M_2RSbO_6:R~(3+)复合氧化物的合成组成结构和性能的研究(M = Ba、Sr、Ca, R = La、Gd、Y、Bi, R' = Sm、Eu、Dy、Ho、Er、Tm)

对于稀土与非稀土所组成的二元复合氧化物的研究国外已有较多的报导。但是，对于稀土和锑的复合氧化物只是近年来才开始有些研究工作。含锑与稀土的多元复合氧化物的报导就更少。本文在我们实验室张静筠等人三元复合氧化物研究的基础上，开展Mo—Sb_2O_5—R_2O_3—R'_2O_3—Bi_2O_3多元体系的研究工作，这对于我国丰产元素稀土和锑的应用以及利用Bi~(3+)的激活与敏化将是有益的。本文按Thornton等人的方法合成了Ba_2BiSbO_6，Ba_2GdSbO_6，按EγΦECEHKO等人的方法合成了M_2RSbO_6 (M = Ba、Sr、Ca, R = La Y)。并以M_2RSbO_6为基质，掺Sm~(3+)、Eu~(3+)、Dy~(3+)、Ho~(3+)、Er~(3+)、Tm~(3+)和Bi~(3+)，研究它们的化学组成，晶体结构与发光性能的关系及规律，Bi~(3+)的荧光和敏作用。同时研究了它们的磁学和热学性能。化学组成的分析结果表明，计算的含量与实验测得的含量符合较好，说明化学反应是按化学计量比进行的。通过X-射线粉沫物相分析和晶胞参数的理论计算确定M_2RSbO_6(M = Ba、Sr、R = La、Y、Gd、Bi)复合氧化物是属于立方钙钛太型化合物。空间群为Fm3m，点群为Oh。用计算机计算了Ca_2YSbO_6的晶胞参数并结合荧光光谱分析确定它属于畸变的单斜钙钛矿，空间群为P_(21)。用磁天平测量了样品M_2RSbO_6 (M = Ba、Sr、Ca; R = Gd、Y、Bi)的磁化率。除Ba_2GdSbO_6是顺磁性物质外共余的都是反磁性的物质。按所用原料Sb_2O_5计算的磁化率与测量值符合较好，表明在所研究的M_2RSbO_6化合物中锑是正五价的。用热重热差分析仪测量了样品在反应中的热性能，观察到在化合物形成的过程中所用原料Sb_2O_3大约在520 ℃左右氧化变为Sb_2O_5。除所用原料碳酸盐分解外没有挥发性的物质，这就进一步证明化学组成分析和磁化率测量的结果是正确的。光学测量的结果表明，所有的磷光体随着激活离子浓度的不同其光谱都发生规律性的变化。对于不同Eu~(3+)浓度的Ba_2YSbO_6:Eu~(3+)和Br_2YSbO_6:Eu~(3+), Bi~(3+)体系用254nm激发时均能观察到Eu~(3+)于595nm的尖峰发射。用基质和Bi~(3+)的激发峰325nm激发时，明显地看到敏化剂Bi~(3+)到Eu~(3+)的能量传递，使Eu~(3+)于595nm的发射大大增强，我们认为Bi~(3+)对Eu~(3+)的敏化作用是由于基质和Bi~(3+)的~1S。→ 3P_1的跃迁吸收了激发的能量，然后无辐射弛豫到Eu~(3+)的激发态~5D_0，产生~5D_0 → 7F_1的磁偶极跃迁。对于不同Eu~(3+)浓度的Sr_2YSbO_6:Eu~(3+)和Sr_2YSbO_6:Eu~(3+), Bi~(3+)体系用245nm激发时均能观察到Eu~(3+)于595nm的尖峰发射。用基质和Bi~(3+)的激发峰335nm激发时，观察到基质和Bi~(3+)对Eu~(3+)具有某种能量传递。敏化作用机理与上述的Ba_2YSbO_6:Eu~(3+)和Ba_2YSbO_6:Eu~(3+), Bi~(3+)体系相同。对于不同Eu~(3+)浓度的Ca_2YSbO_6:Eu~(3+)和Ca_2YSbO_6:Eu~(3+), Bi~(3+)体系用396nm激发时，均能观察到Eu~(3+)于613nm很强的尖峰发射。用基质和Bi~(3+)的激发峰313nm激发时，见到Bi~(3+)和基质对Eu~(3+)具有某种能量传递，这种敏化作用主要是由于基质和Bi~(3+)的3P_1 → ~1S_0的400nm的宽带发射和Eu~(3+)的~7F_0 → ~5L_6的396nm的吸收相匹配产生~5L_6→~5D_0→~7F_2的跃迁。通过对激发光谱和荧光光谱的分析给出了Ca_2Y_(0.96)Eu_(0.04)SbO_6的能级图，从实验上可见，Eu~(3+)的发光强烈地依赖于钙钛矿的结构，当Eu~(3+)在空间群为Fm3m 的Ba_2YSbO_6和Sr_2YSbO_6中处于Oh点对称性时，主要是~5D_0 → ~7F_1的磁偶极跃迁。当Eu~(3+)在空间群为P_(21)的单斜钙钛矿中时，主要是~5D_0 → ~7F_2的电偶极跃迁。对于不同掺杂浓度M_2YSbO_6:R~(13+)(M = Ba、Ca; R' = Sm、Dy、Ho、Er、Tm)体系，通过激发和荧光光谱的研究，合理地确定了谱项。发现基质对Sm~(3+)、Dy~(3+)、Ho~(3+)具有敏化作用。对不同Bi~(3+)浓度的Ca_2YSbO_6:Bi~(3+)，由激发和荧光光谱可见Bi~(3+)具有二个激发带，第一激发带位于240nm处相当于~1S_0 → ~1P_1的跃迁，第二激发带位于315nm处相当于~1S_0 → ~3P_1的跃迁。有一个很强的兰紫色发射位于400nm处相当于~3P_1 →~1S_0的跃迁。

