Nizhnyaya Tunguska
The Nizhnyaya Tunguska is a river in Siberia, Russia, that flows through the Irkutsk Oblast and the Krasnoyarsk Krai. The river is a :wikt:right bank|right tributary of the Yenisey joining it at Turukhansk. Settlements on the river include Tura, Yukti and Simenga. The ice-free period on the Nizhnyaya Tunguska starts in mid-June and ends in the first half of October. The river forms the western limit of the Lena Plateau.
Hydrography
The Nizhnyaya Tunguska is the second largest right tributary of the Yenisey, and joins it near the town of Turukhansk. It is long, and has a drainage basin of. According to the character of the stream, constitution of the river's valley and its shores, it can be divided into two parts: the first one starts at the source of the river and continues down to the village Preobrazhenskoye and the second section of the river lies downstream of this village in a canyon-like relief.Upper stream
The upper part of Nizhnyaya Tunguska is long and follows a wide valley with flat slopes that was formed by sand and clay deposits. The speed of flow at rafts reaches and drops significantly as the river's channel stretches.This section of river has a meandering channel that closely approaches the Lena, another great Siberian river. The minimum distance between them is as short as in the neighbourhood of Kirensk town. All of the upper course of Nizhnyaya Tunguska is within the Irkutsk Oblast.
Lower stream
Downstream of Preobrazhenskoye village the Lower Tunguska flows across the Tunguska Plateau of the Central Siberian Plateau in a narrow and deep valley with high, often rocky shores. The entire landscape here has volcanic origins, the relief alters the flow of Nizhnyaya Tunguska into a westerly direction. The river channel frequently has lake-like widenings with lengths up to and longer. The locations with close approaches of crystalline layers create numerous rapids on the river. The most significant of them have names such as: "Sakko", "Vivinskiy", "Uchamsky" and "Bolshoy". The rapids on the river has relatively high speeds of water flux reaching. In some places downstream of the rapids the river channel becomes very deep with maximum depths of. In the river's lowest flow, downstream of join with its tributary river Severnaya, Nizhnyaya Tunguska runs between limestone rocks, which steeply rise from the water. The speeds of flow here grow to.The channel and water flow of the river's lower stream has its own distinguishing features, which can be seen in some places at Nizhnyaya Tunguska, including the following:
- The strips of stones with sizes, which stretch near water along the shore line. This peculiar feature of Arctic stony rivers with the local name "bechevnick" is formed during every period of ice drift and river inundation at spring. At some locations these sorts of pebbles are polished and pressed together to the extent that they create a cobbled road of their own kind.
- The slopes of the river canyon during its evolution underwent stone avalanches that formed stone runs of individual rocks as big as in diameter. These slide-slopes have a local name, korga, and create zones of calm backwater downstream.
- The stream in the channel of the Lower Tunguska sometimes forms whirlpools. They originate downstream of cliffs which channels flow to the opposite shore. These whirlpools can reach depths to and occur most often during high-water periods in early summer.
Tributaries
On the whole, the right tributaries of Nizhnyaya Tunguska dominate over the left and add more water. The river has no big lakes in its basin; the biggest is Vivi with a surface area of. Inflows to the Nizhnyaya Tunguska are strongly seasonal.
Hydrology
The value of average water discharge of Nizhnyaya Tunguska gives it eleventh place amongst largest rivers of Russia. The annual water discharge at the river's mouth is equal to. The minimum value observed in 1967 was ; the maximum was in 1974 or, respectively, for the estuary of the river it was about and about. The water supply of the river is from melting snow and summer rains. During winter season Nizhnyaya Tunguska contains little water as its basin lies in the region of permafrost and it has no subterranean water sources. According hydrological observations during 52 years, the minimum average monthly discharge was in March 1969—it was exceptionally dry winter—and the maximum value corresponds to June 1959 and was The diagram below contains mean values of monthly average discharges calculated on the base of a 52-year-long period of observations at hydrological station "Bolshoy Porog".Colors=
id:lightgrey value:gray
id:darkgrey value:gray
id:sfondo value:rgb
id:barra value:rgb
ImageSize = width:600 height:280
PlotArea = left:40 bottom:40 top:20 right:20
DateFormat = x.y
Period = from:0 till:20000
TimeAxis = orientation:vertical
AlignBars = justify
ScaleMajor = gridcolor:lightgrey increment:4000 start:0
ScaleMinor = gridcolor:lightgrey increment:2000 start:0
BackgroundColors = canvas:sfondo
BarData=
bar:Jan text:Jan.
bar:Fév text:Feb.
bar:Mar text:Mar.
bar:Avr text:Apr.
bar:Mai text:May
bar:Jun text:Jun.
bar:Jul text:Jul.
bar:Aoû text:Aug.
bar:Sep text:Sep.
bar:Oct text:Oct.
bar:Nov text:Nov.
bar:Déc text:Dec.
