This statement is false. Open winding will affect the resistance reading of the start winding as well as the resistance reading between the run and start terminals.
The resistance reading of the start winding, as well as the resistance reading between the Run and Start terminals, will be unaffected by open winding. If a resilient-mounted motor develops a short to the frame, the technician can simply cut the ground strap wire as a permanent repair.
The winding terminals are open in an open winding. This type of armature winding is only found in AC machines such as induction machines and synchronous machines.
There are two types of motor windings, i.e., stator winding and rotor winding.
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During the course of its history Egypt was invaded or conquered by a number of foreign powers, including the Hyksos, the Libyans, the Nubians, the Assyrians, the Achaemenid Persians, and the Macedonians under the command of Alexander the Great.
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Answer: Although the European Renaissance is commonly studied, it is routinely considered only in the context of European artistic developments and rarely global artistic trends. Korean art of the same period (1400-1600CE) was going through a similar pattern of rebirth and development. Both groups were dealing with political and social change that was reflected in the development of new and revival art styles. There are three main elements that occur in both areas, secularism, retention of religious art, and the revival of classical styles. Secularism became increasingly popular, while traditional religious works, based on Christianity and Buddhism remained present and were sponsored by royal patrons. Artistic revival differs in the topics being revived, but both cultures looked to past artists to inspire new works. The Koreans looked to Song Dynasty classics and other landscapes to inform their new works, while Italian artists looked to classical Greek subjects and style, reviving the flowing fabrics and glorification of the human form that was lost in medieval works.
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Igneous rocks form when magma cools and crystallizes, either at volcanoes on the surface of the Earth or while the melted rock is still inside the crust. All magma develops underground, in the lower crust or upper mantle, because of the intense heat there. Igneous rocks can have many different compositions, depending on the magma they cool from. They can also look different based on their cooling conditions. For example, two rocks from identical magma can become either rhyolite or granite, depending on whether they cool quickly or slowly.
