watcr coolccl rotor
;id
stiltor of the alt~i.li;it~r.
A
r;ithcr srn;tli ruallcr tip di;im~-tcr rcsi~ltcd in
n
ncarly hook-fornictl runner v;tnc tvith
;i
ratlicr thick and round i~osc
and
;in i~ilct ;~nglc of tically
90'.
Thc
runner
of
350
311,
\vcight, wclded together iroin cast stcel huh and sliroutl scctions with siilmps
for tlic
14
vancs, was trans~~ortctl by
;I
special ship via the Lenio c;~n;il, Ice Occa~i and 11pstrt:nrn the
lcwcr
course
of the Ycnissci. Contrary to thc usual rccommcn~::itions, tlic numbil. of gates is an
integer
multiple,
n;lmcly twicc tlic runner vane numbcr. This tog~thcr with tlic ratlicr blunt runncr
vanc inlet edge parallcl to the shaft may cause a noisy operation of the scts; wliicli was also reported.
Another fca:urc is that the wcldcd spiral casing has
2
intakes (Dwuchnaja spiralnaja kamara) which
should obviously
lower transportation weights, but also may rcducc radial forcc and
secondary
flow
in
thc volute casing.
The
wclded shaft of
2,3
m diameter has a water lubricated lowcr journal bearing.
The Mitchell thrust bcaring rated at
3400
tons is supported by
a
conical trunk
011
the head cover.
The gates are opcratcd by two pairs of oppositc plunger servomotors, mounted on the hezd cover,
[2.35].
The exploitation of the middle Yenissei is yet to be carried out. The deve1opmei;t of the
lower Yenissei (1250 km with
0,006% slope) has been made in two steps: Ossinov and
Igarka.
Speirking of the harnessable potential of the Yenissei proper, has excludcd its greatest
tributary the
P.n_gara. This famous and only outflow of the Haikal Lake has a length of
1850
km
ar.d
a
drop in level
of
378
m
between Baikal
and
its conflue~lce with the Yenissci.
The
average slopc
of
the Angara is 0,02%, but the dc?th of the valley permits
development at
three sites having 76 to 106
m
head and at four other sites
with
smaller
liead.
The
lint
plant in service is Irkutsk with
31
m
head and
8
KT
of
82,5
MW
each
with vibrating oil
hcads above the a1terna;ors. Irkutsk serves pertly as an outflow regrlla!or for tlic Iiuge
700
kni long
rescrvoir of thc Baikal
Lnkz.
In a typical Soviet manner the spillnays werc built here as by-pass
outlets around the semi-spiral casing
and dralt tube of cach machine and act during spillage a; a
head enlarger by virtue of the hydraulic jump then formed past the draft tube outlet (see Fig.
3.3.2).
This
Tacilitatcs also thz deflection of ice floes during the very cold (temperature drops down to
-
59'C)
and long lnstiriy winter in this region of nearly
0'
average temperature.
On account of the large
specific
heat of water, the heat insulation of the ice sheet and thc heat flow
from the
ictcrior of thc earth, all the great northwardly flowing Siberian streams crossing about
1500
km of perrna-frost-soil do not freeze completely even in winter time whilst at the river mouth
there ere zones with
-
17
-C
average temperature.
3)
Bratsk: This is thz
next
station in service downstream of Irkutsk with an annual
production of
22
TiVh. This was the greatest station output before the inauguration of
Churchill Falls in 1970. After commissioning Grand Coulee
III in 1979, La Grande
2
in
1980, Sayano Shushensk and Itaipil (between 1985 and 90) Bratsk then will be the fifth
larsest plant on the basis
of
annual energy production. With respect to its output of
4050
MW
Bratsk was the most powerful station from 1962 until 1968 when Krasnojarsk
started. Now
it
is the fourth largest after Krasnojarsk, Gran Coulee 1-12-111 and Churchill
Falls.
Also the high voltage transmission of
500
kV
built with the assistance of Savoisiennc (France) was
the
first of this type. The
220
MW
FTs once were amongst the most powerfill, consisting of
icteg-ally cast runner hdvcs, bolted together on site with welded shzft,
and
having 14 runner vanes.
The
rescrvoir
oi
Bratsk with a capacity of
169
km3
remains however the largest artificial lake located
in the
midst of the nearly everlasting virgin needle forest of Siberia, the so-called Taiga.
It is closed
by
a
1500 m long and 110 m high gravity dam with a
400
m
long power house
on its
base (Fig 3.4.49). Owing to the time taken to fill the reservoir, energy production
of Bratsk started with
a
llalf filled basin. This caused
a
rather r,oisy stalling cavitation in