黄土高原植被恢复与新产业带形成的生态学基础研究

从生态地理背景论草地畜牧业产业在黄土高原农业可持续发展中的战略地位 黄土高原要实现生态与生产双赢的目标，契机是退耕还林还草，突破口是建立能兼顾生态生产协调发展的主导产业。从地形地貌、水热分布及自然植被特征的角度分析，黄土高原实施以农为主或农林牧综合发展的方略，均有悖于黄土高原生态地理背景。而草地畜牧业产业的生产要素及其过程在较大程度上吻合了黄土高原的生态地理背景，具有生态的适应性和生产的有效性，应作为黄土高原优化的生态生产范式建制中的主导产业。未来黄土高原产业的发展格局应该是以草地畜牧业为主导，农业和林业作为补充和完善的产业发展体系。此外，未来黄土高原草地畜牧业家畜养殖应以舍饲为主。 黄土高原自然植被演替过程中的物种特征与土壤养分动态研究 在3—149年的时间尺度上，对黄土高原自然植被次生演替过程中物种特征和土壤养分动态进行了研究。结果表明：1）随着演替时间尺度的延伸，土壤全C、全N含量呈增加趋势，而土壤全K、全Na和土壤pH值呈下降趋势，土壤全P变化趋势不明显;此外，表层( 0~10 cm)土壤Ca0含量呈下降趋势，深层( 20-30 cm，40-50 cm)则呈增加趋势。演替过程对土壤养分动态影响的程度随着取样深度的增加而减弱;2）植物群落物种丰富度在演替的中间阶段最高，后者对应于中等土壤养分水平;3）在演替的早期阶段，植物群落优势种往往具有稳定的土壤种子库，CR-生活史对策和S．繁殖对策，在贫瘠的土壤上具有较强的竞争能力;而具有较强的水平扩展能力和克隆繁殖能力，C-生活史对策、对土壤C，N具有较强竞争能力的多年生植物在演替中后期占据群落的优势地位。此外，在所涉及的物种生物学特征中，多年生生活史，C-、CR-、SC-、SR-、S．对策，以及R-、W-、Bs-、VBs-和V-繁殖对策等在非优势物种中有较高的出现频率。4）C-、 SC-对策，克隆能力，多年生生活史，水平扩展能力，种子的动物传播方式，秋季开花，荚果、坚果等特征的比例在一定程度上与土壤全C，全N和全K含量正相关; 而S一、SR-、R-、CR-对策，一、二年生生活史，种子繁殖，S．繁殖对策，以及胞果、蒴果等特征的比例与土壤全Na，Ca0含量和土壤pH正相关。在演替过程中出现的物种均属草本植物生活型，因此，草原可能是黄土高原上受制于大尺度环境条件（显域生境）下的优势植被类型（特别是降雨量不超过550 mm的地区）。 黄土高原植被恢复过程中几种优势植物叶片碳稳定性同位素和氮含量的动态特征 探讨了黄土高原植被恢复过程中六种优势植物叶片碳稳定性同位素(6 13C)和氮含量的季节动态、种间差异及其与植被恢复过程的关系。