ACSR Conductor Selection
ACSR Conductor Selection
Guidelines for the Selection and Operation of Bare ACSR Conductors with
Regard to Current-Carrying Capacity
HOWARD A. SMOLLECK
Department o f Electrical and Computer Engineering, New Mexico State University, Las Cruces, NM 88003
(U.S.A.)
JERRY P. SIMS
Tucson Electric Power Company, Tucson, AZ 85701 (U.S.A.)
(Received January 18, 1982)
 limit for a power line is the l i m i t a t i o n s o f the   where I is the c o n d u c t o r current (A at 60 Hz),
conductor           fittings  (such as splices and             qc is the convected heat loss (W per unit
 deadends) used on a transmission line. The                    length of conductor), qr is the radiated heat
 fittings used on the line must be capable of                  loss (W per unit length of conductor), qs is
transferring the maximum available current in                  the solar heat gain (W per unit length of con-
the line. In addition, they must support the                   ductor), and r is the c o n d u c t o r resistance (~2
mechanical loads applied by the system                         per unit length at 60 Hz).
during both normal and abnormal exposure to                       Equation (1) is usually written in terms of
elevated temperatures.                                         current as
     It has been found by Howitt and Simpkins
 [ 2 ] that fittings properly designed and selected            I = [ ( q c + qr - - qs)/r] o.~                       (2)
are n o t a limiting factor for the permissible
operating temperature of a transmission line                      The most difficult heat-loss quantity to
under emergency conditions. Additional inves-                  predict is that caused by convection. Even in
tigation by Dallas Power and Light Company                     a dead calm, heat is dissipated by a natural
 [3] resulted in a similar conclusion. However,                convective effect known as the c h i m n e y e f f e c t ;
limitations of c o n d u c t o r fittings should be            thus, many researchers feel that a value of
carefully evaluated by each individual utility.                zero for wind velocity is not realistic. Con-
     The evaluation and consideration of the                   vection is further complicated by the fact that
thermal limits of a p o w e r line due to sag, loss            wind conditions may differ extensively along
of c o n d u c t o r strength, and fitting limitations         a long transmission line. The equations shown
usually result in a maximum allowable con-                     below for convected heat loss apply to the
ductor temperature or thermal rating for the                   most general as well as the special cases of still
transmission line. For a specified maximum                     air at sea level and still air for elevations above
allowable c o n d u c t o r temperature and a given            10 000 feet.
set of ambient weather conditions, the con-
tinuous current-carrying capacity (ampacity)
                                                               C o n v e c t e d h e a t loss qc
of a power line can also be determined by
                                                                   When D P ~ V / 1 2 U f is between 0.1 and 1000,
applying heat-balance equations to the elec-
trical     conductors.         The   current-carrying
capacity of a c o n d u c t o r as a function of con-
ductor temperature, ambient temperature,
                                                                      I
                                                               qc = 1.01 + 0 . 3 7 1 \ - - ~ f ]
TABLE 1
Viscosity, density and thermal conductivity of air
Temperature                             Abs. viscositya (Ib/h ft)   Density b of air, Pf (lb/ft 3)            Thermal con-
                                                                                                              ductivity c of air
(°F)    (°C)       (°K)   (OK/100) 4    Uf            At sea         5000 ft    10 000 ft      15 000 ft      K f ( W / f t 2°C)
                                                      level
aHilsenrath and Touloukian, The viscosity, thermal conductivity and Prandtl number for air and other gases,
ASME Trans., 76, (1954) 967 - 981.
hR. D. Madison (ed.), Fan Engineering, Buffalo Forge Company, Buffalo, New York, 5th edn., 1948.
cw. H. McAdams, Heat Transmission, McGraw-Hill, New York, 3rd edn., New York, 1954.
ity of air (lb/h ft), K~ is the thermal con-                        where 'elev' is the elevation of the c o n d u c t o r
ductivity of air (W/ft 2 °C), tc is the average                     above mean sea level (ft), and
temperature of the conductor (°C), and ta is
the ambient temperature (°C).                                       tf = air film temperature
   Values for P~, U~ and Kf can be approxi-                            = (gc + ga)/2 (K)                                      (10)
mated from Table 1; however, the following
equations obtained from a regression analysis                       Radiated heat loss, qr
by Lutwen [4] are more useful for computer
applications:
                                                                                      [\100/         \100] ]
p~ = 21.6578eele~(-3.9o6 96 × io-5)×
                                                                         (W per ft of conductor)                              (11)
          tfelev(1.512 18× 10--7)--0.996 239
                                                                    where K¢ is the conductor temperature (K),
       (lb/ft 3)                                        (7)         Ka is the ambient temperature (K), D is the
                                                                    ambient c o n d u c t o r diameter (in), and E is the
                     tf                                             coefficient of emissivity (E for a new con-
Uf =                                   (lb/h ft)        (8)         ductor = 0.23; E for a black c o n d u c t o r = 0.95).
