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{{Main|ପଦାର୍ଥର ଅବସ୍ଥା}}
Classically, states of matter are distinguished by changes in [[specific heat capacity]], [[pressure]] and [[temperature]]. States are distinguished by a discontinuity in one of those properties: for example, raising the temperature of ice produces a clear discontinuity at 0 °C as energy goes into [[phase transition]], instead of temperature increase.
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