The nonmarine environment of Quaternary foraminifers in Yanghuzhuang, China: Evidence from boron and strontium isotopes

The concentrations and isotopic compositions of boron and strontium of Quaternary foraminifera and bivalve fossils collected in the Yanghuzhuang section of Yanqing, Beijing and of modern gastropods living in the Guishul River and of river water were measured. The concentrations and isotopic compositions of Quaternary foraminifera and bivalve fossils differed from those of modern marine foraminifers and were similar to those of modern terrestrial gastropods from the Guishui Riven These results Indicate that early Quaternary foraminifera in the Yanghuzhuang section inhabited a nonmarine environment and that these foraminifera were not the result of a transgression or sea flooding. The foraminifera were not special halobios and can survive in the terrestrial condition that resembled those of the ocean.     

SrAl_2O_4：Eu~(2+)，Dy~(3+)磷光体基质的固相反应历程及成相规律

从材料物理化学角度,研究了SrAl_2O_4:Eu~(2+),Dy~(3+)磷光体基质的同相反应历程及成相规律,探明了SrAl_2O_4:Eu~(2+),Dy~(3+)磷光体基质铝酸据相的固相反应历程为:1000℃首先开始形成Sr_3Al_2O_6相,约1080℃开始形成SrAl_2O_4相,约1300℃开始形成Sr_4Al_(14)O_(25)相,高于1300℃稳定存在的不是单相,而是SrAl_2O_4和Sr_4Al_(14)O_(25)的混合相。     

K2O·4TiO2晶须与锶离子的交换及浸沥性能

为了探索高放废物的处理方式,笔者用固相合成法制备了K2O.4TiO2晶须,并以该物质作为载体,研究在不同介质、不同温度下与锶的离子交换情况和浸出性能。利用XRD,SEM对载体的物相和形貌进行了表征,利用ICP-AES测定离子交换量和浸出量。结果表明:控制合适的条件可以合成具有高长径比的四钛酸钾晶须;载体的交换量随着交换温度的提高而增大,在实验条件下交换量最高可达93%;交换后进行高温固定是必要的,最佳焙烧温度为500℃,交换样品在整个pH值范围内都具有较低的浸出率。     

溶胶-凝胶法制备(Ba,Sr)TiO3超细粉体的研究

以硝酸锶、硝酸钡、钛酸四丁酯、氨水、柠檬酸为前驱体原料,采用溶胶-凝胶法制备超细Ba0.7Sr0.3TiO3（BST）陶瓷粉体,详细研究了柠檬酸量、溶液pH值、分散剂、热处理温度对BST粉体粒径的影响。结果表明：通过控制前驱体溶液pH值可以得到均匀的溶胶。当溶液的pH值为7,分散剂含量为2.5 ml,热处理温度为800℃时,得到了性能较好的BST粉体。相比于传统工艺,热处理温度大大降低,粉体粒度分布较窄,平均粒径约为100 nm。     

Sr_4Al_(14)O_(25)∶Eu~(2 ),Dy~(3 )长余辉发光材料的合成及正交实验设计法

研究了燃烧温度、Eu2 和Dy3 的搀杂量、助熔剂硼酸的加入量、尿素加入量及Al/Sr的比例对Sr4Al14O25∶Eu2 ,Dy3 长余辉发光材料发光性能的影响,从而确定了长余辉发光材料Sr4Al14O25∶Eu2 ,Dy3 的最佳合成工艺.对所得产物分别进行了XRD、TEM、荧光测试和亮度测试.结果表明:磷光体存在403和482 nm 2个发射峰,分别对应于Eu2 在基质中2种不同的存在方式,与传统的高温固相法相比发射主峰出现了蓝移;亮度测试找到了最佳的原料配比及合成条件.     

