Bin County, Harbin City, Heilongjiang Province

Binxian County Binxian county belongs to Harbin City, Heilongjiang Province. Bin county is located in the south of Heilongjiang Province. It borders on Fangzheng County, Yanshou county and Shangzhi City in the southeast, Bayan County, Mulan county and Tonghe County across the Songhua River in the north and Feiketu River in the West. The total area is 3844.6 square kilometers.

Binxian is located in the South Bank of Songhua River, zhangguangcai Mountain West foot branch. The territory is mountainous and hilly, high in the South and low in the north. It is a mid temperate continental monsoon climate zone with an average annual temperature of 3.9 ℃ and an average annual precipitation of 681 mm. There are copper, marble, iron, gold, silver, graphite, quartz and so on. G1011 hatong highway, 221 national highway transit, along the Songhua River with three wharves.

Binxian has a total area of 3844.6 square kilometers. In 2016, Binxian's GDP reached 31.91 billion yuan, an increase of 11.9% over 2015. As of 2016, Binxian has 12 towns and 5 townships with a total population of 579303.

In November 2018, it was identified as the first batch of innovative counties (cities) by the Ministry of science and technology.

Historical evolution

Before Qing Dynasty

Bin County was a part of the xishen nationality during the reign of Emperor Shun.

During the summer solstice, Qin was a part of Sushen nationality.

In the Sixteen States of the Han Dynasty, Sushen was changed to yilou, and later was ruled by Dayu people, who were one part of yilou and Fuyu people.

In the northern and Southern Dynasties, in 494, Buji occupied all the territory of Fuyu and established seven units, which were part of Buji's anchegu department.

In the early Sui and Tang Dynasties, the name of the Wuji nationality was changed to 靺鞨. In the Bohai Sea, it belonged to Shangjing qiejie Prefecture, and now Acheng County, Baicheng, is Gaozhou.

In the southern and Northern Dynasties, in the fourth year of Tongguang (926) of the later Tang Dynasty, Qidan built Liao Dynasty, belonging to the Wanyan Department of Nuzhen in Tokyo. Nuzhen Aguda destroyed Liao Dynasty and built Jin Dynasty. Qujiang County was set up at the mouth of the Songhua River where the flail plate River entered. Now Renhe, an ancient city of Jin Dynasty, is located in Xindian town. It belongs to Huining mansion on Shangjing road and is under the jurisdiction of Baicheng county.

In the Liao and Jin Dynasties, there was Binzhou in the west of Changchun.

Yuan Dynasty is a part of wandolin wanhu mansion in Kaiyuan Road of Liaoyang province.

In February of the fourth year of Yongle (1406), Emperor Chengzu of the Ming Dynasty, jiahewei was established in the qiban River Basin, salaerwei was established in the lynx River Basin in July of the same year, and feihewei was established in the Feiketu River Basin in September of the same year. In the sixth year of Yongle in Ming Dynasty (1408), feiketuwei was built. In the 11th year of Wanli (1583), Nuerhachi, the leader of Nuzhen in Jianzhou, set up an army and occupied all parts of nuergandu in Ming Dynasty. In the 44th year of Wanli in the Ming Dynasty (1616), after the establishment of the post Jin regime, Huang Taiji inherited the throne of Khan and changed Nuzhen to Manchuria. In 1636, Huang Taiji became emperor, changed Jin Dynasty to Qing Dynasty, and established Shengjing as the capital. The Jin and Qing Dynasties continued the Ming Dynasty in Northeast China, and the guest territory was under the jurisdiction of general ningguta. In 1644, the Qing army and Manchu people entered the pass. Binxian county was less populated, more and more barren, more and more mountains and forests, forming a natural wild plant farm.

Qing Dynasty

From the 10th year of Shunzhi reign to the 23rd year of Qianlong reign (1653-1758), he returned to angbang Zhangjing of ningguta, guarded ningguta and other generals, and guarded Jilin Wula. From the ninth year of Qianlong to the sixth year of Guangxu (1744-1880), it belonged to Jilin general alechuka. In 1879, Wang Shaoyuan, a member of the general yamen school in Jilin Province, came here to investigate and decided to build an official Yamen in Weizigou. In 1880, the Qing government approved the construction of the Binzhou hall in Weizigou. In 1902, the Department of Pennsylvania was upgraded to the Department of Pennsylvania Zhili, and Yanshou county was established in the southeast of the Department, which was under the jurisdiction of the Department of Pennsylvania Zhili. In December of the first year of Xuantong (1909), the Zhili Hall of Pennsylvania was upgraded to the government of Pennsylvania. Acheng county was established in the southwest and Fangzheng County in the East. The government of Pennsylvania governs Yanshou and Acheng counties, while Fangzheng county belongs to Yilan hall.

the Republic of China era

On March 11, 1913, by the order of the president of the Republic of China, the government system was abolished, and the government of Pennsylvania was changed into Binxian county. This is the origin of Binxian. On September 18, 1931, Japanese imperialism invaded Northeast China. In 1932, the puppet Binxian County Office was established. In October 1934, Binxian county was under the jurisdiction of Binjiang province from Jilin Province. On August 15, 1945, Northeast China was restored. In November 1945, Binxian government was established under the leadership of Binjiang province. In mid November, Binjiang province was renamed Songjiang Province, and Binxian county was under the leadership of Songjiang province.

