Overview of the basin of the Taoer River, the birthplace of the Taoer River

Tao River is an important tributary of the upper reaches of the Yellow River system, originating in the Xilian Mountains of Henan Mongolian Autonomous County in Qinghai Province, and flowing eastward through Luqu, Lintan and Zhuoni County, to Minxian County.

The tea port turns sharply to the northwest, out of the Jiudian Gorge and Haidian Gorge, through Lintao.

Basin, which flows into the Liujiaxia Reservoir in Yongjing County. It has a total length of 673 kilometers and a basin area of 10,000 square kilometers.

The average annual flow of Goumen Village Station is 172 cubic meters per second, and the annual runoff is 5.3 billion cubic meters, accounting for more than 75 in May and October, providing abundant water resources for central Gansu. The main tributaries are Zhouke River, Kecaiku River, Reukhe, Xiabagou, Chebagou, Truck Ditch, Dayugou, Diezang River, Yangsha River, Yemu River, Nanchuan River, Dongyu River, Sancha River and Guangtong River. Above Haidian Gorge is the upper reaches, with many soil and rocks and high mountains, and the west of Luqu belongs to the mountain plain grassland, which is a natural pasture; The east bank of Luqu is densely wooded, produces a small amount of timber, has farmland in the wide valley, and has excellent dam sites in the canyon, which is conducive to water diversion and power generation.

The lower reaches of Haidian Gorge belong to the Loess Plateau.

The irrigation agriculture in the Lintao Basin is developed, with 4 reservoirs of more than one million cubic meters, and the irrigation land of Taohui, Puji, Tongguang, Linkang and other channels is more than 10,000 mu, and the agricultural products are abundant.

It is the largest tributary on the right bank of the Nenjiang River of the Taoer River. It is located in the northwest of Jilin Province, China. It originates from Gaoyue Mountain at the southeast foot of the Arshan Mountains in the Great Xing'an Mountains of Inner Mongolia.

It is formed by the collection of 10 small rivers of various sizes. The southeast flows through Keyouqian Banner, Taonan City, Zhentai County, injects the moon bubble in the north of Da'an City, and then flows into the Nenjiang River. It is 553 kilometers long and has a basin area of 10,000 square kilometers.

It flows from northwest to southeast to Ulanhot and joins the Guiliu River, and then to Tao'an County, Jilin Province, and then joins the Guiliu River and turns to the northeast to flow into the Nenjiang River. The valley of the Taoer River is wide and flat, and the ratio of the decline is larger, about, but to the Taonan Plain, the ratio of the decline plummets. The average flow rate of the station for many years can reach more than 1,700 cubic meters per second, and the average flow at the estuary is 50 cubic meters per second, with a total runoff of about 1.6 billion cubic meters.

It is a river fed by snowfall in winter and spring and heavy rain in summer and autumn. The freezing period can be up to 4-5 months.

The middle and upper reaches flow through the mountainous areas of the Inner Mongolia Autonomous Region, from Chaersen through Gegenmiao to the Longhuatu section of Baicheng City, the precipitation is concentrated in July and September every year, flash floods occur, the rivers carry a large amount of sediment, fill the river channels, and the cultivated land along the downstream is often threatened by floods. Below the west of the town enters the plain, the river channel widens, the flow speed slows down, the river meanders develop, and there are more tidal areas. The following of Taonan is the downstream section, sand dunes and sand hills, low-lying land and marshland are widely distributed, there are many rivers and willow shrubs on both banks, when the flood rises, the river water comes out of the trough, the ocean is a piece, and the moon soaks in the water surface to become a piece.

The upstream has abundant hydraulic resources. There is a diversion of Taojihuo (Lin River) project in the downstream. Note:

Now the Taoer River is already full of holes, there is no water source, only the sand at the bottom of the river remains, the wind comes, the dust does not see the day, the nearby residents live hard, the land is seriously desertified, and the shrubs no longer exist. Due to the upstream interception, there has been no water for several years, especially in winter, and there is no ice. We need everyone to speak out for governance!

It's miserable! Man destroys nature!

In the western part of Jilin Province, more than 30 million mu (about 2 million hectares) of grassland have been salinized and sandy, and the desertification area has reached more than 10 million mu (about 10,000 hectares), and it is still expanding at an average annual rate. In the western part of the Songnen Plain, a large area of salinization in the lower reaches of the Nenjiang River is expanding eastward, and the Xianghai Reservoir, the wetland water source of China's famous red-crowned crane nature reserve, has shrunk by nearly 2 3 compared with the area surveyed and mapped in 1980.

