group ii alkaline earths ©hopton contents general properties trends in electronic configuration...

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GROUP II GROUP II Alkaline earths Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point Trends in ionisation energy Reaction with oxygen and water Oxides and hydroxides Carbonates Sulphates

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Page 1: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP IIGROUP IIAlkaline earthsAlkaline earths

©HOPTON

CONTENTS• General properties

• Trends in electronic configuration

• Trends in atomic and ionic radius

• Trends in melting point

• Trends in ionisation energy

• Reaction with oxygen and water

• Oxides and hydroxides

• Carbonates

• Sulphates

Page 2: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP PROPERTIESGROUP PROPERTIES

GENERAL • metals

• all have the electronic configuration ... ns2

TRENDS • melting point

• electronic configuration

• electronegativity

• atomic size

• ionic size

©HOPTON

Page 3: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

THE s-BLOCK ELEMENTSTHE s-BLOCK ELEMENTS

Elements in Group I (alkali metals) and Group II (alkaline earths) are known ass-block elements because their valence (bonding) electrons are in s orbitals.

©HOPTON

Page 4: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

THE s-BLOCK ELEMENTSTHE s-BLOCK ELEMENTS

Elements in Group I (alkali metals) and Group II (alkaline earths) are known ass-block elements because their valence (bonding) electrons are in s orbitals.

Gp I

Li

Na

K

Rb

Cs

Fr

ALKALI METALS

1s2 2s1

… 5s1

… 6s1

1s2 2s2 2p6 3s1

1s2 2s2 2p6 3s23p64s1

©HOPTON

Page 5: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

THE s-BLOCK ELEMENTSTHE s-BLOCK ELEMENTS

Elements in Group I (alkali metals) and Group II (alkaline earths) are known ass-block elements because their valence (bonding) electrons are in s orbitals.

Be

Gp I

Mg

Ca

Sr

Ba

Rn

Li

Na

K

Rb

Cs

Fr

Gp II

ALKALINE EARTHSALKALI METALS

1s2 2s2

… 5s2

… 6s2

1s2 2s2 2p6 3s2

1s2 2s2 2p6 3s23p64s2

1s2 2s1

… 5s1

… 6s1

1s2 2s2 2p6 3s1

1s2 2s2 2p6 3s23p64s1

©HOPTON

Page 6: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

THE s-BLOCK ELEMENTSTHE s-BLOCK ELEMENTS

Elements in Group I (alkali metals) and Group II (alkaline earths) are known ass-block elements because their valence (bonding) electrons are in s orbitals.

Be

Gp I

Mg

Ca

Sr

Ba

Rn

Li

Na

K

Rb

Cs

Fr

Gp II

ALKALINE EARTHSALKALI METALS

1s2 2s2

Francium and radium are both short-lived radioactive elementsFrancium and radium are both

short-lived radioactive elements

… 5s2

… 6s2

1s2 2s2 2p6 3s2

1s2 2s2 2p6 3s23p64s2

1s2 2s1

… 5s1

… 6s1

1s2 2s2 2p6 3s1

1s2 2s2 2p6 3s23p64s1

©HOPTON

Page 7: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

Be

1s2 2s2

Mg

…3s2

Ca

… 4s2

Sr

… 5s2

2,2 2,8,2 2,8,8,2 2,8,18,8,2

New e/c

Old e/c

ELECTRONIC CONFIGURATIONELECTRONIC CONFIGURATION

4 12 20 38Atomic Number

Ba

… 6s2

2,8,18,18,8,2

56

©HOPTON

Page 8: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

As the nuclear charge increases, the electrons go into shells further from the nucleus.

Be

1s2 2s2

Mg

…3s2

Ca

… 4s2

Sr

… 5s2

2,2 2,8,2 2,8,8,2 2,8,18,8,2

New e/c

Old e/c

ELECTRONIC CONFIGURATIONELECTRONIC CONFIGURATION

4 12 20 38Atomic Number

Ba

… 6s2

2,8,18,18,8,2

56

©HOPTON

Page 9: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

As the nuclear charge increases, the electrons go into shells further from the nucleus.

