Application of Random Process in Soil Profile Modeling

When using the random process in soil profile modeling, the stationary and ergodicity of thesoil properties in the profile must be tested. This paper describes a procedure for stationary and ergodicity testing. Numerical examples were given for demonstration. A log-cosine function is suggested to simulate the correlation function, which has been proved to be good for soil profile modeling.     

重庆雾害潜势预报、警报系统中的显示服务系统

本文介绍重庆市区雾害潜势预报报警服务系统的显示服务系统。该系统包括资料处理、动力、统计、数值预报、客观推理系统、综合决策(集成)等模式,以及系统简介和显示服务等功能。显示服务系统采用菜单技术,多种语言混合编程,能正确运行各个模式,完成所需功能,具有实用、方便、直观和自动化程度高的特点,在实用中收到良好效果。     

Precise dating of abrupt shifts in the Asian Monsoon during the last deglaciation based on stalagmite data from Yamen Cave, Guizhou Province, China

Based on 33 U/Th dates and 1020 oxygen isotopic data from stalagmite Y1 from Yamen Cave, Guizhou Province, China, a record of the Asian Summer Monsoon (ASM) was established. The record covers the last deglaciation and the early Holocene (from 16.2 to 7.3 ka BP) with an average oxygen isotope resolution of 9 years. The main millennial-scale deglacial events first identified in Greenland (Greenland Interstadial Events: GIS 1e through GIS 1a) and later in China are clearly present in the Y1 record. By analogy to earlier work, we refer to these as Chinese Interstadials (CIS): CIS A.1e to CIS A.1a. The onset of these events in Y1 δ18O records are nominally dated at: 14750±50, 14100±60, 13870±80, 13370±80, and 12990±80 a BP. The end of CIS A.1a or the beginning of the Younger Dryas (YD) event is nominally at 12850±50 a BP and the end of the YD dates to 11500±40 a BP. The δ18O values shift by close to 3‰ during the transition into the Bφlling-Allerφd (BA, the onset of CIS A.1e) and at the end of the YD. Comparisons of Y1 to previously published early Holocene records show no significant phase differences. Thus, the East Asia Monsoon and the Indian Monsoon do not appear to have been out of phase during this interval. The Y1 record confirms earlier work that suggested that solar insolation and North Atlantic climate both affect the Asian Monsoon.     

胜利油区渤南洼陷热液型硬石膏的存在

阐明了深部非常规性硬石膏型储层研究的迫切性。从气候、沉积特征、岩性分布、包裹体均一温度、高温热液蚀变矿物硅灰石、低温热液蚀变矿物片钠铝石等10个方面证据厘定了热液型硬石膏的存在。这种热液型硬石膏,面孔率达28％,是深部有利的储层,同时也是深部热液存在的证据之一。     

基于改进GSI体系确定三峡地下厂房围岩等效变形模量及强度

基于地质强度指标GSI体系和Hoek-Brown强度准则, 研究岩体强度及变形模量时没有考虑到结构面产状对工程岩体参数的影响.结合三峡工程地下厂房, 根据围岩开挖面与结构面分布的空间位置关系, 确定了结构面分布对围岩结构等级SR的影响系数, 改进了GSI体系中围岩SR的统计方法, 确定了围岩的等效变形模量和强度参数.研究表明, 改进后的GSI体系求解的围岩弹性区等效弹性模量、扰动区等效变形模量和粘聚力分别减小了约15%、8%和28%的误差.      

海洋蛭弧菌DA5全基因组测序及序列分析

为深入挖掘和利用海洋蛭弧菌及其基因资源, 本研究利用Illumina HiSeq测序平台对一株属于嗜盐噬菌弧菌(Halobacteriovorax)的海洋蛭弧菌DA5进行了全基因组测序, 对基因组进行组装、基因预测和功能注释, 并与其他8株蛭弧菌进行了比较基因组分析。结果显示: DA5基因组大小为3.27Mb, GC含量为36.5%, 预测编码基因3175个。在DA5基因组中注释到303个基因具有直系同源蛋白簇分类, 与代谢通路相关基因1239个。比较基因组分析表明: DA5符合海洋蛭弧菌基因组的基本特征, 与其他8株蛭弧菌共有467个同源基因家族, 而DA5特有基因为266个。DA5中与细胞运动相关基因62个, 其中编码甲基受体趋化蛋白、鞭毛蛋白、鞭毛马达及其开关蛋白基因均与嗜盐噬菌弧菌BAL6_X的对应基因亲缘关系最近。对DA5全基因组序列的注释和功能分析, 为深入研究其捕食特性和作用机制, 并更有效地利用其防控海水养殖细菌病害提供了基础。     

岩体结构面倾向参数概率分布函数改进的Bayes推断方法

三峡船闸是世界上最大的船闸。该地区断层及节理比较发育,且具有一定的随机统计性,它对岩体力学性质起重要的控制作用。为了研究节理倾向的概率分布特征,本文引入以Bayes 最小熵优度比较检验为基础的概率分布的改进Bayes 统计推断方法,基于三峡工程永久船闸节理岩体3373 条结构面的实测参数,就对岩体力学性质起控制作用的各组结构面的倾向参数的概率分布进行了研究。文章最后还讨论了推断的最优分布参数,估计了结构面参数的检验误差范围。     

A New Sauropod, Gongxianosaurus, from the Lower Jurassic of Sichuan, China

The paper describes an early and primitive sauropod dinosaur, Gongxianosaurus shibeiensis (gen. et sp. nov.), from the Dongyuemiao Member of the Lower Jurassic Ziliujing Formation in Shibei Township, Gongxian County, Sichuan Province, China, which is one of the 5 dinosaur fossils discovered in Gongxian in 1997. Except the skull which is incomplete, the fossils are well preserved. It has some features of both sauropods and prosauropods. It is an intermediate type in the evolution of dinosaurs from prosauropods to sauropods and provides materials for the study of the origin and evolution of the sauropod dinosaur fauna. The discovery of this new sauropod furnishes a way for the stratigraphic correlation between the Early Jurassic Ziliujing Formation in the Sichuan basin and the Lower Jurassic Lufeng Formation in the Central Yunnan basin.     

川西北马脑壳金矿床流体包裹体研究及对成矿条件的制约

川西北的马脑壳金矿床为一赋存于三叠系碎屑岩、碳酸盐岩系的大型微细浸梁型金矿床,通过详细野外地质调查和室内综合研究,可将矿床的热液成矿作用划分为四个阶段,应用均一法测得：Ｉ、ＩＩ、ＩＩＩ、ＩＶ阶段的成矿温度分别为１７５～２３０℃,１７９～２５５℃,１５７～２０７℃,１２０～２００℃,峰值分别为１９０～２１０℃,２００～２３０℃,１７０～１９０℃,１３０～１７０℃,盐度变化范围,Ｉ、ＩＩ、ＩＩＩ、ＩＶ     

Local Anomalies of the Load-Unload Response of the Geomagnetic Field to Solar Wind and Earthquakes in Southwest China

Many earthquakes occurred during the period 1994 -1996 in Sichuan and Yunnan Provinces, Southwest China. Taking the process of the initial main phase recovery phase of the magnetic storm as the process of load-unload response of the geomagnetic field to the solar wind, we have estimated and analyzed the distribution in time and space of the load-unload response ratio P(z) of the storm time disturbance daily variation of the vertical component Z of the geomagnetic field at ten stations in Southwest China. We found that the area with high ratio P(z) was just the area where moderately strong earthquakes would occur from 44 days to 15 months later. The relationship between the high ratio P(z) and weather disasters in both seismic and non-seismic areas is discussed briefly.