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Planet Earth

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Planet Earth

Examples of resources in the Earth: coal, natural gas, metals, NaCl and limestone…

Matters are something that has mass.

Matter Pure substances Elements Can’t be broken into anything simpler by

chemical methods.

Compound Composed of 2+ elements joined

chemically together.

Mixtures – 2+ pure substances which haven’t joint chemically

Some examples of compounds and their uses:

Ammonia ( NH 3 ) – glass cleanser, fertilizer

Calcium carbonate ( CaCO3 ) – calcium supplement tablets

Sodium hydroxide ( NaOH ) : drain cleanser

Mixture Compound

Mixed together in any proportion. In a fixed ratio.

No chemical change when it’s formed Energy is usually released when forming the

compound (chemical change occurred)

Similar properties with the original Can have very different chemical properties then

substances that made up the mixture the elements that it contains

Don’t have a sharp BP/MP (it varies) Have a definite/sharp/unique MP/BP

Can be separated by physical method Have to be separated through chemical method.

(e.g. electrolysis)

Method of separation

1) Decantation

Let the residue sinks in the bottom of the beak and pour the decant away through the glass rod.

It’s suitable for separating insoluble liquid from a liquid.

2) Filtration

Pour the mixture into a filter funnel with filter paper through the glass rod. Residue is in the

beaker underneath and the filtrate left in the filter paper. It’s suitable for separating insoluble

liquid from a liquid. (e.g. separate sand from sea water)

3) Evaporation.

Heat the mixture in a evaporating dish by Bunsen flame. When solution is evaporated, solid

remains. It’s used to separate dissolved solid from a solution. (e.g. NaCl from Sea Water)

4) Crystallization

Method I: Heat the mixture, some solvent boils away, but hot solution can hold more solute.

Cool it down and the solution can’t hold such solute, crystal formed.

Method II: Pour the mixture in a beaker with cover, let the solvent evaporate under room

temperature, it will over-saturated and from crystals.

It’s used to separate dissolved solid from a solution. (e.g. CuSO4 from Water)

5) Distillation (evaporation + crystallization)

Evaporate the solution in a distillation flask, a tube with condenser receives the solution vapour

and turn it into liquid, and collected by the conical flask. It’s suitable to separate dissolved solid

from a solution.

6) Fractional distillation

Remove impurities such as dust, water vapour and CO2 ; compress the air in a high pressure

(by the Ideal Gas Law it’ll get hotter), then it’s cooled in a cool chamber (by water), it’s

expanded (by IGL it’s cooler). Repeated this step until the air is liquefied. Pump the air into the

fractioning column, the temperature is slowly increased. The B.P. of N 2 , Ar and O2 are

196C , 186C and 183C respectively, therefore N 2 is collected in the bottom of the

tower, followed Ar and O 2 .

It’s suitable to separate two miscible liquids.

7) Sublimation

Put the mixture in a beaker covered by a evaporating dish. Heat the beaker until it sublimes.

Those sublimed gas will become solid again in the bottom of the dish.

It’s suitable to separate mixture of two solids which one of them can sublime.

Physical properties are something that can be measured without changing the chemical

composition of the substance.

No new substances are formed during physical change.

Chemical properties describe the ability of a substance to form new substances.

One or more new substances is formed in chemical change. In another way, energy is

absorbed or released.

Test for O 2 : (glowing splint test) Oxygen relights glowing splint.

Test for H 2 : (burning splint test) Hydrogen gives a “pop” sound when burning.

Test for H 2 O : Water turns dry cobalt(II) chloride paper from blue to pink.

Test for some metals (flame test): If it’s not clean, dip it into conc.

HCl solution, heat it until

no characteristic flame is shown. Dip the clean Pt wire into (fresh) conc. HCl solution (or

dip it into conc. HCl solution, heat it until no characteristic flame is shown.), then dip it into

the solid sample power and heat it.

1) Na  gives golden yellow flame.

2

2) Ca gives brick-red flame.

3) K  gives lilac flame.

2

4) Cu gives bluish green flame.

