南黄海表层沉积物稀土元素分布与物源关系

对南黄海295个表层沉积物样品稀土元素的电感耦合等离子体质谱法分析,结果表明,南黄海表层沉积物稀土元素平均含量为188.39μg.g-1,稀土富集与重矿物有密切关系;稀土元素的球粒陨石配分模式均呈现Eu负异常,模式具负斜率,表明表层沉积物物质主要来源于大陆地壳。从稀土元素地球化学特征的区域变化来看,南黄海东部沉积物来源于朝鲜半岛,西部沉积物来源于黄河和长江物质输入,中部细粒沉积物主要与黄河及长江物质东南、东北扩散有关,东南部为朝鲜半岛及黄河、长江物质共同作用的结果。     

植酸与稀土元素的固态配合物的研究

植酸（PllytiC。Cid）又称肌醇六磷酸酯（myo－iflOSitdhX。hSPhOSPh。ie）（简写为H12lHP］常以钙、镁复盐（菲汀Phntin）形式存在于植物中,尤其在谷类和植物的种子中含量较高［'j．植酸具有惊人的骛合能力,除碱金属外几乎能与所有金属离子生成沉淀,一些高价金属离于甚至在强酸性介质中也可定量沉淀［如Ti、Zr、Hf、Th、Ce（IV）和In、Sc等〕,这些性质已初用于Th'"的定量测定L'和SC'"的分离提取「",Gd'"与植酸的配合物被用作核磁共振成倍（MRI）的对比剂［'j．然而,对有关配合物的固态组成及性质研究尚无文献报道．本文…     

稀土元素在长江口及邻近陆架表层沉积物中的分布及物源示踪研究

长江口邻近陆架表层沉积物中稀土元素含量及组成表明其主要来源为中国大陆陆源物质.轻重稀土元素比值对于区分长江和黄河流域来源物质具有一定的示踪意义,古黄河三角洲以较低的轻重稀土元素比值为特征,而长江来源物质以相对较高的轻重稀土比值为特征,沉积物粒度和Cl含量不是控制沉积区内稀土元素分馏的主要因素.通过聚类分析将研究区域划分为长江口近岸区和东海北部陆架区两个分区,黄海沿岸流、长江冲淡水以及台湾暖流是造成分区的关键水动力因素.分区内常量和微量元素以及同位素组成皆表现为不同程度差异,长江口近岸区化学组成和长江流域物质基本一致,东海北部陆架区与黄河流域物质比较接近.     

稀土元素11－钨锌合铝杂多配合物的合成、表征和催化性能

首次合成出稀土元素１１一钨锌合铝杂多配合物，用元素分析、红外光谱、紫外光谱、Ｘ射线光电子能谱和热分析等对合成产物进行了表征。其分子通式为：ＬｎＨ４［Ａｌ（Ｈ２Ｏ）ＺｎＷ１１Ｏ３９］·ｘＨ２Ｏ（Ｌｎ＝Ｌａ，Ｐｒ，Ｎｄ，Ｓｍ）。在此基础上，对其在合成己二酸二（２－乙基己）酯（ＤＯＡ）中的催化性能进行了研究。结果表明，稀土元素１１－钨锌合铝杂多配合物具有较高的催化活性和选择性，且可以重复使用。ＤＯＡ产品质量高，达到食品包装级。     

稀土元素1∶12系列钨硅杂多配合物的合成及性质

用复分解法合成了七种稀土元素Keggin结构钨硅杂多配合物:LnHSiW_(12)O_(40)·xH_2O。用ICP、~(29)SiNMR、XPS、XRD、IR.UV、极谱、CV和TG—DTA对它们进行了系统研究,并讨论了其结构和性质的关系。     

稀土元素11—钨锌合铝杂多配合物的合成,表征和催化性能

首次合成稀土元素１１－钨外合铝杂多配合物，用元素分析，红外光谱，紫外光谱，Ｘ射线光电子能谱和热分析等对合成产物进行了表征。其分子通式为；ＬｎＨ４「Ａｌ（Ｈ２Ｏ）ＺｎＷ１１Ｏ３９」．ｘＨ２Ｏ（Ｌｎ＝Ｌａ，Ｐｒ，Ｎｄ，Ｓｍ）。在此基础上，对其在合成己二酸二酯中的催化性能进行了研究。     

