Segui i suggerimenti del progetto di riferimento. Fisici dell’Istituto di fisica atomica e molecolare dell’olandese FOM hanno studiato i processi di collasso dei condensati e hanno osservato che la condensazione di Bose-Einstein ha inizialmente una coerenza locale e solo in seguito la coerenza si estende su tutto il condensato. Il buco nero acustico dovrebbe esplodere in un impulso di fononi, analogamente ai buchi neri tradizionali che, secondo la teoria di Hawking , dovrebbero evaporare tramite la radiazione di Hawking. Alla Princeton University si ipotizza che la materia oscura possa esser composta da condensati. Nel il gruppo INFM del LENS di Firenze ha prodotto il primo condensato di potassio tramite una tecnica innovativa di contatto termico con un campione di atomi di rubidio in una trappola magnetica. Nel un gruppo di fisici tedeschi ha proposto un metodo per indurre un gas di bosoni ultrafreddi a comportarsi da fermioni e a non condensare. Nel giugno un gruppo del NIST ha verificato l’ effetto Hall quantistico di spin in un condensato di atomi di Rubidio creando un prototipo di transistor spintronico .
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Uncertainty quantification and Uncertainty propagation The most commonly used procedure for calculating measurement uncertainty is described in the “Guide to the Expression of Uncertainty in Measurement” GUM published by ISO. The uncertainty of the result of a measurement generally consists of several components.
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This may be denoted by error bars on a graph, or by the following notations: The precision is symmetric around the last digit. In this case it’s half a tenth up and half a tenth down, so Thus it is understood that
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Condensato di Bose-Einstein
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Structure of the atmosphere Earth’s atmosphere Lower 4 layers of the atmosphere in 3 dimensions as seen diagonally from above the exobase. Layers drawn to scale, objects within the layers are not to scale. Aurorae shown here at the bottom of the thermosphere can actually form at any altitude in this atmospheric layer.
Principal layers In general, air pressure and density decrease with altitude in the atmosphere. However, temperature has a more complicated profile with altitude, and may remain relatively constant or even increase with altitude in some regions see the temperature section, below. In this way, Earth’s atmosphere can be divided called atmospheric stratification into five main layers. Excluding the exosphere, the atmosphere has four primary layers, which are the troposphere, stratosphere, mesosphere, and thermosphere.
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