Baikeng Lake, which originated in Xikeng of Daba Town, entered Baikeng Lake after passing through the dam and Wuduiyang, and was diverted from Wuduiyang at 1972. Cut the spillway along the newly-opened dam to Huibaikeng Lake in Jilongshan, and the Guangnan water enters Lianjiang, Hui Hui, with a length of 12.24 km and a catchment area of 88.4 1 km2. Baikeng Lake is located in front of Baikeng Village in the upper reaches of Baikeng Lake. At the end of Qing dynasty, the lake area was about 2000 mu. After liberation, the water level dropped and the lake surface shrank. 1970, the lake is only about 800 mu. 1970- 1972, the dam commune organized the lakeside farmers to fill the lake again.
Baimaxi, starting from Wangtianding of Da Nan Shan, flows into Lianjiang through Sankeng, Shishi Yangpi, Xiangyuankeng Xishe, Beitou and Liu Ying, with a total length of 23.2 kilometers. The original catchment area is 100 km2, and the catchment area of quicksand drainage trough (neutralization) and downstream reach is 8 1.53 km2 after being cut straight and separated by fences. The upstream slope of water is steep, and water is abundant. There are 2 medium-sized reservoirs and 2 small (I) reservoirs. Hydropower has been developed, with a total installed capacity of 5840 kilowatts.
Tangkeng Creek originates from Dagutan, Nanshan, passes through Tangkeng, Junbu and Shiqiaotou, and flows into Lianjiang at Shigangshan, with a length of 22.7 kilometers and a catchment area of 65.25 square kilometers. There are 2 medium-sized reservoirs and 4 hydropower stations in the upstream water source area, with a total installed capacity of 3630 kilowatts.
The flowing water cut to the west is cut along the south slope of Tieshan Mountain. Small tributaries such as Dakoukou, Beishanshui, Yuxi Water, Longqiu Water, Longqiu Dongshui and Xiaobeishanshui enter Lianjiang River at the toe of the stream, which is a flood retaining river artificially excavated after liberation.
Beigang water originates from Beikeng in Qilin Town and flows through Shuijing, Nanpi and New Southwest. At Longmen Village, it joins Nanjing Water, flows from the east of Huanglong Village through Chaoyang County and flows into Lianjiang, with a flow length of 15km and a catchment area of108.74km2. There are small (I) reservoirs 168 upstream water source pits. The tributaries flowing into Chaoyang District are:
Jinxi, formerly known as Simapu Water or Lin Jinzhu Water. Originating at the peak of Da Nan Shan, it flows through Chendian Xikou and flows into Lianjiang with a flow of 18.7km and a drainage area of 84. 1 km2.
Li Peishui, which originates from the west side of Jiashenling, Nanshan Mountain, flows through Li Pei Village from south to north, flows into Lianjiang River through Xiaokeng, Longxi, Zhangbache and Xiweizhu, with a flow of 17. 1 km and a drainage area of 30. 14 km2.
Liang Ying, called Taoxi in ancient times, is also called gongs and drums water because of the gongs and drums waterfall in the upper reaches. It flows through Liang Ying and is called autumn wind water. Originated in salt ridge, Nanshan, it is the largest tributary of Lianjiang with a drainage area of 168.438+02 square kilometers.
Hongkou Lushui originates from the east side of Wufengjian in Da Nan Shan and flows northward through Lushui Village in Hongkou. It flows to the east of Shibeijiao, where the wind blows, Jianwei and Huihe River meet in the west, and flows into the Turtle Head Sea at Bangang Gate, with a flow of 18.5km and a drainage area of 74.27km2. ..
Daliaoshui, formerly known as Chengtianshui. Originated in the north of Niuguling Mountain in Da Nan Shan, it flows through Shi Die and Dong Zhe, Dou Xian, joins Spider Pushui in Gangtou and crosses Yanting Lake in Xiqi and Ninghu. Named after leaving the Daliao Gate and entering the glans Sea, the flow rate is 18.78km, and the drainage area is 44km2.
Longxi originates from Guanmangping on the east side of Leiling Peak in Nanshan Mountain, and is named after the upstream leading waterfall, with a flow of 25. 1 km and a drainage area of102.6km2..
Hualin water, which originates at the northern foot of Yangyongding in the east of Da Nan Shan, flows northeast through Hualin Village named after it, and then flows to Tian Xin and Beiyang, where it joins the port water and flows out of the glans Sea, with a flow of 8. 15km and a drainage area of 9.8km2 ..
Guiyushui, formerly known as Gui Jiang. Originating from Shezai Cemetery on Puning South Road in Xiaobei Mountain, it turns to the east of Longmen Village from west to east, and reaches the vicinity of Liao Jun in Chaoyang City (county) in the south. It joins with Xieyao Water, another tributary of Chaoyang (originating from the south slope of Dajianshan, passing through Fushan and Shanlipu in the southeast, and passing through Nanyang to Liao Jun in the southwest), and reaches Yujiao Lianjiang in Guiyu in the south, with a flow rate of 17.4km and a drainage area of 65438+.
Lianshui River Basin, a tributary of Lianjiang River. It was called Xianbei water in ancient times. There are many tributaries in the upper reaches. The main stream originates at the southern foot of Pengqing Paishan in Xiaobei Shandong, flows through Shuihou Waterfall to the west, joins Jingmen, Jilongshan and Jingjiao to the south, joins Sanhe, Lingshan and Guraoxi near Xinxing Village, and joins the middle reaches of Lianjiang at Shenshanzai, with a flow of 24. 1km and a drainage area of 128.
Lianbei Water was called Xifeng Water in ancient times. Originating from the Mausoleum of Lucuo in Xiaobei Mountain, it flows westward to Lianbei Village and joins Lianjiang River, with a flow of 6.8km and a drainage area of 13km2.
Roaring water originates from Xiaobei Mountain and Heping Mountain, passes through Shuihoukeng Bridge of Hong (Yang) and Ping (Ping) Highway in the west, and joins Lianjiang River at the end of Guheping Bridge, with a flow of 2.6 kilometers and a drainage area of 3 square kilometers.
Taihe Water originates from the north side of Shuangji Mountain in Xiaobei Mountain, flows through Goumian Village in the west and crosses Taihe Bridge on Guangshan Highway in the south. The lower reaches were called "water-lifting port" in ancient times, which was named after boat people and people from Heping and other places came here to "carry water by boat". Water flows into Lianjiang River between Gao Feng and Baishi, with a flow of 8km and a drainage area of12km2.
Qiligang water, which originated at the southern foot of Shuangji Mountain, is named after Qiligang Bridge on the north side of Guangshan Highway, with a flow of 7.6 kilometers and a drainage area of 10.62 square kilometers.
Dongyanshui originates in Dongshan, flows through Dongyanshui in the south, turns to the southwest, flows out of Fenggang Bridge and flows into the glans Sea, with a flow of 6 kilometers and a drainage area of 12 square kilometers.
Qianxi, south of the east gate bridge of the moat, flows from Fengdu in the northeast to the confluence of the moat and culvert, with a flow of 7 kilometers and a drainage area of 1 1 square kilometer.
Haimenkeng water originates from the mountain in the pit and flows out of Lianjiang River via Haimen Harmony Bridge in the west, with a flow of 3 kilometers and a drainage area of 4 square kilometers.