it will decrease
by placing the gas into a container of any kind and it will simply fill up the whole container, therefore you can observe it and what it does.
A gas consists of particles, which are either atoms or molecules, which all move randomly, and independently of each other. Every time a particle bounces off the wall of a container, it exerts some degree of pressure. The total of all the particles bouncing off the walls creates the pressure that we observe.
You observe the ice melt. You can measure the resulting reduction in the water temperature.
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Thermometers measure temperature. To make their forecasts, metereologists need to observe it as well as other factors such as atmospheric pressure, wind speed, wind direction, humidity and precipitation (rain).
Due to Charles's law, the pressure would increase.
by placing the gas into a container of any kind and it will simply fill up the whole container, therefore you can observe it and what it does.
A gas consists of particles, which are either atoms or molecules, which all move randomly, and independently of each other. Every time a particle bounces off the wall of a container, it exerts some degree of pressure. The total of all the particles bouncing off the walls creates the pressure that we observe.
Desceibe some of the general patterns you observe for temperature and salinity
You can observe water droplets on the surface of a chilled bottle because the temperature of the atmosphere is a different temperature to that of the temperature in the chilled bottle.
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true
solid It is common to observe that gold jewellery is hard, not liquid or gaseous.
You observe the ice melt. You can measure the resulting reduction in the water temperature.
The temperature change is needed to calculate the enthalpy change.
As the magnification of the objective increases, the FOV decreases
Well as you go further down into the ocean, it will be colder. Usually but not always!! Temperature and salinity affect the density of seawater, and in many systems, density increases with depth (as temperature decreases and salinity increases). IT is however possible to observe patterns where dense water at depth is either very salty but warm, or very cold, but nearly fresh.