苏皖四处凹凸棒石粘土矿床稀土元素地球化学研究

研究了苏皖四处凹凸棒石粘土矿床不同类型矿石的烯土元素组成及其变化特征。研究表明玄武岩首先风化形成蒙皂石族粘土矿物，在此过程中稀土元素没有明显的分馏作用，强风化的玄武岩重稀土元素强烈亏损；如果玄武岩在地表进一步风化形成红土型蒙脱石粘土，则发生明显的铈正异常，中稀土亏损而轻稀土和重稀土又重新富集，这反映了当时大陆地表特殊的氧化条件和盆地湖水溶液的胶体吸附作用。玄武岩在原地进行水－岩作用，发生递进化学风化，其稀土元素地球化学特征与玄武岩及其风化产物的稀土元素化学特征基本一致，总量略低，显示REE没有大量迁移流失，沉积型凹凸棒石粘土的稀土元素地球化学特征也与玄武岩及其风化产物的稀土元素地球化学特征相似，但同时表现出轻重稀土比值磁大，铕正异常，表明沉积型凹凸棒石粘土的物源基本上是来源于玄武岩的风化产物，但REE配分模型受玄武岩风化残积物的制约。     

REE AND Sr, Nd, Pb ISOTOPIC GEOCHEMISTRY OF HUANGYISHAN BASALT, KUANDIAN, LIAONING, NORTHEAST CHINA

In the light of major element geochemistry, mineral chemistry and REE and isotopic data, the small but apparent isotopic differences between the Cenozoic volcanic rocks east and west of the Tancheng-Lujiang fault are believed to be caused by the mixing and metasomatism of crustal and mantle material in tho mantle source region in response to Pacific plate subduction. The presence of phlogopite and pargasite in mantle xenoliths lends strong support to mantle metasomatism.     

Efficient synthesis of multiply substituted furans using BF@Propyl/dopamine/Pd as a green catalyst

One of the commonly used methods to synthesize furans is the three-component reaction among aromatic aldehyde, arylamine, and acetylenedicarboxylate. The main advantages of this work are easy reaction work-up, short reaction time, high yield and easy recyclability, reusability of the catalyst. And also basalt fiber applications are surely innovative in many industrial and economic fields, because of its good mechanical, chemical and thermal performances.     

电感耦合等离子体原子发射光谱法(ICP-AES)测定玄武岩中的8种微量元素

采用硝酸-盐酸-氢氟酸高压封闭消解样品,电感耦合等离子体原子发射光谱法测定玄武岩中的8种微量元素。实验确定了方法的分解条件以及测定元素的检出限及干扰条件。用国家一级标准物质GBW07105(玄武岩)进行方法验证,检测结果与标准值基本吻合,符合地质矿产开发的要求。     

土壤发育过程中稀土元素的地球化学指示意义

研究了海南岛北部不同时期喷发的玄武岩上发育土壤中稀土元素的地球化学特征和行为,探讨成土元素的分异及其对土壤发育程序的指示作用。ＲＥＥ总量与成土年龄呈显著正相关,是指示土壤发育程序的良好指标。同时,随土壤发育程度的加深,ＲＥＥ出现分异,土壤中轻稀土逐渐富集,重稀土亏损,伴随的进一步发育,Ｃｅ逐渐向正异常而Ｅｕ向负异常方向演化。     

Characterization and catalytic performance of basaltic dust as an efficient catalyst in the liquid‐phase esterification of acetic acid with n‐butanol

