Sentences with phrase «vapor phases of»

Place vials in the vapor phase of liquid nitrogen storage immediately upon receipt until it is convenient to proceed to subculture.

Not exact matches

Whether in the form of liquid, foam, vapor - phasing cascading or circulation, we incorporate the proper chemistry to eliminate deposits and scaling and maintain the integrity of the system being cleaned.

The forces holding diiodine molecules in the crystal are modest, and liquid iodine is not stable at ordinary temperatures and pressures, so that solid iodine sublimes to give a rather large concentration of diatomic molecules in the vapor phase.

Condensation is a phase transition of matter that occurs when water vapor contained in hot, humid air comes in contact with a cold surface.

The only high - temperature process that could separate the potassium isotopes in this way, said Wang, is incomplete condensation of the potassium from the vapor phase during the Moon's formation.

These customary phase transitions manifest as an abrupt change in the state of matter such as ice melting to water, or water boiling to vapor, at some critical temperature.

High - speed collisions that heat and compress it can give rise to new phases of nuclear matter: a vapor and perhaps a solid and a plasma

It is well known to scientists that the three common phases of water — ice, liquid and vapor — can exist stably together only at a particular temperature and pressure, called the triple point.

83 WebHubTelescope: Marler, you don't seriously believe that there is some new state of matter or new phase transition that allows water vapor to be a positive feedback from 255K to 288K but then do a U-turn and become a negative feedback when the temperature hits 289K?

The height redistribution in the atmosphere of condensation nuclei with a change of the electric field of the atmosphere is accompanied by a change in total latent heat (phase transition of water vapor), by changes in radiation balance, and by subsequent changes of the thermobaric field of troposphere.

Marler, you don't seriously believe that there is some new state of matter or new phase transition that allows water vapor to be a positive feedback from 255K to 288K but then do a U-turn and become a negative feedback when the temperature hits 289K?

The thermodynamics of water are simplified in that only the vapor - liquid phase transition is taken into account, and the latent heat of vaporization is taken to be constant, as in Frierson et al. (2006).

when you can design a model that can even predict a temperature profile of: a 4 degrees of freedom, rotating sphere, that is warmed by the output of a non-linear external heat source, and that is covered in a thermodynamic fluid that is constantly in motion with non-linear chaotic Beyesian characteristics — and then throw in variability due to non-linearity behavior of an element that can cause both positive and negative feed - backs due to the existence of it's three phases; liquid, vapor and solid....

In fact, water in all of its phases, whether ice, liquid, or vapor, moderates temperature.

We have had lengthy heating phase caused by a spurt of insolation, now we have had a big El Nino, a subsequent shift to La Nina and the resulting warm currents moving up the the Western Pacific, causing warming polar oceans and changes in atmospheric water vapor content.

The notion of an H2O positive feedback (which probably is present on a clear day) is squashed by this process.While warmer air can hold exponentially more water vapor, presumably increasing greenhouse effects (an process the IPCC hangs its collective hat on), it is also this exact same property that vastly improves the chances of convective and phase change heat transport by thunderstorms.

Thus, the phase change of water from liquid to gas, after absorbing photons, is a feedback, the absorption of photons and the emission of photons atmospheric water vapor is a forcing, but the photons released when gaseous water become liquid water is a feedback.

The gas - phase reaction of methane sulfonic acid with the hydroxyl radical without and with water vapor

These last equations are useful because they relate equilibrium or saturation vapor pressure and temperature to the latent heat of the phase change, without requiring specific volume data.

These algorithms, developed for national and international operational and research satellite programs, convert sensor / instrument measurements into geophysical parameters such as vertical temperature / water vapor profiles, estimates of cloud amount, type and phase, and land / ocean parameters such as sea surface winds, net heat flux, and forest fire intensity / extent.

So water dances at many speeds, from the unimaginable fast vibrations of its molecules responding to thermal infrared radiation, to the moment - to - moment dance of its phase changes in response to temperature changes, to the week - long dance of its vapor in and out of the atmosphere, to the slow geological pavanes of rock, air and life, of which it too forms an inextricable part.

As the concentration of gaseous water (water «vapor») in the atmosphere is on the order of 3o, 000 to 40,000 ppm, this trace greenhouse gas really * is * the invisible 800 lb gorilla in the room even if we ignore the phase change effects.

With decreasing temperature the equilibrium shifts to favor the liquid phase (with the caveat that the process can be very slow due to the empirically observed tendency of vapor molecules to bounce off droplets when intuition would suggest they would stick at first hit).

In conclusion, liquid CO2 must be produced through following subseafloor processes: phase separation of hydrothermal fluid due to boiling, formation of solid CO2 - hydrate due to cooling of vapor phase, and melting of the solid CO2 - hydrate to liquid CO2 due to a temperature increase within the sedimentary layer.

Without convection and the multiple phases of water vapor, the earth's surface would be close to or above the boiling point of water.

Water in the gaseous phase, water vapor, is a key element in both of these.

However, as the water vapor rises the lapse rate means that the volume of air cools and eventually the water vapor condenses into water droplets and then into ice latent heat is given off to the surrounding air at each of these phase changes, with two effects.

So when the liquid phase change refrigerant is chugging heat past the tropopause and indeed CREATING the tropopause indirectly — CO2 that gets left aloft sort of rides on the top of the lower troposphere after water vapor carries it up repeatedly in convective lift --

Whereas the condensation of water vapor liberates heat and whereas that phase change does not exhibit a temperature change therefore, black bodies from outer space are not telling much about the planet's energy flux.

Any heat radiation penetrating the canopy and incident on the soil again goes towards phase changing water, water in the soil moisture, but this happens in a limited quantity based on saturation point of vapor in the surrounding.

With regard to suricat's ideas: When someone conflates the ideas of liquid / vapor phase transition with an El - Niño / La - Niña phase transition, and tries to bring in the Clausius - Clapeyron equation, I have to assume they are arguing by free - association.

There is nothing in the phase transition from solid ice, or liquid water, to H2O vapor by sublimation or evaporation; that suddenly turns off the ability of those molecules to emit a BB like thermal continuum radiation spectrum according to Planck formula and other applicable laws (don't forget the emissivity).

We propose a different source of potential energy associated with water vapor removal from the gas phase: after the Mayan forests were destroyed, evaporation and condensation ceased to occur over the Yucatan peninsula (irrespective of how its albedo changed).