PlotData=
color:barra width:30 align:left
bar:Jan from:0 till: 313
bar:Fév from:0 till: 237
bar:Mar from:0 till: 197
bar:Avr from:0 till: 195
bar:Mai from:0 till: 6567
bar:Jun from:0 till: 19330
bar:Jul from:0 till: 5024
bar:Aoû from:0 till: 2902
bar:Sep from:0 till: 3286
bar:Oct from:0 till: 1729
bar:Nov from:0 till: 608
bar:Déc from:0 till: 459
PlotData=
bar:Jan at: 313 fontsize:S text: 313 shift:
bar:Fév at: 237 fontsize:S text: 237 shift:
bar:Mar at: 197 fontsize:S text: 197 shift:
bar:Avr at: 195 fontsize:S text: 195 shift:
bar:Mai at: 6567 fontsize:S text: 6.567 shift:
bar:Jun at: 19330 fontsize:S text: 19.330 shift:
bar:Jul at: 5024 fontsize:S text: 5.024 shift:
bar:Aoû at: 2902 fontsize:S text: 2.902 shift:
bar:Sep at: 3286 fontsize:S text: 3.286 shift:
bar:Oct at: 1729 fontsize:S text: 1.729 shift:
bar:Nov at: 608 fontsize:S text: 608 shift:
bar:Déc at: 459 fontsize:S text: 459 shift:
Seventy-three per cent of the entire annual water yield occurs during the spring–summer season. The amplitude of the water-level variations in the lower stream of Nizhnyaya Tunguska is the highest among all notable rivers of Russia. At narrow places in the river channel, ice jams during its seasonal drift, and this creates temporary dams that block normal water flow and raise water levels up to above the mean value. The summer break-up and drifting of ice passes very violently; it leaves traces in the form of torn-apart uprooted trees and polished rocks. During some days of spring freshets the river's discharge can peak at, and it supplies 50 to 60 per cent of the water volume to the lower stream of the Yenisey in the time of its seasonal inundation.
Economy
The channel of Nizhnyaya Tunguska with its tributaries constitutes dense network of rivers and creeks which creates convenient summer pathways through the wide rifted valley of Eastern Siberia. Historically, the river was used as a route for the fur trade, fishery, for transportation of goods and mineral resources. Hunting and fur trade is still a significant part of the local economy.Shipping
Navigation on the river is difficult because of a number of rifts, rapids and whirlpools. The passage of large ships and barges is possible during the spring inundation, and rainy weather during particular years allows short periods of navigation at the end of summer or the start of autumn. The most problematic for the safe navigation of ships are the rapids "Bolshoy", which are from the river's mouth. In 1927 the first steamship passed this rapids and it is considered to be the start of modern navigation on the river from Turukhansk to Tura. As of 2010 the shipping routes of Yenisey River Steamship Lines includes the village Kislokan, from the estuary. Timber rafting is possible throughout entire course of the river.It was suggested in 1911 to build a canal joining the Lena and Nizhnyaya Tunguska rivers in the neighbourhood of Kirensk. Near this locality the rivers are separated by no more than , but here the Nizhnyaya Tunguska is not navigable and flows at an elevation of above sea level, whereas the Lena flows at an elevation of. In the beginning of 20th century the canal project was considered inexpedient due to its complexity and high cost.
Planned damming
Plans to dam the river existed since the early Soviet period. These plans were the subject of criticism by various ecologists. Construction of the dams also became impossible after disintegration of Soviet Union due to economic reasons. In 2005–10 the interest to this project and the discussion of it revived to some extent. According news media the construction of the Turukhanskaya hydroelectric powerplant would begin as soon as in 2010. Since the precise date is unknown, a more likely start-up is between 2010 and 2020.After completion of this project the Lower Tunguska River will be dammed, flooding about of forest and tundra, some of which contains buried nuclear waste, and displacing the indigenous Evenk population. The cost of the plant is estimated at $13 billion dollars, which includes costs of electric power lines. The plant will be built and operated by RusHydro in the Krasnoyarsk region, and the electricity will be channeled to European Russia via a system of power lines.
Notable facts
- The colonisation history of Western Siberia by Russians since 17th and 18th centuries was reflected in various names for the river at different times. At some periods it was called Troitskaya Tunguska, Monastyrskaya Tunguska and Mangaseyan Tunguska.
- In literature, the river Nizhnyaya Tunguska is described in the novel Sullen river by Vyacheslav Shishkov. This writer of the first half of the 20th century visited the river during an expedition in 1911; the name Sullen river was taken from a Siberian song.
- Existing sources indicate that the annual average discharge of water at mouth of its tributary Severnaya is equal to. As this river joins Lower Tunguska downstream of hydrological station "Bolshoy Porog" it means that the known average discharge at mouth of Lower Tunguska is significantly underestimated. It must be in the range of.