南海IODP 349航次U1434站位海相红层成因——来自漫反射光谱与X荧光光谱的制约

提出IODP349航次首次在南海发现的大洋红层,与ODP124 航次苏禄海、苏拉威西海大洋红层以及三水盆地陆相红层相似,都具有直接覆盖于大规模岩浆岩之上的特征,对于揭示红层与岩浆热事件的关系具有重要意义。自上而下采集U1434站位灰绿色-红棕色海相沉积序列进行测试分析,并设计实验模拟沉积-成岩过程中氧逸度和地热温度对红层色素形成的控制作用,通过红色与非红色沉积、实测与实验样品的对比分析,探讨红层成因机制及其地质意义。采用漫反射光谱、荧光光谱分析以及二价铁滴定测试,量化分析了海相沉积与实验样品的颜色红度值、针铁矿、赤铁矿与不同价位铁元素的含量,得到以下新认识：U1434站位红色-非红色海相沉积均形成于较高的氧逸度条件,水体氧化还原环境的差异并不是控制红色与非红色沉积的主要因素;U1434站位大洋红层直接覆盖大洋玄武岩,起源于沉积-成岩阶段的高地温作用;陆相红层和白垩纪海相红层均分布于相应时期的构造-岩浆活动带,暗示了红层对地质热事件具有重要的指示意义。     

中国化学史研究的重要奠基者曹元宇

化学史学家、化学教育家、书画家、诗人曹元宇从研究中国古文献《道藏》中的化学开始,发表了《中国古代金丹家的设备和方法》,开创了中国炼丹术研究的先河;出版了《中国化学史话》,对中国化学史研究及教育做出了重要贡献。     

Introduction to the overall physics design of CSNS accelerators

The China Spallation Neutron Source (CSNS) is an accelerator-based facility. The     

Regional characteristics of naturally occurring radionuclides in surface sediments of Chinese deserts and the Keum River area of Korea

Naturally occurring radionuclides (NORN) such as ⁴⁰K, ²²⁶Ra and ²³²Th from 44 surface sediment samples collected from four desert regions of Chinese were determined to investigate the regional characteristics of the source areas of Asian dust. The radionuclides for 41 surface sediment samples collected from seven sites of the Keum River area in Korea were also determined to compare the regional characteristics with the Chinese desert area. The specific activities (SA) and the specific activity ratios (SAR) of the radionuclides were investigated for distinguishing the source region of Asian dust. The SA of ²²⁶Ra and ²³²Th as well as the SAR of ²²⁶Ra/⁴⁰K and ²³²Th/⁴⁰K were found to be useful to characterize source area and tracing Asian dust.     

东南部欠发达地区县域城乡空间统筹发展的规划思考

随着国内区域经济联动的加强,产业布局的调整升级,以及大区域交通条件的改善,我国城市化经济已经进入了一个＂全球化-区域化＂的新发展时期.东南部欠发达地区的城市化、工业化发展面临着若干重大机遇.通过分析县域城乡空间发展存在的一般性问题和制约因素,提出：东南部欠发达地区的发展应以空间规划作为切入点,通过空间规划与行动集成,将城乡统筹概念落实到县域空间层面上,构建一个综合的发展战略与行动规划.     

汝阳地区熊耳群火山岩内夹层硅质岩的微区特征及地质意义

熊耳群是前寒武纪火山-沉积作用的产物,其顶部的马家河组(玄武)安山质火山岩内发育了夹层状热水成因硅质岩。选择熊耳群马家河组硅质岩夹层中的碧玉岩为对象,利用偏光显微镜,XRD,Raman和EBSD等方法剖析了其微区特征。研究结果显示：硅质岩内石英颗粒的显微镜和EBSD照片均表现出颗粒细小、结晶程度低和紧密堆积结构等特点,这完全吻合热水沉积硅质岩的特征;硅质岩内粒径不同的颗粒呈条带(或薄层)状交互出现,不同条带(或薄层)内矿物的组成存在明显的差异,这应该反映了原始物质供给的周期性变化;XRD分析结果指示硅质岩内的主要矿物为低温石英,其晶胞参数为a=b=0.491 3 nm,c=0.540 5 nm和Z=3;EBSD照片和Raman分析结果显示硅质岩内微量的杂质矿物形成于不同阶段,其中粘土矿物和黄铁矿呈零星分布并反映了原始沉积成因,长英质矿物和铁镁硅酸盐矿物均来源于火山凝灰质沉积;火山凝灰质矿物的颗粒偏大并构成了硅质岩内的粗颗粒条带(或薄层),它们与热水沉积为主的细颗粒矿物条带(或薄层)交互产出,这反映了火山作用的周期性反复活动;后期的碳酸盐热液沉淀于硅质岩内裂隙中,它们还导致石英颗粒边缘有序度升高。虽然熊耳群硅质岩内的矿物种类和成因均极为复杂,但火山物质的输入是导致熊耳群硅质岩SiO₂含量偏低的根本原因并得到了硅质岩内大量火山成因矿物的证实。在硅质岩的微组构研究中,Raman光谱分析可以有效的揭示微区上矿物的类型、微区结构及有序度,这些特征是反映硅质岩内部矿物形成与演化过程中微区变化的重要信息。     

Introduction to the CDEX experiment

It is believed that weakly interacting massive particles (WIMPs) are candidates for dark matter (DM) in our universe which come from outer space and might interact with the standard model (SM) matter of our detectors on the earth. Many collaborations in the world are carrying out various experiments to directly detect DM particles. China Jinping underground Laboratory (CJPL) is the deepest underground laboratory in the world and provides a very promising environment for DM search. China Dark matter EXperiment (CDEX) is going to directly detect the WIMP flux with high sensitivity in the low WIMP-mass region. Both CJPL and CDEX have achieved a remarkable progress in recent three years. CDEX employs a point-contact germanium (PCGe) semi-conductor detector whose energy threshold is less than 300 eV. In this report we present the measurement results of muon flux, monitoring of radioactivity and radon concentration carried out in CJPL, as well describing the structure and performance of the 1 kg-PCGe detector in CDEX-1 and 10 kgPCGe detector array in CDEX-10 including the detectors, electronics, shielding and cooling systems. Finally we discuss the physics goals of CDEX-1, CDEX-10 and the future CDEX-1T experiments.     

基于灰色关联度的中国海洋产业结构分析

简要分析了中国海洋经济的发展现状与趋势, 着重对我国主要海洋产业进行了关联度分析, 得出我国海洋经济的支柱产业和主导产业以及海洋产业结构存在的问题, 并据此提出了中国海洋产业结构优化升级对策等方面的建议.