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 共查询到17条相似文献,搜索用时 126 毫秒
1.
采用氧化物固相反应法制备了锰掺杂改性的Ba(Zr0.06Ti0.94)O3陶瓷.研究了锰的掺杂量对Ba(Zr0.06Ti0.94)MnxO3 (BZTM)陶瓷的结构、介电和压电性能的影响.实验发现,当锰含量x<0.5 mol%时进入晶格,使材料压电性能提高,损耗减小,表现出受主掺杂的特性;当锰含量x>0.5 mo  相似文献   

2.
对Eu1-xSrxMnO3 (ESMO, x=0—1)体系的结构和磁性进行了系统的研究,结果表明Sr的掺入使EuMnO3反铁磁母体的磁结构发生巨大的变化.通过磁化和电输运测量,深入探讨了高掺杂浓度Eu0.4Sr0.6MnO3和Eu0.3Sr0.7MnO3相似文献   

3.
张帆  朱航天  骆军  梁敬魁  饶光辉  刘泉林 《海洋学报》2010,32(10):7232-7238
以室温热电性能优异的传统热电材料Sb2Te3为研究对象,利用化学气相沉积法制备Sb2Te3单晶纳米结构,并研究其生长机理.实验结果表明,不加催化剂时Sb2Te3易生长成六方纳米盘,在金催化剂条件下定向生长成纳米线.Sb2Te3的形貌与其晶体结构和生长机理有关.Sb2Te3为三角结构,Sb和  相似文献   

4.
采用射频磁控溅射方法制备了两种用于相变存储器的Ge1Sb2Te4和Ge2Sb2Te5相变薄膜材料,对其结构、电学输运性质和恒温下电阻随时间的变化关系进行了比较和分析.X射线衍射(XRD)和原子力显微镜(AFM)的结果表明:随着退火温度的升高,Ge1Sb2Te4薄膜逐步晶化,由非晶态转变为多晶态,表面出现均匀的、  相似文献   

5.
陈东猛  刘大勇 《海洋学报》2010,32(10):7350-7356
基于自旋-轨道-晶格Hamilton量,应用团簇自洽场方法,研究了双层钙钛矿结构材料K3Cu2F7基态的晶格、磁及轨道结构,发现近孤立的双层的对称破缺和Jahn-Teller晶格畸变使得Cu2+离子在每层内交替占据 z2-x2〉/ z2-y2〉轨道,进而导致双层的层间表现为强的反铁磁耦合,层内为弱的铁磁耦合.强反铁磁耦合导致层间  相似文献   

6.
邓恒  杨昌平  黄昌  徐玲芳 《海洋学报》2010,32(10):7390-7395
采用传统固相反应法制备了双层钙钛矿结构锰氧化物La1.8Ca1.2Mn2O7陶瓷,并用X射线粉末衍射法,扫描电镜,HL5500PC Hall效应分析仪和综合物性测量系统(PPMS)对其磁、电性质进行了表征.结果表明:经过两次高温烧结可合成具有双层Sr3Ti2O7型四方结构的La1.8Ca1.2Mn2<  相似文献   

7.
用高温熔融法制备了Tm3+/Ho3+/Yb3+共掺碲酸盐玻璃(TeO2-ZnO-La2O3)样品,测试了玻璃样品的吸收光谱和上转换发光光谱,分析了上转换发光机理.结果发现:在975 nm波长激光二极管(LD)激励下,制备的碲酸盐玻璃样品可以观察到强烈的红光(662 nm)、绿光(546 nm)和蓝光(480 nm)三基色上转换发光,红光对应于Tm3+离子  相似文献   

8.
王晓坡  宋渤  吴江涛  刘志刚 《海洋学报》2010,32(10):7158-7163
采用反转法计算得到了O2-CO2混合气体新的势能参数.在此基础上,根据分子动力学理论,计算了混合气体在零密度下的输运性质,包括黏度系数、热扩散系数和热扩散因子,计算的温度范围为273.15—3273.15 K.与实验值比较表明,计算结果可以满足实际工程应用.  相似文献   