4种激光粒度仪对下蜀土湿法粒度测试的对比研究

使用4种应用较为广泛的激光粒度仪(Mastersizer2000、Bettersize2000、Horiba LA950和LS13320)对粒度差异较小的下蜀土(土塘剖面)进行了测试,从而对比分析不同激光粒度仪对于下蜀土的粒度组成测试差异及其这种差异对研究结果可能产生的影响.结果表明:对粉砂颗粒组分的分析,4种激光粒度分析仪分析结果的差异最小,而对砂和粘土颗粒组分分析的差异最大.就粒度频数曲线、概率累积曲线、粒度组分、C-M图、粒度参数散点图及粒度参数剖面垂向变化等统计参数与统计方式而言,4种仪器的测试结果均有一定的差异,其中,概率累积曲线、粒度参数散点图差异较大.粒度参数的剖面变化差异也较大,影响了对剖面的阶段性划分,这在一定程度上影响了研究结果,造成使用不同仪器,可能会得出不同的结果.     

稀土元素1∶12系列钨锗杂多配合物的合成及性质研究

本文首次合成出八种Ｋｅｇｇｉｎ结构的稀土元素钨锗杂多配合物ＬｎＨＧｅＷ１２Ｏ４０·ｘＨ２Ｏ（简写为ＬｎＨＧｅＷ１２，Ｌｎ＝Ｌａ，Ｃｅ，Ｐｒ，Ｎｄ，Ｓｍ，Ｅｕ，Ｇｄ，Ｙｂ；ｘ＝１８～２８）。用ＩＣＰ，１８３ＷＮＭＲ，Ｘ射线粉末衍射，ＩＫ，ＵＶ，循环伏安和ＴＧ－ＤＴＡ热分析等手段，对这些杂多配合物进行了表征和性质研究，讨论了结构和性质的关系，为此类配合物的催化应用提供了有益信息。     

Prospect on Rare Earth Elements and Metals Fingerprint for the Geographical Discrimination of Commercial Spanish Wines

This paper presents a novel tool for Spanish commercial wine discrimination according to their designation of origin (PDO). A total of 65 commercial wines from different Spanish designation of origin (Alicante, Bullas, Campo de Borja, Jumilla, Castilla la Mancha, Ribeiro, Ribera de Duero, Rioja, Rueda, Utiel-Requena, Valdepeñas and Valencia) were characterized. The rare earth elements (REEs) content was determined by a high-temperature torch integrated sample introduction system (hTISIS) coupled to inductively coupled plasma mass spectrometry (ICP-MS). The REE content was used to draw characteristic PDOs radar charts. Results indicated that the REEs fingerprint provides a good prospect to discriminate the different Spanish PDOs, except for Alicante, Castilla la Mancha, Jumilla, Utiel-Requena and Valdepeñas. Finally, for those PDOs that were not properly distinguished, a second fingerprint obtained from Ba, Co, Cr, Mn, Ni, Pb and V content was used for discrimination purposes.     

Studies in the Field of Rare Earth Elements

The article describes developed and implemented technologies in the field of rare earth elements. Besides, new promising technologies for the realization of the work, carried out at the Department of Chemistry MEPhI in recent years, are represented.     

Biohydrometallurgy for Rare Earth Elements Recovery from Industrial Wastes

Biohydrometallurgy recovers metals through microbially mediated processes and has been traditionally applied for the extraction of base metals from low-grade sulfidic ores. New investigations explore its potential for other types of critical resources, such as rare earth elements. In recent times, the interest in rare earth elements (REEs) is growing due to of their applications in novel technologies and green economy. The use of biohydrometallurgy for extracting resources from waste streams is also gaining attention to support innovative mining and promote a circular economy. The increase in wastes containing REEs turns them into a valuable alternative source. Most REE ores and industrial residues do not contain sulfides, and bioleaching processes use autotrophic or heterotrophic microorganisms to generate acids that dissolve the metals. This review gathers information towards the recycling of REE-bearing wastes (fluorescent lamp powder, spent cracking catalysts, e-wastes, etc.) using a more sustainable and environmentally friendly technology that reduces the impact on the environment.     

