AN ANOMALOUS MOSSBAUER SPECTRUM OF SCHORLOMITE

The characteristics of Mossbauer spectra for a sample of schorlomite are described in this paper. There are 7 fitting doublets, three of which are considered as anomalous absorptions and their origin may come front complex electronic processes occurring in the schor]omite. It has been found that the isomer shift (IS) of Fe~(3 ) exhibits an apparent temperature effectin the mineral studied.     

天然石榴子石的穆斯堡尔谱

本文收集了28个石榴石样品,并将其分为5个组。在室温下测量了这些石榴石的穆斯堡尔谱。对于金伯利岩和玄武岩包体中的镁铝榴石来说,Fe~(2 )双峰的两个单峰的线宽和强度不相等,用DA来表示Fe~(2 )双峰的强度不对称度。作者发现DA与镁铝榴石端员分子百分比(X_1),与钙铬榴石和镁铬榴石端员分子百分比(X_2),以及与Cr_2O_3重量百分比(X_3)有密切关系,最后推导出一个多元廻归方程:DA=8.24 0.05X_1 0.63X_2。     

MSSBAUER SPECTRA OF NATURAL GARNETS

Twenty-eight samples of garnet are collected and divided into five groups by thepresent authors. The Mossbauer spectra of the garnets are measured at room temperature.The line width and intensity of two component peaks of Fe~(2 ) doublet for pyropes inkimberlite and inclusions of basalt are always not equal. The degree of intensity asymmetryof Fe~(2 ) doublet is denoted by DA. We have found that the DA is closely related to pyropeend-member molecule percentage (X_1), uvarovite and hanleite end-member molecule percent-age (X_2) and Cr_2O_3 wt.% (X_3). The linear equations are obtained: DA=-8.43 0.31X_1,DA=12.15 0.62X_2, DA=11.92 1.88X_3. Finally a multiple regression equation isderived: DA=8.24 0.05X_1 0.63X_2. The next nearest neighbour effect of Cr~(3 ) ionsin pyrope plays an important role for the origin of the asymmetry of Fe~(2 ) doublet. TheMossbauer spectra of other four groups of garnet are discussed in the present paper.     

钛榴石反常的穆斯堡尔谱

本文描述了一个钛榴石样品穆斯堡尔谱的特征,有七个拟合的双峰,其中三个被认为是反常的吸收,它们可归因于发生在钛榴石中复杂的电子过程.还发现在这种矿物中Fe~(3 )的同质异能移位(IS) 显示明显的温度效应。     

白云鄂博两种稀土矿物中铕的价态

白云鄂博稀土矿床中,现已发现的稀土矿物近40种。为了开发利用该稀土资源,对矿床中稀土元素的存在形式、分布规律的研究是非常重要的。目前通常用化学方法查明稀土矿物的成份、稀土元素的配分等。用现代物理学方法研究白云鄂博稀土矿物中稀土元素的价态还较少见。我们用穆斯堡尔效应测定了白云鄂博两种稀土矿物中铕的价态。 穆斯堡尔效应是一种核物理方法,用它可以解决有关元素的价态等问题。试验