The extra distance of the outer shell from the nucleus affects…

Atomic radius Ionic radius Ionisation energy Melting point Chemical reactivity

Be

1s2 2s2

Mg

…3s2

Ca

… 4s2

Sr

… 5s2

2,2 2,8,2 2,8,8,2 2,8,18,8,2

New e/c

Old e/c

ELECTRONIC CONFIGURATIONELECTRONIC CONFIGURATION

4 12 20 38Atomic Number

Ba

… 6s2

2,8,18,18,8,2

56

©HOPTON

Page 10: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

ATOMIC & IONIC RADIUSATOMIC & IONIC RADIUS

Be Mg Ca Sr

0.106 0.140 0.174 0.191Atomic radius / nm

Ba

0.198

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config. 2,8,18,18,8,2

©HOPTON

Page 11: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

ATOMIC RADIUS INCREASES down Group

• the greater the atomic number the more electrons there are; these go into shells increasingly further from the nucleus

ATOMIC & IONIC RADIUSATOMIC & IONIC RADIUS

Be Mg Ca Sr

0.106 0.140 0.174 0.191Atomic radius / nm

Ba

0.198

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config. 2,8,18,18,8,2

1s2 2s2 2p6 3s2 1s2 2s2 2p6 3s23p64s2

©HOPTON

Page 12: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

ATOMIC RADIUS INCREASES down Group

• the greater the atomic number the more electrons there are; these go into shells increasingly further from the nucleus

ATOMIC & IONIC RADIUSATOMIC & IONIC RADIUS

Be Mg Ca Sr

0.106 0.140 0.174 0.191Atomic radius / nm

Ba

0.198

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config. 2,8,18,18,8,2

• atoms of Group II are smaller than the equivalent Group I atom

the extra proton exerts a greater attraction on the electrons

1s2 2s2 2p6 3s2 1s2 2s2 2p6 3s23p64s2

12 protons1s2 2s2 2p6 3s2

11 protons1s2 2s2 2p6 3s1

©HOPTON

Page 13: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

ATOMIC & IONIC RADIUSATOMIC & IONIC RADIUS

Be Mg Ca Sr

0.106 0.140 0.174 0.191Atomic radius / nm

Ba

0.198

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config. 2,8,18,18,8,2

Be2+ Mg2+ Ca2+ Sr2+

0.030 0.064 0.094 0.110Ionic radius / nm

Ba2+

0.134

2 2,8 2,8,8 2,8,18,8Electronic config. 2,8,18,18,8

©HOPTON

Page 14: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

ATOMIC & IONIC RADIUSATOMIC & IONIC RADIUS

Be Mg Ca Sr

0.106 0.140 0.174 0.191Atomic radius / nm

Ba

0.198

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config. 2,8,18,18,8,2

Be2+ Mg2+ Ca2+ Sr2+

0.030 0.064 0.094 0.110Ionic radius / nm

Ba2+

0.134

2 2,8 2,8,8 2,8,18,8Electronic config. 2,8,18,18,8

IONIC RADIUS INCREASES down Group

• ions are smaller than atoms – on removing the outer shell electrons, the remaining electrons are now in fewer shells

©HOPTON

Page 15: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

ATOMIC & IONIC RADIUSATOMIC & IONIC RADIUS

Be Mg Ca Sr

0.106 0.140 0.174 0.191Atomic radius / nm

Ba

0.198

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config. 2,8,18,18,8,2

Be2+ Mg2+ Ca2+ Sr2+

0.030 0.064 0.094 0.110Ionic radius / nm

Ba2+

0.134

2 2,8 2,8,8 2,8,18,8Electronic config. 2,8,18,18,8

IONIC RADIUS INCREASES down Group

• ions are smaller than atoms – on removing the outer shell electrons, the remaining electrons are now in fewer shells

