Maybe the dividing slash has been omitted and it should read kg/m3, that is kilograms per cubic meter
Convert: 1kg/m3 to g/cm3 1kg=1000g 1m3=100*100*100=1000000cm3 therefore: 1000g/1000000cm3 = 0.001g/cm3 4200kg/m3 * 0.001g/cm3 = 4.2g/cm3
The pressure at a depth of 100 m below the surface can be calculated using the formula: pressure = density x gravitational acceleration x depth. Given the density of 1150 kg/m^3 and assuming a gravitational acceleration of 9.81 m/s^2, the pressure at 100 m below the surface would be approximately 1147,850 Pa.
You can solve this in two steps. (1) Calculate the ball's volume. Use the formula for a sphere, and remember that the radius is 1/2 the diameter. Convert the result it either to cubic decimeters (= liters) or to cubic meters. (2) Divide the mass by the volume.
"Struck" is the past tense of the verb "strike," which can mean to hit, collide with, or make contact with forcefully. It can also mean to be affected by a particular situation or emotion.
Mean square distance is a statistical measure that provides information about the dispersion of data points from the mean. It is commonly used in various fields such as physics, engineering, and finance to quantify the variability of a dataset. A smaller mean square distance indicates that data points are closer to the mean, while a larger mean square distance suggests more variability in the data.
The volume is 5m3 density=1,200 kgm3 what is the mass
11995 kgm3
7850 kg/m3
density
MPa (Megapascal) is a unit of pressure, while kg/m^3 (kilograms per cubic meter) is a unit of density. They measure different physical properties and cannot be directly converted from one to the other.
1 gram/centimeter3 (g/cm3) equals 1000 kilogram/meter3 (kg/m3)
=57.04 See related link "API Gravity" for more information
It is 352000 kg/m^3. This is absurdly dense: Osmium, the most dense element on earth has a density of 22.6 g/cm^3 - less than a fifteenth of your substance.
P= density x gravity x height and the answer is negative because air is reduced in the straw
We estimate the pressure difference (specifically due to hydrostatic effects) as follows:Δp = ρgΔh =(pgh1-pgh2)(1.06 × 103 kg/m3) (9.8m/s2) (1.83 m-0) =1.90 × 104 Pa .
There are 1 g/mL in 1 kg/m^3. This is because 1 kg/m^3 is equivalent to 1000 g/L, and since 1 L is equal to 1,000 mL, 1000 g/L is equivalent to 1 g/mL.
The buoyant force on a submerged object is equal to the weight of the displaced fluid. The density of the water is 1,000 kg/m3, so its weight is 1,000 N/m3. The volume of the rock is 0.3 m3. The buoyant force = weight of the displaced water = (0.3 x 1,000) = 300 N.