Denggan River is an important tributary of Dongliao River. Originating from the north of Shifeng Village, Yishan Township, Dongliao County, the source of the river is 367 meters above sea level. From the source to the southwest, it flows through Yishan Town and Anshi Town to the south of Weiguo Village in Shoushan Town, and flows into the Dongliao River. It has a total length of 31km, a drainage area of ??280.8km2, a maximum water level of 282.56cm, and a sand content of 3.23kg/m3. The river slope is 3.03‰. The average annual runoff volume is 36.05 million cubic meters, the annual average runoff depth is 109.2 mm, and the annual average runoff module is 3.4 sec/km2.
The Erdao River, a tributary of the Dongliao River, originates from Renxian Dongling, Beilong Village, Shihe Township, Dongliao County. It flows westward from the source through Jian'an Township, and joins the Sandao River in the West Garden of Zhongxin Township. The village flows into the Dongliao River. The total length is 38.2km, the drainage area is 191.8km2, the sand content is 11.5kg per cubic meter, the total drop is 164.7m, and the river channel ratio is 2.1‰. The average annual runoff volume is 2.07 million cubic meters, the annual average runoff depth is 108.5 mm, and the annual average runoff module is 3.4 sec/km2.
The Gongzhuling River belongs to the Dongliao River system. It is formed by the intersection of three erosion ditches in the central and western part of Gongzhuling City: the Inland River, the Weizigou River, and the West Weizigou River. It divides Gongzhuling City into Henan and Hebei. . From southeast to northwest, it flows into the Dongliao River through the urban area and is an important tributary of the middle and upper reaches of the Dongliao River.
Gushan River, also known as Beida River, is a large tributary on the right side of the upper reaches of Dongliao River. It originates from the southeast of Liujiayuan, Xiwei Township, Yitong County, and flows northwest, from Hongwei Village, Xiwei Township to the junction of Dagushan Town. It is the boundary river between Yitong County, Siping City and Dongliao County, Liaoyuan City. Yangshu River is a tributary on the left side of Xiaogujiazitun, Hongsheng Village, Kaoshan Town. It turns southwest at Hebian Village, Kaoshan Town, and merges into the Erlongshan Reservoir on the west side of Zhouhu Village. Gushan River is 55.2 kilometers long, with an average ratio of 1.40. The basin area is 531 square kilometers, of which Yitong County accounts for 295.3 square kilometers, accounting for . 55.38 0. Huanxiling Reservoir (medium size) is built on Yangshu River, a tributary of Gushan River. Zhouhutun Hydrological Station (with a basin area of ??480 square kilometers) is located 7.4 kilometers upstream of the river mouth. During the period 1956-'. '1980, the measured water level changed by 4.0 meters. The annual average flow is 1.60 m3/s, the annual runoff is 50.4 million m3, the maximum flow is 384 m3/s (July 1.965), and the minimum flow is 0; the multi-year average sand content is 3.84kg/m3, and the maximum sand content in the section is 39.3 kg/m3 (19765438 June 0), the annual average sand transport volume is 192,000 tons, and the annual erosion modulus is 400 tons/km2.
The Karen River is a large tributary on the right side of the lower reaches of the Dongliao River. There are two sources: First, the Hongxi River is the main source, which originates from Hongxitang Village, Liuyang Village, Huanglingzi Township, Yitong County. After leaving the source, it flows northwestward, passing through Hujialu Village, Liufangfang Town, Gongzhuling City, and flows into the south of Xingzhi Village. Karen Reservoir; the second one is Taojiatun River, which originates from Jiajialing, Xiushan Village, Jingtai Town, Yitong County. It flows northwest from the source, passes through Taojiatun Town, Gongzhuling City, crosses the Beijing-Harbin Railway in the west, and ends at Heilinzi The southern part of Shuangmiaozitun Town flows into the Karen Reservoir. When the two sources merge, it is called the Karun River. After leaving the warehouse, it flows westward to Xingjialaoyuan Village, Erbantun Village, Dayushu Township, flows north along the right side of the main canal of Qinjiatun Irrigation District, and crosses the main canal of Qinjiatun Irrigation District at the mouth of the Chenjia River to the Zhanghuatun inverted siphon. It flows westward and flows into the Dongliao River northwest of Qinjiatun Town. In 1966, according to the planning opinions of the Dongliao River Basin issued by the Jilin Provincial Water Conservancy Survey and Design Institute, an inverted siphon was built north of Xingjialaoyuantun in the second half of the main diversion canal of the Qinjiatun Irrigation District to divert the Kalun River to the Dongliao River nearby. After diversion, the process is shortened.