       5165.9 + 5.167 08t~
                                                                    Solar heat gain, qs
k~ = 1.204 98 × 10 - 3 + tt(2.265 45 × 10 -5 )
TABLE 2                                                                        TABLE 3
Total heat received by a surface at sea level normal to                        Altitude and azimuth (in degrees) of the sun at various
the sun's rays a                                                               latitudes a, b (declination 23.0 °, Northern Hemisphere,
                                                                               June 10 and July 3)
Solar altitude H c         Qc (W/ft2)
(deg)                                                                          Latitude           Local sun time
                           Clear                       Industrial              (°N)
                           atmosphere                  atmosphere                                 10:00AM         12:00noon        2:00PM
 5                         21.7                        12.6                                       Hc    Zc        Hc    Zc        He         Zc
10                         4O.2                        22.3
15                         54.2                        30.5                    20                 62     78       87      0        62        282
20                         64.4                        39.2                    25                 62     88       88    180        62        272
25                         71.5                        46.6                    30                 62     98       83    180        62        262
                                                                               35                 61    107       78    180        61        253
30                         77.0                        53.0
                                                                               40                 60    115       73    180        60        245
35                         81.5                        57.5
40                         84.8                        61.5                    45                 57    122       68    180        57        238
45                         87.4                        64.5                    50                 54    128       63    180        54        232
50                         90.0                        67.5                    60                 47    137       53    180        47        223
                                                                               70                 40    143       43    180        40        217
60                         92.9                        71.6
70                         95.0                        75.2                    aThe American Nautical Almanac, U.S. Naval Obser-
80                         95.8                        77.4                    vatory, Washington, DC, 1957.
90                         96.4                        78.9                    bSight Reduction Tables for Air Navigation, U.S.
                                                                               Navy Hydrographic Office, H.O. Publ. No. 249, Vols.
aHeating, Ventilating and Air-Conditioning Guide
                                                                               II and III.
1956, American Society of Heating and Air-Condi-
tioning Engineers, New York.
                                                                               e f f e c t o n a c o n d u c t o r ' s a m p a c i t y . The effect
w h e r e a is t h e c o e f f i c i e n t o f s o l a r a b s o r p t i o n   o f wind speed on ampacity is probably the
(a f o r a n e w c o n d u c t o r = 0 . 2 3 ; a f o r a b l a c k             single m o s t influential factor in calculating
c o n d u c t o r = 0 . 9 5 ) , A ' is t h e p r o j e c t e d a r e a o f     conductor ratings. T h e f o l l o w i n g T a b l e , p u b -
t h e c o n d u c t o r = D / 1 2 ( f t ) , a n d Qs is t h e t o t a l        lished by Waghorne and Ogorodnikov                                   [6],
solar and sky radiated heat (W/ft2).                                           quantifies various wind speeds:
                                                                                             .... J                 ........
                                                                                                           . . . . . . . . .                                                                    -----WITHOUt
                                                                                                                                                                                                   1 Awm~au~lSUN
                                                                                                                                                                                                              ,
                                                                                             I ~ 0 0       +        +         '          +         +        p       +         '             '           1         ~       "       +
+ . ~ , J . . . . .
~120C
O.
~    110£
I--
Z 100t
rr
~.~ 800
                                                                                        ~    1~00 %.                                                             %.'+"                                      '~'
0
                                                                                        z,                     ~,,,,~%.                        ~       +                              '',,,,+p~.                  ,   ~+° +,6F
800
70C
     60(
                                                                          +     :            IOO0          .             .          .              .                                            .% ~,. ,~
, 2+~~o' -l ( !
     40(                                                                                                E. 0.7
            !                                          ~10~ND~YI3 +                                     vll.a~ae              ~+PH                 :        --                                          ",~                       +
     30¢
• , y ' . , , , ,
                10.80) 11+36) 12.051 12.731 (3.41) (4.06) 14.771 15.46) (6.141 (6.82)                   B~T_W~ENt,IJ~_                         10 A N e J U t
                                                                                              ?00       E EV             ZO       U'(         ~L             +                +             .       .        .    .   .       .
