The study of the microstructures of clay sediments: a case study of marly sediments from N. Péloponnèse

Τ.Α. Χριστοδουλοπούλου, Παναγιώτα Σ. Τσώλη-Κατάγα, Γεώργιος Χ. Κούκης, Νικόλαος Κοντόπουλος
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引用次数: 1

Abstract

This paper deals with the systematic study of the microstructural characteristics of clay sediments. These characteristics which are closely connected to the physical and mechanical character of the sediments, are concerned with: a)the structural constituents, b)the microporosity and c)the structural bonds of the sediments. For the determination of the structural characteristics of clay sediments the Scanning Electron Microscope (SEM) and the Optical Microscope are widely used with a supplementary mineralogical analysis of sediment components and the determination of several physical and mechanical characteristics. The observations under the microscope must be focused on the distribution of mineralogical facies and micropores, on the size and shape of clay (micro-)aggregates, as well as on the kind of authigenic facies (e.g. micrite, sparry calcite) which play the role of cementing material. The proposed methodology was applied to the study of the microstructures of marly sediments from Northern Péloponnèse and the following types of microstructures were determined: a)matrix-skeletal, mixed type, coarse dispersed of low orientation, b)matrix, coagulative, medium dispersed of medium orientation and c)crystallized-cementated, fine or medium dispersed of low orientation.
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粘土沉积物微观结构的研究:以N. psamuloponn沼泽沉积物为例
本文对粘土沉积物的微观结构特征进行了系统的研究。这些特征与沉积物的物理力学特性密切相关,涉及:a)沉积物的结构成分,b)沉积物的微孔隙度和c)沉积物的结构键。为了确定粘土沉积物的结构特征,广泛使用扫描电子显微镜(SEM)和光学显微镜,并辅以沉积物成分的矿物学分析和几种物理和力学特征的测定。在显微镜下的观察必须集中在矿物相和微孔的分布,粘土(微)集合体的大小和形状,以及起胶结作用的自生相(如泥晶、亮晶方解石)的种类。将所提出的方法应用于passicloponn北部沉积物的微观结构研究,确定了以下类型的微观结构:a)基质-骨架型,混合型,低取向的粗分散;b)基质-凝固型,中取向的中分散;c)结晶-胶结型,低取向的细分散或中分散。
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