火焰原子吸收分光光度法测定地表水中铜含量的不确定度评定

根据GB 7475—87《水质铜、锌、铅、镉的测定火焰原子吸收分光光度法》建立地表水样测定的数学模型,并根据JJF 1059.1—2012《测量不确定度评定与表示》的要求,计算测量过程中的不确定度分量,最终得出扩展不确定度.经检测计算,该地表水样品中的铜含量为1.53 mg/L,其扩展不确定度为0.036 mg/L,包含因子k=2,地表水样品中铜含量的测量结果应报告为(1.53±0.036) mg/L, k=2.结果表明,火焰原子吸收分光光度法测定地表水样中铜含量的不确定度主要来源于标准曲线拟合、标准溶液配制和样品重复测量.     

Polarized Emission of Molecular Film With Lanthanide (Ⅲ) Complex

1 Results In the coordination system by using complexation with organic ligand, the ff emission of lanthanide(Ⅲ) (Ln(Ⅲ)) is induced the excitation energy transfer form the organic chromophore under the light-irradiation. However, there are not so much number of reports to discuss the energy relaxation mechanism in such complexes with Ln(Ⅲ). Recently, we succeeded firstly to estimate the rate constant of the energy transfer between the ligand and Ln(Ⅲ) in Pr(Ⅲ)-phenanthroline analogs[1]. Here, we will di...     

高分子担载卟啉稀土络合物的合成

高分子担载卟啉稀土络合物的合成王荣民，王云普，雷自强，熊键，王顺（化学系）第一作者简介王荣民，男，２８岁。１９９１年毕业于西北师范大学化学系，获理学硕士学位，现为西北师范大学化学系讲师。主要研究方向为高分子金属有机化学，已在国内外学术刊物上发表有关论...     

氢化物发生-原子荧光法测定菊花和大云中的铅

应用AFS—2202a型双道原子荧光分光光度计和断续流动的氢化物发生技术，采用HNO3-H2O2酸性体系和高压釜消解样品，对样品中的铅含量进行了测定。同时，研究了光电管负高压、灯电流、屏蔽气和载气流量、载流的选择、酸度等对实验的影响。在选定实验条件下，铅的检出限为0．08μg／L，标准物质桃叶(GBW08501)的验证结果与推荐值一致，相对标准偏差为1．9％。该方法简便、快速、灵敏，对于实际中药样品的测定得到了满意的结果。     

石墨探针收集,GPFAAS测定APM中痕量铝

一定规格的多孔石墨探针可在一特制的过滤装置中直接收集大气微粒物质(APM),通过石墨探针炉原子吸收光谱(GPFAAS)直接测定其中痕量铝的含量。采用基体改良剂Mg(NO_3)_2,含量低于2.5ng,吸光度(峰面积方式)低于0.25的铝,其分析校正曲线显示良好的线性且无记忆效应发生。采用本法测定标准参比材料(SRM 1604,城市微粒物质),铝的回收率为101％,相对标准偏差为3.8％,测定实验室大气微粒物质中铝的含量为749ng/m~3,相对标准偏差为8.1％。     

基于掺铕钨酸盐荧光强度比的非接触温度传感

为了突破传统测温技术应用的局限性,利用NaY （WO₄）₂：Eu³⁺玻璃陶瓷（glass ceramics,GC）实现了具有非接触、实时响应、自校准等优势的双模荧光强度比（luminescence intensity ratio,LIR）测温。采用高温熔融淬灭法制备出含NaY （WO₄）₂：Eu³⁺纳米晶的透明GC样品,并进行系列光谱测量和热敏性能分析。结果表明,样品中Eu³⁺的激发态能级⁵D₁和⁵D₀和基态能级⁷F₂和⁷F₀为两对独立的热耦合能级,可分别基于这两对热耦合能级实现性能优异的双模LIR温度传感。该双模LIR测温技术数据可靠、测温范围广、灵敏度高,再结合GC材料优势,是可用于光纤温度传感器的核心技术材料。     

紫苏微量元素的测定

利用火焰原子吸收涨研究了紫苏根、茎、叶中８种微量元素的含量,并通过实验拟定了各待测元素的最佳分析条件,呼元素的回收率在９６－１０５％之间,相对偏差小于６％,方法快速、准确、实用性强、同时,对紫苏的药理作用进行了探讨,为办的开发提供实验依据。     

High-precision timing of the Quaternary standard samples with thermal ionization mass spectrometry (TIMS) U-series method

Two national stalagmite standard (GBW04412, GBW04413) and one international coral standard (RKM_4) have been determined by using thermal ionization mass spectrometry (TIMS) method. The values of ( 234 U/ 238 U) act , ( 230 Th/ 234 U) act and age are all consistent in error range with the standard values obtained by using α spectrometry.     

Osmium isotope determination on mantle-derived peridotite xenoliths from Panshishan with N-TIMS

The¹⁸⁷Os/¹⁸⁸Os ratios of spinel lherzolite xenoliths from Panshishan determined with N-TIMS are lower than that of the primitive mantle, which shows depleted mantle characteristics. Their positive correlation with Al₂O₃/MgO suggests that the geochemical behavior of trace elements Re and Os is similar to that of Al₂O₃ and MgO respectively during the magmatic evolution and Re-Os isotopic system is largely immune to mantle metasomatism. A model age of 2.8–3.4 Ga obtained by¹⁸⁷Os/¹⁸⁸Os-Al₂O₃/ MgO correlation might represent the homogeneous age of the mantle lithosphere beneath the area.