HYDROLOGICAL DATA ON SELECTED SOVIET RIVERS

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• Collection: General CIA Records
• Document Number (FOIA) /ESDN (CREST): CIA-RDP79-01009A001200020004-3
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• Document Creation Date: December 20, 2016
• Document Release Date: February 17, 2006
• Sequence Number: 4
• Publication Date: January 1, 1956
• Content Type: IR

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GEOGRAPHIC INTELLIGENCE REPORT
HYDROLOGICAL DATA ON SELECTED SOVIET RIVMS
CIA/RR GR-86
January 196
Department of Interior Release
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IVail BEVIESatit
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Copy No.
asoaaAnac INTELLIGENCE REPORT
HYDROLOGICAL DATA. ON SELECTED SOVIET RIVERS
CIA/ER -c-e6
January 1956
CFSTRAL INTELLIGENCE Amcor
Office of Research an4 Reports
oiliertirs
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T. Introduction .
CONTENTS
Sources and Evaluation of Data
111E,
- ..
1
III. Hydrological Data. . .........
A. The OW River System
1. OW River ... . . ..... ? . ? ? ?
V ? ? ? ?
.?
Tobol River. .
?
w ....... ?
Tobol River Tributaries. . . .
B. The Oka River System . ......
Oka River. .
V ? ?
? ? ? l? ? A JO ?
2
3
2. Oka River Tributaries. . . , 8
Tables
Tabie No,
1 Location of Stations and indicated Hydrological Data
for Ob River System. , ? ? ? v 10
Average Monthly and Yearly Discharge Values far GC'
River System. . , 1I
Chemical Composition of Waters of Ob" River System.
4
6
Location of Stations and Indicated Hydrological Data
for Oka River System. ....... , . , 14
Average Monthly and Yearly Discharge Values for Oka
17.iver System. . c ? 0 ? ? ? V ?? ? ? ? i5
Chemical p it: f Wi.ers of Oka River System.
1 OW River Network . .
2 Oka River Network
14.12.s.
!!1P P2.
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HYDROLOGICAL DATA OE SELECTED SOVIET RIVERS
I. Introduction
This study provides hydrological information for rivers of the OW and
Upper Volga Basins. Detailed data on the discharge of the selected rivers
and. the chemical composition of their waters are presented in Tables 2, 3,
5, and 6. River discharge values, stated in monthly and yearly averages,
are given for locations at intervals not exceeding 200 kilometers in length.
The chemical composition of the water is given in amounts of various ions
and total hardness. In the accompanying text, these data are briefly
analyzed and compared.
The rivers selected are located in two regions, Western Siberia and
Central European USSR. For Western Merle, data are given for the head-
water section of the OW River and for the Tobol River along with its west-
bank tributaries.. For Central European USSR, information covers the Oka
River and several of its tributaries.
Sources and Evaluation of Data
Much of the information in this study was obtained from Russian pebli-
cations. Other information came from domestic sources, such as publications
of the U. S. Geological Survey of the Department of the Interior.
The most up-to-date AtAtESP.-, were -givenalareCRiiiiian publication, The River
Regimes of the Southern Receis of Western Siberia Northern and Central
Katakhstan by P. S. Euzin; Leningrad, 1953. The publication gives numerous
long-term records for the discharge and chemical composition of waters of
rivers in Western Siberia. Included are many older hydrological records, as
well as recent data based upon observations and samplings during the period
from 1940 to 1950. The information on the chemical composition of river
waters is particularly significant because it represents samplings taken at
various times during the year, as well as at various stages of river flow.
Average discharge values Irene obtained for 31 selected stations along
the rivers of Western Siberia, some with records up to 56 years in length.
In most cases the data were adequate for this study.
1.tia, on the discharge and chemical composition of rivers in the upper
Volga system were obtained from older publications, principally the
Handbook on the Water Resources of the USSR, Vol. III, "Basin of Upper Volga
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and Oka)" 1935. This publication includes data on discharge rates at selected
stations along rivers of the Oka River basin. For the most part the values
given are adequate for the Oka, Moskva, and Elyaz'sa Rivers. Where data were
incomplete or lacking, interpolations were made. Data on the chemical com-
position of the water in this area, however, are scant.
III. ydrologicaiata..
The rate of discharge is given in cubic meters per second for selected
points along the courses of the rivers. These discharge rates are given in
average monthly and yearly values. If monthly discharge rates were not avail-
able for at least one point in every 200-kilometer stretch of river, interpola-
tions were made on the basis of average yearly values. The discharge regime
for the interpolated point vas calculated by determining the monthly percentage
of flow for other stations along the river's course. For some stations,
approximate discharge values were based upon values for nearby rivers with
similar regimes. The interpolated and approximate values may vary somewhat
from the true rates of discharge because no two rivers have identical
discharge characteristics. In cases where records were not for the same
periods of observation, average rates of discharge may vary considerably.
The Months of high water and low water are indicated in the tablas. The
greatest monthly volumes of water usually coincide with the period of spring
thaw and the breaking-up of the ice on the rivers. The low monthly discharge
occurs during the winter, when freezing restricts the amount of run-off. In
their upper courses the rivers have little or no flow during the winter
months when the rivers are frozen solid.