六种优势植物分别是猪毛蒿( Artemisia scoparia)，出现在演替的先锋阶段：达乌里胡枝子( Lespedeza davurica)，出现在演替的第二阶段;长芒草(Stipabungeana)、万年蒿(Artemisia gmelinii)和茭蒿(Artemisia giraldii)，出现在演替的第三阶段; 白羊草( Bothriochloa ischaemun)出现在演替的顶级阶段。六种优势植物叶片碳稳定性同位素比率分别是-26.89±0.66‰，-26.24±0.48‰, -26.21±0.49‰, -26.86±1.09‰, -27.61±0.39‰和-15 .81±1. 79‰;氮含量分别是2.36±0.63%，2.38±0.29%，2.0±0.29%，2.0±0.25%，1.50±0.37% 和1.24±0.19%。白羊草、长芒草、茭蒿和达乌里胡枝子叶片氮含量季节变化与土壤水分呈正相关．猪毛蒿和铁杆蒿叶片氮含量季节变化与土壤水分呈负相关。白羊草叶片δ 13C与土壤水分呈正相关，而其他5个优势种叶片δ 13C与土壤水分呈负相关。不同演替阶段优势种的δ 13C值和氮含量特征表明：处于演替顶级阶段的优势种具有最高的水分利用效率，净光合产量较低，但光合作用动态对土壤水分的季节波动表现出较强的可塑性;相反，处于先锋阶段的优势种水分利用效率较低，叶片净光合产量较高，光合作用对土壤水分波动的可塑性较低。本文的主要结论是：黄土高原植被恢复过程中处于不同演替阶段的优势种无论是在叶片δ 13C，氮含量均存在差异。优势种叶片δ 13C和氮含量季节动态反映了不同物种在环境（主要指土壤水分）波动条件下的生理生态对策。具有最高的水分利用效率（而非最高光和能力）和最高光合可塑性的物种将成为黄土高原自然植被顶级植物群落中的最终统治者。 黄土高原草地畜牧业产业形成与发展的牧草生产力基础 遵循生产-生态兼顾的原则，在黄土高原197个区县土地利用方式重新规划的基础上，对支撑黄土高原畜牧业产业形成与发展的牧草生产潜力进行了分析预测。结果表明：规划的牧、林、农、果用地占生产用地的比例分别是草地44%、林地22%、基本农田20%、果园14%; 197个县区预测的总牧草生产潜力达1，0488，1028t.y-l，可载畜1，0488，1028个羊单位．y-1。按1999年不变价格计算，黄土高原预测的畜牧业总产值将达到524，4051万元．y-1，是1999年畜牧业总产值的5.3倍，超过1999年黄土高原农业总产值14 %。农业人口人均预测畜牧业产值大于1000元的区县占59%;小于1000元的区县占41%。此外，黄土高原预测的农业总产值将达到1147.2234亿元RMB.yr-1。畜牧业、果业、林业和基本农田产值占农业总产值的比例分别是46%、27%、14%和13%。随着畜牧业产业链的逐步建立与完善，产业发展布局的日趋合理，黄土高原畜牧业生产总值将有较大幅度的提高。黄土高原草地畜牧业蕴藏着巨大的发展潜力，有望成为黄土高原优化的生产．生态范式建制中的主导产业。

