Ceramic mosaic is a relatively ancient craft, the traditional mosaic. Ceramic mosaic, in the other dazzling array of generous tiles, its delicate posture. Some ceramic mosaics are polished and irregularly formed, creating the erosion of the years to shape a sense of history and nature. These mosaics retain the simplicity and weight of pottery. The bright spot lies in its profound cultural connotations. Designers generally like to design ceramic mosaics as bathroom owners Ceramic mosaic.
The waist line of the tile wall on the wall, because today’s ceramic mosaic burns out the color is richer, with each kind of color collocation collocation collages the pattern, may inlay on the wall to make the picture. Covered in the floor can play the role of carpet decoration. Ceramic mosaic to give people the feeling is more noble and elegant, antique effect is very good. Bathroom suitable for classical style. Ceramic mosaics have different quality requirements for products used in different occasions
Clay is a finely-grained natural rock or soil material that combines one or more clay minerals with traces of metal oxides and organic matter. Geologic clay deposits are mostly composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure. Clays are plastic due to their water content and become hard, brittle and non–plastic upon drying or firing. Depending on the soil’s content in which it is found, clay can appear in various colours from white to dull grey or brown to deep orange-red.
Although many naturally occurring deposits include both silts and clay, clays are distinguished from other fine-grained soils by differences in size and mineralogy. Silts, which are fine-grained soils that do not include clay minerals, tend to have larger particle sizes than clays. There is, however, some overlap in particle size and other physical properties. The distinction between silt and clay varies by discipline. Geologists and soil scientists usually consider the separation to occur at a particle size of 2 µm (clays being finer than silts), sedimentologists often use 4–5 μm, and colloid chemists use 1 μm. Geotechnical engineers distinguish between silts and clays based on the plasticity properties of the soil, as measured by the soils’ Atterberg limits. ISO 14688 grades clay particles as being smaller than 2 μm and silt particles as being larger.
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