1s2 2s2 2p6 3s2 1s2 2s2 2p6

©HOPTON

Page 16: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

ATOMIC & IONIC RADIUSATOMIC & IONIC RADIUS

Be Mg Ca Sr

0.106 0.140 0.174 0.191Atomic radius / nm

Ba

0.198

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config. 2,8,18,18,8,2

Be2+ Mg2+ Ca2+ Sr2+

0.030 0.064 0.094 0.110Ionic radius / nm

Ba2+

0.134

2 2,8 2,8,8 2,8,18,8Electronic config. 2,8,18,18,8

IONIC RADIUS INCREASES down Group

• ions are smaller than atoms – on removing the outer shell electrons, the remaining electrons are now in fewer shells

1s2 2s2 2p6 3s2 1s2 2s2 2p6 3s23p64s21s2 2s2 2p6 1s2 2s2 2p6 3s23p6

©HOPTON

Page 17: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

MELTING POINTMELTING POINT

Be Mg Ca Sr

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config.

1283 650 850 770Melting point / ºC

Ba

2,8,18,18,8,2

710

©HOPTON

Page 18: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

DECREASES down Group

MELTING POINTMELTING POINT

Be Mg Ca Sr

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config.

1283 650 850 770Melting point / ºC

Ba

2,8,18,18,8,2

710

©HOPTON

Page 19: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

DECREASES down Group

• each atom contributes two electrons to the delocalised cloud

• metallic bonding gets weaker due to increased size of ion

MELTING POINTMELTING POINT

Be Mg Ca Sr

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config.

1283 650 850 770Melting point / ºC

Ba

2,8,18,18,8,2

710

Larger ions mean that the electron

cloud doesn’t bind them as strongly

©HOPTON

Page 20: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

DECREASES down Group

• each atom contributes two electrons to the delocalised cloud

• metallic bonding gets weaker due to increased size of ion

• Group I metals have lower melting points than the equivalent Group II metal because each metal only contributes one electron to the cloud

MELTING POINTMELTING POINT

Be Mg Ca Sr

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config.

1283 650 850 770Melting point / ºC

Ba

2,8,18,18,8,2

710

Larger ions mean that the electron

cloud doesn’t bind them as strongly

©HOPTON

Page 21: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

GROUP TRENDSGROUP TRENDS

DECREASES down Group

• each atom contributes two electrons to the delocalised cloud

• metallic bonding gets weaker due to increased size of ion

• Group I metals have lower melting points than the equivalent Group II metal because each metal only contributes one electron to the cloud

NOTE Magnesium doesn’t fit the trend because crystalline structure can also affect the melting point of a metal

MELTING POINTMELTING POINT

Be Mg Ca Sr

2,2 2,8,2 2,8,8,2 2,8,18,8,2Electronic config.

1283 650 850 770Melting point / ºC

Ba

2,8,18,18,8,2

710

Larger ions mean that the electron

cloud doesn’t bind them as strongly

©HOPTON

Page 22: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

FIRST IONISATION ENERGYFIRST IONISATION ENERGY

©HOPTON

Page 23: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

FIRST IONISATION ENERGYFIRST IONISATION ENERGY

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

©HOPTON

Page 24: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

FIRST IONISATION ENERGYFIRST IONISATION ENERGY

DECREASES down the GroupDespite the increasing nuclear charge the values decrease due to theextra shielding provided by additional filled inner energy levels

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

©HOPTON

Page 25: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

FIRST IONISATION ENERGYFIRST IONISATION ENERGY

DECREASES down the GroupDespite the increasing nuclear charge the values decrease due to theextra shielding provided by additional filled inner energy levels

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

BERYLLIUMThere are 4 protons pulling on the outer shell electrons

1st I.E. = 899 kJ mol-1

4+

©HOPTON

Page 26: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

FIRST IONISATION ENERGYFIRST IONISATION ENERGY

DECREASES down the GroupDespite the increasing nuclear charge the values decrease due to theextra shielding provided by additional filled inner energy levels

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

BERYLLIUMThere are 4 protons pulling on the outer shell electrons

1st I.E. = 899 kJ mol-1

12+4+

MAGNESIUMThere are now 12 protons pulling on the outer shell

electrons. However, the extra filled inner shell shields the nucleus from the outer shell

electrons. The effective nuclear charge is less and the electrons are easier to remove.