The chemical composition of the river water is based upon quantitative
analysis. Most of the samplings on record include the amount of significant
ions and dry residue present and the hardness of the water.
In this study the hardness of the water in rivers of the Ob' system
is indicated as total hardness in parts per million, based on equivalent
values of calcium and magnesium. For the Oka River system the data on total
hardness were converted to parts-per-million values from degrees of hardness.
In order to compare the total hardness for different rivers and different
localities, a relative total hardness scale has been 11mA. This scale is
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bneed upon the subdivisions of A. 0, Al kin* as given below:
Relative Hardness Partsjper Million
Very soft
0 - 75
Soft
75
- 150
Moderately hard
150
- 300
Hard
300
- 450
Very bard
Over 450
A. The Ob River System
The Ob' River and its tributaries form one of the major river systems
of Siberia. The system drains a large area of Western Siberia from the
Altay Mountains on the south to the Arctic Ocean on the north and from the
eastern flank of the Urals eastward toward the edge of the Siberian Lowland.
The Oh' River proper is formed by the confluence of the WWII' and
Hips Rivers at latitude 52?3011 and longitude 85?R near the city of Bayek.
The river flows roughly northwest and enters Ob' Bay at approximately 66?451N -
69?00'E. The section of the river examined extends from the junction of the
Katuni and Bila Rivers to the point 'where the Tom' River joins the Ob'.
The Tdbol River and its tributaries drain the eastern elope of the Ural
Mountains. The Taol itself empties into the Irtysh River at 56?1041 - 68P1011a
This report gives data for the Tabol and two of its tributaries-- (1) the bast'
and its tributary the Techa, and (2) th Tura River and its tributaries the
Reyva and the Mem Rivers,
Map 1, showing the Ob' River system, gives the location of 31 stations,
which are keyed by number to Table 1. The table gives the name of each station,
its location, the distance to the mouth of the river, and selected hydrological data.
Table 2 gives the average monthly and yearly discharge values for the same
stations and the length of record for each. Discharge values are givei in
cubic meters per second for the stations along the river'fis course. Where
inforantion was not available for at least one point in every 200-kilometer
stretch of river, estimeted values are given and the stations for which
estimates are made are identified. Table 3 dhows the chemical composition
of the water for selected rivers in the Ob' River system and gives the
number of samples taken at each station. The chemical composition is stated
* As presented in: alimentov, P.P., Gidrogeologiya (Hydrogeology),
aosgeolotekhiedat, Moskva, 1955, p. lop._
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in parts per million of calcium, magnesium, sodium and potassium, bicarbonate,
sulfate, and chloride. Total hardness is also given in parts per million.
Chemical composition of the water, listed as ions of elements and the
total hardness, is given in average, maximum, and minimum values. For
maximum and minimum values, the months in which they occur are given.
1. Ob' River
For the headwater section of the Oh River: long-term records
of river discharge are available for Barnaul, Novosibirsk
and estimated values for Shelabolikha and Nozhevnikevo.
The average annual discharge Increases from 1440 m3/sec. at Barnaul to
1610 m3/sec. at Nozhevnlkovo above tee junction with the Tam' River tributary.
At Barnaul, low eater occurs in March and high water in June. Front Name.
nee0bi to Noebevnikevo at the end of the headwater section of the river, March
continues to be the month of low water but May is the month of high water.
The months of high and low average discharges correspond with the dates
of the breaking up of the ice. As indicated on Table 2, the month of lowest
discharge along the Ob' River is March, just before the beginning of the
spring thaw. On the average, the Ob' River is ice-free at Barnaul by 10
April and at lovOsibirak by 30 April. The peak seasonal discharge occurs
during the period of spring thaw and ice break-up.
The chemical cempOeitioe of ihe vete: is given for 2 stations on the
Ob' River. At Barnaul, the averages were based on 6 samplings, which were
taken during the spring and fall months. When these samplings were taken,
the average river discharge was 2.2 times the yearly average. Under these
conditions, the concentration of constituent elements may be slightly lower
than average. At Novosibirsk, on the other hand, 56 samplings were taken
during all seasons of the year, and theee readings were averaged, The
average river discharge at the time of these samplings was 1.7 times the
yearly average.
The total hardness of the water varies from very soft at Barnaul to soft
at Novosibirsk. The softness of the water is due to the low concentration
of calcium and magnesium. At Novosibirsk the average concentration is
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37.7 parts per million of calcium and 8 parts per million of magnesium.
The maximum concentration of calcium and magnesium occurs during the
autumn and early spring, tAken the river discharge is relatively law, whereas
the minimum conceatration occurs during the months of high water in late
spring and early summer.
2. Tobol River
Discharge values axe given for 9 stations along the Tobol
River from its headwaters near tae southeastern end of the Ural Mountains
to the point where it empties into the Irtysh River. The average yearly
discharge of the Tobol River increases from 19.1 m3/sec. at Grishenka
near the source to 810 mi/sec. at Lipovka, 103 kilometers above the river's
mouth. At Orishenka, the Tbbol River has no flow during January, and February,
and peak flow occurs in April.