海南岛南渡江近岸河口沉积物稀土元素地球化学

用电感耦合等离子体(ICP-MS)测定了海南岛南渡江近岸河口11个站位沉积物中的稀土元素(REEs)以及U,Th,Ti,Sr,Mn等元素的含量,探讨了沉积物中REE分布模式和变化规律,推断沉积物的来源及演化过程。结果表明,研究区沉积物ΣREE平均含量为124.94 mg.kg-1,河口沉积物ΣREE含量低于滨浅海沉积物。虽然各站ΣREE含量存在较大差别,但分布模式相似,均为轻稀土富集型和Eu负异常,为陆壳型沉积。沉积物中REE与U,Th,Ti和Zr有显著的正相关性,与Sr,CaO相关性较弱,表明沉积物主要来源是花岗岩陆源物质,其次是生源碳酸盐物质。     

稀土元素分离检测技术新进展

对2003年以来稀土元素分离检测技术的新进展进行了评述，重点集中于各种新型分离技术、新型检测技术及其在稀土元素分析中的应用。对于离子液体、纳米材料、离子印迹聚合物等新型材料以及浊点萃取、膜萃取、毛细管电泳等新型技术在稀士元素分离中的应用进行了详细讨论，并对中子活化分析、等离子体原子发射光谱和等离子体质谱在稀土元素检测中的应用进行了综述，重点讨论了等离子体质谱技术的应用。在回顾稀土元素分离检测技术进展的同时，对其在未来几年的发展趋势进行了评述。     

动能歧视(KED)-电感耦合等离子体质谱(ICP-MS)法测定贵州沉积型稀土矿中16种稀土元素

贵州沉积型稀土矿主要含有高岭土-锐钛矿石等矿物,存在高含量Si、Al、Fe、Ti、Zr等难溶基体元素,采用高压密闭微波消解法处理难以将其完全溶解,易使测定结果偏低,需再次消解或进一步电热板敞开酸溶处理,方法耗时长,不利于大批量样品检测需求。同时电感耦合等离子体质谱法(ICP-MS)在测定稀土元素时存在基体效应和质谱干扰,影响了检测数据的准确性。本文采用过氧化钠熔融分解样品,熔融物冷却后引入三乙醇胺溶液,在碱性溶液中,大量基体元素与三乙醇胺形成稳定配合物,并与大量溶剂钠盐存于溶液中,稀土元素与Ca、Mg、Sr、Ba等留存于沉淀,经过滤,实现稀土元素与大量基体元素分离,随后沉淀用(1+1)硝酸复溶,并以103Rh和185Re为在线注入内标协同降低基体干扰;启用动能歧视(KED)模式以降低测定过程中潜在的质谱干扰。实验结果表明:高压密闭微波消解法消解液浑浊有残渣,溶矿耗时长,测试结果偏低,碱溶法酸化后溶液清亮透明,稀土元素测定值准确性高;经条件试验,采用10%三乙醇胺溶液提取能较大降低基体干扰;启用KED模式可降低测定过程中的质谱干扰,且准确度优于STD模式;碱溶法方法检出限为0.008μg/g~0.049μg/g,测定下限为0.034μg/g~0.195μg/g,相对标准偏差RSD在0.78%～10.2%之间,相对误差RE在0.0225%~13.5%之间。经实际样品验证,碱熔法较适用于贵州沉积性稀土矿中16种稀土元素的测定。     

微量稀土元素的药效及保健作用

根据国内外微量稀土元素在医药方面应用的研究,介绍了稀土元素的一系列特殊的药效及保健作用。稀土元素可广泛用于治疗烧伤,炎症,皮肤病,血栓病等。     

Thermal Stability of 4-Chloro-3-Nitro- and 5-Chloro-2-Nitrobenzoates of Rare Earth Elements

The physico-chemical properties and thermal stabilities in air of rare earth element 4-chloro-3-nitrobenzoates and 5-chloro-2-nitrobenzoates were compared and the influence of the positions of the Cl and NO₂ substituents on their thermal stabilities was investigated. The complexes of both series are crystalline, hydrated or anhydrous salts with colours typical of Ln³⁺. The carboxylate group in these complexes is a bidentate, chelating ligand. The NO₂ group in the chloronitro complexes does not undergo isomerization. The thermal stabilities of the 4-chloro-3-nitrobenzoates of Y and the lanthanides were studied in the temperature range 273-1173 K, but those of the 5-chloro-2-nitrobenzoates of these elements were studied only at 273-523 K, because they decompose explosively above 523 K. The positions of the Cl and NO₂ substituents on the benzene ring influence the thermal properties of the complexes and their decomposition mechanisms. The different thermal stabilities of the complexes are connected with various inductive and mesomeric effects of the Cl and NO₂ substituents on the electron density in the benzene ring. This revised version was published online in July 2006 with corrections to the Cover Date.