Simple orthorhombic is a type of crystal lattice system characterized by three mutually perpendicular axes of differing lengths. In this structure, each unit cell is defined by the lengths of the three axes, which are typically denoted as a, b, and c, where a ≠ b ≠ c. This arrangement allows for a variety of crystal shapes and properties, making it an essential category in the study of lattices and Bravais lattices.
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