云南双沟变质橄榄岩中蛇纹石的稀土元素空间分布

本文探讨变质橄榄岩的ＬＲＥＥ富集型及Ｕ型分布的ＲＥＥ球粒陨石模型,是橄榄石固有的还是后期蚀变形成的。并寻求复原蚀变前橄榄石的ＲＥＥ丰度及型式。我们用蛇纹石颗粒代表蚀变后的橄榄石,用分选法和化学分层剥离法对样品进行予处理。用中子活化分析（ＮＡＡ）手段进行了测试。结果表明：分选法确定了ＬＲＥＥ的主要赋存载体是蛇纹石。分层剥离最后内核的ＲＥＥ丰度及模型,可近似地作为原来（未蚀变前）橄榄石的ＲＥＥ丰度及模型。     

A hypoplastic model for gas hydrate‐bearing sandy sediments

Gas hydrate‐bearing sediments (GHBSs) have been considered as a potential energy resource. In this paper, the mechanical properties of GHBS are firstly investigated by the integrated test apparatus for synthesis of GHBS using silty sand as skeleton. Triaxial tests indicate an obvious transition of stress‐strain relationship from strain hardening under low hydrate saturation and strain softening under high hydrate saturation. The hypoplastic models coupled with Drucker‐Prager criterion and the Mohr‐Coulomb criterion are proposed to analyze the stress‐strain relationship of GHBS with considering the effective porosity because of the hydrate filling in the pores of GHBS. The strain hardening and softening behaviors are well predicted with less material parameters compared with the classical models. Compared with the test results, the proposed hypoplastic models are verified to be capable of capturing the salient features of the mechanical behaviors of GHBS under the conditions of little temperature change and no hydrate dissociation.     

Novel dynamical indices for the variations of the western Pacific subtropical high based on three-pattern decomposition of global atmospheric circulation in a warming climate

Previous studies have often used the 500 hPa geopotential height to define indices of the western Pacific subtropical high (WPSH). However, some studies reported that global warming caused a significant increase in geopotential height, particularly at the middle and lower latitudes, leading artificial results about long-term trend of the WPSH. To avoid the spurious signals resulting from global warming, this study first redefines the area, intensity, westward ridge point and ridge line indices of the WPSH by adopting the stream function R of horizontal circulation in the three-pattern decomposition of global atmospheric circulation (3P-DGAC). Subsequently, the climatic characteristics of the WPSH in summer are investigated by applying the new indices based on four reanalysis datasets. The results show that the circulation features of the WPSH could be revealed by the stream function R in 3P-DGAC. Moreover, the rain belt over East Asia is located at the northwest periphery of the zero-value isoline of the stream function R. We conclude that the climatological average WPSH is contracted and retreated eastward during 1979–2018 relative to 1948–1978. Nevertheless, by analyzing interdecadal changes of the time series of the new indices during 1948–2018, we find that area and intensity indices decrease with time before the end of 1970s and increase slightly with time after the end of 1970s, the western ridge point index moves eastward with time before the end of the 1970s and moves westward slightly with time after the end of 1970s, as well as there is no obvious interdecadal variations in the ridge line index. Because of the evident dynamical meaning, the stream function R in 3P-DGAC can be used as an objective indicator to describe the interdecadal variation of the WPSH under global warming.

     

THE EVOLUTION OF STENOLS AND STANOLS IN MARINE SEDIMENT CORE FROM BEIBU BAY, THE SOUTH CHINA SEA

Ten stenols and stanols were identified by TLC , GC and GC-MS-DS in a marine sediment core from Beibu Bay , the South China Sea .C27, C28 and C29 A5 stenols and 5a- stanols mainly come from zoopiankton, algae and phytoplankton in marine environment. C29 24-ethylcholest- 5 - en- 3B- ol is thought to indicate input of terrigenous organic matter . The increase of C27 . C28 and C29 5a-stanol /5 stenol ratios with sediment depth shows the evolution of stenols and stanols in the marine sediment core .     

黄铁矿随时间（t）变化对金吸附的动态实验

在Ａｕ（Ⅲ）－Ｃｌ络合溶液和常温常压条件下，黄铁矿随时间（ｔ）变化对金吸附的动态实验表明：整个吸附过程明显分为两个阶段．前一个阶段是快速达到平衡的吸附过程，随着平衡的建立，金的沉淀速度迅速变小，随后即进入缓慢吸附阶段，溶液中金的浓度按指数函数关系衰减．不同粒度黄铁矿实验结果的横向比较显示，粒度越细，金的沉淀速度越快，沉淀金的总量也越多。     

鲁奇管壳型合成塔合成燃料甲醇的数学模型

采用单速率模型建立了鲁奇（ｌｕｒｇｉ）管壳型合成塔合成燃料甲醇的数学模型，并对影响数学模型一些主要因素进行了模拟计算及讨论，得出了鲁奇管壳型合成塔适用于合成燃料甲醇的生产工艺条件。     

端承桩在常轴力作用下的地震反应分析

对分层弹性地基中端承桩基础按ｗｉｎｋｌｅｒ（温克尔）地基土模型并通过特性分析建立了合理的力学模型。经过动力分析，给出了端承桩横向自振特性及在常轴力与横向地震载荷作用下强迫反应解析解，为具有常轴力与横向地震载荷作用下的无限层弹性地基中端承桩的动力反应分析提供了一种新的解析方法。     

文峪金矿成矿物理化学条件及深部预测研究

通过对含金石英脉中矿物包裹体的研究，探讨了文峪金矿形成的物理化学条件，指出文峪金矿是在地表较浅部位形成的中－低温热液型矿床，其成矿母液为低盐度Ｎａ－Ｃａ－Ｃｌ－ＣＯ２系列热液流体。运用了包体测温和包体化学成分以及盐度、密度等资料，对该矿进行了深部成矿预测，认为文峪金矿深部有宫金矿体存在，具有广阔的找矿勘探前景。     

Numerical modelling of wintertime circulation in the East China sea

In order to understand the properties of the winter circulation in the northern China Sea, a two-dimensional numerical model has been established and calculated for an ideal sea basin. In the model we employed a quadratic conservative scheme for a complete set of dynamic and thermodynamic equations. The systematic analysis of stability produced a series of mathematically and physically restrictive conditions which are more general than those derived by Irvine, and Chen. Using this model we made calculations on a series of interesting phenomena, such as the Yellow Sea Warm Current, two gyres in the Yellow Sea, etc. as well as their developing processes. The simulation can also explain the generation mechanism of the phenomena. Contribution No. 1523 from Institute of Oceanology, Academia Sinica     

On the joint robust estimation of parameters and variance

A method of joint estimation of the parameters and the variance σ² in the linear model is presented in this paper. The M-estimators with finite rejection points are adopted for estimating the parameters. In order to estimate the variance σ², the Grubbs statistics and the Kurtosis test statistics are adopted to test the residual sequence {;r_i};. And the sample variance of {;r_i}; after discarding the outliers is taken as the estimation of σ². This method of estimating σ² is less computational demanding and more accurate, compared with the well-known method which takes 1.483 med_i |r_i| as the estimation of σ. The breakdown point of the above estimation of σ² is more than 20%, while the brekdown point is less than 10%, if only the Grubbs statistics is used.