Along the lower course of the Tobol. River, the peak flow occurs during
May. Here, as on the Ca' River, the month of high discharge follows the
breaking-up of the Jen.
The chemical covosition of the water is given for 3 points along the
Tobol River. The eamplings at Grishenka were taken during periods when the
discharge of the river was 32 times its annual average; the 16 samplings
at Kustanfei when the discharge was 12 times its yearly average; and the 22
samp1ie4s at Kurgan when the discharge was 3.3 times the yearly average.
The sun of the ions in parte per million was 294 at Grishenka, 866 at
Kestanay ,and 738 at Inrgan. In this area, as along the Ob River, the
aaximum concentration of mineralu occurs during periods of low water, and
the minimum concentration during high water.
The total hardness of the water for the Tobol River is much higher than
that of the Ob'. At Kustanay on the Tobol the hardness of water is about
445 parts per million, whereas at Novosibirsk on the Ob' River the hardness
is 127 parts per 'million.
3. Tobol River Tributaries
Along the Iset' River, average annual and monthly discharge
values are given for 7 stations. The annual discharge increases from
4.95 m3/sec. at Sverdlovsk to 80.3 m3/sec. at Isetskoyo, 631 and 117
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kilometers above the mouth of the river, respectively. High water occurs
in May as far downstream as Bobrovakoye. Along the remaining downstream
section of the Zest' River, April is the month of peak discharge. Low water
occurs during August at Sverdlovsk at the head of the river, during
December along the middle course, and during January and February on the
lower course,.
On the Techa River, a tributary of the Iset' River, the average yearly
discharge increases from 2.12 m3/sec. at BrodoItalmalc, 125 kilometers from
the mouth, to 12.8 m3/sec. at Perehinsk.oye, 26 kilometers above the mouth.
April is the month of high water and January the month of low water.
The Neyva River flows into the Bits& River, which in turn is a tributary
of the Tura River. Along the Neyva-Nitsa the annual discharge increases
from 8.81 m3/sec. at Chereashanka on the Neyva to 44.1 m3/sec. at Irbit on the
Nitea. High water occurs in April and May and low water during the period
from December to March.
The average annual discharge of the Tura River increases from 27.2 m3/sec.
at Verkhotur 'ye, 706 kilometers upstream, to 178 m3/sec. at Tyumen', 175
kilometers above the mouth of the river. On the Tura River, May is the month
of high water and. February the month of low water.
Dams located on the Tura and IVeyva Rivers tend to equalize the flow of
the two rivers. The peak spring flaw is used to build up the water supp4 in
the reservoir. This water is later released to regulate the operating
discharge through the low-water period or winter.
On the Neyva River, a series of dams hap been built above the city of
Alapayevsk to maintain the flow of the river at an even level along the
remainder of its course. The record of discharge for the Neyva River at
Alapayevsk, as given in Table 2, is based on older records taken before
these dams were built.
The estimated discharge values at Verkhotur'ye on the Tura River were
based. on the regulating effect of dams on the headwater section of the river.
M the Verkhotursk hydroelectric installation the controlled discharge is
14.6 m3/sec.
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The chemical composition of the water of the Wool River tributaries
is indicated by eamplinge taken at. 6 points on the Iset?, Techa, Neyva,
Ritsa, and Tara Rivers. The data for these stations are presented on
Table 3.
The total amount of minerals found in the water of the Tobol River
tributaries is much lower than that of the Tobol River proper. At
Tarinsk on the Tara River, the sum of the ions is 176 parts per million as
compared with 738 parts per million at Knrgan on the Tobol River. The total
hardness of the water of the tributaries is also much lower. At Volkoma on
the 'set the total hardness is 139 parts per million, as contrasted with
326 parts per million at Enrgan on the Tobol River.
B. The Oka River System
The Oka River system, which has a drainage area of 245,000 spare
kilometers, is located in the central part of European USSR. In this
investigation, the Oka River and its tributaries, the NOkeha, the Protva,
the Moskva, and the Elyaz'ma Rivers are discussed.
The location of these rivers as well as the stations along their courses
are indicated =Kap 2. Table 4 lists the stations and their locations,
along with the available hydrological data. Table 5 gives the average
monthly and yearly discharge values for rivers in the Oka River system.
The chemical compositon of the water is Shown in Table 6.
1. Oka River
The Oka River has its source at about latitude 52?2041 and longitude
36010? and from there follows an irregular course northward and then
northeastward. At about 56?2o,N-440p0?a the river empties into the Volga.
The Oka River has a length of 10480 kilometers and a drainage area of
2450000 avers kilometers.
The average annual discharge of the Oka River increases from 20.1 10/sec.
at Orel to 936 m73/sec. at Hurom The greatest average discharge occurs in
April. The lowest average discharge occurs in januery near the source of
tho river and in February from Kaihira downstream to the mouth of the river.
