NMR STUDIES ON THE HYDRATION OF IONS IN MICROEMULSION——THE NAPHTHENIC ACID SOAP-ALCOHOL-KEROSINE-WATER MICROEMULSION SYSTEM

The difference △δ between the proton shift of water of hydrauon of metar ions δ(H_2O(M~4))and that of pure liquid water δ_(H_2O(1)) so far observed is very small, only about ± 0.1 ppm,because the ratio of metal ions to H_2O molecules M~ /H_2O cannot exceed 0.36 even in veryconcentrated aqueous solutions. In the present investigation, we study the hydration of metalions in microemulsions and propose a novel method to vary M~ /H_2O ratio from 100:1 to1:100. Under such conditions, we have obtained the limits of δ(H_2O(M~ )) for various cations asfollows: 7.54 ppm (NH_4~ ), 7.08(Li~ ), 6.22(Na~ ), 6.00(K~ ), while δ(H_2O(1)) = 4.80 ppm, sothat the largest △δ observed amounts to 2.74 ppm, thus rendering NMR method an effectivemeans to study the hydration of metal ions.     

镧系离子与L-羟脯氨酸、DL-瓜氨酸配位作用研究

稀土与体内广泛存在的生物配体氨基酸的配位作用，尤其是三元体系的研究对于阐明稀土元素在体内的存在形态及探索稀土生物效应具有重要意义．羟脯氨酸和瓜氨酸均是人体中存在的重要氨基酸，它们在人体血浆中的浓度与必需的氨基酸相近［‘j．稀土与氨基酸配位作用的研究已有较多报道「’‘，但模拟生理条件下稀土离子与羟脯氨酸、瓜氨酸的二元、三元配合物的PH电位法研究尚未见报道．本文报道在模拟生理条件下（37C，0·15mol／LNaCI）湖系离子（Pm和Lu除外）与上述2种氨基酸的二元及三元配合物PH电位法研究结果．1实验部分1．1试剂和仪…     

稀土、钙的DL苹果酸和L羟脯氨酸混配配合物研究

在模拟生理条件（３７℃，０．１５ｍｏｌ．Ｌ＾－１ＮａＣｌ）用ＰＨ电位法测定了１４种稀土、钙的ＤＬ－苹果酸和Ｌ－羧脯氨酸二元、三元配合的稳定常数，用计算机优化确定了 二元体纱，苹果酸配合物存在１１０１、１１００和１２００型，     

FOURIER TRANSFORM FAR INFRARED SPECTRA AND NORMAL COORDINATE ANALYSIS OF FIFTEEN RARE-EARTH OXALATE HYDRATES

The Fourier transform far infrared spectra of oxalate hydrates of whole rare-earth series except Pm and Sc are investigated in the range of 100-400 cm~(-1). The assignment of vibrational frequencies is made on the basis of normal coordinate analysis using our NORVIB program. The model used for the hghter elements of the lanthanide series (La to Eu) is based on the crystal structure of Nd_2(C_2O_4)_3. 10H_2O, in which each lanthanide ion is surrounded by nine O atoms, six from three oxalate ions and three from Water molecules.The model adopted for the heavier elements of the lanthanide series (Gd to Lu) and Ytterbium is based on the crystal structure of Yb_2(C_2O_4)_3· 6H_2O, in which each ion is surrounded by eight atoms, six from three oxalate ions and two from water molecules. The variation of the metal-ligand frequencies and force constants with the atomic numbers of lanthanides is plotted and discussed.     

氮杂大环钕配合物[Nd(L)(CH~3CN)(CF~3sO~3)~3]的合成和结构

本文报道了三价钕与氮杂大环(简称L)配合物的合成和晶体结构.配合物组成为[Nd(L)-(CH_3CN)(CF_3SO_3)_3],晶体属于三斜晶系,空间群为PI,晶胞参数α=0.8738(2),b=1.2870(3),c=1.2900(3)nm;α=85.63(2),α=87.25(2),γ=78.30(2)°;最终偏差因子R=0.0370,R_w00385.配合物中钕为8配位,其配位多面体为扭曲的四方反棱柱体.     

十五种稀土草酸盐水合物的Fourier变换远红外光谱与简正坐标分析

本文研究了除Pm和Sc以外整个稀土系列草酸盐水合物在100—400cm~(-1)范围的Fourier变换远红外光谱。应用NORVIB程序,在简正坐标分析的基础上,对振动频率作了指认。对La至Eu的含水草酸盐络合物,红外分析所采用的结构模型依据Nd_2(C_2O_4)_(?)·10H_2O的晶体结构确定,即每个稀土离子周围有九个氧原子,六个氧原子来自三个草酸根离子,其余三个氧原子由水分子提供。对Gd至Lu以及Y的含水草酸盐络合物,则依据Yb_2(C_2O_4)_3·6H_2O的晶体结构确定,即每个稀土离子周围有八个氧原子,六个氧原子来自三个草酸根离子,其余二个氧原子由水分子提供。作图示出金属-配体的振动频率及力常数随镧系原子序数的变化关系,并对此作了讨论。#原图像不清楚     

二-(2-乙基已基)磷酸与稀土络合物的福里埃变换红外光谱

二-(2-乙基已基)磷酸(D2EHPA)是一种重要的萃取剂,已广泛地应用于稀土元素、核燃料等湿法冶金及分析技术中。我们采用Nicolet 7199B型福里埃变换红外光谱仪,对钇和14个镧系元素与D2EHPA生成的络合物进行深入研究,观察其特征峰的变化,并运用电子计算机的减法功能,获得减法光谱,得到了一些新的结果。这些研究结果有助于进一步了解稀土与D2EHPA络合物的结构与性质。     

希土胺羧酸配合物的研究——Ⅲ.吡啶-2,6-二甲酸钕配合物{[Nd(HDPA)(DPA)(H2O)2]·4H2O}n合成及其晶体结构

关于吡啶-2,6-二甲酸希土配合物晶体结构有Na₃[Ln(DPA)₃]·yNaClO₄·xH₂O类型的报道^[1]。本文合成了{[Nd(HDPA)(DPA)(H₂O)₂]·4H₂O}_n。配合物单晶并测定了其结构。     

氮杂大环钕配合物[Nd(L)(CH~3CN)(CF~3sO~3)~3]的合成和结构

本文报道了三价钕与氮杂大环(简称L)配合物的合成和晶体结构.配合物组成为[Nd(L)-(CH~3CN)(CF~3SO~3)~3],晶体属三斜晶系,空间群PI.a=0.8738(2),b=1.2870(3),c=1.2900(3)nm,a=85.63(2),β=87.25(2),γ=9785302)°;最终偏差因子R=0.0370,R~w=0.0385,配合物中钕为8配位,其配位多面体为扭曲的四方反棱柱体.