DENSITY
1. Mass and Volume
Mass is the amount of matter in a material; all matter has mass.
Mass is measured in kilograms (kg) or grams (g).
The SI unit for mass is the kilogram (kg).
Apparatus commonly used to measure mass: triple beam balance, mass meter, electronic scale.
2. Volume
Volume can be measured with: measuring cylinder, graduated beaker, measuring flask, burette.
For solids, volume units include: m³, cm³, mm³.
For liquids, volume units include: mL and L.
Volume formula for a rectangular solid: V = l \times w \times h.
The volume of an irregular object can be found by water displacement (see Section 1.4).
1 mL = 1 cm³ = (1 cm × 1 cm × 1 cm).
1 L = 1000 cm³ = (10 cm × 10 cm × 10 cm).
3. Density
Density of a material is the amount of mass in a given volume of that material.
Formula: \text{density} = \frac{\text{mass}}{\text{volume}} = \frac{m}{V}
Common density units include: \text{g mL}^{-1} \text{ (or g·mL}^{-1}), \text{g cm}^{-3}, \text{kg L}^{-1}, etc.
The unit for density depends on the mass and volume units used.
Density units table (variables):
m: mass
V: volume
d: density
Density symbol: d
Units examples: \text{g mL}^{-1},\; \text{g cm}^{-3},\; \text{kg L}^{-1}
Important note on units: for density calculations, mass and volume units must be compatible. If mass is in g, volume should be in mL or cm³; if mass is in kg, volume should be in L.
Key relationships:
d = \frac{m}{V}
V = \frac{m}{d}
m = d \times V
4. Factors that affect density
The density of a material depends on:
The nature of the particles and the strength of the forces between particles.
The size and type of the particles.
The size of the spaces (voids) between particles.
Therefore, different materials with different internal structures will have different densities.
5. Density Calculations (worked examples)
Example 1: If a 10 g object occupies 2.5 cm³, what is its density?
d = \frac{m}{V} = \frac{10\,\text{g}}{2.5\,\text{cm}^3} = 4\,\text{g cm}^{-3}
Example 2: What is the mass of methanol that fills exactly a 200 mL container if the density is 0.789\ \text{g mL}^{-1}?
m = d \times V = 0.789 \times 200 = 157.8\ \text{g}
Example 3: Copper block density
Mass m = 1896\ \text{g}.
Dimensions: l = 8.4\ \text{cm},\; w = 5.5\ \text{cm},\; h = 4.6\ \text{cm}
Volume: V = l \times w \times h = 8.4 \times 5.5 \times 4.6 = 212.52\ \text{cm}^3
Density: d = \frac{m}{V} = \frac{1896}{212.52} \approx 8.92\ \text{g cm}^{-3}
6. Measuring density of irregular objects (water displacement method)
Principle: When an object is submerged in water, it displaces an amount of water equal to its volume.
This method is especially useful for irregularly shaped objects (e.g., rocks).
Procedure (illustrative):
Fill a graduated cylinder with water (record initial volume).
Submerge the irregular object fully.
Record the new water level (final volume).
Volume of object = final volume − initial volume.
Example 4: Rock volume by displacement
Initial water: 50 mL; final water after submersion: 62 mL.
Volume of rock = 62 − 50 = 12 mL = 12 cm³.
Example 5: Rock density with mass and volume
Volume = 47 mL; Mass = 78 g.
Density: d = \frac{m}{V} = \frac{78}{47} \approx 1.66\ \text{g mL}^{-1}
7. Practice problems and worksheets (summary of problem types and solutions)
Worksheet 1 (types of problems): density calculations using d = m/V and V = m/d with various data; checks on understanding that larger density implies more mass for the same volume.
Example 1 (from Worksheet 1):
Given mass 500 g and final volume 555 mL, density d = \frac{m}{V} = \frac{500}{555} \approx 0.90\ \text{g mL}^{-1}
Example 2 (Chalk):
Mass 50 g, density 2.6 g/mL, volume V = \frac{m}{d} = \frac{50}{2.6} \approx 19.23\ \text{mL}
Example 3 (Coal vs Cork):
Given a volume of 100 mL, densities: coal d{coal} = 0.25\ \text{g mL}^{-1} and cork d{cork} = 1.50\ \text{g mL}^{-1}
Masses: m{coal} = d{coal} \times V = 0.25 \times 100 = 25\ \text{g}
m{cork} = d{cork} \times V = 1.50 \times 100 = 150\ \text{g}
Conclusion: For identical volumes, the denser material has a larger mass (coal vs cork in this example).
Worksheet 2 (additional problems): varied values for density calculations, including
Example: d = \frac{m}{V},\; m = 12.9\ \text{g},\; V = 8\ \text{cm}^{3} \Rightarrow d = \frac{12.9}{8} = 1.61\ \text{g cm}^{-3}
Example: d = \frac{m}{V},\; m = 43.5\ \text{g},\; V = 50\ \text{mL} \Rightarrow d = \frac{43.5}{50} = 0.87\ \text{g mL}^{-1}
Worksheet 3/Examples (more practice problems):
Example: m = d \times V,\; V = 15\ \text{mL},\; d = 2.5\ \text{g mL}^{-1} \Rightarrow m = 2.5 \times 15 = 37.5\ \text{g}
Example: V = \frac{m}{d},\; m = 65\ \text{g},\; d = 5.45\ \text{g mL}^{-1} \Rightarrow V = \frac{65}{5.45} \approx 11.93\ \text{mL}
Example: d = \frac{m}{V},\; m = 176\ \text{g},\; V = 4\ \text{cm}^3 \Rightarrow d = \frac{176}{4} = 44\ \text{g cm}^{-3} (note: ensure units are consistent; this example demonstrates formula usage)
Worksheet 4 (more large-volume/mass figures):
Example: d = \frac{m}{V},\; m = 2700\ \text{g},\; V = 10\times 15 \times 35\ \text{cm}^3 = 5250\ \text{cm}^3 \Rightarrow d \approx \frac{2700}{5250} \approx 0.51\ \text{g cm}^{-3}
Example: d = \frac{m}{V},\; m = 78\ \text{g},\; V = 60\ \text{mL} \Rightarrow d = \frac{78}{60} = 1.30\ \text{g mL}^{-1}
Example: d = \frac{m}{V},\; m = 1300\ \text{g},\; V = 743\ \text{cm}^3 \Rightarrow d \approx \frac{1300}{743} \approx 1.75\ \text{g cm}^{-3}
8. Practical tips and key reminders
Always ensure mass and volume units are compatible before calculating density.
If mass is in g, use volume in mL or cm³.
If mass is in kg, use volume in L.
Remember the difference between solids and liquids in how volume is reported and measured.
For irregular objects, water displacement gives a direct measurement of volume, which is often easier than calculating by geometry.
Use the formulae consistently:
d = \frac{m}{V}
V = \frac{m}{d}
m = d \times V
Density is a material property that helps identify substances and compare materials under the same conditions.
Real-world relevance: density is used in material science, quality control, buoyancy, and identification of substances. It can indicate composition and purity when measured under standard conditions.