The birthplace of Taoer River: Jiudaogou of the White Wolf Forestry Bureau of Gaoyue Mountain, at the southeast foot of the Arshan Mountains in the Daxing'an Mountains of Inner Mongolia.

Taoer River is the largest tributary on the right bank of the Nenjiang River. It is located in the territory of Xing'an League in Inner Mongolia, China and the northwest of Jilin Province. It originates from Jiudaogou of the White Wolf Forestry Bureau of Gaoyue Mountain, southeast foot of Arshan Mountain, Daxing'an Mountains, Inner Mongolia.

It is formed by the collection of 10 small rivers of various sizes. It flows southeast through Keyouqian Banner, Ulanhot City, Taonan City, Zhentai County, injects a moon bubble in the north of Da'an City, and then flows into the Nenjiang River. It is 553 kilometers long and has a basin area of 10,000 square kilometers.

It flows from northwest to southeast to Ulanhot to converge on the Guiliu River, and turns to the northeast to flow into the Nenjiang River in Taonan City, Jilin Province.

The Tao River originates from Leerdang, at the eastern foot of the west-dipping mountain in the territory of Hainan Mongolian Autonomous County, Qinghai Province.

The Tao River is the largest tributary of the upper reaches of the Yellow River. It originates from Qinghai Province and flows into Gansu Province through the western foothills of Luqu County. In total, the basin passed through Gannan, Dingxi, Linxia and other places.

It flows into the Yellow River upstream of the Liujiaxia Reservoir Dam. The main stream is 673 kilometers long and has a basin area of 25,527 square kilometers.

The Tao River not only plays a great role in the irrigation projects of the areas through which it flows, but also promotes the development of tourism in the relevant areas, and also provides abundant resources for the development of hydropower.

There are two mountains next to each other on the northeast side of Gaoyue Mountain in the Great Khing'an Mountains, forming a wedge-shaped valley, and the strands of mountain springs seeping out from the grass roots and fallen leaves gather to the bottom of the valley to flow into a small stream, which is said to be a tributary of the Nenjiang River - the source of the Taoer River (unverified).

Maqu, the source of the Tao River, is located in Gannan Tibetan Autonomous Prefecture, Gansu Province. It flows from southwest to northeast.

The Tao River originates in the eastern foothills of the West Dip Mountain in Hainan Tibetan Autonomous Prefecture, Qinghai Province, and flows into the Liujiaxia Reservoir Area of the Yellow River in Yongjing County, Gansu Province.

Tao River is 673 kilometers long, the basin area is 25,527 square kilometers, according to the statistics of the Goumen Village Hydrological Station, the average annual runoff is 5.3 billion cubic meters, the annual sediment transport volume is 100 million tons, the average sediment content is only kilograms per cubic meter, and the water is more and less sand. The Tao River, known as Luqu (meaning spring flowing from the palace of the Dragon King) in Tibetan, is a large tributary on the right bank of the upper reaches of the Yellow River.

Among the tributaries of the Yellow River, the Tao River ranks second only to the Wei River in terms of annual water volume. The runoff modulus is 10,000 cubic meters per square kilometer, second only to the Baihe River and the Heihe River, and is the tributary with the largest amount of water in the upper reaches of the Yellow River.

Originated in Xitian Mountain, Henan Mongolian Autonomous County, Qinghai Province, I hope it will help you.

Tao River is an important tributary of the upper reaches of the Yellow River system, originating in the Xiqian Mountain Bar of Henan Mongolian Autonomous County, Huangnan Prefecture, Qinghai Province

Explanation of Tao River.

1).The name of the water. in the southwest of gansu province .

2).Borrowed from Tao Yan . Niu Xiudankai, "Yao Yu Shi Yan", quoted by Pan Lei, "Jiatang Fu":

Duanxi inkstone is also suitable for the pen, not left behind, the operation is not sluggish, the ink is full of solid Tian, and the ink is exhausted and ......Bitao River and Rock Rock, no one dares to compete with them. See also " Tao Yan ".

Word decomposition Explanation of Tao á washing. Ancient Tong "Tao", wash away impurities. Radical :

San; Explanation of river River é A common name for a watercourse: a river channel. River ditch.

River valley. Rivers. Beach.

Riverside. River fresh (fresh river fish, river shrimp, etc. for consumption). River port.

River bend. River. River.

