究开发提供了基础数据。     

地震序列性质与断层分维研究

本文引入地震断层的自扩展破裂模式,用以解释地震序列的特征并计算地震断层的分维数。由自扩展破裂模式,本文导出地震断层的分维数为D=ln(1+Abln q/1+q)/ln q/1+q,其中q为余震区长度与主震的破裂尺度之比,A=2.1。在q≥1时,D=Ab,这与Aki的公式b=D/2是一致的。     

On the vertical families of two-dimensional tori near the triangular points of the Bicircular problem

This paper focuses on some aspects of the motion of a small particle moving near the Lagrangian points of the Earth–Moon system. The model for the motion of the particle is the so-called bicircular problem (BCP), that includes the effect of Earth and Moon as in the spatial restricted three body problem (RTBP), plus the effect of the Sun as a periodic time-dependent perturbation of the RTBP. Due to this periodic forcing coming from the Sun, the Lagrangian points are no longer equilibrium solutions for the BCP. On the other hand, the BCP has three periodic orbits (with the same period as the forcing) that can be seen as the dynamical equivalent of the Lagrangian points. In this work, we first discuss some numerical methods for the accurate computation of quasi-periodic solutions, and then we apply them to the BCP to obtain families of 2-D tori in an extended neighbourhood of the Lagrangian points. These families start on the three periodic orbits mentioned above and they are continued in the vertical (z and ż) direction up to a high distance. These (Cantor) families can be seen as the continuation, into the BCP, of the Lyapunov family of periodic orbits of the Lagrangian points that goes in the (z, ż) direction. These results are used in a forthcoming work [9] to find regions where trajectories remain confined for a very long time. It is remarkable that these regions seem to persist in the real system. This revised version was published online in July 2006 with corrections to the Cover Date.     

n维欧几里得空间中一类康托型集的Hausdorff维数

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地震序列的一个自相似扩展模式

本文引入地震序列的一种自扩展模式,其地震序列的发生由地震断层的不同尺度的闭锁段相继破裂而发生,同时给出了以力学参数和几何参数定标的断层的自相似破裂机制,用以解决地震断层的分形特征及破裂的慢化过程。