The chemicel composition of the water of the Oka River is repreeented
by samplingc taken along it course at 3 points: (1) near the mouth of the
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Frotva River, (2) above the mouth of the Moskva River, and (3) 20 kilometers
above the point where the Oka River empties into the Volga. These samplings
are given in average, maximum, and minimum values. The dissolved solids are
listed as dry residue measured at 1100C.
The chemical analyses of water of the Oka River indicate that the
mineral content decreases from the source to the mouth. The average amount
of dry residue drops from 295.2 parts per million at Drakino to 259.6 parts
per million at Protopopovo. The concentration of calcium and magnesium also
decreases downstream from Drakino. The total hardness of water decreases from
263 parts per million at Drakino to 224 parts per million at Novirilei.
2. Oka River Tributaries
The discharge records of the Oka River tributaries, which were made ,
prior to 1931, are listed as monthly and yearly values for 6 stations, 4 of
which are located on the Moskva River and 2 on the Klyatzma River.
The estimated discharge values of the MIAs River shown on Table 4 are
based on known average yearly discharge values for all selected stations and
a record of the monthly discharges at Mbkraya Polyana for the period from
April to Devember.
Discharge values are given for 4 stations along the Meskva River.
The average ennual discharge increases from 9., m3/sec. at Mozhaysk to 58.6
m3/sec. at Babgegorodek Dam in the city of Moscow. The discharge is highest
in April. Lowest average discharge occurs in January on the headwaters of
the river and in February from Zvenigorod downstream.
For the Xlyaema River, the major tributary of the Oka River, discharge
records are available for only 2 stations--Favlovskiy Pelted, neer Gorodok2
and Ussoll? 423 kilometers above the mouth of the Klyaema River. The
monthly discharges for the stations of Vladimir and Kovrov were estimated.
April is the month of high water and February of low water. This monthly
flow pattern is characteristic of the entire Oka River system. The discharge
in lowest dien the rivers are frozen over apd run-off is at a minimum.
Maximum discharge, on the other hand, occurs when the ground thaws and the
ice breaks up.
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The chemical composition of the water of the Oka River tributaries is
indicated by samplings taken at 3 stations on the Moskva River, 3 on the
Elyaz'ma River, and 1 on the ProtVa River. Estimates of the chemical
composition of the waters of the 01,e, and Moskva Rivers ere also
derived by averaging a number of samplings taken at various points along
each of the rivers. The Meskva River samples were taken at RUblevo, at
Tatorovo, and in Moscces at Moskvoretsiy. Bridge where samples were taken for
nearly every month of the year during 1926. In the figures for the
chemical composition of the water )f the lilyaz'ma River, based on 6 samplinge
taken at 3 points alreng the river, ealcium and magnesium are listed together.
When the cherecal composition eel' the water of the Oka River tributaries
is compared with that of the Oka River proper, several generalizations can be
made..., The concentratioi of minerals In the water of the tributaries,
particularly the sulfate concentratio&? is much lower than that of the Oka
River. The total water hardness of the tributaries is also considerably
lower than that of the Oka River prop4r. Finally, the concentration of
mineral eonstitutents in the tributaries, like that of the mein river,
decreases from the sources to the mouths.
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Table 1
LOCATION OF STATIONS AND INDICATED BYLEOLOGICALDATA FOR OS' RIVER SYSTEM
Station
River Nb.
II
It
if
It
? Tobol
It
'set'
Techa
It
Neyva
Nitsa
Tura
Pt
ft
I'
It
Station
Name
1 Barnaul
2 Shelabolikha
3 Kamen*,-na-Obi
Novosibirsk
5 Kozhevnikovo
6 Grishenka
7 Kustanay
8 Ust*-Uyskoye
Zverinogolovskoye
10- Kurgan
11 Ust'-Suerskoye
12 Yalutorovsk
13 Ievlevo
14 Lipovka
15 Sverdlovsk
16 Bobrovskoye
17 Temnovskoye
18 Volkovo
19 Dalmatovo
20 Nbkhonskoye
21 Isetskoye
22 Brodokalmak
23 Pershinskoye
24 Cheremshanka
25 Alapayevsk
26 Xrbit
27 Verkhotur'ye
28 Bolotova
29 Turinak
30 UStr-Nitsa
31 Tyumen'
Coordinates
N.Latz-E.Lonqz.
-Distance late
from Mouth of Chemical
in KM... Discharm a/ 2920.pition
53?19'-83?19. 3,429
3,290
3,164
55?004-82057, 2,955
56015,-24000, 2,768
52?23,-61?434 1,395
53!12'-63!38' 1,203
54w164-63w584 1,003
540284-640524 891
55026,-650234 708
56?02,-65?50,
56?414-669214
57?35,-67?09,
57?494.67?244
56?504-60?37,
56?404-60?584
56,7,-61?33'
56-224-62?024
56?15,-62?56,
56009, _64034 ,
029 .6 502 ,
55?35 ? -62?o6'
56?061-62?45*
57?44t-60?410
57?52'.61?42*
57?40'.63005.
58050 , .60047 ,
58?32'.62?6'
58?04f-6324V
57?571.64w30'
5701044,0321
530251..820401
53?47 * -81?22'
575
416
137
103
631
593
529
452
368
205
117
125
26
139
64
183
706
555
30
238
179
iperels...*.mat*
Est.
