Titlebook: Inorganic Constituents in Soil; Basics and Visuals Masami Nanzyo,Hitoshi Kanno Book‘‘‘‘‘‘‘‘ 2018 The Editor(s) (if applicable) and The Auth

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Primary Minerals,f the Earth’s crust, rocks, and minerals. Soils at the top of the Earth’s crust are also within the rock cycle. Silicate and silica minerals, which constitute more than 90% of the minerals in the Earth’ crust, are outlined. Samples of relatively un-weathered and weathered primary minerals were obtai

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Secondary Minerals, soils, are phyllosilicates that have 1:1 or 2:1 type layers. The 1:1 type minerals are kaolinite and halloysite. The 2:1 type minerals are smectite, vermiculite, micaceous minerals, and chlorite. Gibbsite and manganese oxides are introduced as examples of hydroxides and oxides, respectively. This c

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Inorganic Soil Constituents Sensitive to Varying Redox Conditions, are analyzed using optical and electron microscopes, energy dispersive X-ray spectroscopy (EDX), and X-ray diffraction (XRD). Many of these minerals are sourced from paddy field soils, which undergo reducing and oxidizing conditions in the plow layer every year. Iron mottles formed at the soil redo

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Book‘‘‘‘‘‘‘‘ 2018outlines of soil minerals, new methods and recent developments in the field, with a special focus on visual aids. .The chapters on primary minerals, secondary minerals, non-crystalline inorganic constituents and inorganic constituents sensitive to varying redox conditions will help readers understan