Temperature

The specific heat capacity of lead is approximately 0.128 J/g°C. The temperature change is 85.6°C - 25.5°C = 60.1°C. Using the formula Q = mass x specific heat x temperature change, the heat required is 69g x 0.128 J/g°C x 60.1°C = 530.88 Joules.

The freezing point of water is 0°C or 273K in correct SI units.

Yes, of course. 36 is a lower number than 46. 32 degrees (F) would be freezing.

The Earth's mantle has a temperature range of about 500 to 900 degrees Celsius (932 to 1652 degrees Fahrenheit) near the upper boundary with the crust, and can reach temperatures of up to 3700 degrees Celsius (6692 degrees Fahrenheit) near the core-mantle boundary.

-25.6 degrees Fahrenheit.

The region being described is the thermosphere. It extends from about 50 km to 500 km above Earth's surface and is known for its high temperatures due to the absorption of solar radiation by the few particles present in this layer.

The highest recorded temperature in San Antonio, Texas is 111°F (44°C), which occurred on September 5, 2000.

180 degrees Celsius is 356 degrees Fahrenheit.

An electrolyte has a greater effect on the boiling point compared to a non-electrolyte when dissolved in water. This is because electrolytes break into ions in solution, increasing the number of particles and thus raising the boiling point more significantly through colligative properties compared to non-electrolytes which do not dissociate into ions.

The corona of the Sun has a temperature of about two million degrees Kelvin. It is the outermost layer of the Sun's atmosphere and is visible during a total solar eclipse as a glowing halo around the darkened disk of the Moon.

It is -10 deg F.

46.4°F is equal to 8°C.

The specific heat capacity of water is 4.18 J/g°C. To raise the temperature of 0.25 kg (250 g) of water by 10°C, you would use the equation Q = m * c * ΔT, where Q is the heat energy, m is the mass, c is the specific heat capacity, and ΔT is the change in temperature. Thus, Q = 250g * 4.18 J/g°C * 10°C = 10450 Joules.

When the temperature cools to 1000 degrees Celsius, the water vapor molecules lose energy and slow down, eventually condensing into liquid water droplets as they reach their saturation point. This process is known as condensation.

4.2 Kelvin is -268.95 degrees Celsius.

It is very cold because water freezes at 32 degrees Fahrenheit

Start by taking the number in Celsius and multiply it by 9. Then divide that number by 5, and then add 32. This is how you convert Celsius to Fahrenheit or use the equation F = (9/5)C + 32
In this case, the answer is about 143.6 degrees Fahrenheit.

That depends upon the air pressure around the water. At one atmosphere, the average air pressure at sea level on Earth, it would be a gas.

Yes, but this is only caused by difference in effect of evaporation during cooling or warming up. It costs energy to evaporate and that is mainly acquired from the liquid, so stimulating the cooling (faster) and counteracting at warming up (slower).

33.7 degrees celsius is 92.66 degrees fahrenheit.

33.7 degrees fahrenheit is 0.94 degrees celsius.

The Celsius temperature scale has 100 degrees between freezing and boiling.

The boiling point of a liquid is the temperature at which the vapor pressure of the liquid equals the atmospheric pressure, causing the liquid to change into a gas. It is a characteristic property of the liquid and can be influenced by factors such as pressure and impurities in the liquid.

It doesn't have a melting point as it is a thermosetting plastic, meaning it can be heated but it will not melt, instead the temperature will be raised until it burns.

Hope this help :D

There is a great range of temperatures on Earth. These temperatures range from far be low zero to more than 100 degrees Fahrenheit just on Earth's crust.

50 degrees is hotter on the Celsius scale.