冲绳海槽西南端中全新世以来的沉积特征及其物源与环境意义

作为大陆向大洋的过渡带，由于享有得天独厚的沉积环境，具有独特的构造特征以及与黑潮主流之间的密切关系，一直以来，冲绳海槽都是中外学者研究的重点靶区。2005年5月，由我国与法国联合主持的IMAGES 航次在台湾东北海域获取MD05-2908柱状岩芯（24º48.04′N,122 º29.35′E,水深为1275米），该柱状岩芯为一34.17米长高质量的连续沉积记录，岩性以深灰色粘土质粉砂为主，含水量较高，粘性、可塑性强，含有数层厚度不等的夹层。岩芯年龄模式依据17个AMS 14C定年数据建立，岩芯底部年代约6.8ka，为中全新世以来的沉积。在实验室对样品按照2cm的间隔进行分割后分别进行了粒度分析、粘土矿物提取与测试、碎屑矿物提取与鉴定、常微量元素和稀土元素分析等实验。 粒度分析结果显示，MD05-2908岩芯沉积物粒度垂向上总体比较均一，以细颗粒的粘土与粉砂质为主，但不同层位也稍有差别，表现为底部层位粒度较粗，含砂量较高，说明底部沉积环境比较复杂。粘土粒级（<2µm）矿物主要由四种粘土矿物和少量石英、长石碎屑组成。其中，粘土矿物相对含量变化中，伊利石（～68％）与绿泥石（～17%）构成主要成分，含有蒙皂石（～10％）和高岭石（～5％）。结合台湾东北外海表层沉积物的研究，利用粘土矿物伊利石/蒙皂石和绿泥石/高岭石比值得出岩芯粘土矿物主要为陆源碎屑粘土矿物，其源岩主要为台湾中央山脉的变质岩与台湾东部的沉积岩。重矿物分析共选取了41个层位，对63~250μm粒级的样品在实体镜和偏光显微镜下进行鉴定，结果显示，岩芯重矿物主要由绿泥石（29%）、普通角闪石（22%）、白云石（10%）、黑云母（8%）、绿帘石（7%）、白云母（7%）、褐铁矿（5%）等组成。稳定矿物少，矿物成熟度低。碎屑矿物风化程度低，磨蚀不明显，分选较差，表明沉积物来自于近源，后期改造作用不明显。常量元素分析结果表明，SiO2 、Al2O3和Fe2O3是岩芯沉积物中的最主要组分，这三种组分占沉积物总量的82%左右。 整个岩芯自下而上各常量组分变化不大，其平均值与东海陆架沉积物基本接近。微量元素变化比较明显， Ba、Cr、Cu、Zn元素的含量比东海陆架沉积物中的含量要高，而Sr的含量明显低于东海陆架。对常微量元素的R型因子分析表明，常量元素SiO2、Al2O3、Fe2O3、MgO和K2O，微量元素Cr、Cu、Ni、Zn、Pb、Rb和Mn可代表陆源物质；常量元素CaO和微量元素Sr、Ba可代表生物源物质。岩芯沉积物以陆源物质为主，生源物质的贡献起次要作用。岩芯沉积物中稀土元素总量平均为169.87×10-6，并且轻稀土含量均高于重稀土，LREE/HREE平均值为10.14，表明了轻稀土对稀土总量的贡献远高于重稀土，沉积物富集轻稀土，反映了沉积物的陆源特征。 岩芯MD05-2908中全新世以来平均5m/ka的高沉积速率主要源于丰富的物质供应和适宜的沉积环境。岩芯细粒级沉积物中，地球化学特征表明沉积物主要来源于陆源碎屑物质，粘土矿物特征与台湾东部陆源物质相同；粗粒级沉积物中，重矿物含量及矿物特征也表明岩芯沉积物粗颗粒组分主要来自于近源沉积。台湾宜兰境内的兰阳溪每年携带约一千万吨冲积物入海成为研究区重要的物质来源。由于受到黑潮的强烈影响，逆时针涡流及底层反向流的存在是岩芯高沉积速率重要控制因素。因此，利用动力分选的粉砂组分可以用来示踪古洋流强度，结果显示，6.8ka以来黑潮的强弱波动频繁，并表现出一定的旋回性变化，频谱分析表明，其具有的千年尺度周期（1500a）、百年尺度周期（604a、242a、192a、153a、133a）与十年尺度周期（22a）的周期性变化均与太阳辐射量变化有密切关系，因此，黑潮的强弱变化在大背景上是由太阳活动所控制的。 根据测年资料可以识别出岩芯存在5期快速堆积事件，这与区域性降水增加有关，降雨量增加导致陆源物质输入的增加。另外，岩芯位于大陆斜坡区，附近存在有三支海底峡谷，并且地震活动频繁，沉积在宜兰陆架及东海陆架处的浅海沉积物由于受到地震、风暴等活动的影响而受扰动崩塌、因重力作用而向低处输送，产生二次侵蚀并经由海底峡谷搬运到冲绳海槽南段堆积,使得沉积环境更为复杂，但同时也为冲绳海槽提供了丰富的物质供应。

