www.ijape.org International Journal of Automation and Power Engineering (IJAPE) Volume 2 Issue 2, February 2013
C
ab (19)
So, total resistance: RT = R1 + R2 +R3
and we will receive the formulas as in the case of the GEM layer of cylinder form.
RT
l2 1 1 ln C t C 2 l ( 2 )
(25)
d C(2t C) 2 ln 3 ln dt 2l
Grounding Resistance of Single Horizontal Rod
Grounding Resistance of Equivalent Horizontal Rod
1) GEM Layer of Cylinder Form Single horizontal rod with diameter d , length l and resistivity 3 is fixed in the ground with the depth t . It is environed by the GEM environment with resistivity 2 and the soil environment with resistivity 1 (see FIG. 6)
We use the calculating method as at the above point and receive the results as follows: 1)
The Component in the Metal Environment
R 1 ' 2)
3 d (26) ln 2 l 2 l
The Component in the Equivalent Soil Environment
R ' 3
FIG.6 SINGLE GROUNDING HORIZONTAL ROD WITH THE GEM LAYER
Applying (1) and after some transformations, we found the magnetic field that is created by the horizontal rod at the point (x, z) ( x ) I ln l 1 2 l 2 x
l 1 (20) 2x 2
and the magnetic field is created by the image of the horizontal rod at the point (x, z):
2 ( x)
I l ln 2 l 2(2t x) x
We use the calculating method as at the above point and receive the results as follows :
R
T
l2 1 eq ln 2 l dt
2) The Component in the GEM Environment R 2 2 2 ln C ( 2 t C ) (23) I 2 l dt 3) The Component in the Soil Environment
3 I 1 l2 R 3 (24) ln I 2 l C ( 2 t C )
28
d (28) 3 ln 2l
Hence, In order to determine the equivalent resistivity we will equalize (25) and (28), from this
l2 C ( 2t C 2 ln C t C dt ( 2 )
1 ln
l eq ln dt 2
0
The equivalent soil resistivity will be
eq
l2 ln C ( 2t C )
1
C ( 2t C ) dt
2
(29)
l2 ln dt
1) The Component in the Metal Environment
1 d (22) 3 ln I 2l 2l
(27)
Total resistance: RT = R’1 + R’3
2 l (21) 1 2(2t x)
Grounding Resistance of Horizontal Rod with the GEM
R1
eq l2 ln 2 l dt
So, we can count as single grounding horizontal rod (with parameters d , l ,3) that is only buried in one single soil layer with equivalent resistivity ρeq. This equivalent resistivity is calculated by equation (29) (see FIG.7). In reality, 3
0 , from (28) we have:
R T
eq 2 l
l 2 (30) ln dt