MnO4- + Cl-
Mn2+ + Cl2
First break the equation into two half reactions, one for Mn and one for Cl
MnO4- Mn2+
-
MnO 4-  Mn 2+
-
MnO 4-  Mn 2+ + 4 H 2O
-
8 H + + MnO 4-  Mn 2+ + 4 H 2O
-
5 e - + 8 H + + MnO 4-  Mn 2+ + 4 H 2O
-
10 e- + 16 H+ + 2 MnO4- 2 Mn2+ + 8 H2O
|
Cl- Cl2
-
2 Cl -  Cl 2
-
...
-
...
-
2 Cl -  Cl 2 + 2 e -
-
10 Cl- 5 Cl2 + 10 e-
|
10 e- + 16 H+ + 2 MnO8-+ 10 Cl-
2 Mn2+ + 8 H2O + 5 Cl2 + 10 e-
16 H+ + 2 MnO4- + 10 Cl-
2 Mn2+ + 8 H2O + 5 Cl2
Basic Solution:
Separate the reaction into two half-reactions.
Balance each half-reaction separately as in acid:
-
Balance atoms other than O & H by inspection.
-
Balance O by adding H2O to the opposite side.
-
Balance H by addding H+ as appropriate.
-
Balance the charge by adding electrons (e-) - add to same side as excess of positive charge, or opposite side if excess negative charge.
-
Balance the charges of the two half-reactions by multiplying appropriately.
Balance as in acid above, then:
-
Add enough OH- (equal numbers to both sides) to cancel the H+. (This is necessary because there will not be protons present in a basic solution!). (There are a couple of other conventions for balancing in basic solutions. If you are familiar with another and prefer it, you may use it instead.)
-
Combine the H+ and OH- on the appropriate side of the equation to give waters.
-
Go back and cancel waters which appear on both sides to give the final equation.
Water Properties
-
Extremely high mp and bp:
|
MW |
m.p. |
b.p. |
Water |
18 |
0°C |
100°C |
Methane |
16 |
-183°C |
-161°C |
-
High Heat capacity: 18 cal/°C mol vs. 8 cal/°C mol for methane
-
High viscosity
-
Solid form is less dense than the liquid form at the same temperature (ice floats on water - very rare)
-
High dielectric constant (78.5 vs. 1.9 for hexane; 'blocks electric fields')
-
High surface tension.

public domain image via Wikipedia Creative Commons

public domain image via Wikipedia Creative Commons

public domain image via Wikipedia Creative Commons

public domain image via Wikipedia Creative Commons
© R A Paselk
Last modified 16 February 2015