SnAgCu合金粉末的真空蒸镀涂层机理

对SnAgCu合金粉末的真空蒸镀涂层硬脂酸的成膜机理进行了研究.采用扫描电镜(SEM)和透射电镜(TEM)对涂覆后合金粉末的形貌及结构进行观测,采用傅里叶红外光谱仪(FTIR)和X射线光电子能谱仪(XPS)对涂覆后粉末的透射吸收谱和光电子能量进行测试.结果表明:硬脂酸在合金粉末表面形成一层均匀致密、厚度为5～10 nm的薄膜,硬脂酸涂层SnAgCu合金粉末的行为属于物理吸附行为,其生长方式遵循岛状生长机理模式,其过程实质是一个气--固转换、晶体生长的过程.     

喷雾干燥-碳热还原法制备介孔球形LiFePO4/C正极材料

以聚乙二醇(PEG)为辅助模板剂和碳源,以廉价的三价铁为铁源,采用喷雾干燥-碳热还原法制备了LiFePO4/C正极材料,并对该材料的微观结构及PEG添加量、焙烧温度等对材料结构和性能的影响进行了表征和研究.结果表明:制得的LiFePO4/C材料呈介孔结构,具有漂亮的差级球状形貌、高的比表面积和容量、优异的循环性;PEG...     

用柠檬酸法改性锰矿及其对重金属离子的吸附性能

以Cu2+为模拟污染物,研究了柠檬酸法改性锰矿制备重金属离子吸附剂的实验条件及其吸附性能.结果表明:m(柠檬酸)∶m(TR)为1∶20时,H2SO4浓度为0～3 mol/L,随H2SO4浓度的增大吸附率-pH曲线向左移动,pH50由5.2降低到2.6;H2SO4浓度为3 mol/L,m(柠檬酸)∶m(TR)分别为0,1∶100,1∶50,1∶20时,pH50分别为3.8,3.0,2.5,2.6;pH=5.5条件下,m(柠檬酸)∶m(TR)=1∶50的柠檬酸改性锰矿对Cu2+的饱和吸附量增大到35.97 mg/g.     

基于遗传算法的直觉模糊C均值聚类算法

 针对一般直觉模糊C均值聚类算法在寻优过程中易陷入局部最优解的问题,利用遗传算法具备全局寻优的优点,提出了一种基于遗传算法的直觉模糊C均值聚类算法。在该算法中聚类中心为直觉模糊数,这使得遗传过程中个体信息变得复杂,进而增大了约束问题的处理难度。本文对产生的个体采用适时分段的归一化方法,很好地解决了该问题。仿真结果表明该算法所得聚类结果不仅准确而且更为细致。     

两种基于苯并咪唑衍生物配体的新型铱(Ⅲ)配合物的合成及发光性能研究

合成了新型配体N-异丙基-2-苯基苯并咪唑(bi)和N-异丙基-2-(4-氟苯基)苯并咪唑(fbi),并用它们与三氯化铱和乙酰丙酮反应,制备了相应的环金属铱(Ⅲ)配合物发光材料(bi)2Ir(acac)和(fbi)2lr(acac)(acac=乙酰丙酮).对其结构用1H NMR和元素分析方法进行了表征,研究了配合物的UV-vis,荧光光谱及电化学性质.两种材料的最大发光波长分别位于514 nm和493nm.电化学研究表明,在苯环上引入氟原子后,配合物的HOMO和LUMO间能隙增大(分别为O.12 eV和0.15 eV),与最大发光波长蓝移结果吻合.     

金属有机骨架材料上气体吸附存储与分离的研究进展

对金属有机骨架(MOFs)材料的结构及合成方法做了简要概述;结合国内外研究现状详细介绍了MOFs材料在吸附存储与分离领域的研究进展,并对MOFs材料在该领域的应用进行了展望.     

Response of the northwestern Pacific upper water δ~(13)C to the last deglacial ventilation of the deep Southern Ocean

The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes.     

Influence of B,Al and Nb addition on the glass forming ability and stability of mechanically alloyed Zr-Ni amorphous alloys

We investigated the influence of minor additions of B,Al and Nb that have representative atomic sizes on the glass forming ability (GFA) and stability of Zr-Ni amorphous alloys during mechanical alloying. The results show that the minor addition of B,Al or Nb does not shorten the initial time of the full amorphization reaction or improve the glass forming ability of the Zr-Ni alloys at a low rotation speed. However,B addition can effectively improve the mechanical stability of the amorphous phase against me...     

The occurrence and significance of C25HBI in Cenozoic saline lacustrine source rocks from the Western Qaidam Basin,NW China

The saline lacustrine deposit of the Oligocene Lower Ganchaigou Formation is the main source rock for the Western Qaidam Basin,NW China.In this study,abundant highly branched isoprenoids with 25 carbon atoms (C25HBI) were detected in the upper section of the Lower Ganchaigou Formation.C25HBI is a biomarker for diatoms,and can provide information regarding biogeochemical processes during production and preservation of sedimentary organic matter.The carbon isotopic values of C25HBI in these source rocks were in the range of-18‰ to-20‰.The relative enrichment in 13C of C25HBI suggests that these isoprenoids were derived from diatom blooms.In this case,the diatoms used HCO3-as an additional carbon source to dissolved CO2 in water column due to their high biological productivity.Conversely,the diatom blooms indicated an abundant nutrient supply to the environment and high primary productivity.Thus,the occurrence of 13C-enriched C25HBI could be an ideal marker for good source rocks.The decreased concentration of CO2(aq) in the water column induced by diatom blooms can result in an enrichment in 13C of organic matter synthesized by primary producers.This may be a possible reason for the occurrence of 13C-enriched organic matter in the Cenozoic source rocks of the Western Qaidam Basin.Previous studies have shown that the high carbon number n-alkanes sourced from diatoms have no carbon preference.Hence,the sources of n-alkanes in regional source rocks are complex,and should be considered when discussing the sources of organic matter in future studies.     

K2O对氧化物原料合成Al8B4C7的影响

采用硼砂、金属铝和碳粉为原料一步合成Al8B4C7.在合成过程中掺入不同含量的K2O,研究杂质K2O对合成Al8B4C7的影响.将原料混合均匀,在200MPa的压力下压制成φ20mm×20mm的圆柱型试样,将干燥后的试样在不同温度下的流动氩气气氛中进行合成.利用化学分析、XRD和SEM等分析测试技术,研究了K2O含量以及烧结温度对反应合成材料物相组成和显微结构的影响.结果表明:尽管加入不同含量的K2O,但其高温烧结反应后,若K2O的质量分数在0.019%～0.028%之间,就不出现含K的新相.K2O的加入不利于Al8B4C7的合成,它可将Al8B4C7的开始生成温度提升至1 400℃,而且1 700℃时,Al8B4C7含量较不加入K2O时明显减少.添加K2O合成的Al8B4C7为1μm左右大小的无规则小颗粒.