100块南极格罗夫山陨石的类型划分及其岩石学特征

根据岩石矿物学研究，包括岩石结构、橄榄石的Fa值和低钙辉石的Fs值以及金属模式含量等，100块格罗夫山陨石分别被划分为：4块H3型、11块H4型（其中一块为H4-an）、10块H5型、3块H6型、2块L3型、6块L4型、31块15型、32块L6型和1块LL4型。格罗夫山普通球粒陨石在类型分布上，其比例和南极以及非南极普通球粒陨石有显著不同，说明可能存在相当数量的成对陨石。分类陨石样品比较新鲜，其中98块陨石的风化程度为W1，仅有2块陨石风化程度分别为W2和W3。另外，这些陨石中冲击程度较高的样品占有一定比例，它们是研究冲击作用的理想样品。

Direct observation of subsurface oxygen on the defects of Pd(100)

Oxygen adsorption and desorption on a Pd(100) surface with a mesoscopic defect were studied by photoemission electron microscopy (PEEM). The defect surface, with an area of approximately 200 x 60 mu m(2), behaved differently from the perfect Pd(100) surface towards the adsorption of oxygen. When saturated, both surface oxygen and subsurface oxygen coexisted on the defect surface, whereas only surface oxygen was present on the Pd(100) surface. Upon heating, subsurface oxygen diffused back to the surface and desorbed with surface oxygen at the same time. The difference in oxygen adsorption ability between the defect surface and the perfect Pd(100) surface can be attributed to different structures of these two surfaces. (C) 1999 Elsevier Science B.V. All rights reserved.