Hu Chi Hu Nei River. Refers specifically to the Yellow River in China: the Hetao.

River defense. Finger pants block "Milky Way": Tianhe.

Ha Han . Radical: 氵.

Henan Mongolian Autonomous County, Huangnan Tibetan Autonomous Prefecture, Qinghai Province, is at the eastern foot of the mountain. Tao River Tibetan language called Luqu, ancient name Luoshui, is the upper reaches of the Yellow River on the right bank of the first major Xinhe tributary, from west to east in Gansu Province Min County in the territory of the north flow, end in Yongjing County into the Yellow River Liujiaxia Reservoir, Tao River basin east to bird and mouse mountain, horse bit mountain and Wei River, Zuli River water division, west to Zhagaliang and Daxia River as the boundary, north of the Yellow River mainstream, south to the west of the Qinling Mountains and Bailongjiang River as the boundary. With a total length of 673 kilometers and a basin area of 25,527 square kilometers, the average annual runoff is 5.3 billion cubic meters, the annual sediment transport volume is 100 million tons, and the average sediment content is only kilograms per cubic meter.

When it flows through the Loess Plateau in Longxi, it carries a large amount of sediment and is relatively turbid.

Tao River, located in the south of Gansu Province, China, is the first major tributary of the upper reaches of the Yellow River, originating in the territory of Henan Mongolian Autonomous County, Qinghai Province, the western foothills of the eastern foothills of Leerdang, this section of the river is called Daifu Sangqu, in the western part of Luqu County, Gansu Province, the western foothills of the western slopes of the eastern foothills flow into Gansu Province. The Taohe River Basin covers Henan Mongolian Autonomous County in Huangnan Tibetan Autonomous Prefecture in Qinghai Province, Luqu County, Lintan County, Zhuoni County, Xiahe County, Cooperative City and Diebe County in Gannan Tibetan Autonomous Prefecture in Gansu Province, Hezheng County, Guanghe County, Dongxiang Autonomous County, Kangle County and Yongjing County in Linxia Hui Autonomous Prefecture, and Minxian, Weiyuan County and Lintao County in Dingxi City, a total of 15 counties. It flows into the Yellow River upstream of the Liujiaxia Reservoir Dam in Yongjing County, Linxia Hui Autonomous Prefecture.

The main stream is 673 kilometers long and has a basin area of 25,527 square kilometers. The elevation of the source of the Tao River is 4260 meters, the elevation of the estuary is 1629 meters, and the drop is 2631 meters. The average annual flow of Goumen Village Station is 172 cubic meters, with an annual runoff of 5.3 billion cubic meters.

The total amount of self-produced water resources is 100 million cubic meters. 5 October accounted for more than 75%, and the sliding cover faction provided abundant water resources for central Gansu.

Henan Mongolian Autonomous County, Huangnan Tibetan Autonomous Prefecture, Qinghai Province, is at the eastern foot of the mountain. Tao River Tibetan language called Luqu, ancient name Luoshui, is the first major tributary of the upper right bank of the Yellow River, from west to east in Gansu Province Min County to the north flow, end in Yongjing County into the Yellow River Liujiaxia Reservoir, Tao River basin east to bird and mouse mountain, horse bit mountain and Wei River, Zuli River water division, west to Zhagaliang and Daxia River as the boundary, north of the main stream of the Huangyinhan River, south to the west of the Qinling Mountains and Bailongjiang River as the boundary. <

Henan Mongolian Autonomous County, Huangnan Tibetan Autonomous Prefecture, Qinghai Province, is at the eastern foot of the mountain. Tao River Tibetan language called Luqu, ancient name Luoshui, is the first major tributary of the right bank of the upper reaches of the Yellow River, from west to east in Gansu Province Min County in the territory of the north flow, end in Yongjing County into the Yellow River Liujiaxia Reservoir, Tao River basin east to Bird Mouse Mountain, Horse Bit Mountain and Wei River, Zuli River divide water, west to Zhagaliang and Daxia River as the boundary, north of the Yellow River mainstream, south to the west of the Qinling Mountains and Bailongjiang River as the boundary. With a total length of 673 kilometers and a basin area of 25,527 square kilometers, the average annual runoff is 5.3 billion cubic meters according to the statistics of the Goumen Village Hydrological Station, and the annual sediment transport volume is 100 million tons, and the average sediment content is only kilograms per cubic meter.

When it flows through the Loess Plateau in Longxi, it carries a large amount of sediment and is relatively turbid.