The smooth flow of water reduces flooding in the lower reaches of the original river. After the Karen River was diverted, its basin area was 523 square kilometers and its river channel was 60.8 kilometers long, with an average decrease of 1.3‰. There are embankments on both sides. According to the hydrological data of small and medium-sized reservoirs in Siping City, the average annual flow rate of the river channel under the Karun River Reservoir is 0.81 cubic meters per second.
The Xingkai River is the larger tributary on the left side of the lower reaches of the Dongliao River, originating east of Xiwanfatun, Wanfa Township, Lishu County. After flowing out of the source, it flows northwest and flows into the Glass City Reservoir (small 1) in the west of Glass City Village in Quanyanling Township. After leaving the warehouse, it flows through Dongjiawobao Township and Quanyanling Township, passes through Dazibao Aqueduct, the first diversion canal in the Lishu Irrigation District, at Yuejiatun in Tuanjie Township, and flows into the mouth of the Dongliao River west of Chenjiatuozitun in Liujiagang Branch Town. The Xingkai River from its source to Leijiatun was originally called Donggouzi; from Leijiatun to Zhangjiabaozi, it was a swamp flood; the river channel below Zhangjiapuzi was wide and shallow, and the locals called it Yuejiagouzi. The original river channel was intermittent, especially in the middle reaches, where there was no obvious channel and the water flow was not smooth. Every year when there is plenty of water, there are floods. When the Lishu Irrigation Area was developed in 1943 (the 32nd year of the Republic of China), a section of the river from Daziwobo to Yuanbaoshan was dredged in the western area of ??the Lishu Irrigation Area as the eighth main canal, hence the name Xinkai River (today's Xingkai River). The Xingkai River basin covers an area of ??808 square kilometers and the river length is 89.7 kilometers. The river channel is 20-30 meters wide, and the largest river width is 50 meters. The average slope of the river is 0.90‰, and the curvature coefficient is 1.38.
The Xiaoliao River, the larger tributary on the right side of the lower reaches of the Dongliao River, originates from Wudaoquanzi Village, Lianhuashan Township, Gongzhuling City. After flowing out from the source, it flows through Baoquan Township, reaches Heiquanyan River, the right tributary of Changling County, Xiataizi Town, Yangdachengzi, and then flows into Yangdachengzi Reservoir. The right tributary Sanxianbao River originating from Changling County flows into the reservoir area. After leaving the warehouse, it flows to the Shengxing River, the left branch of Wangjiawobao, Yangchengzi Town, and then to the south of Zhangjiatun and north of Kongjiatun, Bawu Township. The left branch of Jinpen River joins the Daqingshan River here. It flows to Jiangxiao River, the right tributary of Shifupina in Sangshutai Town, flows in the southwest direction, passes through the five-hole culvert of the main diversion channel of Shuangshan Irrigation District, and merges into the Dongliao River at Zhoujiawopu. In the autumn of 1966, Gongzhuling blocked water due to a five-hole culvert, diverting the lower reaches of the Xiaoliao River. The river course turns from the northwest of the original 15th Tun Village to the south, and merges into the Dongliao River 150 meters upstream of the head barrage in Shuangshan Irrigation District. After the Xiaoliao River was rerouted, the river channel is 88.4 kilometers long, with an average ratio of 0.90/oo, and a drainage area of ??1,140 square kilometers. According to actual measurements at the Sandaohuan Hydrological Station in the middle reaches from 1956 to 1976, the water level fluctuated 4.20m, the average flow rate was 1.74 m3/s, the maximum flow rate was 640 m3/s (July 12, 1967), the minimum flow rate was 640 m3/s, and the average sand content 5.44kg There is a terrace above Zhaojiatun, a narrow and deep river, and willow trees along the bank. Below Zhaojiatun is a plain with curved river channels, sandy river beds, and large changes in erosion and siltation. On both sides are farmland and embankments.
The upper reaches of the Qinghe River flowed into the Xiliao River in 1949. The lower reaches pass through Aoji, Kaoshan, Shanchang, Qiandayou, Pingqi Road 96km Bridge, Guojiadian, west of Shidaren Tomb, Yaojia shack, Xiaoerjiazi west, Zhang Lama shack east, Cheng Xiang shack east, From the west of Jiajia shack, to the west of Liujiapu, to the Liaohe River in the east of Qinghezuiji.