After the founding of new China

In 1954, pine and Heilongjiang provinces merged, and Bin County was a county directly under Heilongjiang Province. In August 1958, it belonged to Harbin. In August 1965, it was put under the Songhuajiang administrative office. On February 22, 1967, Binxian provisional takeover Committee was established. On March 22 of the same year, Binxian Revolutionary Committee of "Three Combinations" was established. On October 8, 1980, Binxian people's government was restored.

administrative division

Binxian county has a total of 17 township level administrative regions, including 12 towns and 5 townships, namely, Binzhou Town, Juren Town, Binxi Town, Tangfang Town, Bin'an Town, Xindian Town, Shengli Town, Ningyuan Town, ferry town, Pingfang Town, Manjing Town, Chang'an Town, Yonghe Township, Niaohe Township, Minhe Township, Jingjian Township and Sanbao township. The people's Government of Binxian county is located at 4 West Street, Binzhou town.

geographical environment

Location context

Binxian county is located on the South Bank of Songhua River. It spans 126 ° 55 ′ 41 ″ - 128 ° 19 ′ 17 ″ E and 45 ° 30 ′ 37 ″ - 46 ° 01 ′ 20 ″ n. The perimeter of Binxian county is 377 km, with the widest from east to west of 107.8 km and the widest from north to south of 58.8 km. The total area is 3861.5 square kilometers, or 5792292.8 mu. The county is located in Binzhou Town, in the west of the territory, 127 ° 29 ′ E and 45 ° 45 ′ n. Starting from Binzhou Town, yaolingzi demarcation line is 75 km east to Fangzheng and Yanshou, 41 km south to taipingling and Shangzhi, 27 km west to Feiketu River, adjacent to Acheng, 17 km north to Songhua River, across from Hulan, Bayan, Mulan and Tonghe.

details

Geology and geomorphology

Binxian is located in the second uplift zone of Xinhua Xia system, which is transitional with Songliao Plain of the second subsidence zone. In the south of Binxian is Yuquan formation, which is distributed in gongpengzi, lijiadian, suijiadian, limekiln and tuoyaoling. It is roughly divided into three layers: the lower part is sandstone slate, the middle part is mainly intermediate acid pyroclastic rock, intercalated with normal sedimentary slate and marble transparent body, Pyroclastic rocks and slate are metamorphosed and hornfels; the upper layer is thick marble and thin limestone hornfels. There are Quaternary alluvium in the distribution. The exposed strata in the north are relatively complete, from Paleozoic to Cenozoic, and the quaternary system is widely exposed in the southern hilly area. The quaternary system is mainly distributed in the valley plain, the upper part is loam or loess like loam, and the lower part is sand, gravel or unstable sand, gravel layer. Due to the influence of neotectonic movement, in some places, such as the east of Feiketu River and Taoqi River, there is no gravel layer, loess like clay directly contacts with bedrock, while the bedrock in Datuan mountain, Xiaotuan mountain and Bin'an is exposed in the form of shallow hills, and the bedrock in the south bank of Songhua River is distributed in strips, forming a steep terrain. The eastern and southeastern hilly areas have been rising areas for a long time, while the north, West and East are controlled by the southeast direction. Since the Quaternary, they have been in the intermittent subsidence area, with obvious East-West faults and collapses. The most prominent fault is the Songhuajiang fault and the fault depression in Binxi Shengli area. The terrain of the county is high in the southeast and low in the northwest. In the southeast, Daqingshan is the highest in the county at an altitude of 952 meters, and in the north, huangyuquangou, Dongfang village, ferry Township, is the lowest at the entrance of Songhua River at an altitude of 105 meters, with an altitude difference of 847 meters.

Climatic characteristics

Binxian is a cold temperate continental climate zone, with an average annual temperature of 4.4 ℃, precipitation of 570 mm and frost free period of 146 days. The territory is divided into five climatic zones

1： From Shengli in the east to Binxi in the west, 2.5km away from the mountain in the South and 2km away from Songhua River in the north, it belongs to warm semi-arid and heavy spring arid area.

2： The low-lying area on the South Bank of Songhua River belongs to mild semi humid area with light spring drought.

3： Dongfang, Minli and Minfa villages in ferry and Ningyuan, southern Qixin village in Qingyang, Jixing, Fuxing and Guangen village in Guangen, Sanbao, Yuanbao, daquanzi, Baoshan and Xinxing villages in Sanbao, newly established Nanyang and Baoquan villages, Pingfang and Nanhua villages in Pingfang, Yiyang village in Songjiang, Jixing, Minfu, Minxing, Youlian and youyou villages in Yingjie, and Changqing and Caodian villages in Binxi It belongs to mild and semi humid shallow mountain area with light spring drought.

4： Wanrenhuan and Lemin villages for ferry; Shuangfeng Village in Ningyuan and Daqingshan village in Qingyang; weishungou village in Guangen and Xinxing village in Sanbao; Songjiang town and the south of caodianzi in Binxi belong to warm and humid areas with mild spring drought.

5： In the southeast of Ningyuan, Hongshan small basin belongs to the special zone of cold and humid, light drought and easy waterlogging.

natural disaster

The main natural disasters in Binxian are wind, waterlogging, hail, insects, drought and early frost.

natural resources

water resource

The total length of the eight main rivers in Binxian county is 363.9 km, the total drainage area is 3389 square kilometers, the average annual runoff is 394.31 million cubic meters, and the total water volume at the end of the year is 739.31 million cubic meters.

The surface water in Binxian county mainly depends on atmospheric precipitation, and the surface water resources are directly proportional to the amount of rainfall. The average annual runoff of annual rainfall is 405 million cubic meters; when the guarantee rate is 50%, the average annual runoff is 366 million cubic meters

Chinese PinYin : Hei Long Jiang Sheng Ha Er Bin Shi Bin Xian