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Also known as phase of matter
однородная часть разнородной термодинамической системы, обобщение агрегатного состояния вещества
A phase is a portion of a substance where all the properties—like temperature, density, and chemical makeup—are essentially the same throughout, and it's often physically separate from other parts of the material. Understanding phases matters because it helps us predict how substances behave and change, such as when water turns to ice or steam, and how different materials interact with each other.
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Phases – The Physics Hypertextbook
The 3 most famous phases of matter are solid, liquid, and gas. Did you know that glass is also a phase? Or that plasma is the most common phase in the universe?, The 3 most famous phases of matter are solid, liquid, and gas. Did you know that glass is also a phase? Or that plasma is the most common phase in the universe?
physics.info →Notes from some long forgotten source. "Chaos (χαος) was used to define the most disperse and fluid state of matter, that in which no particular order could be observed. Interestingly enough, when van Helmont wanted to refer to steam-state of materials he was studying used the term chaos but in the particular Flemish accent, converting it to gas, by which the state is known to us today." To my mind it appears that the difficulty is only imaginary and not real. Rigidity and plasticity are not absolute terms but relative, and all solids are in fact both rigid and plastic. The apparent contrast between the two properties belongs to the laboratory and to those phenomena of nature involving small masses and small forces. When great masses and great forces are involved, as for example in the making of continents and mountain chains, the distinction loses value. The phenomena of mountain structure demonstrate that under sufficient strains great bodies of rock both bend and flow. Increased pressure increases the range of temperatures over which a substance can exist as a liquid. Reduced pressure reduces this range. At a certain special pressure the boiling and melting points will equal, and the substance can no longer exist as a liquid. Below this pressure, the only possible phase transition is from solid to gas (and vice versa). This phase change is called sublimation (the reverse process is called deposition or desublimation) and the temperature at which it occurs is called the sublimation point (or sublimation temperature). That's the essence of the upcoming discussion. If this is enough info for you, stop reading and jump to the next section. If you want to understand what I'm talking about then keep reading. Knowing why some phenomenon occurs is often more important than knowing that it occurs. (Of course, the reverse is also true, which is why I offer you the option to read on or jump ahead.) To a certain extent, liquids are like a minimum security prison. (Solids are like a maximum security prison in permanent lock down, but that's another matter.) The molecules within have limited freedom and can only leave infrequently or with great effort. As long as a liquid has some surface area exposed to the atmosphere, here and there a molecule within the liquid near the surface will be moving fast enough to escape the liquid prison and enjoy the freedom of a vapor molecule in the surrounding atmosphere. But rather unlike a a prison, the reverse process is also possible. From time to time, a molecule in the atmosphere will be traveling fast enough to plow its way through the tightly guarded walls of the liquid only to find itself trapped within. Both events are happening simultaneously, but not necessarily with equal probability. What is boiling and how is it different from evaporation? Both processes involve the same liquid to gas phase transition, but where evaporation can occur at any temperature boiling occurs only at a specific temperature. Let's return to the description of evaporation just discussed. Evaporation occurs whenever more molecules leave a liquid than enter. Condensation occurs whenever more enter than leave. These changes are driven by the concentration of liquid molecules in the atmosphere. When their concentration is low, it's more likely that molecules will leave the liquid phase than enter it, so evaporation rules. When their concentration is high, it's more likely that molecules will enter the liquid phase than leave it. When neither process dominates it must be because the atmosphere has just the right concentration of liquid molecules floating around within it — no more, no less than what it can handle. Under these circumstances the atmosphere is said to be saturated. The most energetic vapor molecules present in the atmosphere are fighting their way into the liquid. The most energetic liquid molecules are fighting their way out into the atmosphere. There's room in the atmosphere, but it has a limit. When
Термодинами́ческая фа́за — гомогенная часть гетерогенной системы, ограниченная поверхностью раздела. Менее строго, но более наглядно фазой называют гомогенную часть системы, отделенную от остальных частей видимой поверхностью раздела, на которой скачком меняются какие-либо характеристики фазы, например плотность, состав, оптические свойства. При этом совокупность отдельных гомогенных частей системы, обладающих одинаковыми свойствами, считается одной фазой (например, совокупность кристаллов одного вещества или совокупность капелек жидкости, взвешенных в газе и составляющих туман). Каждая фаза системы характеризуется собственным уравнением состояния. При переходе через поверхность раздела хотя бы одно термодинамическое свойство вещества изменяется скачком. Часто (но не всегда) поверхность раздела является видимой невооружённым глазом. Гомогенная система содержит только одну фазу; гетерогенная система состоит из двух или более фаз. Система «лёд — вода — влажный воздух» — гетерогенная трёхфазная. В однокомпонентной системе разные фазы могут быть представлены разными агрегатными состояниями или разными полиморфными модификациями твёрдого вещества (ромбическая и моноклинная сера, серое и белое олово и др.). Число фаз в гетерогенной системе подчиняется правилу фаз Гиббса. В многокомпонентной системе фазы могут иметь различный состав и структуру. В любом случае при наличии раздела фаз подразумевается принципиальная возможность перехода вещества из одной фазы в другую. Многофазная система находится в термодинамическом равновесии, если все её фазы находятся в механическом, тепловом и фазовом равновесии друг с другом.
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Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).
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