The thermophysical properties of low‐temperature Pb plasma

The thermophysical properties of low‐temperature Pb plasma are calculated at temperatures 10–100 kK and densities below 0.2 of the solid‐state value. The thermodynamic values (pressure and internal energy) and transport coefficients (electrical conductivity, thermal conductivity, and thermal power) are considered. The plasma composition and thermodynamic parameters are obtained within the chemical approach, namely by means of the solution of the corresponding system of the coupled mass action law equations. Atom ionization up to +4 is taken into consideration. The electronic transport coefficients are calculated within the relaxation time approximation. The results obtained by means of the present model are compared with the available data of other models and experiments.     

利用显微拉曼光谱技术鉴别印文形成时间的应用研究

采用激光显微拉曼光谱技术,选择10种不同品牌和型号的印泥(油)盖印印文的历时性样本,利用印文拉曼光谱中的1089 cm~(-1)和1235 cm~(-1)处特征峰的相对面积值(I)分析纸张、温度、热老化因素对印文形成时间的影响,探讨盖印时间与峰面积相对值(I)的关系。结果表明,I值随时间呈现规律性变化,尤其在近期内盖印印文的变化规律明显,适用于印文形成时间的鉴别,是一种准确、无损的检验方法。     

Zur hydrogeologischen Interpretation von Isotopendaten im Zusammenhang mit Stofftransportprozessen

The migration of radionuclides and other tracers in porous layers is determined by substance transport. The physical and hydraulic basis of retardation is investigated. A definition of a factor of retardation is given, describing the ratio between the pore velocity of the water and the velocity of tracer migration. Consequences to the groundwater protection are discussed.     

浙江天台盆地下陈萤石矿床地质特征及 ESR 年代学

探讨浙江天台盆地下陈萤石矿床的矿床地质特征与成矿时代，为寻找成因类似的矿床提供理论依据。通过该矿床的野外地质特征和岩矿石显微镜下特征的研究，并利用热活化电子自旋共振测龄法对矿区内不同矿脉上与萤石共生的石英进行了测定，结果表明下陈萤石矿床为热液充填型脉状萤石矿床，成矿年龄平均为75．3±7．0 Ma，其成矿时代主要为晚白垩世。对浙江不同地区萤石矿床成矿时代的规律进行总结，显示浙江的萤石矿成矿时代呈现多期次性，在早白垩世早期、早白垩世晚期、晚白垩世均有成矿作用发生，主要集中在晚白垩世。     

Constraints on an asymptotic safety scenario for the Wess–Zumino model

Using the nonrenormalization theorem and Pohlmeyer's theorem, it is proven that there cannot be an asymptotic safety scenario for the Wess–Zumino model unless there exists a non-trivial fixed point with (i) a negative anomalous dimension (ii) a relevant direction belonging to the Kähler potential.     

Synthesis and Characterization of Some Novel Dialkyldithiophosphate Derivatives of Macrocyclic Complexes of Pb(II) Having N2 S2 Potential Donors in 14- to 20-Membered Rings

Dialkyldithiophosphate derivatives of macrocyclic complexes of Pb(II), having N₂S₂ potential donors, of the general formula, [Pb(L)S₂P(OR)₂] (where L = macrocyclic ligands L¹, L², L³, L⁴ & L⁵ and R = CH₃-, C₃H₇ ⁿ- & C₃H₇ ⁱ-) have been Synthesized from the reactions of [Pb(L)X₂] (where X = Cl, NO₃, or CH₃COO) with sodium dialkyl dithiophosphates in 1:2 molar ratios in THF. Fifteen new derivatives have been synthesized by the combination of five macrocyclic complexes of 14–20 member rings with three different types of dialkyldithiophosphate. These compounds have been characterized by elemental analysis, molar conductance, molecular weight determination, IR, ¹H NMR, ¹³C, and ³¹P NMR. Molecular weight determinations of these complexes indicate their monomeric nature. An octahedral structure is proposed.     