1st I.E. = 738 kJ mol-1

©HOPTON

Page 27: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

FIRST IONISATION ENERGYFIRST IONISATION ENERGY

DECREASES down the GroupDespite the increasing nuclear charge the values decrease due to theextra shielding provided by additional filled inner energy levels

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

BERYLLIUMThere are 4 protons pulling on the outer shell electrons

1st I.E. = 899 kJ mol-1

12+4+

MAGNESIUMThere are now 12 protons pulling on the outer shell

electrons. However, the extra filled inner shell shield the

nucleus from the outer shell electrons. The effective

nuclear charge is less and the electrons are easier to remove.

1st I.E. = 738 kJ mol-1

©HOPTON

©HOPTON

Page 28: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

SUCCESSIVE IONISATION ENERGIESSUCCESSIVE IONISATION ENERGIES

Successive Ionisation Energy values get larger

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

©HOPTON

Page 29: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

SUCCESSIVE IONISATION ENERGIESSUCCESSIVE IONISATION ENERGIES

Successive Ionisation Energy values get larger

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

12+

1st I.E. = 738 kJ mol-1

©HOPTON

Page 30: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

SUCCESSIVE IONISATION ENERGIESSUCCESSIVE IONISATION ENERGIES

Successive Ionisation Energy values get larger

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

12+

1st I.E. = 738 kJ mol-1

12+

2nd I.E. = 1500 kJ mol-1

There are now 12 protons and only 11 electrons. The

increased ratio of protons to electrons means that it is

harder to pull an electron out.

©HOPTON

Page 31: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

Successive Ionisation Energy values get larger

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

12+

1st I.E. = 738 kJ mol-1

12+ 12+

2nd I.E. = 1500 kJ mol-1

There are now 12 protons and only 11 electrons. The

increased ratio of protons to electrons means that it is

harder to pull an electron out.

3rd I.E. = 7733 kJ mol-1

There is a big jump in IE because the electron being removed is

from a shell nearer the nucleus; there is less shielding.

SUCCESSIVE IONISATION ENERGIESSUCCESSIVE IONISATION ENERGIES

©HOPTON

Page 32: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

Successive Ionisation Energy values get larger

Be Mg Ca Sr

899 738 590 550 1st I.E. / kJ mol-1

Ba

500

1800 1500 1100 1100 1000

14849 7733 4912 4120 3390

2nd I.E. / kJ mol-1

3rd I.E. / kJ mol-1

12+

1st I.E. = 738 kJ mol-1

12+ 12+

2nd I.E. = 1500 kJ mol-1

There are now 12 protons and only 11 electrons. The

increased ratio of protons to electrons means that it is

harder to pull an electron out.

3rd I.E. = 7733 kJ mol-1

There is a big jump in IE because the electron being removed is

from a shell nearer the nucleus; there is less shielding.

SUCCESSIVE IONISATION ENERGIESSUCCESSIVE IONISATION ENERGIES

©HOPTON

Page 33: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CHEMICAL PROPERTIES OF THE ELEMENTSCHEMICAL PROPERTIES OF THE ELEMENTS

Reactivity increases down the Group due to the ease of cation formation

©HOPTON

Page 34: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CHEMICAL PROPERTIES OF THE ELEMENTSCHEMICAL PROPERTIES OF THE ELEMENTS

Reactivity increases down the Group due to the ease of cation formation

OXYGEN react with increasing vigour down the group

Mg burns readily with a bright white flame

0 0 +2 -22Mg(s) + O2(g) —> 2MgO(s)

Ba burns readily with an apple-green flame

2Ba(s) + O2(g) —> 2BaO(s)

©HOPTON

Page 35: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CHEMICAL PROPERTIES OF THE ELEMENTSCHEMICAL PROPERTIES OF THE ELEMENTS

Reactivity increases down the Group due to the ease of cation formation

OXYGEN react with increasing vigour down the group

Mg burns readily with a bright white flame

0 0 +2 -22Mg(s) + O2(g) —> 2MgO(s)

Ba burns readily with an apple-green flame

2Ba(s) + O2(g) —> 2BaO(s)