Chemical bond characteristics, thermal expansion property and compressibility of AR(2)O(4) (A = Ca, Sr, Ba; R = rare earths)

Theoretical researches were performed on the CaFe2O4-type binary rare earth oxides AR(2)O(4) (A = Ca, Sr, Ba; R = rare earths) by using chemical bond theory of dielectric description. The chemical bond properties of these crystals were explored, and then the thermal expansion property and compressibility were studied. The theoretical values of linear thermal expansion coefficient (LTEC) and bulk modulus were presented. The calculations revealed that the LTECs and the bulk moduli do have linear relationship with the ionic radii of the rare earths. In the cases of Sc and Y, both the LTEC and bulk modulus values are larger than the lanthanide series. We attribute this to the difference in the electronic configuration between Sc (Y) and lanthanide series. For SrY2O4 and BaY2O4 crystals, the theoretical values of LTEC and bulk modulus agree well with experimental ones.

Design of Low Power Multi-Standard Active-RC Filter for WLAN and DVB-H

In this paper, a low-power, highly linear, integrated, active-RC filter exhibiting a multi-standard (IEEE 802.11a/b/g and DVB-H) application and bandwidth (3MHz, 4MHz, 9.5MHz) is present. The filter exploits digitally-controlled polysilicon resister banks and an accurate automatic tuning scheme to account for process and temperature variations. The automatic frequency calibration scheme provides better than 3% corner frequency accuracy. The Butterworth filter is design for receiver (WLAN and DVB-H mode) and transmitter (WLAN mode). The filter dissipation is 3.4 mA in RX mode and 2.3 mA (only for one path) in TX mode from 2.85-V supply. The dissipation of calibration consumes 2mA. The circuit has been fabricated in a 0.35um 47-GHz SiGe BiCMOS technology, the receiver and transmitter occupy 0.28-mm(2) and 0.16-mm(2) (calibration circuit excluded), respectively.

