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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
Fase duidt in de scheikunde en de natuurkunde op de verschijningsvorm van een stof met macroscopisch gezien homogene chemische en fysische eigenschappen. Deze eigenschappen hebben het karakter van een statistisch gemiddelde. Bijgevolg is het begrip fase enkel gedefinieerd voor een hoeveelheid materie van voldoende grootte. Twee fasen worden van elkaar gescheiden door een scheidingsvlak; meer specifiek is de meniscus het scheidingsvlak tussen twee niet mengbare vloeistoffen, of tussen een vloeistof en een gas. Klassiek onderkende men als macroscopische verschijningsvormen de aggregatietoestanden vast, vloeibaar en gasvormig. Later werden daaraan nog de aggregatietoestanden plasma en bose-einsteincondensaat toegevoegd. Met name binnen de vaste verschijningsvorm bestaan nog verschillen, zoals tussen grafiet en diamant, twee verschillende fasen van vaste koolstof. De chemische thermodynamica houdt zich bezig met de studie van verschillende fasen en de overgangen daartussen, de faseovergangen, zoals smeltpunt en kookpunt. De eenvoudigste faseovergangen zijn die tussen vaste stof, vloeistof en gasfase. Vaste stof komt voor als kristallijne, of als amorfe materie: glas, rubber, gel. Vloeistof is meestal isotroop, maar er bestaan ook anisotrope vloeistoffen (vloeibare kristallen). Veel kristallijne vaste stoffen vertonen, afhankelijk van temperatuur en druk, chemisch identieke, maar fysisch onderling verschillende, kristallijne fasen; ijs komt bijvoorbeeld in ten minste vijftien verschillende fasen voor. Iedere kristallijne fase (polymorf) van een gegeven stof is stabiel bij een karakteristieke temperatuur en druk. Het voorkomen van een samengestelde, vaste stof in meer dan een kristalstructuur wordt polymorfie genoemd. Het voorkomen van verschillende fysische verschijningsvormen van een enkelvoudige, vaste stof wordt allotropie genoemd. Diamant, een allotroop van koolstof, wordt diep in de aardkorst als stabiele fase van koolstof gevormd, onder enorm hoge druk en bij hoge temperatuur. Na delving blijven diamanten, onder lagere druk en temperatuur, als metastabiele fase van koolstof bestaan. Bij extreem lage temperaturen zijn nog andere aggregatietoestanden mogelijk: * bose-einsteincondensaat * superfluïde fase (komt voor bij helium). * supergeleidende fasen. Daarnaast zijn er stoffen met een ferromagnetische fase en een paramagnetische fase. Een andere bekende fase is de glasfase. Bij zeer hoge temperaturen treedt de plasmafase op.
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