In both cases…

the metal is oxidised Oxidation No. increases from 0 to +2

oxygen is reduced Oxidation No. decreases from 0 to -2

Mg —> Mg2+ + 2e¯

O + 2e¯ —> O2-

©HOPTON

Page 36: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CHEMICAL PROPERTIES OF THE ELEMENTSCHEMICAL PROPERTIES OF THE ELEMENTS

Reactivity increases down the Group due to the ease of cation formation

©HOPTON

Page 37: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CHEMICAL PROPERTIES OF THE ELEMENTSCHEMICAL PROPERTIES OF THE ELEMENTS

Reactivity increases down the Group due to the ease of cation formation

WATER react with increasing vigour down the group

©HOPTON

Page 38: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CHEMICAL PROPERTIES OF THE ELEMENTSCHEMICAL PROPERTIES OF THE ELEMENTS

Reactivity increases down the Group due to the ease of cation formation

WATER react with increasing vigour down the group

Mg reacts very slowly with cold water

Mg(s) + 2H2O(l) —> Mg(OH)2(aq) + H2(g)

but reacts quickly with steam

Mg(s) + H2O(g) —> MgO(s) + H2(g)

©HOPTON

Page 39: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CHEMICAL PROPERTIES OF THE ELEMENTSCHEMICAL PROPERTIES OF THE ELEMENTS

Reactivity increases down the Group due to the ease of cation formation

WATER react with increasing vigour down the group

Mg reacts very slowly with cold water

Mg(s) + 2H2O(l) —> Mg(OH)2(aq) + H2(g)

but reacts quickly with steam

Mg(s) + H2O(g) —> MgO(s) + H2(g)

Ba reacts vigorously with cold water

Ba(s) + 2H2O(l) —> Ba(OH)2(aq) + H2(g)

©HOPTON

Page 40: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

OXIDES OF GROUP IIOXIDES OF GROUP II

Bonding • ionic solids; EXCEPT BeO which has covalent character

• BeO (beryllium oxide) MgO (magnesium oxide) CaO (calcium oxide) SrO (strontium oxide) BaO (barium oxide)

©HOPTON

Page 41: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

OXIDES OF GROUP IIOXIDES OF GROUP II

Bonding • ionic solids; EXCEPT BeO which has covalent character

• BeO (beryllium oxide) MgO (magnesium oxide) CaO (calcium oxide) SrO (strontium oxide) BaO (barium oxide)

Reactionwith water Be Mg Ca Sr

NONE reacts reacts reactsReactivity with water

Ba

reacts

Insoluble Sparinglysoluble

Slightlysoluble

Quitesoluble

Verysoluble

- 9-10

Solubility of hydroxide g/100cm3 of water

pH of solution

©HOPTON

Page 42: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

OXIDES OF GROUP IIOXIDES OF GROUP II

Bonding • ionic solids; EXCEPT BeO which has covalent character

• BeO (beryllium oxide) MgO (magnesium oxide) CaO (calcium oxide) SrO (strontium oxide) BaO (barium oxide)

Reactionwith water

React with water to produce the hydroxide (not Be)

e.g. CaO(s) + H2O(l) —> Ca(OH)2(s)

Be Mg Ca Sr

NONE reacts reacts reactsReactivity with water

Ba

reacts

Insoluble Sparinglysoluble

Slightlysoluble

Quitesoluble

Verysoluble

- 9-10

Solubility of hydroxide g/100cm3 of water

pH of solution

©HOPTON

Page 43: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

HYDROXIDES OF GROUP IIHYDROXIDES OF GROUP II

Properties basic strength also increases down group

©HOPTON

Page 44: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

HYDROXIDES OF GROUP IIHYDROXIDES OF GROUP II

Properties basic strength also increases down group

• this is because the solubility increases• the metal ions get larger so charge density decreases• get a lower attraction between the OH¯ ions and larger 2+ ions• the ions will split away from each other more easily• there will be a greater concentration of OH¯ ions in water

©HOPTON

Page 45: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

HYDROXIDES OF GROUP IIHYDROXIDES OF GROUP II

Properties basic strength also increases down group

• this is because the solubility increases• the metal ions get larger so charge density decreases• get a lower attraction between the OH¯ ions and larger 2+ ions• the ions will split away from each other more easily• there will be a greater concentration of OH¯ ions in water

