Why is the water clear and the water muddy How to explain it geographically

Weishui flows from Gansu Wurat Mountain through Shaanxi into the Yellow River, and the land of Qinchuan is the Guanzhong Plain and 800 miles of Qinchuan; The whole process of Jingshui flows through the Loess Plateau, which is an area with serious soil erosion. As far as the sediment content of the river water is concerned, it should be greater than that of Weishui. According to statistics, the Jing River currently transports an average of 100 million tons of sediment to the Wei River every year, with an average sediment content of 196 kilograms per cubic meter. Before it was included in the Jing River, the Wei River transported an average of 100 million tons of sediment per year, with an average sediment content of kilograms per cubic meter.

Judging by the numbers, it is still turbid, especially in the dry season. However, in modern times, due to human activities in the Weihe River Basin, especially in the upper reaches of the river, the environment has been seriously damaged, and soil erosion is also an important problem. Due to the mineral content of the soil in the area where the Wei River flows, when the sediment content of the Wei River reaches 10 kilograms per cubic meter, the water color becomes reddish-yellow.

On the surface, the natural landscape of Jingshui is still distinct, but the color of Weishui is darker than that of Jingshui.

The Wei River makes the tributaries of the Yellow River, so it is turbid. Jingshui is a tributary of the Wei River, and it is much clearer when compared to him.

The Jing River and the Wei River are two very different rivers. The Jing River originates at the eastern foot of Liupan Mountain in southern Ningxia, flows southeast through Gansu, and enters the Wei River in Gaoling County, Shaanxi. The Wei River is the largest tributary of the Yellow River, which originates in the Bird and Mouse Mountain in Weiyuan County, Gansu Province, flows eastward across the Weihe Plain in Shaanxi, and enters the Yellow River in Tongguan County. The water of the Jing River is very clear, while the water of the Wei River is very turbid, and there is a very obvious boundary at the confluence of the two rivers in Gaoling, which has become a peculiar landscape with a clear distinction between Jing and Wei.

Whether the river is clear or not has a lot to do with the area it flows through.

Summary. Hello, this is because the Wei River is a tributary of the Yellow River, so it is a yellow river, and the Jing River is an ordinary river, so it is clear water.

Why is the water clear and the water muddy?

Hello, this is because the Wei River is a tributary of the Yellow River, so it is a yellow river, and the Jing River is an ordinary river, so it is clear water.

The famous Jingwei River is located at the confluence of the Jingwei River, which is the largest tributary of the Yellow River, and the Jing River is the largest tributary of the Wei River.

The clear distinction between Jing and Wei refers to the difference in the degree of turbidity between Jing water and Wei water.

The Jing River and the Wei River are both major rivers in the Yellow River Basin, which mainly flow through the Shaanxi region. The Wei River is the largest tributary of the Yellow River, and the Jing River is the largest tributary of the Wei River, when the Jing River and the Wei River meet in Gaoling District, Xi'an City, due to the different sediment content of the two rivers, it presents a peculiar landscape of one clear and one turbid, and the clear water and turbid water flow with each other and the river does not blend with each other, so the scene of Jing and Wei is clearly distinguished.

The Wei River is the largest tributary of the Yellow River, and the Jing River is the largest tributary of the Wei River, and the Jing River and the Wei River meet in Lupei Gaoling District, Xi'an City. When the water of the Jing River flows into the Wei River, it is clear and turbid, so it presents the phenomenon of one clear and one turbidity, and people call this phenomenon the distinction between Jing and Wei.

The formation of this phenomenon is mainly due to the fact that the sediment content of the Jing River and the Wei River is different, and a relatively obvious boundary is formed after the intersection of the two.

The geographical reason for the clear distinction between Jing and Wei is mainly due to the different sediment content of the Jing River and the Wei River.

The Jing River is the largest tributary of the Wei River, which flows through the Loess Plateau, which has long been an area with serious soil erosion. Therefore, the sediment content of the Jing River is relatively high. When the water of the Jing River flows into the Wei River, it is clear and unmixed, forming a clear landscape of Jing and Wei.

Jing"Refers to the Jing River, located in Shaanxi Province, China, and is a tributary of the Yellow River.

Wei"It refers to the Wei River, which is also in Shaanxi Province and is also a tributary of the Yellow River.

The two rivers meet in the city of Weinan in Shaanxi Province, but their water quality, color and nature are very different. The Jing River is clear and cool, the Wei River is turbid and warm, and their confluence is very noticeable and there is no mixing. Therefore,"The distinction is clear"This idiom is used as a metaphor for things or boundaries that are very clear and there is no confusion.

This idiom is often used to describe a person's personality, boundaries, interfaces, etc., emphasizing clarity and distinctness, and is not easy to confuse or mix.

<> is the Wei River referred to in the picture.

and Jing River. In ancient times, the small river was not called a river, but water, so it was called Weishui. Jingshui.

The names of these two rivers are actually the names of the two rivers. The name of one river is Weishui, and the name of the other is Jinshui. These two rivers are the last to meet each other, and the idiom clearly comes from this situation.

They refer to the Wei River and the Jing River, respectively, that is, "Jing Wei is distinct".

The Wei River is the largest tributary of the Yellow River, originating in Gansu and flowing into the Yellow River through Shaanxi. The Jing River is also a tributary of the Shenlao Luwei River, which originates in Ningxia. The two waters meet in Gaoling District, Xi'an City.

The well-known idiom of "Jing Wei is clear", that is, the source of the swim is the confluence of the two rivers of Jing and Wei. It is said that at the intersection of Jingshui and Weishui, the turbidity is clear, and the boundary is clear and does not contain base mixture, which is used as a metaphor for clear boundaries.

The effects of historical climate evolution are possible.

In ancient times, the water of these two rivers was different from today.

The average annual runoff of the Wei River is 100 million cubic meters, and that of Shaanxi is 100 million cubic meters. The regional distribution of runoff was uneven, and the general trend was to decrease from south to north, with a high in the Qinling Mountains and Guanshan Mountains, and a low in the original and valley areas. The western part is larger than the eastern part of the country, and the midstream is richer than the downstream runoff. The runoff modulus of the northern slope of the Qinling Mountains is high, which is 9 15 liters per square kilometer, while the runoff modulus in the loess plain area is only one liter second per square kilometer, and only the runoff modulus of Qianhe is higher, and the runoff modulus of Qianyang Station is higher than that of liters per square kilometer.

The runoff modulus of the main stream of the Weihe River is litres per second square kilometer, and the Weijiapu and Xianyang stations are higher, which is caused by the addition of tributaries.

It can be clearly seen from the runoff depth contour map that the runoff depth on the northern slope of the Qinling Mountains increases with the increase of mountain elevation, from less than 100 mm to more than 600 mm, and the highest centers are in Taibai Mountain and South Wutai Mountain. The alluvial plain of the Weihe River is very flat, with a high degree of water conservancy, and belongs to the low-yield area.