H
Brief Description |
The source of this river lies in the
Kanglung Kang Glacier near the Kailash range of The catchment area of the river falls in four countries.
Although the main river does not flow through the
The The southern ( In
The culturable area of the basin is 12.15 M-ha which is 6.2% of the culturable area of the country. | |||||||||||
Stream Network |
The numbers represents average flow in cumec. | |||||||||||
Drainage Area of the Basin |
Name of
State |
Drainage
area (in Km2) | ||||||||||
Arunachal Pradesh |
81,600
| |||||||||||
|
70,700
| |||||||||||
Meghalaya |
11,800 | |||||||||||
Nagaland |
10,900
| |||||||||||
|
7,300 | |||||||||||
|
12,700
| |||||||||||
Total
Drainage Area of the Basin (in Km2) |
195,000 | |||||||||||
Topography |
The | |||||||||||
Nature of Topography |
Area under Topography (sq. km) |
Geographical Location | ||||||||||
High Tibetan Plateau |
293,000 |
Southern Part of the
| ||||||||||
High Himalayan
mountains |
137,050 |
Part of Himalayan
| ||||||||||
|
56,200 |
Part of
| ||||||||||
Lower ( |
37,200 |
Part of 3 states of
| ||||||||||
Plains |
56,550 |
Part of the 2 plains
districts of | ||||||||||
Coastal Region |
Negligible |
Coastal region of
| ||||||||||
Water potential |
Surface
Water potential (Km3) |
537.2 | ||||||||||
Ground
Water potential (Km3) |
27.9 | |||||||||||
Total
Water potential in the basin (Km3) |
565.1 | |||||||||||
Hydropower Potential |
The hydroelectric potential of the Brahmaputra basin has been assessed 66065 MW. Out of the identified schemes in the basin , schemes with a total installed capacity of 2120 MW are in operation as on 31.7.2014 and schemes with an installed capacity of about 5592 MW are in various stages of construction. (Source: www.cea.nic.in). The status as on 2010 is given below: | |||||||||||
Sub-basin wise estimated hydro potential of | ||||||||||||
Basin/Rivers |
No. of schemes identified
|
Potential at 60% load factor (MW) | ||||||||||
Dihang-Dibang |
28 |
13,615 | ||||||||||
Lohit |
11 |
4,152 | ||||||||||
Subansiri |
25 |
6,893 | ||||||||||
|
19 |
789 | ||||||||||
Kameng |
34 |
1,982 | ||||||||||
Kalang (Kopili) |
16 |
510 | ||||||||||
Teesta |
30 |
3,021 | ||||||||||
|
03 |
50 | ||||||||||
Barak and neighboring
rivers |
60 |
3,908 | ||||||||||
Total |
226 |
34,920 | ||||||||||
Water
Utilization |
Surface
Water Utilization |
Drinking purposes | ||||||||||
Irrigation purposes | ||||||||||||
Ground
Water Utilization |
Drinking purposes | |||||||||||
Irrigation purposes | ||||||||||||
Tributaries with drainage area in sq. km. |
Name of the Tributary |
Drainage area (Km2) | ||||||||||
Jiadhol |
77.3 | |||||||||||
Subansiri |
4.3 | |||||||||||
Ranganadi |
23.8 | |||||||||||
Borgong |
36.4 | |||||||||||
Jia-Bharali |
28.1 | |||||||||||
Gabharu |
80.7 | |||||||||||
Belsiri |
75.4 | |||||||||||
Dhansiri (N) |
65.2 | |||||||||||
Noa-nadi |
81.4 | |||||||||||
Nonoi |
76.2 | |||||||||||
Barnadi |
82.8 | |||||||||||
Puthimari |
66.6 | |||||||||||
Pagladiya |
75.8 | |||||||||||
Manas |
14.1 | |||||||||||
Champamati |
86.8 | |||||||||||
Gaurang |
81.5 | |||||||||||
Tipkai |
90.2 | |||||||||||
Sankosh |
7.6 | |||||||||||
Doyang | ||||||||||||
Water
Quality of Basin |
The major ion chemistry of the
Surface suspended sediments range from
fine sand to clay, the size fraction greater than 12
mm constituting an important size population. Surface suspended
sediments are moderately to poorly sorted with
greater amounts of finer material in the distribution, particularly during
the rainy season. The detrital contribution in
the form of Quartz, Feldspar and Mica make up more than 80% of the
mineralogy. Chlorite, Illite, and Kaolinite constitute about 95% of the clay minerals.
Sediment chemistry does not reveal any
marked spatial or temporal variation. However, spatial variation in the
metal/aluminum ratio in some cases has been observed. This may be
attributed to continuous addition of freshly eroded materials by a large
number of tributaries at different points of the main stem. Since there is
hardly any major industry in the catchment area
and the amounts of sediment carried by the tributaries are enormous, there
is not enough ground to link any occasional rise in metal concentration to
any point source.
The major sources of carbon in the
Suspended sediments play a significant
role on the overall solute and sediment biogeochemistry of the river. The
biogeochemistry of | |||||||||||
Mythology |
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