Be Mg Ca Sr

NONE reacts reacts reactsReactivity with water

Ba

reacts

Insoluble Sparinglysoluble

Slightlysoluble

Quitesoluble

Verysoluble

- 9-10

Solubility of hydroxide in water

pH of solution

©HOPTON

Page 46: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

HYDROXIDES OF GROUP IIHYDROXIDES OF GROUP II

Properties basic strength also increases down group

• this is because the solubility increases• the metal ions get larger so charge density decreases• get a lower attraction between the OH¯ ions and larger 2+ ions• the ions will split away from each other more easily• there will be a greater concentration of OH¯ ions in water

Be Mg Ca Sr

NONE reacts reacts reactsReactivity with water

Ba

reacts

Insoluble Sparinglysoluble

Slightlysoluble

Quitesoluble

Verysoluble

- 9-10

Solubility of hydroxide in water

pH of solution

Lower charge density of the larger Ca2+ ion means that it doesn’t hold onto the

OH¯ ions as strongly. More OH¯ get released into the water. It is more soluble

and the solution has a larger pH.

©HOPTON

Page 47: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

HYDROXIDES OF GROUP IIHYDROXIDES OF GROUP II

Uses

Ca(OH)2 used in agriculture to neutralise acid soils

Ca(OH)2(s) + 2H+ (aq) —> Ca2+(aq) + 2H2O(l)

Mg(OH)2 used in toothpaste and indigestion tablets as an antacid

Mg(OH)2(s) + 2H+ (aq) —> Mg2+(aq) + 2H2O(l)

Both the above are weak alkalis and not as caustic as sodium hydroxide

©HOPTON

Page 48: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CARBONATES OF GROUP IICARBONATES OF GROUP II

©HOPTON

Page 49: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CARBONATES OF GROUP IICARBONATES OF GROUP II

Properties

• insoluble in waterMgCO3 CaCO3 SrCO3 BaCO3

1.5 x 10-4 1.3 x 10-5 7.4 x 10-6 9.1 x 10-6Solubility g/100cm3 of water

©HOPTON

Page 50: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CARBONATES OF GROUP IICARBONATES OF GROUP II

Properties

• insoluble in water

• undergo thermal decomposition to oxide and carbon dioxide e.g. MgCO3(s) —> MgO(s) + CO2(g)

MgCO3 CaCO3 SrCO3 BaCO3

1.5 x 10-4 1.3 x 10-5 7.4 x 10-6 9.1 x 10-6

980

Solubility g/100cm3 of water

Decomposition temperature / ºC 400 1280 1360

©HOPTON

Page 51: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CARBONATES OF GROUP IICARBONATES OF GROUP II

Properties

• insoluble in water

• undergo thermal decomposition to oxide and carbon dioxide e.g. MgCO3(s) —> MgO(s) + CO2(g)

• the ease of decomposition decreases down the group

MgCO3 CaCO3 SrCO3 BaCO3

1.5 x 10-4 1.3 x 10-5 7.4 x 10-6 9.1 x 10-6

980

Solubility g/100cm3 of water

Decomposition temperature / ºC 400 1280 1360

©HOPTON

Page 52: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CARBONATES OF GROUP IICARBONATES OF GROUP II

Properties

• insoluble in water

• undergo thermal decomposition to oxide and carbon dioxide e.g. MgCO3(s) —> MgO(s) + CO2(g)

• the ease of decomposition decreases down the group

MgCO3 CaCO3 SrCO3 BaCO3

1.5 x 10-4 1.3 x 10-5 7.4 x 10-6 9.1 x 10-6

980

Solubility g/100cm3 of water

Decomposition temperature / ºC 400 1280 1360

EASIER HARDER

©HOPTON

Page 53: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CARBONATES OF GROUP IICARBONATES OF GROUP II

Properties

• insoluble in water

• undergo thermal decomposition to oxide and carbon dioxide e.g. MgCO3(s) —> MgO(s) + CO2(g)

• the ease of decomposition decreases down the group

MgCO3 CaCO3 SrCO3 BaCO3

1.5 x 10-4 1.3 x 10-5 7.4 x 10-6 9.1 x 10-6

980

Solubility g/100cm3 of water

Decomposition temperature / ºC 400 1280 1360

One might think that the greater charge density of the smaller Mg2+ would mean that it would hold onto the CO3

2- ion more and the ions would be more difficult to separate.