9.
蒋明波  吴智雄  周敏  黄荣进  李来风 《海洋学报》2010,32(10):7314-7319
利用机械合金化和冷压烧结法制备得到n型和p型Bi2Te3基热电材料,在80—300 K温度范围测量了电导率、Seebeck系数,结果表明其具有良好的低温热电性能.采用Bi2Te3基热电材料制备出半导体热电器件,并配合附属设备搭建出一套半导体温差发电装置.利用液氮汽化时释放的冷能,对半导体热电器件的发电性能进行实验研究,得出这种半导体热电器件输出电压、输出功率与电流关系式,测得最大的输出功率达到1.33 W,从而证明了冷  相似文献   

10.
目的:探讨蛭龙活血通瘀胶囊(以下简称“ZL”)对H2O2诱导细胞氧化损伤的保护作用。方法:以正常H9C2心肌细胞、PC12细胞作为对照,分别以不同浓度的H2O2处理细胞4 h,建立氧化损伤模型;在H2O2处理细胞前用ZL预处理24 h,作为ZL药物组,采用CCK-8法检测以上各组细胞存活率。结果:与未经H2O2处理的细胞比较,400 μmol/L H2O2处理的H9C2心肌细胞存活率下降至(47.25±4.14)%(P<0.01);600 μmol/L H2O2处理的PC12细胞存活率下降至(52.53±4.31)%(P<0.01);经10~320 mg/ml的ZL预处理后,H9C2心肌细胞、PC12细胞的存活率均高于模型组,差异有统计学意义(P<0.05)。结论:ZL对H2O2诱导的H9C2心肌细胞、PC12细胞氧化损伤有保护效果。  相似文献   

11.
This paper reports that stoichiometric, amorphous, and uniform Er2O3 films are deposited on Si(001) substrates by a radio frequency magnetron sputtering technique. Ellipsometry measurements show that the refractive index of the Er2O3 films is very close to that of a single layer antireflection coating for a solar cell with an air surrounding medium during its working wavelength. For the 90-nm-thick film, the reflectance has a minimum lower than 3% at the wavelength of 600 nm and the weighted average reflectances (400--1000 nm) is 11.6%. The obtained characteristics indicate that Er2O3 films could be a promising candidate for antireflection coatings in solar cells.  相似文献   

12.
通过共沉淀法制备纳米Fe_2O_3-SnO_2光催化剂,采用XRD、SEM等测试手段对其进行形貌、物象、粒径一系列的表征,研究结果显示制得的催化剂仍保持纯SnO_2四方金红石型结构.研究了Fe_2O_3-SnO_2光催化剂投加量、Fe_2O_3与SnO_2物质的量比、煅烧温度、煅烧时间、氨氮初始浓度、p H值、H2O2浓度以及光照反应时间等因素对海水养殖废水中氨氮降解效率的影响.在紫外光照射下进行正交实验,确定最优化反应条件:催化剂投加量为0.4 g/dm3,煅烧时间为3 h,物质的量比为1∶2,氨氮初始含量为50 mg/dm3,光照反应时间为2 h.这5个因素对Fe_2O_3-SnO_2光催化氧化速率影响的大小程度依次为:Fe_2O_3与SnO_2物质的量比煅烧时间Fe_2O_3-SnO_2光催化剂投加量氨氮初始浓度光照时间.氨氮去除率可以达到85.1%,相同条件可见光下也可达到82.3%.  相似文献   

13.
生物固氮作用是一个重要的海洋新氮来源,在海洋生物地球化学循环中扮演着不可替代的角色。基于稳定同位素(15N2)示踪吸收法,是目前直接测定海洋生物固氮速率最有效的手段。其中,高效、洁净地将15N2引入海水培养体系,并准确定量培养体系底物的同位素示踪水平,是同位素示踪吸收法准确获取固氮速率的关键。本研究针对15N2同位素示踪剂引入这一关键环节进行了探讨,确认改进气泡法是将15N2引入海水培养体系的首选操作。在对培养体系造成的较小扰动的情况下,可将培养体系氮气底物的15N原子丰度提升至10%以上,相对于另一种导入同位素示踪剂的手段——预溶解海水法,改进气泡法将培养瓶中氮气底物的15N原子丰度提升了近200%。此外,改进气泡法还具有最小化痕量金属沾污、操作简便等优点。将改进气泡法结合与稳定同位素比值质谱测定结合,是准确测定水体生物固氮速率的推荐方法。  相似文献   