高Tc超导体R_1Ba_2Cu_3O_(2-x)(R-rare earth)的磁性和超异电性研究

本论文合成了R_1Ba_2Cu_3O_(2-x) (R = La、Nd、Sm、Eu、Gd、Dr、Ho、Er、Tm、Yb)、Y_2Ba_2Cu_3O_(2-x) (x = 0.10～1.17)和Y_1Ba_2Cu_3O_(7-x)S_x (x = 0～2)，并对磁性和超导电性进行了较为系统的研究。R_1Ba_2Cu_3O_(2-x)的磁化率在T > Tc的很宽的温度范围内服从Curic-Weiss定律，求得的有效磁矩略大于理论值，差值与Y_1Ba_2Cu_3O_(2-x)中Cu~(2+)磁矩相近，说明Cu~(2+)的磁矩对体系磁性有额外贡献，这贡献随R~(3+)离子中自旋平行的电子权的增多而增大。其高温下的磁化率CT > 700K)相对Curic-Weiss定律发生较大偏离，这偏离可能的来源有三个：高温下稀土离子发生较大的能级反转效应，高温下结构相变对磁性的影响，高温下氧含量减少造成Cu~(2+)磁矩增大。R_1Ba_2Cu_3O_(2-x)磁化率在T < Tc时也服从Curic-Weiss定律，R~(3+)磁矩是定域的，表明超导与磁性相互独立。互不相关，稀土磁矩与传导电子间无相互作用。用Sr取代R_1Ba_2Cu_3O_(2-x)中的Ba，没能使体系产生磁有序的变化，但却使有效磁矩增大，并完全破坏了样品的超导电性。Sm~(3+)磁化率不服从Curic-Weiss定律，在Sm_1Ba_2Cu_3O_(2-x)中Sm~(3+)显示了典型Van VlccK离子的特性。Y_1Ba_2Cu_3O_(2-x)随氧含量减少发生超导体一半导体一绝缘体的转化，当氧含量由6.90减小至6.49时发生由正交到四方的结构相变。当(7-x) = 5.83时有较多杂质相出现，123相开始分解。样品磁化率均服从Curic-Weiss定律，并随氧含量增大磁化率－温度曲线越来越趋于平缓（直线），当(7-x) = 6.90时磁化率基本不随温度变化，这时Pauli顺磁性占主导地位，这说明氧含量增加定域磁矩减少，求得的有效磁矩Peff随氧含量增大总趋势减小。提出了电子“巡游”的观点，较好地解释了上述现象，并推测出Cu(2)的d电子是离域的，对样品磁矩没有贡献，样品Peff来源于部分Cu(1)的定域Cu~(2+)的磁矩，上述推测被EPR结果证实。正交相Y_1Ba_2Cu_3O_(2-x)的EPR谱显示了中心对称成准立方晶场中Cu~(2+)(d~9, S = 1/2, I = 3/2)的EPR物性。而四方相样品的EPR谱却出现了明显的各向异性，说明观察到的为Cu(1)的EPR信号，由Cu(1)~(2+)的写域磁矩产生。Y_1Ba_2Cu_3O_(2-x)的EPR信号束源于本体相，而非Y_2Cu_2O_5、BaCuO_2、Y_2BaCuO_5等杂质相。各样品EPR信号的自旋浓度远小于1spin/cu，并随氧含量减小而增大，当(7-x) = 6.49、6.40时自旋浓度出现陡增，这时伴随由正交到四方的转化，证明了电子“巡游”观点的正确。用硫部分取代Y_1Ba_2Cu_3O_2g中的氧，当Y_1Ba_2Cu_3O_(2-x)Sx中x = 0.11时Tc = 92.6K，比Y_1Ba_2Cu_3O_(7-x)升高2K，但由于杂质相的存在，ΔTc加宽。其他样品多为半导体和绝缘体。硫取代0，当x = 0.04，0.06，0.11和1.20时磁化率服从Curic-Weiss定律，并且x = 0.87，1.2时分别在230K、240K出现反铁磁有序。其他样品由于Cu被还原为＋1价而变成抗磁性。x = 0.11 (Tc = 92.6K)，EPR谱为正交场中Cu~(2+)的信号。自旋浓度与温度无关。当所有Cu均为Cu~(1+)时，测问的是-s-的EPR信号，而Cu为混合价态(+1和+2时)测问是上述两种信号的叠加。

Comparative study on the doping effect of 3d elements in Bi(1.5)Pb(0.2)Sr(2)Ca(2)Cu(2.8)M(0.2)O(y) (M=Sc,Ti,V,Cr,Mn,Fe,Co,Ni, or Zn)

With XRD, R-T, and ac chi measurements a comparative study on the doping effects of 3d elements in Bi(1.5)Pb(0.2)Sr(2)Ca(2)Cu(2.8)M(0.2)O(y) (M = Sc, Ti, V, Cr, Mn, Fe, Co, Ni, or Zn) has been carried out. The effects of the former five members are significantly different, both on phase formed and on T-c, from the latter four. It seems that the effect on phase stabilization correlates with the valency of the doped cation. In connection with the instability of the 2223 phase, the correlation has been discussed.

