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====Metallography==== Differential hardening will produce two different zones of hardness, which respond differently to grinding, sharpening, and polishing. The back and center of the blade will grind away much quicker than the edge, so the polisher will need to carefully control the angle of the edge, which will affect the geometry of the blade. An inexperienced polisher can quickly ruin a blade by applying too much pressure to the softened areas, rapidly altering the blade's shape without much change to the hardened zone.<ref name="autogenerated3">Smith</ref> [[File:Katana hardened edge pic with inset of nioi.JPG|thumb|A katana, shown at a long angle to reveal the nioi, which is the bright line following the hamon. The inset shows a close up of the nioi, which appears as the speckled area between the bright hardened edge and the darker soft zone. The wood-grain appearance is from the folding techniques used during [[forging]].]] Although both the pearlite and martensite can be polished to a mirror-like shine, only the back and spine are usually polished to such an extent. The hardened portion of the blade (yakiba) and the center portion (hira) are often given a matte finish instead, to make the differences in the hardness stand out. This causes the various microstructures to reflect light differently when viewed from different angles. The pearlite takes on longer, deeper scratches, and either appears shiny and bright, or sometimes dark depending on the viewing angle. The martensite is harder to scratch, so the microscopic abrasions are smaller. The martensite usually appears brighter yet flatter than the pearlite, and this is less dependent on the viewing angle.<ref name="autogenerated3"/> When polished or etched with acid to reveal these features, a distinct boundary is observed between the martensite portion of the blade and the pearlite. This boundary is often called the "temper line", or the commonly used Japanese term, the "[[hamon (swordsmithing)|hamon]]". Between the hardened edge and the hamon lies an intermediate zone, called the '"nioi" in Japanese, which is usually only visible at long angles. The nioi is about a millimeter or two wide, following the hamon, which is made up of individual martensite grains (niye) surrounded by pearlite. The nioi provides a very tough boundary between the yakiba and the hira.<ref name="Smith, pp. 49β52"/>
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