Three natural basaltic samples were collected and used as efficient catalysts for the liquid‐phase synthesis of n‐butyl acetate. The samples were characterized by X‐ray fluorescence analysis (XRF), X‐ray diffraction (XRD), thermogravimetry (TG), differential thermal analysis (DTA), Fourier transform infrared (FT‐IR), scanning electron microscopy (SEM), and N₂ sorption. The acidity of the samples was determined using isopropanol dehydration, and the strength of the acid sites was measured using chemisorption of basic probes. The catalytic activity of the samples towards the esterification of acetic acid with n‐butanol was extensively examined. The influence of different parameters, such as the reaction refluxing time, molar ratio, catalyst loading, reusability, and calcination temperature, on the esterification reaction was studied in detail. The results revealed that all samples had high catalytic activity with a selectivity of 100% to n‐butyl acetate formation. In addition, the sample obtained from the top hill of Volcano had the highest activity with a 80% yield of n‐butyl acetate. Moreover, the significant catalytic performances were well correlated with the acidity of the samples and to the reaction rate constants.     

The Effect of Adhesion Interaction on the Mechanical Properties of Thermoplastic Basalt Plastics

The effect of temperature, adhesion time, and surface treatment of a reinforcing filler on the mechanical properties of thermoplastic basalt plastics based on a high-density polyethylene and a copolymer of 1,3,5-trioxane with 1,3-dioxolan is investigated. An extreme dependence for the adhesive strength in a thermoplastic-basalt fiber system is established and its effect on the mechanical properties of basalt plastics and the influence of the adhesion contact time on the adhesive strength in the system are clarified. The surface modification of basalt fibers in acidic and alkaline media intensifies the adhesion of thermoplastics to them owing to a more developed surface of the reinforcing fibers after etching. It is found that the treatment in the acidic medium is more efficient and considerably improves the mechanical properties of basalt plastics.     

海底管道的弹塑性稳定性和屈曲传播

本文根据我国南海海底输油气铺管的要求系统分析了海底管道在弯曲与外水压力共同作用下的弹塑性稳定性和屈曲传播.研究了管道的极值型屈曲和分枝型屈曲.在考虑管道的初始非圆度和材料的物理非线性的情况下提出了临界屈曲载荷的计算方法.综述和评论了屈曲传播现象的本质和各种计算方法.介绍了我们所进行的全尺寸管道实验.在分析理论结果时与现行的有关设计规程进行了比较和评论.     

Phase Composition of Iron Compounds in the Products of Annealing of the Tertiary Basaltic Rock from Góra Obłoga (the Lower Silesia, Poland)

The work presents results of the research on thermal transformations of iron minerals which are present in basalt rock from Góra Obłoga in Pogórze Złotoryjskie District. The rock under study shows microporphyric texture and compact microstructure and contained: olivine, augite, diopside, plagioclases, serpentines, zeolites, apatite and also opaque minerals (oxides). The basalt was annealing within the temperature range between 573–1473 K, in air, and then, microscopic observations, X-ray diffraction as well as Mössbauer spectroscopy measurements were performed. During the heat treatment of the rock it was found that the content of olivine and augite was gradually decreasing due to progressive oxidation of iron compounds, resulting in formation of magnetite and hematite. The comparison of the results of thermal Mössbauer spectral analysis showed that transformation of iron minerals occurred already under conditions when the basic rock mass underwent only insignificant changes.     

The Selective Flux of Sulfur and Implications for Magmatic Sulfur Isotope Fractionation

The selective flux of sulfur during magma emplacement is proposed to explain some abnormal δ³⁴S data from granitic and basaltic rocks. It is assumed that on the one hand a quasi-equilibrium isotope fractionation exists between sulfate and sulfide during magma cooling, and on the other hand a non-equilibrium fractionation occurs between the fluxed sulfur and the magmatic sulfur. The results show that at high fO₂, ³⁴S is preferably enriched in sulfate with decreasing temperature, without a corresponding depletion of sulfide in ³⁴S. The δ³⁴S value of solidified rocks is then significantly shifted in the positive direction due to the selective degassing or assimilation. Conversely, at low fO₂, ³⁴S is preferably depleted in sulfide as temperature declines, while a corresponding ³⁴S-enrichment in sulfate does not occur. As a consequence, δ³⁴S value of the rocks is driver in the negative direction.