Erdaohezi: Erdaohezi has two main tributaries. One is called Langdongzi River, which flows through Baliyingzi, Houyamenqian, Majiatundong, Liu Taipei, and then flows to Jishuipaozi and merges into Wende River. The main stream of the Wende River originates from the south of Daliushu, Lishu Town, Gongzhuling City, and passes through Xiaochanlingzitun east of Chuantou Village, Sunjia Shack west of Xingfu Village, east Fengji Tunnel, and east Wende Tunnel to Jishuipao Zi, meet up with Langdongzi. It starts from pumping water into the pao, passes through Changpaozi, Wangjiaweizi, Shuangyashu, Qinggouzi, Gaojiatun, Housanjupao, Dabingpao, Bajiazi Tunbei and Xiaoqishudong to reach Dahaojiazi. People in Xinli Township, Liutiao Township and Dongming Town are accustomed to calling it Erdaohezi. In 1958, the upper reaches of the Langdongzi River were cut off by Shuangshan, and the lower reaches were cut off by a row of tree trunks in the mountainous waterlogged area. The middle part was leveled by the Rongjun Farm (later known as the state-owned Shuangliao Farm) and planted with paddy fields. There are also some ruins in Xinli Township (called Moon Pagoda). In 1962, the Changfa-Jishui flooding section of the lower reaches of the Wende River became artificial drainage, extending to the Dongliao River in Shandong Province, and was called the Shuangshan Waterlogging Area Drainage.
Erdaohezi "went through the cantaloupe" in the main river network in 1958. A large flat pool from Jishui was called Shuangshan Canal, and a large flat pool from Jishui to Beibajiazi was called Shuangshan River Network.
Jinjiagouzi: Jinjiagouzi has two main tributaries. One is Guanjingzi River, originating from Dabaozi in front of Aobao, Nanpaozi and Yueliangpao in front of Baicai in Hongqi Town. The two streams of water meet at Guanjingzi, pass through Nanwazi, Daqishhudong, Xiaoqishu to Dahejiazi, and then enter the Dongliao River through the Taiping Grain Depot Courtyard, Li Chunling, Liangjia Shack, and Jinjiagouzi. Another tributary of Jinjiagouzi comes from Liutiao River (called Bailiu River). The Bailiu River originates from the north of Dabaitun in Liuxiang and passes through Xiaobaitun to Liutiaogou. It turns out that the water has reached Willow's "home". In 1938, wicker Nantuo was dug manually, and the water passed through Baiting Village and entered Erdaohezi. In 1958, the main trunk of the river network was manually dug and led to the Agricultural Exhibition Hall to collect water for soaking. The upper reaches of Jinjiagouzi start from the north of Daqishu, pass through Xiaoqishu, and end at Dahaojiazi. Jinjia ditch is dug manually in rows and passes through several sections. The downstream of Jinjiagouzi, from the yard of Dongming Grain Depot to the mouth of Jinjiagouzi, is still a natural river, but the entrance is noisy again. At 1938, the Dongniu River was manually excavated, spitting out a small dry river, and drained to Liuhumulu, connecting it with the Laobei River. After 1938, it became the main drainage channel in Shuangshan flood area.
Laobei River flows out from in front of the big flag tree and passes through Panshan, Songgentun, Gujiazi, Tieluowang, Liupengpu, Xujiangwozi, Zhangwenbing shack, Dongjiajiebei, Tangjiazi Weizi, Luojiajie East, Chengguang Qingtun, Bianjia Street East to the mouth of the Old Hubei River, where it merges into the Dongliao River. In addition, there is a branch road from Xujiang Whirlpool through Liu Huamule to Xiakoumenzi. The main stream of Laobei River, from 1958 large flag trees to ancient dwarf quilts, is known as the third main stream of the Shuangshan Waterlogging Area. The Old Ho Chi Minh River is still a natural river originating from the railway huts. In the middle, an artificial drainage ditch was dug from Luojia Street, and the water was introduced into the dry river channel dug in 1938. The water flowed to the mouth of Qinghe River and merged into the Dongliao River. This section is known as the Back River and Wadi River.
The Gonghe River starts from the Jixing shack, along the dragging roots, passes through Lianhuapao, Jindabaozi (also known as Aobaopaozi), Zhanghongju, Duba River, Gonghe River, and enters Beihe River. Most of this river is still a natural river channel, interrupted by the main trunk of the river network in 1962. This section is called Sanpaigan (connected to the Taiping section Sanpaigan).
The Niuwenge Chi River originates from the southwest foot of Hanshan Mountain in Tuhushuo Township, Bazar, Inner Mongolia, flows through Youkeyzhong Banner and Tuanjie Township, Tongyu County, and finally merges into the Dongliao River. The river in Tongyu County is 63 kilometers long, with a drainage area of ??about 1,000 square kilometers. The Niuwengechi embankment is 35.24 kilometers long and protects nearly 10,000 acres of cultivated land.