CHEMISTRY

CHEMISTRY — KNOWT NOTES
PHYSICAL QUANTITIES, MEASUREMENT, ERRORS & PERIODIC TABLE

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PHYSICAL QUANTITIES & MEASUREMENT
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7 SI BASE QUANTITIES

Length → meter → m
Length formula → DVT

Mass → kilogram → kg
Mass formula → MDV

Time → second → s
Time formula → DVT

Temperature → kelvin → K
Temperature formula → K = °C + 273.15

Amount of substance → mole → mol
Mole formula → n = m/M

Electric current → ampere → A
Current formula → I = Q/t

Luminous intensity → candela → cd
No basic formula needed.

DVT:
D = distance
V = velocity
T = time

MDV:
M = mass
D = density
V = volume

n = moles
m = mass
M = molar mass

I = current
Q = charge
t = time

COMMON CONVERSIONS

1 kg = 1000 g

1 g = 1000 mg

1 L = 1000 mL

1 mL = 1 cm³

1 m = 100 cm

1 km = 1000 m

°C → K = add 273.15

K → °C = subtract 273.15

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SIGNIFICANT FIGURES
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Significant figures = meaningful digits in a measurement.

Nonzero digits are always significant.

Zeros between nonzero digits are significant.

Leading zeros are NOT significant.

Trailing zeros after a decimal are significant.

Trailing zeros in whole numbers without a decimal are ambiguous.

456 = 3 significant figures.

405 = 3 significant figures.

0.0045 = 2 significant figures.

0.03040 = 4 significant figures.

2.500 = 4 significant figures.

500 = generally 1 significant figure.

500.0 = 4 significant figures.

Memory:
Before first nonzero → NOT significant.

Between nonzero numbers → significant.

After decimal → significant.

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ACCURACY & PRECISION
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Accuracy = closeness to the TRUE or ACCEPTED VALUE.

Precision = closeness of measurements TO ONE ANOTHER.

Memory:
ACCURACY → TRUE

PRECISION → TOGETHER

High accuracy + high precision = close to true value AND close together.

High accuracy + low precision = close to true value but spread out.

Low accuracy + high precision = far from true value but close together.

Low accuracy + low precision = far from true value and spread out.

Important:
A measurement can be precise but inaccurate.

Exam clue:
Values close to EACH OTHER → precision.

Values close to the TRUE VALUE → accuracy.

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DENSITY
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Density = mass per unit volume.

Density is an intensive physical property.

Density does NOT depend on sample size.

Density triangle:
M on top
D and V on bottom

D = M/V

M = D×V

V = M/D

Asked for density → M ÷ V.

Asked for mass → D × V.

Asked for volume → M ÷ D.

Common density units:
g/cm³

g/mL

Important:
1 mL = 1 cm³.

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DENSITY & TEMPERATURE
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General rule:

Temperature increases → volume increases.

Volume increases → density decreases.

Temperature increases → density generally decreases.

Temperature decreases → density generally increases.

Memory:
HOTTER → BIGGER VOLUME → LOWER DENSITY

Water is an exception from 0°C to 4°C.

From 0°C to 4°C → water density increases as temperature increases.

Ice is less dense than liquid water.

Ice floats because it is less dense than liquid water.

Freezing water → open hydrogen-bond structure → volume increases → density decreases.

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PERCENT ERROR
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Accepted value = true/correct value from a reliable reference.

Experimental value = value measured during an experiment.

Error = difference between experimental and accepted values.

Error = Experimental − Accepted

Percent Error = |Experimental − Accepted| ÷ Accepted × 100

Memory:
SUBTRACT → ABSOLUTE → DIVIDE → ×100

Percent-error steps:

  1. Experimental − Accepted.

  2. Take absolute value.

  3. Divide by Accepted.

  4. Multiply by 100%.

Experimental value = accepted value → 0% error.

Higher accuracy → lower percent error.

Lower accuracy → higher percent error.

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TYPES OF ERROR
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Systematic error = consistent/repetitive error.

Systematic error has the same general magnitude and direction under the same conditions.

Memory:
SYSTEMATIC → SAME

Systematic error is also called cumulative error.

Systematic error mainly affects accuracy.

Examples of systematic error:
Incorrect calibration.

Balance always reads 0.50 g too high.

Thermometer always reads 2°C too low.

Random error = unpredictable variation between measurements.

Memory:
RANDOM → CHANGES

Random error is different from one measurement to another.

Random error mainly affects precision.

Examples of random error:
Different viewing angles.

Changing wind conditions.

Slight posture differences.

Air currents affecting a balance.

Random error can be reduced by repeating measurements.

Averaging repeated measurements helps reduce random error.

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SOURCES OF ERROR
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Natural error = caused by environmental conditions.

Memory:
NATURAL → ENVIRONMENT

Examples:
Wind.

Air temperature.

Atmospheric pressure.

Humidity.

Gravity.

Earth curvature.

Atmospheric refraction.

Instrument error = caused by imperfect, incorrectly adjusted, or poorly calibrated equipment.

Memory:
INSTRUMENT → EQUIPMENT

Examples:
Poor calibration.

Imperfect equipment.

Incorrect adjustment.

Human error = caused by physical limitations or inconsistent human actions.

Memory:
HUMAN → OBSERVER

Examples:
Misreading a scale.

Misalignment.

Improper setup.

Incorrect observation.

DO NOT CONFUSE:

Types of errors:
Systematic + Random

Sources of errors:
Natural + Instrument + Human

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HISTORY OF THE PERIODIC TABLE
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1808 → DALTON

Dalton assigned atomic weights to early elements.

Dalton → atomic weights.

1817 → DÖBEREINER

Dobereiner grouped elements with similar properties into groups of THREE.

Three elements → TRIADS.