14.
The generalised gradient approximation based on density functional theory is used to study the structural and electronic properties of the endohedral fullerene dimer (N2@C60)2. Four N atoms sit at the cage centres in the form of two N_2 molecules. The density of states and Mulliken charge analysis explore that the energy levels from -6 to -10 eV are mainly influenced by the N2 molecules.  相似文献   

15.
The effect of the orientation on the magnetostriction in Fe81Ga19 alloy has been investigated experimentally and theoretically. The Fe81Ga19 [001] and [110] oriented crystals were prepared and the magnetostriction was measured under different pre-stress. The saturation magnetostriction of the [001] oriented crystal increases from 170×10-6 to 330×10-6 under the pre-stress from 0 to 50 MPa. The [110] oriented crystal has a saturation magnetostriction from 20×10-6 to 140×10-6 with the compressive pre-stress from 0 to 40 MPa. The magnetostriction of [001] and [110] oriented crystals has been simulated based on the phenomenological theory. The domain rotation path has been determined and the resultant magnetostriction calculated under different pre-stress. The experimental and simulated results both show that the [001] oriented crystal exhibits better magnetostriction than [110] oriented crystal. The enhancement of the saturation magnetostriction by the compressive pre-stress in the [110] oriented crystal is higher than that in the [001] oriented crystal.  相似文献   

16.
模拟海底微环境,研究促使C4,C5异构体分异的因素。39 d后,i-C4/n-C4变化率:灭菌固液混合组为1.67%,灭菌固液分离组为7.96%,未灭菌固液混合组为2.54%,未灭菌固液分离组为14.21%;i-C5/n-C5变化率:灭菌固液混合组为1.19%,灭菌固液分离组为8.18%,未灭菌固液混合组为2.26%,未灭菌固液分离组为10.19%。表明海底环境对烷烃组分产生复杂的溶解、吸附和生物降解作用,使异构体产生分异效应;碳原子数增加,综合作用相对减弱;同碳原子数,对正构烷烃的作用效果更显著。碳同位素分析发现:i-C4,n-C4,i-C5,n-C5的δ13C均有微弱的变重趋势,CO2的δ13C则发生明显的变轻趋势,并且未灭菌组比灭菌组变化大。表明海底环境使烷烃组分发生了碳同位素分馏,生物降解作用显著。  相似文献   

17.
To study the dissolved carbonate system in the South China Sea (SCS) and to understand the water mass exchange between the SCS and the West Philippine Sea (WPS), pH, total alkalinity and total CO2 were measured aboard the R/V Ocean Researcher 1. Because of the sill that separates these two seas in the Luzon Strait with a maximum depth of 2200 m, the SCS Deep Water has characteristics similar to those of water at about 2200 m in the WPS. The minimum pH and the maxima of normalized alkalinity and total CO2 commonly found in the open oceans at mid-depth also prevail in the WPS but are, however, very weak in the SCS. Rivers and inflows from Kuroshio Surface and Deep Waters through the Luzon Strait as well as those through the Mindoro Strait transport carbon to the SCS year-round. Meanwhile, the outflowing Taiwan Strait water as well as the SCS Surface and Intermediate Waters of the Luzon Strait transports carbon out of the SCS year-round. The Sunda Shelf is also a channel for carbon transport into the SCS in the wet season and out of the SCS in the dry season.fCO2 data and mass balance calculations indicate that the SCS is a weak CO2 source in the wet season but an even weaker CO2 sink in the dry season. With these facts taken together, the SCS is likely a very weak CO2 source. Anthropogenic CO2 penetrates to about 1500 m in depth in the SCS, and the entire SCS contains 0.60 ± 0.15 × 1015 g of excess carbon. Typical profiles of pH as well as the degree of saturation of each of calcite and aragonite in 1850 and 1997 are presented, and those for 2050 AD are projected. The maximum decrease in pH is estimated to be 0.16 pH units in the surface layer when the amount of CO2 is doubled. It is anticipated that aragonite in the upper continental slope will likely start to dissolve, thereby neutralizing excess CO2 by around 2050 AD. This paper is unique in that it presents the results of the first attempt ever to estimate the past, present and future physico-chemical properties of the world's largest marginal sea.  相似文献   

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