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Additional subjects inDOI: 10.9734/PSIJ/2015/18291
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The SU(3) symmetry in DOI: 10.9734/PSIJ/2015/18291 The SU(2) x U(1) symmetry is well covered in DOI: 10.9734/PSIJ/2015/18291 and its corrigendum, both published in Physical Science International Journal. The SU(3) is briefly described so we will focus on the SU(3) symmetry. The best way to do so is to return to the Godbillon-Vey class and to the Reeb class. There are several ways to show the SU(3) symmetry, either be replacing with and expression that depends on 3
fields or by adding these fields in the rotor calculation of (17) and (18). For now we will adopt the second approach. We add three normalized gradients of scalars that change along the F foliation, This can always be done by integration along a grid that is defined in the foliation , We define the scalars , , as integration along curves in
the foliation and
P
)( kPF 1V 2V 3V
V1dx
dV1 gradient by the coordinates . x
),3*3
3
2*2
2
1*1
1
*(
),3*3
3
2*2
2
1*1
1
*(
ˆ
VV
V
VV
V
VV
V
PP
P
VV
V
VV
V
VV
V
PP
P
A
Obviously we sloppily wrote the norms because we should write
2/)*111*1()1(,2/)**(
VVVVVZPPPPZ etc.
Such that the three vectors are gradients of scalars that vary only along the Godbillon-
Vey foliation , )( kPF ))((3,2,1 kPFTVVV so . It is
sufficient that the norms of the gradients of such fields are stationary
0321
PVPVPV
along . Then we
have
P
... 2/)*111
VVV
), )2(*)1( VZPVZ
0*3*2
PVPV
*1()1( VVZ and we write as in the
paper so and
obviously since the gradients are along curves in
the foliation, then locally using the Scarr-Friedman law for homogeneous acceleration, we get
1()1( VZVZ
*1 PV
0*)3(*
PVZP
2
**),(),(
*ˆ
U
Z
PA
Z
P
Z
P
Z
P
Z
PA
half the curvature vector.
This is a type of invariance that can be expressed by the 3x4 matrix
)33
3,
22
2,
11
1(
VV
V
VV
V
VV
V so if the three columns change with such that
the norms are invariant along and they are in then equation (46) in the
paper remains invariant. The 3x3 matrix determinant in the basis ,V , can’t
change sign.
P
P ))(( PFT
1V 2 3V
Zero charge field in DOI: 10.9734/PSIJ/2015/18291 We can write
2/32/3 2222 Z
ZP
Z
ZP
Z
UP
Z
UPA
UZ
P
Z
ZP
Z
ZP
Z
PA
*)
22(2
*2
2/32/3
**
;4))4
*
4(
*;(4
))4
*
4
*(
*;(4
)2
*)
22(
*;(4)
2
**;(4
))2
*;*(
*;(4);
*(4;2
32
33
2/32/32/32/3
2/3
UUZ
PA
Z
ZPZP
Z
ZZ
Z
PA
Z
ZPZP
Z
ZZPP
Z
PA
Z
ZP
Z
ZP
Z
ZP
Z
PA
Z
ZPA
Z
PA
Z
ZP
Z
PA
Z
PA
Z
PAU
Zero charge can be written either as
**
;4 UUZ
PA
Or more formal as,
UUUUZ
PA
Z
PA **);*
*;(4
An interesting case is if the curvature vector is a null vector. U
Then we have 0);**
;(4 Z
PA
Z
PA
.
Majorana fields revisited Suppose is a real geodesic scalar, i.e. its time-like gradient is parallel to geodesic
curves. Then we can write and it is easy to show that for some
scalar function .
q
qqY aqY
a
;~
;2)2
;(2;2
)2
;(2;2);(2
2/3
2/3
UY
qA
Y
qaq
Y
qA
Y
qA
Y
Yq
Y
qA
Y
qA
Y
qA
Such that U~
is the acceleration vector derived from Y
q
.
If is purely imaginary then, ;A
0;*~
;~
);*;(2
UUY
qA
Y
qA