全长6387千米!
长江干流自西而东横贯中国中部,位于东经90°33′~122°25′,北纬24°30′~35°45′之间。
长江 发源于“世界屋脊”——青藏高原的唐古拉山脉各拉丹冬峰西南侧。
干流流经青海省、西藏自治区、四川省、云南省、重庆市、湖北省、湖南省、江西省、安徽省、江苏省、上海市共11个省级行政区(八省二市一区),于崇明岛以东注入东海,全长6387公里,在世界大河中长度仅次于非洲的尼罗河和南美洲的亚马孙河,居世界第三位。
长江源由北源楚玛尔河,南河当曲和正源沱沱河组成,楚玛尔河发源于可可西里自然保护区深处的可可西里湖,藏语意为“红水河”,全长约515公里,流量小,夏季经常断源,最后流入长江上游的通天河。
长江干流宜昌市以上为上游,长4504千米,占长江全长的70.4%,控制流域面积100万平方千米。宜宾市以上称金沙江,长3464千米,落差约5100m,约占全江落差的95%,河床比降大,滩多流急,加入的主要支流有雅砻江;宜宾至宜昌长1040千米,加入的主要支流,北岸有岷江、嘉陵江,南岸有乌江。
宜昌市至湖口县为中游,长955千米,流域面积68万平方千米,本段加入的主要支流,南岸有清江及洞庭湖水系的湘、资、沅、澧等四水和鄱阳湖水系的赣、抚、信、修、饶等五水,
北岸有汉江,本段自枝城至城陵矶为著名的荆江,南岸有松滋、太平、藕池、调弦(已堵塞)四口分水和洞庭湖、水道最为复杂。下游湖口县至出海口为下游,长938千米,面积12万平方公里,加入的主要支流有南岸的青弋江、水阳江水系、太湖水系和北岸的巢湖水系。
江阴以下为长江河口段,全长约200千米,呈喇叭形。长江口潮汐属非正规浅海半日周期,平均一个周期为12小时25分,平均潮差4.62m。平均总进潮量洪季大潮53亿m,枯季小潮13亿m。长江的潮流界汛期至江阴,枯季可达镇江;潮区界汛期至大通,枯季可达安庆。
经过1300多年的变迁,口门处已形成面积达1083千米2的崇明岛。崇明岛将长江分为北支和南支。北支正在逐渐淤浅萎缩。南支是长江径流下泄的主要水道。
南支在吴淞口附近由长兴岛分成南港和北港,南港又被九段沙分为南槽和北槽。南槽原是长江主泓道,但“近年”主泓道已逐渐转向北槽。长江口入海航道的滩顶水深一般在6m左右。不足10m水深的滩长,北港约40千米,南港约64千米。
长江流域有人口约4亿人,占全国1/3,其中农业人口约3.2亿人。在流域总人口中,约94%为汉族;还有50多个少数民族,2000余万人,其中超过100万人的有土家、苗、彝、侗、藏、回等6个民族,各少数民族主要居住在云贵高原、青藏高原、川西、湘西和鄂西一带。
The total length is 6,387 kilometers!
The main stream of the Yangtze River runs across central China from west to east, located between 90°33′~122°25′ east longitude and 24°30′~35°45′ north latitude.
The Yangtze River originates from the southwest side of the Geladandong Peak of the Tanggula Mountains on the Qinghai-Tibet Plateau, the "Roof of the World".
The main stream flows through 11 provincial administrative regions (eight provinces, two cities and one district) including Qinghai Province, Tibet Autonomous Region, Sichuan Province, Yunnan Province, Chongqing City, Hubei Province, Hunan Province, Jiangxi Province, Anhui Province, Jiangsu Province and Shanghai City, and flows into the East China Sea east of Chongming Island. The total length is 6,387 kilometers, which is the third longest river in the world, second only to the Nile River in Africa and the Amazon River in South America.
The source of the Yangtze River is composed of the northern source Chumaer River, the southern river Dangqu and the main source Tuotuo River. The Chumaer River originates from the Kekexili Lake deep in the Kekexili Nature Reserve. It means "Red Water River" in Tibetan. It is about 515 kilometers long, with a small flow. It often stops flowing in summer and finally flows into the Tongtian River in the upper reaches of the Yangtze River.
The main stream of the Yangtze River is above Yichang City, which is 4,504 kilometers long, accounting for 70.4% of the total length of the Yangtze River, and controls a basin area of 1 million square kilometers. The Jinsha River above Yibin City is 3,464 kilometers long, with a drop of about 5,100 meters, accounting for about 95% of the drop of the whole river. The riverbed has a large gradient, many beaches and rapid currents. The main tributaries joining it are the Yalong River; Yibin to Yichang is 1,040 kilometers long, and the main tributaries joining it are the Minjiang River and Jialing River on the north bank and the Wujiang River on the south bank.
The middle reaches of the river are from Yichang City to Hukou County, with a length of 955 kilometers and a drainage area of 680,000 square kilometers. The main tributaries added to this section are the Qingjiang River and the four rivers of Xiang, Zi, Yuan and Li in the Dongting Lake system and the five rivers of Gan, Fu, Xin, Xiu and Rao in the Poyang Lake system on the south bank.
The Hanjiang River is on the north bank. This section from Zhicheng to Chenglingji is the famous Jingjiang River. On the south bank, there are the four water diversions of Songzi, Taiping, Ouchi and Diaoxian (blocked) and Dongting Lake, and the waterway is the most complex. The downstream from Hukou County to the estuary is the downstream, with a length of 938 kilometers and an area of 120,000 square kilometers. The main tributaries added are the Qingyi River, Shuiyang River system, Taihu Lake system on the south bank and Chaohu Lake system on the north bank.
The section below Jiangyin is the estuary of the Yangtze River, with a total length of about 200 kilometers and a trumpet shape. The tides at the Yangtze River Estuary are irregular shallow sea semi-daily cycles, with an average cycle of 12 hours and 25 minutes, and an average tidal range of 4.62 meters. The average total tidal volume is 5.3 billion m3 in the flood season and 1.3 billion m3 in the dry season. The tidal boundary of the Yangtze River reaches Jiangyin during the flood season and Zhenjiang during the dry season; the tidal boundary reaches Datong during the flood season and Anqing during the dry season.
After more than 1,300 years of changes, Chongming Island with an area of 1,083 square kilometers has been formed at the mouth. Chongming Island divides the Yangtze River into the North Branch and the South Branch. The North Branch is gradually silting up and shrinking. The South Branch is the main waterway for the Yangtze River runoff to flow down.
The South Branch is divided into South Port and North Port by Changxing Island near Wusongkou, and the South Port is divided into South Channel and North Channel by Jiuduansha. The South Channel was originally the main channel of the Yangtze River, but in recent years, the main channel has gradually turned to the North Channel. The beach top water depth of the Yangtze River estuary channel is generally about 6 meters. The length of the beach with a depth of less than 10m is about 40 kilometers in the north port and about 64 kilometers in the south port.
The population of the Yangtze River Basin is about 400 million, accounting for 1/3 of the country, of which about 320 million are agricultural population. Of the total population in the basin, about 94% are Han; there are more than 50 ethnic minorities, more than 20 million people, of which more than 1 million are Tujia, Miao, Yi, Dong, Tibetan, Hui and other 6 ethnic groups. The ethnic minorities mainly live in the Yunnan-Guizhou Plateau, Qinghai-Tibet Plateau, western Sichuan, western Hunan and western Hubei.