广西凤山县鸳鸯泉水文地质成因探讨

【目的】研究凤山县鸳鸯泉的水文地质成因,为鸳鸯泉这一地质奇观提出科学的解释。【方法】根据实地调查和现场试验,结合地层岩性、地质构造以及岩溶发育情况,查明鸳鸯泉的岩溶水文地质条件;根据地下水示踪试验,确定鸳鸯泉的源头和主要的岩溶含水介质类型,并通过稳定氢氧同位素和钙锶比(Ca/Sr)分析,研究管道介质岩溶大泉的补径排过程和水循环特征。【结果】鸳鸯泉的源头为年里落水洞补给的外源水,公塘和母塘两个出口的主径流管道基本一致;鸳鸯泉具有以岩溶管道为主的含水介质特征,以及快速流的补给、径流和排泄过程。这种水文地质现象的成因与管道流集中排泄的方式有关。【结论】鸳鸯泉同属于一个管道系统,管道流的两个出口在水循环速度上存在差异,相比公塘,母塘具有较短的径流途径和较快的更新速率。     

Age and genesis of the Myanmar jadeite: Constraints from U-Pb ages and Hf isotopes of zircon inclusions

Myanmar jadeite (jadeitite) is well known for its economical value and distinctive tectonic locality within the collisional belt between India and Eurasian plates. However, it is less studied for its genesis and geodynamic implications due to precipitous topography, adverse weather and local military conflicts in the area. By means of combined ICP-MS and LA-MC-ICPMS techniques, we have carried out in-situ trace elements, U-Pb and Lu-Hf isotopes for zircon inclusions in a piece of jadeite gem sample. CL imaging suggests that the zircons are metasomatic in origin, and contain mineral inclusions of jadeite and omphacite. Seventy-five analyses on 16 grains of the zircons yield a U-Pb age of 158 ± 2 Ma. The Myanmar zircons differ from other types in that they have no significant Eu anomalies despite high HREE concentrations. Measured ¹⁷⁶Hf/¹⁷⁷Hf ratios range from 0.282976 to 0.283122, with an average value of 0.283066 ± 7; ε_Hf(t) value of 13.8 ± 0.3 (n=75). These results indicate that the Myanmar jadeite was formed in the Late Jurassic, probably by interaction of fluid released from subducted oceanic slab with mantle wedge. Therefore, its formation has no genetic relationship to the continental collision between Indian and Euroasian plates. Supported by National Natural Science Foundation of China (Grant No. 40673039) and the Science Plan Foundation of Guangdong (Grant No. 2007B031200005)     

焦磷酸锶镁：锡荧光体的发光特性

用高温固相反应法合成了（Ｓｒ１－ ｘ Ｍｇｘ ）２ Ｐ２Ｏ７ ∶Ｓｎ（３．３×１０－ ２ ）和（Ｓｒ０．９Ｍｇ０．１ ）２ Ｐ２Ｏ７ ∶ｘＳｎ两个体系系列样品,在紫外线激发下,详细地测量了它们的发射光谱,讨论了Ｍｇ 含量对（Ｓｒ１－ ｘ Ｍｇｘ ）２Ｐ２Ｏ７ ∶Ｓｎ 和Ｓｎ 含量对（Ｓｒ０．９ Ｍｇ０．１ ）２Ｐ２ Ｏ７ ∶ｘＳｎ 体系发光性能的影响,认为（Ｓｒ０．９Ｍｇ０．１ ）２Ｐ２Ｏ７ 是Ｓｎ２＋ 较好的一种基质材料．     

峨眉山柿子坪热田地下水碳氧同位素特征初步研究

在峨眉山柿子坪热田地质调查及热水勘探过程中 ,采用了碳、氧同位素地球化学方法 ,结果发现不同成因类型的地下水其碳、氧同位素组成特征各不相同 ,为查明地下热水的形成条件提供了重要依据 ,表明用地下水中 HCO-3 的碳、氧同位素组成来研究地下热水系的发育特征是有前景的     

华南晚泥盆世腕足动物壳体保存状况及其氧碳同位素比较研究

对华南湘中地区上泥盆统弗拉/法门(F/F)界线附近的几种腕足动物化石壳体结构所进行的详细研究表明,其原始结构主要表现为两种类型：一是具有棱柱状第三层,二是缺失棱柱状第三层。基于壳体保存程度的详细分析,以阴极发光程度、壳体显微结构为参数建立了壳体成岩作用改造程度的量化模式,经化石壳体氧、碳同位素值的验证,这一模式基本可以用来对不同保存环境下的样品进行筛选。在对比研究中发现,以无洞贝目(Atrypida)为代表的具有柱状第三层结构的样品不仅在保存状况上优于只具有纤维层结构的壳体,而且其氧、碳同位素数值的分布也较为集中,从而说明无洞贝目的壳体是进行氧、碳同位素研究较为理想的材料。