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- W1198444954 abstract "Soil is a three-phase system. This chapter focuses on the solid phase, which is the permanent component of the soil. The soil's solid phase consists of mineral particles having various shapes and sizes, as well as amorphous compounds such as organic matter and hydrated iron oxides, which are generally attached to the particles. Soil particles are classified according to their sizes, and the soil is characterized as a whole in terms of the relative proportions of those size groups. The groups may differ from one another in mineral composition as well as in particle size. It is these attributes of the soil solid phase, particle size, and mineral composition that largely determine the nature and behavior of the soil, its internal geometry and porosity, its interactions with fluids and solutes, its compressibility, strength, and thermal regime. Soil texture and range of particle sizes in a soil carry both qualitative and quantitative connotations. Qualitatively, it represents the feel of the soil material, whether coarse and gritty or fine and smooth to the touch. An experienced soil classifier can feel, by rubbing the moistened soil with his fingers, whether it is coarse textured or fine textured, and can even assess, semiquantitatively, the textural class to which the soli belongs." @default.
- W1198444954 created "2016-06-24" @default.
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- W1198444954 date "2003-01-01" @default.
- W1198444954 modified "2023-09-27" @default.
- W1198444954 title "Particle Sizes, Shapes, and Specific Surface" @default.
- W1198444954 doi "https://doi.org/10.1016/b978-012348655-4/50004-6" @default.
- W1198444954 hasPublicationYear "2003" @default.
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