Yes. It would be hard to find a rock with that volume, but I'm sure there is one out there.
1,500 mL
It would be 60 ml
Density = Mass/Volume = 50g/12.5mL = 4 g per mL
The level of the liquid in the cylinder rose by 10 mL when the rock was submerged in the liquid.
Yes. It would be hard to find a rock with that volume, but I'm sure there is one out there.
The mass of water added is 110 g minus the initial empty cylinder mass. The mass of the rock is the total mass of 250 g minus the mass of the water and empty graduated cylinder. The density of the rock can then be calculated using the mass of the rock and its volume (37 mL - 30 mL).
The volume of a typical glass of juice is 250 mL.
To find the volume of the rock, you can use the formula: Volume = Mass / Density. Plug in the values: Volume = 16 grams / 4 g/ml = 4 ml. So, the rock occupies a volume of 4 ml.
The volume of the object can be calculated by subtracting the initial volume (250 ml) from the final volume (300 ml), which gives a difference of 50 ml. Since 1 ml is equal to 1 cubic centimeter, the volume of the object is 50 cubic centimeters.
The water volume is 212,5 mL.
The volume of water will still be 250 mL once the ice melts. The ice will melt into water, but the total volume of the container will remain the same.
250 ml. A cc (cubic centimeter) and a mL (millilitre) are equal to each other in terms of volume.
(volume) x (density) = mass (250 ml) x (1 g/ml) = 250 grams 1 ml = 1 cc
You have answered this question for yourself. The Density is 0.94 g/mL However, do you mean , 'what is the rocks volume?' Remember the eq'n density = mass./ volume. Algebraically rearranged volume = mass / density Hence volume = 20g/ 0.94 g/mL volume = 2.276 mL
Porosity is calculated by dividing the volume of voids (pores) by the total volume. In this case, the volume of voids is the difference between the volume of water added and the volume left on top of the saturated soil (400 mL - 150 mL = 250 mL). The total volume is the sum of the dry soil volume and the water added (500 mL + 400 mL = 900 mL). Therefore, the porosity of the soil is 250 mL / 900 mL, which is approximately 0.28 or 28%.
250 mL = about 8.5 US fluid ounces.