To find the Celsius temperature of 100.0 g of chlorine gas in a 55.0-L container at 800 mm Hg, we can use the Ideal Gas Law: PV = nRT. First, calculate the number of moles (n) of chlorine (Cl2), which has a molar mass of approximately 70.9 g/mol. Thus, n = 100.0 g / 70.9 g/mol ≈ 1.41 moles. Next, convert the pressure from mm Hg to atm (800 mm Hg / 760 mm Hg/atm ≈ 1.05 atm), and then rearranging the Ideal Gas Law gives T = PV/nR. Using R = 0.0821 L·atm/(K·mol), we can calculate T and convert it to Celsius. The final temperature is approximately 382.6 K, which is about 109.5 °C.
1000 degrees celsius to 3,700 degrees celsius
The temperature at a depth of 1000 km inside the Earth can reach around 1000 to 2000 degrees Celsius. This heat is primarily generated by the radioactive decay of elements in the Earth's mantle and core.
When you transfer the helium gas from a 500 mL container to a 1000 mL container, its pressure will decrease while the temperature remains constant, according to Boyle's Law. The density of the helium will also decrease because density is defined as mass divided by volume. However, the amount of helium (in grams) and its temperature will not change during this process.
The maximum temperature that can be achieved by the yellow flame of a Bunsen burner is around 1,000 to 1,300 degrees Celsius. The temperature can vary depending on the air-to-gas ratio and the quality of the burner.
it is estimated to be about 7000 degrees celsius 1000 degrees hotter than the outer core (6000 degrees celsius)
with the help of pyrometer
At 1000 degrees Celsius, oxygen exists in a gaseous state. Oxygen gas (O2) is a colorless and odorless gas at this temperature.
At 1000 degrees Celsius, xenon is in the gaseous state. Xenon is typically a gas at room temperature and pressure, and it remains gaseous even at higher temperatures like 1000 degrees Celsius.
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
1000 degrees celsius to 3,700 degrees celsius
in normal lapse rate 6.4* Celsius is reduced per 1000 m height whether adiabatically 9.8* Celsius per 1000 m elevation
At 1000 degrees Celsius, oxygen exists in a gaseous state. This high temperature well exceeds oxygen's boiling point of -183 degrees Celsius, causing it to be present as a gas.
The average temperature gradient in the Earth's crust is approximately 25-30 degrees Celsius per kilometer of depth. Therefore, the total temperature change between 1000 m and 4000 m in depth would be around 75-120 degrees Celsius.
At 1000 degrees Celsius, iron is in a solid state and is likely glowing red hot. This temperature is below iron's melting point of 1538 degrees Celsius, so it would still retain its solid form.
No. The lowest temperature , with oxygen closed off and a yellow flame , is about 1000 degrees Celsius. With oxgen feed open temperature of the flame can reach 1300 degrees.
1000 deg Celsius = 1273.15 deg Kelvin
1,000 degrees Celsius = 1,832 degrees Fahrenheit