+ ',n& s % + 12H + → ',n 2+ + 2MoO'+ + 8H 2 O !H#O2 −
2−
−
+
!$r
(e) 2 HAsO ' (f) 2 +
2+
(b) 2 H 2 MoO"
(d) $rO'
(O 2
!H 2 O2 + 6H
−
2−
+ "H + → $iO + + 2Ce "+ + 2H 2 O + #a +
O 2 & g % + 2 H 2 O → 2 Fe 2
+
(c) 2MnO"
'+
A)& s % + Cl
+
6+
+
(a) 2 Fe '+
+
→
8H 2 O → 10 O "
+
+
+
H
+
→
C6 H ! #H 2
2Mn
+
2+
'H
+
+
! #O'
→
−
+
'H 2O
$r 'C6 H ! #H 2
+
−
'$r
+
'H 2 O
+ O 2 & g % → 2 HAsO " 2−
2 H#O 2
+
2H
+
+
→ 2 +
2 #O + 2 H 2 O
Only in the presence of Cl- ion is A) a sufficiently )ood reducin) a)ent to e /ery useful for prereductions. +n the presence of Cl- the half-reaction occurrin) in the alden reductor is A)& s % + Cl
−
− → A)Cl & % +e
s
Fundamentals of Analytical Chemistry: 8th e ed d.
Chapter 20
he e3cess HCl increases the tendency of this reaction to occur y the common ion effect.
20-4
Amal)amation of the 4inc pre/ents loss of rea)ent y reaction of the 4inc 5ith hydronium ions. 2+
+ 2A)& % + "H + + 2 Cl −
→ ←
+ 2A)Cl& % + H 2 O
(O 2
20-6
2iO
20-7
tandard solutions of reductants find some5hat limited use ecause of their susceptiility
2+
s
+
,n& s %
+
" H
+
→ ←
2i
'+
+
(
"+
20-5
,n
2+
s
+
2H 2 O
to air o3idation.
20-8
tandard MnO" solutions are seldom used to titrate solutions containin) HCl ecause of the tendency of MnO"- to o3idi4e Cl- to Cl2 thus causin) o/erconsumption of MnO "-.
20-9
Cerium &+*% precipitates as a asic o3ide in al7aline solution.
20-10 2 MnO "
−
+
'Mn 2
+
+
2 H 2 O → !MnO 2 & s % + " H
+
20-11 Freshly prepared solutions of perman)anate are ine/italy contaminated 5ith small
amounts of solid man)anese dio3ide 5hich cataly4es the further decompositions of perman)anate ion. $y remo/in) the dio3ide at the outset a much more stale standard rea)ent is produced.
20-12 tandard perman)anate and thiosulfate solutions are )enerally stored in the dar7 ecause
their decomposition reactions are cataly4ed y li)ht.
Fundamentals of Analytical Chemistry: 8th e ed d.
20-13 " MnO "
−
Chapter 20
+ 2H 2 O → " MnO 2 & s % + 'O 2 & g % + "OH − ro5n
20-14 olutions of 2Cr 2O are used e3tensi/ely for ac7-titratin) solutions of Fe 29 5hen the
latter is ein) used as a standard reductant for the determination of o3idi4in) a)ents.
20-15 +odine is not sufficiently sufficiently solule in 5ater to produce a useful standard rea)ent. +t is uite
solule in solutions containin) e3cess + - ecause of formation of triiodide. 20-16 he solution concentration of + '- ecomes stron)er ecause of air o3idation of the e3cess
+-. he reaction is
6+
−
+
O 2 & g % + " H
+
20-17 2 O '
2−
+
→
2+ '
+
H → HO'
−
+
−
+
2H 2 O
& s %
20-18 hen a measured /olume of a standard solution of +O' is introduced into an acidic
solution containin) an e3cess of iodide ion a 7no5n amount of iodine is produced as a conseuence of a reaction. −
−
+
+O '
+
!+
+
→
6H
+
'+ 2
'H 2 O
20-19
$rO' +2
+
−
+
6+
−
e3cess
2 2 O '
2−
+
6H
→
+
2+
−
−
→
$r
+
+
"O6
2−
'+ 2
+
'H 2O
Fundamentals of Analytical Chemistry: 8th e ed d.
Chapter 20
20-20
Cr 2 O
2−
+
6+
20-21 2+ 2
+
e3cess 2−
+
+2
−
# 2 H "
−
→
2 2 O ' +
1" H 2+
→
+
→
2Cr '
+
+
'+ 2
+
H 2O
2−
+
"O6
# 2 & g % + " H
+
+
"+
−
20-22 tarch is decomposed in the presence of hi)h concentrations of iodine to ) )i/e i/e products
that do not eha/e satisfactorily satisfactorily as indicators. his reaction is pre/ented y delayin) the addition of the starch until the iodine concentration c oncentration is /ery small.
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