密闭高压消解–ICP–AES测定进口铜精矿中铅、镉、汞、砷

采用密闭高压消解法对样品进行消解,用电感耦合等离子体发射光谱法(ICP–AES)测定进口铜精矿中的铅、镉、砷、汞有害元素。铅、镉、砷、汞的工作曲线分别在0~10,0~1,0~4,0~0.6μg/mL范围内线性良好,线性相关系数大于0.999。各元素加标回收率均为91.0%~104.7%,相对标准偏差均小于3%(n=7)。将密闭高压消解法与电热板加热法和微波消解法进行了比对分析,结果显示,密闭高压消解–ICP–AES法适合用于铜精矿样品的消解与测定。     

Flotation separation and electrothermal atomic absorption spectrometric determination of lead in water samples

Abstract

The application of macro- and micro-electrodes constructed using the new ionophore were tested in a range of solution compositions reflecting concentrations found in fresh waters, and containing Cl^?, NO₃ ^?, SO₄ ^2-, HCO₃ ^2-, H₄SiO₄ and a natural humic acid. The inhibition of the electrode responses to these ions was quantified using a mixed-solution method by optimising the agreement between the measured potentials and predictions from the Nicolsky-Eisenman equation. In addition, measurements were made in separate solutions of KC1 to enable results to be compared with the literature. Apart from the results obtained for humic acid, mean selectivity coefficients for 16 macro- and 21 micro-electrode experiments are given. The results indicate inhibition of the electrode response to phosphate for all the anions in the concentration ranges of 0.05–1 mM Cl^?, 0.1–1.0 mM NO₃ ^?, 0.1–10.0 mM HCO₃ ^? and 0.1–1.5 mM SO₄ ^2- with high selectivity for HPO₄ ^2- in the presence of both dissolved silicon and a standard humic acid. This means that the application of the electrodes to hard waters is impracticable although studies of soft waters and laboratory studies in controlled conditions, e.g. calcium phosphate precipitation experiments, are feasible.     

Solid-phase extraction and preconcentration of trace Pb(II) from water samples with folic acid modified silica gel

A chelating matrix prepared by immobilising folic acid on silica gel-bound amine phase was used as a new solid-phase extractant. This sorbent has been developed only for preconcentration of trace Pb(II) prior to determination by inductively coupled plasma atomic emission spectrometry (ICP-AES). Experimental conditions were investigated by batch and column procedures. The optimum pH value for the separation of Pb(II) on the new sorbent was 4.0. The adsorbed Pb(II) was quantitatively eluted by 2.0?cm³ of 0.5?mol?dm^?3 of HCl. Common coexisting ions did not interfere with the separation and determination of Pb(II). The maximum static adsorption capacity of the sorbent under optimum conditions was found to be 69.23?mg?g^?1 for Pb(II). The detection limit of the method defined by International Union of Pure and Applied Chemistry was 0.28?ng?cm^?3. The relative standard deviation (RSD) of the method was lower than 2.0% (n?=?8). The developed method has been validated by analysing certified reference materials and successfully applied to the determination of Pb(II) in water samples with satisfactory results.     

哈尔滨东部海西期钾长花岗岩的锆石U-Pb年代学及其地质意义

通过对哈尔滨东部地区海西期钾长花岗岩年代学、地球化学特征的研究,讨论兴蒙造山带的演化.研究区钾长花岗岩呈肉红色细粒,主要由钾长石、斜长石、石英和黑云母组成.岩石中siO2的质量分数为74.70％～75.70％,为酸性岩.Al2 O3的质量分数为12.07％～13.18％;Na2O+K2O的质量分数为7.78％～8.09％,K2O/Na2O为0.93％～1.60％.里特曼指数为1.85～2.06.∑REE的质量分数为96.32×10-6～172.83×10-6,δEu为0.21～0.77,为铕负异常;铝饱和指数为0.88～1.12,属于高钾钙碱性花岗岩,与造山带垮塌导致的大规模岩石圈伸展作用有关.该花岗岩LA-ICP-MS锫石U-Pb年龄为(298.54士0.86) Ma(MSWD=0.94),属于晚石炭世,形成于古亚洲洋闭合后兴安地块和松嫩地块碰撞拼合后的伸展作用.