Est.
Est.
Est.
Eat.
X
Eat,
Est.
Est.
a. "x" indicates that the information is available; "Est." indicates an estimated rate.
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Table 2
AVERAGE MONTHLY AND YEARLY DISCHARGE VALUES FOR OW RIVER asmix
t
River
???11?.......1?Cgo
Station
No.
station
Yrs.
of
Record
Dischar...e in Cubic Meters
r Second
Jan
Feb
Mar
Apr
Jun
Jul
12-M
Em
Oct
Nov
Dec
Yearly
Ob
Barnaul
27
302
271
266*
1,949
3,453
3,598**
2,457
1,691
1,235
12001
596
366
1,440
2
3
Sbelabolikba ej
Kamenf-na-Obi
42
320
331
270
280
230*
237*
1,370
1,425
3,810**
3,966**
3,570
3,718
2,500
2,602
1,630
1,704
1,115
1,164
915
953
530
554
390
408
1,365
1,420
4
Novosibirsk
56
392
334
315*
1,880
5,170**
4,260
3,030
2,020
1,440
1,160
698
483
1,760
It
Tobol
5
6
Kozkevnikovo 2/
Grisbenka
6
395
0.0*
337
0.0*
319*
13.4
2,170
173**
5,310**
4.99
4,300
1.65
3,050
0.97
2,030
0.78
1,450
0.54
1,180
0.56
707
1.15
487
0.69
1,810
19.1
7
Kustamay
15
1.0
0.83*
1.80
192**
33.7
6.81
3.71
3.78
2,78
2.89
2.65
1.53
22.8
8
Ustl-Uyskoye
1.2
1.0*
2.2
234**
41.0
8.5
4.5
4.5
3.4
3.5
3.2
1.9
27.8
9
Zverinogolovskoye
a/
3.6
2.9*
4.1
79.2
194**
55.5
14.3
15.0
10.3
9.8
9.0
4.1
33.5
10
Kurgan
30
4.3
3.81*
3.85
140
264**
53.6
18.7
15.9
13.6
12.2
10.5
6.7
47.7
11
Ustt-Suerskoye
4.3
3.9*
3.9*
141
267**
54.0
19.0
16.0
13.7
12.3
10.6
6.8
48.2
12
Yalutorovsk
40
23.1
22.1*
23.0
204
494**
211
72.6
61.8
46.3
42.7
32.8
25.4
101
13
Ievlevo
24
45.3
44.5*
45.9
180
1,041
1,406**
505
231
165
112
56
48.6
291
14
Lipovka
47
151
128
125*
515
20441
2,560**
1,622
849
618
519
346
222
810
iset'
15
Sverdlovsk
9
3.45
3.83
4.15
4.91
9.70
5.77
3.54
3.30*
3.87
4.56
4.81
4.53
4.95
16
Bobrovskoye
4
16.5
13.2
13.4
18.4
25.1**
14.0
11.1
8.9
12.2
8.84
5.82
4.51*
12.5
17
Temnovskoye
5
3.40
4.06
6.05
15.7
10.5
5.93
4.74
4.14
4.31
3.60
3.11*
5.91
18
Volkovo
15
5.06
4.69*
5.39
61.7**
32.0
17.2
16.2
15.3
12.8
10.4
7.43
5.52
16.2
to
to
19
rie).
CA.
21
Dalmatovo
Mekbonskoye
Isetskoye
8
13
10
3.08
18,6
17.0*
2.91*
17.7*
17,5
4.93
18.5
19.6
68.7**
293**
2724.1**
22.4
193
207
19.0
66.4
63.1
15.0
48.3
51.5
12.8
54.7
55.6
10.0
40.4
44.8
8.48
39.6
48.6
8.01
31.1
39.8
4.25
22.2
23.0
14.8
79.0
80.3
Techa
22
Brodokalmak
1
0.33*
0.94
0.41
5.94**
2.80
2.11
2.75
3.83
2.40
1.51
2.05
0.47
2.12
23
Pershinskoye
9
3.15*
3.59
3.79
28.8
13.6
11.6
9.56
8.93
10.7
8.22
3.16
12.8
Neyva
24
Cheremsbanka
11
2.88
3.53
4.09
29.2**
17.7
9.09
8.07
8.67
7.58
6.80
5.28
2.87*
8.81
25
Alapayevsk
6
5.07
4.46
4.04*
32.5**
29.9
16.8
12.1
10.9
10.1
9.05
6.99
5.41
9.85
Nitsa
26
Irbit
56
11.6*
11.6*
10.8
147
154**
55.4
36.4
29.9
25.9
21.2
15.1
12.3
44.1
Tura
27
28
Verkhotur'ye
Volotova y
11.0
15,0
10.0*
13.0*
10.0*
13.0*
30
140
90**
415**
50.0
215
26.o
130
23.0
95.0
20.0
90.0
17.0
70.0
14.0
40.0
12.0
20.0
27.2
105
T-rinsh
16.5
14.4*
14.5
1A2
1!76**
248
148
1ce-
102
82.8
42.9
92.0
120
30
Ust'-Nitsa
26.0
25.0*
27.0
220
665**
410
190
130
105
95.0
65.0
37.0
165
31
Tyumen'
55
27,4
27,1*
28.7
232
707**
437
204
138
112
100.0
68.9
39.3
178
a. All except the yearly values are estimated.
