R A T I N G S A N D C H A R A C T E R I S T I C C U R V E S 1 N 4 0 0 1 T H R U 1 N 4 0 0 7
F I G .1-F ORWA RD C URREN T DERA TI N G CU RVE
FI G.2- TY PI C AL I NST ANTA NEO U S FO RWA RD
1
.
0
CH ARA CTERI STI CS
0
0
0
.
.
.
8
6
4
2
1
0
0
SIN GLE PH ASE H ALF WAVE 60 H z
R ES IST IVE OR IN D U C T IVE LOAD
1
1
0
.
2
0
T
J
=
2
5
C
0
25
5
0
7
5
10
0
1
2
5
1
50
175
P
U
L
D
S
U
E
T
W
Y
I
C
D
Y
T
H
C
=
L
300 S
E
0.
1
%
A
M
B
I
EN
T
T
E
M
PE
R
A
T
U
R
E
(
C
)
0.01
0.
6
0.
8
1.
0
1
.
2
1
.
4
1.5
F IG .3-M A XI M UM N O N -REPETI TIV E P EAK
FO RWA RD SURGE C URREN T
I N ST A N T AN EO US F OR WA R D VO L T A GE ( V O LT S )
5
0
8
.
E
3
m
s
S
C
IN GLE H ALF SIN E- WAVE
M ethod)
(
J
D
E
4 0
3 0
2 0
1 0
0
F
I
G
.
4
-
T
Y
P
I
C
A
L
R
E
V
E
R
S
E
C
H
A
R
A
C
T
E
R
I
S
T
I
C
S
10
1
10
1
0
0
T
J
=
1
0
0
C
1
0
.
0
N
U
M
B
E
R
O
F
C
Y
C
L
E
S
A
T
6
0
H
z
F IG .5-TY P I CA L J UN C TI O N C APA CI TA N CE
.
1
1
T
J
=
2
5
C
1
0 0
0
.
0
0
2
0
4
0
6
0
8
0
1
0
0
1
2
0
1
4
0
T
J
=
2
5
C
P
E
R
C
E
N
T
O
F
R
A
T
E
D
P
E
A
K
R
E
V
E
R
S
E
V
O
L
T
A
G
E
%
1
0
1
0
.
1
1
1
0
1
0
0
R
E
V
E
R
S
E
V
O
L
T
A
G
E
.
(
V
O
L
T
S
)
6
-
7
J
I
N
A
N
J
I
N
G
H
E
N
G
C
O
.
,
LT
D
.
N
O
.
5
1
H
E
P
I
N
G
R
O
A
D
J
I
N
A
N
P.
R
.
C
H
I
N
A
T
E
L
:
8
6
-
5
31
-
8
6
9
4
3
6
5
7
FA
X
:
8
6
-
5
3
1
-
8
6
9
4
7
0
9
6
W
W
W
.
J
I
F
U
S
EM
I
C
O
N
.
C
O
M