Dobereiner → TRIADS.

1864 → NEWLANDS

Newlands noticed repeating properties every EIGHTH element.

Eight → OCTAVES.

Newlands → OCTAVES.

1869 → MENDELEEV

Mendeleev arranged elements using relative atomic mass and chemical/physical properties.

Mendeleev left GAPS for undiscovered elements.

Mendeleev predicted properties of undiscovered elements.

Mendeleev → Father of the Periodic Table.

1913 → MOSELEY

Moseley arranged elements by ATOMIC NUMBER.

Moseley → atomic number.

MEMORY:
Dalton → WEIGHTS

Dobereiner → THREE

Newlands → EIGHT

Mendeleev → GAPS

Moseley → NUMBER

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PERIODIC TABLE ORGANIZATION
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Atomic number = number of PROTONS.

Neutral atom:
Protons = electrons.

Atomic mass = average mass of naturally occurring isotopes.

Isotope = atoms of the same element with the SAME number of protons but DIFFERENT numbers of neutrons.

Memory:
ISOTOPE → SAME PROTONS, DIFFERENT NEUTRONS

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PERIODS
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Periods = HORIZONTAL ROWS.

Periodic table has 7 periods.

Atomic number increases LEFT → RIGHT across a period.

Elements in the same period have the same number of electron shells.

Memory:
PERIOD → ACROSS

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GROUPS / FAMILIES
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Groups = VERTICAL COLUMNS.

Periodic table has 18 groups.

Groups are also called families.

Elements in the same group generally have similar chemical properties.

Similar properties are related to similar electron configurations/valence-electron patterns.

Memory:
GROUP → DOWN

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METALS, NONMETALS & METALLOIDS
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Metals → LEFT + CENTER.

Nonmetals → UPPER-RIGHT.

Metalloids → STAIR-STEP LINE.

Metalloids have properties of both metals and nonmetals.

Nonmetals are generally dull.

Nonmetals are generally brittle when solid.

Nonmetals are generally poor conductors.

Nonmetals tend to GAIN electrons.

Memory:
LEFT/CENTER → METALS

STAIR-STEP → METALLOIDS

UPPER-RIGHT → NONMETALS

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PERIODIC TRENDS — MASTER MAP
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UPPER-RIGHT

Electronegativity ↑

Ionization energy ↑

Electron affinity ↑

Nonmetal reactivity ↑

BOTTOM-LEFT

Atomic radius ↑

Metal reactivity ↑

MASTER MEMORY:

UPPER-RIGHT → PULLS/WANTS ELECTRONS.

BOTTOM-LEFT → BIGGER ATOMS + MORE REACTIVE METALS.

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ELECTRONEGATIVITY
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Electronegativity = ability of an atom to ATTRACT electrons in a chemical bond.

Electronegativity increases toward the UPPER-RIGHT.

Highest electronegativity = FLUORINE (F).

Memory:
EN → ATTRACT

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IONIZATION ENERGY
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Ionization energy = energy required to REMOVE an electron from a neutral gaseous atom.

Ionization energy increases toward the UPPER-RIGHT.

High ionization energy = harder to remove an electron.

Memory:
IE → REMOVE

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ELECTRON AFFINITY
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Electron affinity = tendency of a neutral atom to GAIN an electron.

Electron affinity generally increases toward the UPPER-RIGHT.

Electron gain generally releases energy.

Important exception:
CHLORINE (Cl) has the highest electron affinity, NOT fluorine.

Memory:
EA → GAIN

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ATOMIC RADIUS
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Atomic radius = size/distance from nucleus to outermost electron shell.

Atomic radius increases toward the BOTTOM-LEFT.

Largest atomic radius = CESIUM (Cs).

Memory:
RADIUS → SIZE

BOTTOM-LEFT → BIGGEST

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REACTIVITY
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Reactivity = ability to undergo a chemical reaction.

Metal reactivity increases toward the BOTTOM-LEFT.

Nonmetal reactivity increases toward the UPPER-RIGHT.

Memory:
METALS → BOTTOM-LEFT

NONMETALS → UPPER-RIGHT

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PERIODIC TREND EXAM SHORTCUT
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Highest electronegativity → UPPER-RIGHT.

Highest ionization energy → UPPER-RIGHT.

Highest electron affinity → generally UPPER-RIGHT.

Electron affinity exception → CHLORINE.

Largest atomic radius → BOTTOM-LEFT.

Most reactive metal → BOTTOM-LEFT.

Most reactive nonmetal → UPPER-RIGHT.

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FASTEST FINAL MEMORY SHEET
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BIG NUMBER → LEFT → +

SMALL NUMBER → RIGHT → −

ACCURACY → TRUE

PRECISION → TOGETHER

DENSITY → M/V

MASS → D×V

VOLUME → M/D

KELVIN → °C + 273.15

CELSIUS → K − 273.15

% ERROR → |E−A|/A ×100

SYSTEMATIC → SAME

RANDOM → CHANGES

NATURAL → ENVIRONMENT

INSTRUMENT → EQUIPMENT

HUMAN → OBSERVER

PERIOD → HORIZONTAL

GROUP → VERTICAL

ATOMIC NUMBER → PROTONS

ISOTOPE → SAME PROTONS, DIFFERENT NEUTRONS

METALS → LEFT/CENTER

METALLOIDS → STAIR-STEP

NONMETALS → UPPER-RIGHT

EN → ATTRACT

IE → REMOVE

EA → GAIN

RADIUS → SIZE

UPPER-RIGHT → EN, IE, EA, NONMETAL REACTIVITY

BOTTOM-LEFT → RADIUS, METAL REACTIVITY

EXCEPTIONS:
Water 0–4°C → density increases as temperature increases.

Ice → less dense than liquid water.

Chlorine → highest electron affinity.