                                VELOCITY        FPS (MPH)
                                                                                                        ~dl'~.-,THUu,-]uz"                         NomprM +                   I             +           '         t       +       ~   '
Fig. 1. Effect o f w i n d speed on a m p a e i t y (Drake
                                                                                              4100~0                ,O                  IlO                60                100                    110               130
795 000 cm, 26 x 7 ACSR).
                                                                                                                              AMBIENT                      TEMPERATURE                              ('F)
range from 0.122 to 0.183 m/s (0.2727 - 0.409                                           Fig. 2. Effect o f a m b i e n t t e m p e r a t u r e on                                                                                 ampaeity
mile/h) as a result of the chimney effect at                                            (Drake '795 000 era, 26 x '7 ACSR).
the heated conductor. Because of the uncer-
tainties of wind velocity along a transmission                                          thermal limit for normal operation of stranded
line, it has been the practice of the industry                                          aluminum and ACSR conductors [1, 9].
to consider a wind velocity of 0.608 m/s
(1.36 mile/h) as a safe lower limit [5, 7, 8]. If                                       Coefficient o f emissivity, E
it is known from climatological data t h a t                                               Radiated heat loss to the surrounding at-
wind velocities much greater than 0.608 m/s                                             mosphere by a conductor is a function of the
prevail, however, considerably higher load                                              surface condition which is described by the
currents can be obtained on an existing con-                                            coefficient of emissivity E. Well-weathered
ductor or a smaller conductor may be used                                               conductors, after being energized for a period
for a new line design.                                                                  of time, have a dark surface which radiates
                                                                                        well and may have an emissivity as high as
M a x i m u m conductor temperature, t c                                                0.98. New conductors, on the other hand,
   The maximum allowable conductor temper-                                              may have an emissivity as low as 0.23. The
ature is the thermal limit of the conductor                                             length of time needed to develop a high emis-
and must be determined after reviewing design                                           sivity was studied by House et al. before 1963
temperatures for sag, loss of conductor                                                 [10]. They found that conductors energized
strength and thermal capabilities or limitations                                        above 15 kV in an industrial atmosphere
of line fittings. As seen in Fig. 2, variation in                                       reached an emissivity of 0.9 in 8 years. In
conductor temperature t~ affects ampacity                                               rural atmospheres, conductors energized
considerably. The specification of the maxi-                                            above 15 kV attained an emissivity of 0.9 in
m u m allowable conductor temperature t¢                                                about 30 years. These results may be expressed
must be the first step in defining the maxi-                                            by the (highly empirical) relation
m u m allowable conductor current. If there
are no other limitations due to sag, fittings,                                                     0.70 Y
                                                                                        E = 0.23 + - -                                                                                                                                (15)
etc., 93 °C (200 °F) is considered to be a safe                                                    1.22+Y
184
Elevation, elev
    The effects of elevation on ampacity of a
c o n d u c t o r can be quite noticeable due to
changes in air density Pf. For example, Pf =
0.0740 at sea level and 25 °C (77 °F), whereas
at 3050 m (10 000 ft) and the same temper-
ature P~ = 0.0508. If the lower ambient tem-
perature associated with higher elevation is                       ,oo     t                   t                 ,           i
considered, the difference in P~ is even greater
                                                                   eo,o.   t         •         l                 .           .               .               .
                                                         Tc:210o F
                                                                            and other single-metal conductors, however,
      100
                                                                            creep may reach very dangerous values at high
             ~
                                                                            temperatures under certain conditions of span
                                                             T ¢- :~O0*F
      g8                                                                    tension.
gQ
                                                                            TIME-TEMPERATURE CHARACTERISTICS OF
                                                                            ACSR
3:    g4
I--
Z
uJ                                                                             The heat-balance equations presented earlier
Or)   g2                                                                    in this paper have been used to determine
                                 .i.ii
z                                                                           steady-state or long-term conductor ampaci-
Z
<c
      80
                                                                            ties. With the increasing complexity of inter-
LU
rr-                                                                         system ties, load currents during and following
                                                                            system disturbances may reach values well in
      88
                                                                            excess of the continuous current rating of the
                                                                            line. This condition, however, might exist for
      86                                                                    perhaps only half an hour or so, by which
            ~u.r_E0._7                                                      time the generation would have been increased
                                                                            and switching performed.