LUMINESCENCE OF BI(3+) AND THE ENERGY-TRANSFER FROM BI(3+) TO R(3+) (R=EU,DY,SM,TB) IN ALKALINE-EARTH BORATES

At room temperature, the Bi3+ ion shows broad band characters of its luminescence in Ca2B2O5, M3B2O6 ( M=Ca,Sr ) and SrB4O7. The maxima of the Bi3+ S-1(0)-->P-3(1) absorption bands are located in the range of 240-300nm, but the energy variation of the corresponding P-3(1)-->S-1(0) emissions is very large. The maxima of these emission bands change from 350nm in Ca3B2O6;Bi3+ to 586nm in SrB4O7:Bi3+. The Stokes shift of the Bi3+ luminescence increases from 6118 cm-1, in Ca2B2O5:Bi3+, to 24439 cm-1, in SrB4O7:Bi3+. The emission intensity of the Bi3+ luminescence increases with the decreasing Stokes shift. It has been found that in Ca2B2O5, the Bi3+ ion could transfer its excitation energy to the R3+ ions ( R=Eu, Dy, Sm, Tb ) , but in, Ca3B2O6 and Sr3B2O6, only Bi3+-->Eu3+ was observed. No energy transfer from Bi3+ to R3+ was detected in SrB4O7.

湘中锡矿山锑矿床的Sr同位素地球化学

对湘中锡矿山锑矿床围岩灰岩、硅化灰岩、煌斑岩和脉石矿物进行了系统的Sr同位素研究。结果表明，矿区围岩发生了隐性蚀变，灰岩中Sr亏损，而^87Sr/^86Sr高于同时代的海相碳酸盐，这种隐性蚀变很可能是水／岩反应所致。矿体附近的硅化灰岩中Sr更加亏损，而^87Sr/^86Sr明显增加。成矿期方解石的^87Sr/^86Sr较高，成矿体系中变化的W／R比造成了方解石中^87Sr/^86Sr值的明显波动。成矿流体为一富放射成因^87Sr的溶液。成矿流体来自或流经基底地层，流体中的Sr由基底碎屑岩提供，矿质Sb也可能主要来自富Sb的元古宇基底。水／岩反应的理论模拟显示，锡矿山成矿流体中的Sr约为3．0μg/g，^87Sr/^86Sr为０．７１７；蚀变－成矿体系为一开放体系，矿石的沉淀机制主要为水／岩反应，成矿体系中W／R 比较高。

The Displacement and Strain Field of Three-Dimensional Rheologic Model of Earthquake Preparation

Based on the three-dimensional elastic inclusion model proposed by Dobrovolskii, we developed a rheological inclusion model to study earthquake preparation processes. By using the Corresponding Principle in the theory of rheologic mechanics, we derived the analytic expressions of viscoelastic displacement U(r, t) , V(r, t) and W(r, t), normal strains epsilon(xx) (r, t), epsilon(yy) (r, t) and epsilon(zz) (r, t) and the bulk strain theta (r, t) at an arbitrary point (x, y, z) in three directions of X axis, Y axis and Z axis produced by a three-dimensional inclusion in the semi-infinite rheologic medium defined by the standard linear rheologic model. Subsequent to the spatial-temporal variation of bulk strain being computed on the ground produced by such a spherical rheologic inclusion, interesting results are obtained, suggesting that the bulk strain produced by a hard inclusion change with time according to three stages (alpha, beta, gamma) with different characteristics, similar to that of geodetic deformation observations, but different with the results of a soft inclusion. These theoretical results can be used to explain the characteristics of spatial-temporal evolution, patterns, quadrant-distribution of earthquake precursors, the changeability, spontaneity and complexity of short-term and imminent-term precursors. It offers a theoretical base to build physical models for earthquake precursors and to predict the earthquakes.