*Minimum,
**Maximum.
Approved For Release 2006/03/0E.: GIA-RDP79-01009A001200020004-3
S-E-C
 '4.10.11axesseVeneValo..0...elmeerft,
Af.ver
Sta.
No.
Station
..e.aasarMagalumtrason6.441C1h...-.......
No.
of
Samples
Ob'
1
Barnaul
6
;;
4
Novosibirsk
56
Tobol
Griebenka
2
9
7
Fustanay
16
10
Kurgan
22
18
Volkovo
11
20
Mekhonskoye
4
MPO/IA
Pormllinkozp
5
?
Max,
Min.
17Ma'
x.
Min.
tv, , 28,6
Max. 30.0--Apr
Min, 27.1--Apr
1A.,v'114.8
Max, 214.3--Dec
Min. 22.8--Apr
Av, 71,5
Max. 121.9--0..;:t
Min. 28.2--Apr
cv. 37.5
Max. 63.2--Apr
25.1--Apr
Approved For Release 2006/03/06 :.CIA-RDP79-01009A001200020004-3
E-C
Table 3
Cimmicai.. COMPOSITION OF WATERS OF OB' RIVER SYSTEM
Chemical ion in Parts
Calcium Magnesium Sodium Potassium Bicarbonate
Ca Mg avIC MO'
Million
Sulfate
Chloride
Ci
23?5
38,0--May
17.0--May
37.7
76.0--Mar
24.0--Aug
7.3
10.8--May
5.0--May
8.o
16.2--Nov
1.0--May
7.4
15.3--3une
1.0--Sept
9.2
37-5--July
0.2--Apr
91
128.0 --May
49,1--May
152.1
323.3--Pov
40.8--Sept
18.7
33.6--May
6.6--Sept
10.6
20.6--Mar
June
3.3--Apr
b. 7
13.0--May
4,95
15.3--July
Max,
Min,
pMv.
iax.
(gin,
12,0
13.1--Apr
10.9--Apr
38.6
64,6-mar
5.6--Apr
36,7
9,8.4--Mar
11;1
21,4--Apr
4.0--Apr
4449 15,0
64.1--Dec 23.6--Sept
19.9--May 4.4--May
41.7 13,2
5A.:6--5.1mpt
19.9 - -Apr
21:3-.4pr
56--Apr
, 12
S-E-C-R-E-T
48.9
78.0--Apr
1948--Apr
112.4
234,5--Mar
3.0--jbne
104,8
225.0--Aug
16.2--Apr
27.0
66,5-:-
7.8--Apr
Sept.
20.5
32.3--Dec
9,2--Sept
88
21
3,8--Apr
977
120.4--Apr
75.3--Apr
211.6
273.2--Apr
60.2--Aur
249.6
402.6--Mar
98.8--Apr
i6o,4
232.0--Apr
A9.4--Apr
169.3
232,4--Dec
72.0--May
155.0
244.1,--Apr
67.1--Apr
Approved For Release 2006/03/06 : CIA-RDP79-01009A001200020004-3
Total
pardness
88,5
140--May
63.0--May
127
242--Mar
70-June
Aug
30,8
15.7
121
40.3--Apr
102,6.-Apr
129--Apr
21.3--Apr
48,7--Apr
113--Apr
140.9
253,9
445.0
305. 2--My
517.5--Dec
790--Dec
33.7--Mar
15.6--A-or
80--Apr
143.9
131.0
326
244.0--Mar
17.6,-Oct
28.5
4y,2--Apr
16.3--June
/.f
60.4--Dec
25.7--May
27,8
37,3--Apr
20,4--Sept
2073--Mar
36.7--Apr
21,5
41,0--Apr
10,0--May
25.6
35.5--Dec
14.3
17.3-Apr
8.9--Apr
530--Mar
140--Apr
139.0
246--Apr
92--May
174
239--Dec
68--May
159
218--A-11
73--Apr
Approved For Release 2006/03/06 : CIA-RDP79-01009A001200020004-3
Table 3 (Cont.)
CHEMICAL COMPOSITION OP WATERS OF OB' RIPER SYSTEM
Kir.
Max,
Min.
{
Max.
Min.
tv,
Max.
Min.
Chemical Compos,ition in Parta per Million
Sodium Potassium Bicarbonate Sulfave
MAC HCO3 SOIL
River
Sta.
No.