EASIER HARDER

©HOPTON

Page 54: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

CARBONATES OF GROUP IICARBONATES OF GROUP II

Properties

• insoluble in water

• undergo thermal decomposition to oxide and carbon dioxide e.g. MgCO3(s) —> MgO(s) + CO2(g)

• the ease of decomposition decreases down the group

MgCO3 CaCO3 SrCO3 BaCO3

1.5 x 10-4 1.3 x 10-5 7.4 x 10-6 9.1 x 10-6

980

Solubility g/100cm3 of water

Decomposition temperature / ºC 400 1280 1360

One might think that the greater charge density of the smaller Mg2+ would mean that it would hold onto the CO3

2- ion more and the ions would be more difficult to separate.

The driving force must be the formation of the oxide. The smaller ion with its greater charge density holds onto the O2- ion to make a more stable compound.

EASIER HARDER

©HOPTON

Page 55: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

MgSO4 CaSO4 SrSO4 BaSO4

3.6 x 10-1 1.1 x 10-3 6.2 x 10-5 9.0 x 10-7Solubility g/100cm3 of water

GROUP TRENDSGROUP TRENDS

SULPHATESSULPHATES

©HOPTON

Page 56: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

MgSO4 CaSO4 SrSO4 BaSO4

3.6 x 10-1 1.1 x 10-3 6.2 x 10-5 9.0 x 10-7Solubility g/100cm3 of water

GROUP TRENDSGROUP TRENDS

SULPHATESSULPHATES

SOLUBILITY DECREASES down the Group

• as the cation gets larger it has a lower charge density• it becomes less attracted to the polar water molecules

©HOPTON

Page 57: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

MgSO4 CaSO4 SrSO4 BaSO4

3.6 x 10-1 1.1 x 10-3 6.2 x 10-5 9.0 x 10-7Solubility g/100cm3 of water

GROUP TRENDSGROUP TRENDS

SULPHATESSULPHATES

SOLUBILITY DECREASES down the Group

• as the cation gets larger it has a lower charge density• it becomes less attracted to the polar water molecules

Greater charge density of Mg2+ ion means that it is more attracted to water

so the ionic lattice breaks up more easily

©HOPTON

Page 58: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

MgSO4 CaSO4 SrSO4 BaSO4

3.6 x 10-1 1.1 x 10-3 6.2 x 10-5 9.0 x 10-7Solubility g/100cm3 of water

GROUP TRENDSGROUP TRENDS

SULPHATESSULPHATES

SOLUBILITY DECREASES down the Group

• as the cation gets larger it has a lower charge density• it becomes less attracted to the polar water molecules

Greater charge density of Mg2+ ion means that it is more attracted to water

so the ionic lattice breaks up more easily

Lower charge density of larger Ca2+ means that it is less attracted to water so the ionic lattice breaks up less easily – IT IS LESS SOLUBLE

©HOPTON

Page 59: GROUP II Alkaline earths ©HOPTON CONTENTS General properties Trends in electronic configuration Trends in atomic and ionic radius Trends in melting point

MgSO4 CaSO4 SrSO4 BaSO4

3.6 x 10-1 1.1 x 10-3 6.2 x 10-5 9.0 x 10-7Solubility g/100cm3 of water

GROUP TRENDSGROUP TRENDS

SULPHATESSULPHATES

SOLUBILITY DECREASES down the Group

• as the cation gets larger it has a lower charge density• it becomes less attracted to the polar water molecules

USE barium sulphate’s insolubility is used as a test for sulphates

Greater charge density of Mg2+ ion means that it is more attracted to water

so the ionic lattice breaks up more easily

Lower charge density of larger Ca2+ means that it is less attracted to water so the ionic lattice breaks up less easily – IT IS LESS SOLUBLE

©HOPTON