      84
  310                           -
                                                                                                      If this process is continued until the entire
                                                                     ~                 15C %-      rating period has been accumulated, the final
                                                                                                   temperature calculated can then be compared
  .......                            /
                                     p
                                                             .,                              -
                                                                                                   with the allowable c o n d u c t o r temperature.
oI 2to                                                                                                The equations for r, qc, qr, and qs used
                                                                                                   here are those previously defined. The con-
                                                                                                   ductor heat capacity P can be expressed for
                                                                                                   A C S R as
~2so                   ~                                                               12C   %-
                                                                                                   P = 4.186 (453.6) ( C 1 W 1 + C2W2)
tant load. Conductor temperature underwent          CM conductor cited, no loss of strength can be
rapid changes and in one case varied as much        observed for operation up to 10 000 hours for
as 50 °C within 20 minutes during a change in       a conductor temperature at or below 116 °C
weather conditions from a period of almost          (240 °F) for the conditions given (see Fig. 5).
complete calm to one of high wind velocity.         Contrast this with the Alcoa recommended
BG&E f o u n d that m a x i m u m conductor tem-    temperature limit for normal operation of
peratures, as calculated by the methods pre-        stranded aluminum and ACSR conductors,
sented in this paper, actually do occur,            which is 93 °C (200 °F) [9].
although rarely; but a conductor carrying a              It is our conclusion that, in general, the
constant current will operate well below the        temperature limit of 93 °C (200 °F) can be
theoretically calculated m a x i m u m temper-      established as aminimum level for the normal,
ature during most of i t s life. Correlation bet-   continuous operation of ACSR lines. Higher
ween the field test curves and the calculated       continuous temperature limits may be estab-
curves was very good except for the zero wind       lished after sag and loss-of-strength limitations
velocity condition. The test temperature rises      are reviewed. Emergency short-time operation
were always lower than the calculated rises at      at higher temperatures may also be considered
zero wind velocity.                                 after review of the loss-of-strength equations.
   Investigation of transmission and distribu-      Of course, sag limitations must still be observed
tion load capabilities at Dallas Power and Light    during emergency operating conditions. The
Company [3] further confirmed the accuracy          t i m e - t e m p e r a t u r e relations given here can be
of predicting conductor temperatures by cal-        used to prevent the exceeding of the sag limi-
culation. DP&L found that the steady-state          tations during any emergency overload con-
heat-balance equations presented in this paper      dition.
were accurate to within 1 °C for the range bet-
ween 81 and 171 °C in their laboratory tests.
They did, however, note a decrease in the           Localizing the ampacity parameters
cooling effect of wind m o v e m e n t when the        Once a m a x i m u m conductor temperature
direction of flow was parallel to the conductor     has been established, the heat-balance equa-
and not perpendicular to it as is assumed           tions illustrated in this paper can be applied
when using the equations given in this paper.       to determine the conductor's continuous
                                                    current-carrying capacity for a given set of
                                                    ambient weather conditions at the specified
                                                    conductor temperature. These equations can
CONCLUSIONS AND RECOMMENDATIONS                     be used to localize such factors as weather,
                                                    solar heat gain, elevation, and emissivity to
Establishing a thermal rating                       the particular section of line and to adopt
   The m a x i m u m operating temperature of an    individual and seasonal ratings. The results of
overhead ACSR transmission line conductor is        such studies should in many cases allow de-
established by reviewing thermal limitations        ferral of reconductoring or line rebuilding.
of the conductor due to sag and loss of                The Aluminum Association [18] correctly
strength. For most lines, conductor fittings        states that:
will n o t be a limitation if chosen properly.
   Sag limitations can usually be determined           "There is nothing magic about an ampacity
from the transmission line design criteria. For     table published by Alcoa, Alcan, Kaiser,
example, sag design temperatures for three          Noranda, Anaconda or Reynolds. You have to
transmission lines in the Tucson Electric Power     look at any ampacity table in light of para-
transmission system are 121, 132 and 146 °C         meters that are governing that calculation."
(personal communication to J. P. Sims from
K. Wright, Tucson Electric Power Company,           It makes sense to base the ampacity rating of
February 13, 1978).                                 any particular transmission line upon the
   Harvey's equations greatly simplify the loss-    ambient environment and operational demands
of-strength consideration in establishing           associated with that particular line whenever
thermal limits for lines: The results can be        possible.
quite startling. As an example, for the 795 000        The effects of various parameters on the
                                                                                                 189