24
26
29
Station
Ho.
of
Samples
el
Hardness
Calcium -----Ragnesium
Ca m4,
Neyva
Rites,
Tura
Cheremsban-tca
Irbit
Turinsk
6
42
42
29.9 12.4
36.5-Sept 15.8-Sept
19.3--May 10.1-May
29.0 10.0
52.2-Mar 19.0-Aar
13.7--May 3,5-Apr
26.2 8.2
64.3-Feb 18.7.-Feb
7.2-Aay 2.2--June
5.7
7.3-4301;
4.0,-Sept
4.9
9,5.-Sept
0.5-Aay
8.4
27.2-Aar
87,4
96.6.-Sept
67.1-May
104.3
170.8.-Sept
146.4-Aar
92.9
262.3--Feb
18.3--May
52.3
61.4-Sept
35.0--May
29.3
82.1-Mar
11.0-May
27.0
86.2--Mar
Feb
9,0--June
7.6
10.0-Sept
6.1--Sept
5.4
12.0-Mar
0.9--Apr
11.2
26.8--Aug
1.5--June
126
150-Sept
90--May
114
208-Aar
52-May
106
238--Feb
31-May
-
S-E-C-R-E-T
Approved For Release 2006/03/06 : CIA-RDP79-01009A001200020004-3
Approved For Release 20063/67861:(.6AT-RDP79-01009A001200020004-3
Table 4
LOCATION OF STATIONS AND INDICATED EYDROLOG/CAL DATA FOR OI, RIVER SYSTEM
vaeObsamossr....M1*** nwo Ige.*.ften.wft.O.V.......,+.140Mr.....nenr
River
Oka
ft
ft
It
11
ft
If
f1
ft
ft
ft
Moksha
It
ft
Protva
MoskYa
If
If
11
ft
It
Klyaz*ma
ft
TI
ft
It
Sta.
No. Station
????????s???-?ae tat, oed Imo
12 Orel
33 Lichvin
34 Kalnga
35 Drakino
36 Kashira
37 Protopopovo
38 Shthurovo
39 Polovskoye
40 Kasimov
41 Mnram
Novinki
Mokraya
?olyana
Warovchat
2emnikov
Spas-Zagorsk
Mozhaysk
Zvetigorod
Rub) evo
Paythino
Babiegorodsk
Dam
Moskvoretsiy
- Bridge
51 Mchelkovo
54 4spenskoye
55 Pavlovskiy Posad
near Gorodok
56 Mad
57 Vladimir
58 Kovrov-
I, 3
45
46
I, 7
48
49
51
Distance
Coordinates from
1buth in K*1.
5P?58'.36004*
54?06,-36016'
54 030 * .36?16*
54051' -37?17
54050 *-38?10'
55O3 -38?.6
55?04'.38?51*
54?28 *-40?13'
54056 6 mict.,1324. 6
55035fW42Cb4t
?12 -43053'
53?34'.44c23'
53?92'.43?44,
51..?38' .243?:L1
I
55,?,05-
55-30 .36?811
55?431'36?51*
55?46'467?211
559481.37?221
550451_374335,
55?44* -37?38
55o.w.3800121
55?52'-33?30'
55?47 -38?42 '
55?52l-39!98*
56 cb7*- 40-25*
55 ?23*-41?.L.8*
1,450
1,256
1,171
1,050
986
919
915
704
442
232
20
570
465
200
70
387
295
241
236
188
176
516
490
468
423
276
165
Rate
of Chemical
?Discharge logposition
Est.
Est.
Est.
Est.
Est.
Est.
Est.
Est.
=
Est.
Est.
oreon
amsubwerouralarorrotosonmenasas
a. "x" indicates that the information is available; "Est," indicates an estitiated rate.
S-E-C-R-E-T
Approved For Release 2006/03/06 : CIA-RDP79-01009A001200020004-3
Sta.
River No.
Ststior
Oka 32 Orel
33 Lichvin 2/
34 Ealugla
1Casblra.
38 Shanrovo 2/
39 Poltvekoye 2/
4o Kasimov 2/
41 MUrom
Moksha 43 . Marva
Polyana
44 Varovcbat 2/
45 Temnikov 2/
Protva 46 Spas-Zagorsk 2/
Moskva 47 Mozhaysk
te 48 Zvenigorod
50 Pavsbino
51 Bab'egorodsk
Dam
Klyaz'ma 55 Pavlovskiy Posad
near Gorodok
56 Dsad
57 Vladimir 2/
58 Kovrov 2/
ft
ci
Ti
.1.?????emtommemmonomf
Yrs.
of.