Test for chloride: add (dilute) nitric acid followed by silver nitrate solution, Cl  gives white

ppt (participate).

Four layers of Earth’s atmosphere: troposphere, stratosphere, mesosphere and ionosphere.

Composition of atmosphere – 78% of N 2 , 21% of O 2 , 0.9% of noble gases, 0.03% of

CO2 , variant amount of H 2 O and some other gases.

Sea covers over 70% surface area of the Earth. It dissolved different salts. Most salts are

brought by rivers. Composition of sea salt (3.5% of the sea water): about 68% of NaCl ,

15% of MgCl 2 , 11% of Na 2 SO4 , 3% of CaCl 2 and some other salt.

A solution forms when a substance (solute) dissolves in another (solvent). Dilute solution

contains a very small amount of solute in given amount of solution. When solute increase, it

becomes concentrated, and finally saturated. Saturated solution means it can’t dissolve

anymore solute in a given temperature.

Electrolysis of water

electricity r

e l e c ty i c i t

2 H 2 O  2 H 2  O2  H 2 ( g )  Cl 2 ( g )  N a O Hl )

s e aw a t e r (

Manufacture of ammonia ( NH 3 )

Hydrogen As rocket fuel ( 2 H 2  O2  H 2 O )



Manufacture of hydrochloric acid ( HCl )



Sterilizing drinking water

Chloride Sterilizing swimming pool water

Manufacture of PVC (polyvinyl chloride) and organic solvents



Manufacture of bleach

Sodium Hydroxide

Manufacture of soaps and detergents

Particle theory of matter – all substances are made up by very small particles.

Limestone – calcium carbonate ( CaCO3 )

1) Heat and limewater(calcium hydroxide)

Heating calcium carbonate gives calcium oxide (quick lime) and carbon dioxide:



CaCO3  CaO(s)  CO2 ( g )







Adding water to calcium oxide gives lime water (slaked lime in solution):

CaO  H 2 O  Ca(OH ) 2 (aq)

Test for CO2 : turns lime water from colourless to milky:

Ca (OH ) 2  CO2  CaCO3  H 2 O

Excess carbon dioxide makes it becomes colourless again:

Ca (OH ) 2  2CO2  CaCO3  H 2 O  CO2  Ca ( HCO 3 ) 2

2) Acid

Adding (dilute) hydrochloric acid gives calcium chloride, water and carbon dioxide:

CaCO3  2 HCl  CaCl 2  H 2 O  CO2

CaCl2 is soluble in water so that CaCO3 is soluble in hydrochloric acid.

CaCO3 is insoluble in water.

Use of limestone

1) Crushed limestone (CaCO3) – extraction of iron; construction material for road and

buildings.

2) Powered limestone (CaCO3, grinded) – neutralize acidity of soil and sulphur dioxide in

flue gas of power stations; making glass.

3) Quicklime (CaO) – making steel with Fe, neutralize acidity in soil; drying agent in industry.

4) Slaked lime (Ca(OH)2) – neutralize acidity in soil and lake affected by acid rain.

5) Cement (limestone heating with shale) – ingredients of concrete.

Formation of limestone cave

Solid rock broke down and changed into other materials by weathering, its surface is wearied

away while the movement of products of weathering that changed their location is called

erosion. Rainfalls becomes carbonic acid with carbon dioxide in air (H2O+CO2→H2CO3)

(Note that the reaction can occur the inverse direction here) while carbonic acid dissolves the

underground limestone deposits to form calcium hydrogencarbonate:

CaCO3+H2CO3→Ca(HCO3)2

(Ca(HCO3)2 is the main cause of hard water.)

The underground limestone is dissolved in this way over millions of years to form underground

holes called limestone caves.

Formation of limestone

CaCO3 exists naturally in 3 forms: chalk, limestone and marble, depends on their hardness.

When sea animals die, their skeletons and shells (mainly contains CaCO 3) sink into the mud at

the bottom of the oceans. After many years layers built up and pressure from top layers

changes the bottom layers to chalk. Earth movements such as earthquake may lift the layer to

Earth’s surface. They changes to limestone and marble under. higher pressure and heat



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