微碳深冲钢板的非｛111｝织构特征及其对r,△r值的影响

From St15 micro-carbon deep drawing steel sheets, two sets of samples with (r) over bar variant and Deltar constant, and (r) over bar constant and Deltar variant, were selected to carry out texture measurement and ODF analysis. A description of the texture characteristics and an investigation on the effect of the main textures on the (r) over bar and Deltar values were given. The results show that in the tested steel sheets no desired gamma < 111 > parallel to ND orientation line appears but gamma' orientation line located at <()over bar>=0-90 degrees, theta =19 degrees and phi =45 degrees, and L orientation line located around gamma < 111 > parallel to ND orientation line which spirally rotates from Psi =0 degrees, theta =54.7 degrees and phi =62.7 degrees to Psi =90 degrees, theta =40 degrees and phi =45 degrees occur. Among them, the L orientation line has a main influence on the (r) over bar value and the stronger the texture density, the higher the (r) over bar value is, but is somewhat detrimental to the Deltar value; at the same time, the gamma' orientation line has a major effect on the Deltar value in an opposite way, but is somewhat deteriorative to the (r) over bar value. A strong L orientation line superposed by a relatively strong gamma' orientation line may produce fine (r) over bar and Deltar values.

Numerical Simulation of R-M Instability

In order to capture shock waves and contact discontinuities in the field and easy to program with parallel computation a new algorithm is developed to solve the N-S equations for simulation of R-M instability problems. The method with group velocity control is used to suppress numerical oscillations, and an adaptive non-uniform mesh is used to get fine resolution. Numerical results for cylindrical shock-cylindrical interface interaction with a shock Mach number Ms=1.2 and Atwood number A=0.818, 0.961, 0.980 (the interior density of the interface/outer density p(1)/p(2) = 10, 50, 100, respectively), and for the planar shock-spherical interface interaction with Ms=1.2 and p(1)/p(2) = 14.28are presented. The effect of Atwood number and multi-mode initial perturbation on the R-M instability are studied. Multi-collisions of the reflected shock with the interface is a main reason of nonlinear development of the interface instability and formation of the spike-bubble structures In simulation with double mode perturbation vortex merging and second instability are found. After second instability the small vortex structures near the interface produced. It is important factor for turbulent mixing.

The Displacement and Strain Field of Three-Dimensional Rheologic Model of Earthquake Preparation

Based on the three-dimensional elastic inclusion model proposed by Dobrovolskii, we developed a rheological inclusion model to study earthquake preparation processes. By using the Corresponding Principle in the theory of rheologic mechanics, we derived the analytic expressions of viscoelastic displacement U(r, t) , V(r, t) and W(r, t), normal strains epsilon(xx) (r, t), epsilon(yy) (r, t) and epsilon(zz) (r, t) and the bulk strain theta (r, t) at an arbitrary point (x, y, z) in three directions of X axis, Y axis and Z axis produced by a three-dimensional inclusion in the semi-infinite rheologic medium defined by the standard linear rheologic model. Subsequent to the spatial-temporal variation of bulk strain being computed on the ground produced by such a spherical rheologic inclusion, interesting results are obtained, suggesting that the bulk strain produced by a hard inclusion change with time according to three stages (alpha, beta, gamma) with different characteristics, similar to that of geodetic deformation observations, but different with the results of a soft inclusion. These theoretical results can be used to explain the characteristics of spatial-temporal evolution, patterns, quadrant-distribution of earthquake precursors, the changeability, spontaneity and complexity of short-term and imminent-term precursors. It offers a theoretical base to build physical models for earthquake precursors and to predict the earthquakes.

Synthesis of nickel(II) complexes of alpha-isoxazolylazo-beta-diketones and their absorption of spin-coating films and thermal properties for HD-DVD-R

Three kinds of new nickel(II) complexes of alpha-isoxazolylazo-beta-diketones with blue-violet light absorption were synthesized. Their structures were postulated based on elemental analysis, MS and FT-IR spectra. Smooth films on K9 glass substrates were prepared using the spin-coating method. The absorption properties and thermal stability of these complexes were discussed. The static optical recording test for high density digital versatile disc-recordable (HD-DVD-R) system was also studied. (c) 2005 Elsevier B.V. All rights reserved.