Clay and Clay Minerals 2021
DOI: 10.5772/intechopen.97672
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Basics of Clay Minerals and Their Characteristic Properties

Abstract: Clay minerals such as kaolinite, smectite, chlorite, micas are main components of raw materials of clay and formed in presence of water. A large number of clays used to form the different structure which completely depends on their mining source. They are known as hydrous phyllosilicate having silica, alumina and water with variable amount of inorganic ions like Mg2+, Na+, Ca2+ which are found either in interlayer space or on the planetary surface. Clay minerals are described by presence of two-dimensional she… Show more

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Cited by 162 publications
(155 citation statements)
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“…The engineering properties of the naturally available materials will change considerably over time, depending on the stage of chemical weathering (Figure 11 (recreated from [40])). As previously discussed, the mineral composition with specific reference to the silicon content, can have a considerable influence on the bond strengths achieved with the material when using a specific nano-modification of a stabilising agent.…”
Section: Secondary Minerals Defining the Condition Of The Stonementioning
confidence: 99%
See 1 more Smart Citation
“…The engineering properties of the naturally available materials will change considerably over time, depending on the stage of chemical weathering (Figure 11 (recreated from [40])). As previously discussed, the mineral composition with specific reference to the silicon content, can have a considerable influence on the bond strengths achieved with the material when using a specific nano-modification of a stabilising agent.…”
Section: Secondary Minerals Defining the Condition Of The Stonementioning
confidence: 99%
“…The "clay problem" is a subject that in itself requires extensive discussion which will not be covered in any detail within this article. In order to appreciate the considerable challenges offered by materials containing a high percentage of clay, the properties of some of the most commonly found clays are summarized in Table 5 (based on [40]). 5 is of high importance when stabilising materials containing high percentages clay using a nano-silane modifications and the selection of an applicable stabilising agent.…”
Section: Secondary Minerals Defining the Condition Of The Stonementioning
confidence: 99%
“…This property of clay arose from isomorphous substitution, a crystal lattice defect in which a given ionic series may be replaced by another in a crystal lattice [24]. According to Neeraj and Chandra [4], values of CEC range from 3-15 in kaolinites through 15-40 in chlorites and illites, 70-100 in montmorillonite and 100-150 in vermiculite.…”
Section: Cation Exchange Capacitymentioning
confidence: 99%
“…Iron substitute for aluminum and magnesium to varying degrees and appreciable quantity of potassium, sodium and calcium are frequently present [3]. Based on their structures and chemical compositions, the clay minerals can be divided into four main classes of kaolinite, smectites, illites and micas [4]. However, Sarkar et al [5] and Walter [6] refer to two or three classes of clays since illites are sometimes referred to as a 2:1 layer and not a 2:1:1.…”
Section: Introductionmentioning
confidence: 99%
“…The "clay problem" is a subject that in itself requires extensive discussion, which will not be covered in any detail within this article. In order to appreciate the considerable challenges offered by materials containing a high percentage of clay, the properties of some of the most commonly found clays are summarized in Table 5 (based on [40]). The specific surface area of the different clays (in m 2 /g) shown in Table 5 is of high importance when stabilising materials containing high percentages of clay using a nanosilane modifications and the selection of an applicable stabilising agent.…”
mentioning
confidence: 99%