Record
Approved For Release 2006103/06 :6IA-RDP79-01009A001200020004-3
S-E-C-110E-T
Table 5
AVERAGE MOW= AND YEARLY DISCHARGE VALUES IVR OKA RIVER SYSTEM
1,11????,*,,Of
tkibie Meters Seconi
Feb Mar Apr Sul Sept Oct No Dec Yearly
44 5.7* 8.3 40.8 118.2** 17.9 9.3 9.3 6.6 6.3 7.3 8.3 5.9 20.1
45* 50 185 725** 160 70 65 50 45 55 65 6o 130
44 114 117 378 1,717** 429 169 163 124 112* 132 166 159 312
5-46 114 95* 308 2,407** 717 236 220 180 164 191 248 189 391
125 105* 340 20650** 790 260 230 195 180 205 260 200 430
128 112* 211 20530** 11035 275 240 200 185 210 265 205 463
235 210* 260 20700** 2,635 470 360 295 280 290 310 265 700
50 312 282* 350 3,603** 3,516 625 481 394 370 389 412 350 936
0.5a 1.0 5 110** 25 4 3 5 4 4 2 1.0 IA
1.0* 2.0 13 275** 60 10 8 11 10 10 5 3 34
4.0 3.0* 20 440a* 100 15 14 15 16 16 8 4 55.4
3-5* 4.0 7.5 100** 25 11 4.5 4.0 5.0 9.5 15 3.5 16.9
13 2.1* 2.3 4.6 62.9** 14.7 6.6 2.8 2.5 3.2 6.0 9.1 2.3 9.5
12 8.5 7.8* 14.2 166.7** 52.4 16.5 11.0 10.1 9.2 17.8 28.6 12.2 28.2
13 13 11* 19 246** 77 23 16 14 17 29 37 20 43
4 13.0 10.7* 23.3 355.8** 75.8 57.8 24.6 30.8 33.4 21.8 41.8 14.5 58.6
9 8.0 6.4* 10.7 197.7** 76.1 23.3 18.7 14.5 16.4 24.2 39.2 i1.2 37.5
5 23.0 21.4* 27.8 166.5** 106.3 27.3 26.5 24.2 34.0 43.8 73.3 32.8 53.7
31 28* 40 225** 145 37 36 32 46 60 100 43 75
65 55* 80 450** 290 75 70 65 90 120 200 75 148 12/
a. All except the yearly values are estimsted.
0. Based on run-off values.
*Minimum.
**Maximum.
- 15 -
S-E-C-11-E-T
Approved For Release 2006/03/06 : CIA-RDP79-01009A001200020004-3
Approved For Release 200e/MetaRDP79-01009A001200020004-3
_Table 6
OBENECAL COMPOSMION oF tiATVIs OF OKA arnE SYSTEM
?
River
Sta.
No.
Station
No.
of
Sanples
.
. .
Chemical C
sition in Parte r Million
Dry
Residue
Calcium
Ca
Magnesium
m4
Iron
Fe
Sodium
Potassium
Na4K
Bicarbonate
Sulfate
Chloride
Cl
Nitrate
KO3
Total
Hardness
n22_222
--
Drakino
(v
295.2
77.1
17.1
139.1
41.9
2.6
1.43
263
Oka
35
above mouth
- Max.
354.8
93.5
19.9
155.8
53.8
3.7
4.6
315
of Protr.. R.
- Min.
237.7
65.06
12.13
100.2
26.3
1.5
?0.0
214
259.6
69.5
16.3
223.9
29.9
2.6
1.37
240
VI
37
Protopojovo
4AV
Max.
347.6
90.4
20.5
107.4
45.2
4.0
5.18
310
. Min.
105 2
.22.7
7,8
89,4
6.4
0.4
0.0
89
184
66.3
8.9
1.14
224
IT
42
Novinki
{Av.
Max.
261.7
99.6
12.6
11..5
320
' Min.
54
7.2
3.2
0.0
62
Near
Near Drakino
Av.
259.5
69.7
18.2
155.8
6.84
2.6
0.89
251
Protva
35
on
Max,
{
309.0
86.o
19.7
168.9
8.76
3.4
4.60
314
Protva River
230.6
57.5
14.7
124.3
4.68
1.3
0.00
223
Mozhaysk
Moskva
47
at
Ar.
238
62.2
20.3
261.7
5.9
2.1
0.3
239
Marfin Ford
Av.
227.2
61.5
14,2
23.0
250.7
5.6
2.3
1.21
213.6
6.4
49
Rublevo
Max.
/
319.0
92.8
21.0
363,9
8.2
5.0
4.06
307,9
19.6
Moskboretsiy
Min.
Av.
51.6
267.9
11.4
64.3
2.2
14.2
43.6
250.7
0.8
17.8
0.7
8.9
0.0
37.4
220
14.0
Protva
52
Bridge
11
Max.
{
356.7
84.0
18.8
333,2
34.0
14.5
288
26.8
Min.
85.2
34.2
6.6
134,8
5.0
3.5
120
0.0
Klyazima
53
Shchelknvo
,-,
c
x.
17Ma*
Min.
237.6
268
207.2
79.8
79.8
78.7
209.2
244.0
174.5
11.6
1.1.3
10.9
6.3
7.5
5.0
1.3
2.6
0.0
180
216
145
73.3
189.4
8.5
2.3
163
54
Uspenskoye
2
(v.
Max.
228
84.0
202.5
12.6
9.0
11-51
173
62.7
176.3
7.9
0.13
150
Pavlovskiy
Av.
65.5
169.8
5.4
02
144
Moskva
55
Posad near
Gorodok
Entire Course
2
:54
Max.
i min.
Av.
206
242
61.5
78,o
53.1
13,9
178.7
161.0
246.3
12.6
10.3
5.9
5.0
)4.8
1,50
0.09
148
139
210
10.5
Oka
Entire Course
14
Av
306
71.5
16.9
0,19
215.8
43.7
5.4
2.4
245
ftft TWOR.FTWOOft
Approved For Release 2006/0.43/126:?1A-RDP79-01009A001200020004-3
S