Hushuguan Town, Huqiu District, Suzhou City, Jiangsu Province

Hushuguan town

Hushuguan town is located in the northeast of Suzhou high tech Zone and on the East Bank of Beijing Hangzhou Grand Canal. It has a long history of more than 2500 years. It is known as "Jiangnan hub and wuzhonghuo wharf", with a total area of 30 square kilometers and a built-up area of 14 square kilometers.

In 1999, it was named "national advanced cultural township".

In 2014, the public budget revenue was 730 million yuan, an increase of 19.3%; the total industrial output value was 15.5 billion yuan, an increase of 5%; the fixed asset investment was 5.5 billion yuan, an increase of 55.1%; the industrial investment was 3.4 billion yuan, an increase of 39.9%; the domestic registered capital was 1.81 billion yuan, an increase of 13.1%; the domestic registered capital was 640 million yuan, an increase of 30.6%.

Evolution of organizational system

"Hu Shuguan first, then Suzhou city.". Hushuguan town was founded in the Qin Dynasty and has a history of more than 2000 years. It is said that the first emperor of Qin visited the south to "beg for the sword of King Wu and send the tomb of Helu". When he saw the white tiger squatting on the hill (now Huqiu in Suzhou), he led his troops to chase for more than 20 Li, and the tiger disappeared. The name of the place was changed several times. In the Tang Dynasty, He taboo tiger and changed it to "Hu (H û) Li (Li Ú)". Qian Liu, the king of Wu and Yue in the Five Dynasties, avoided the word "Liu", so he changed his name to "Hushu". In the fourth year of Xuande in the Ming Dynasty (i.e. 1429), the Ministry of household set up banknotes, which became one of the seven banknote passes in the country. So he named it "Hushu pass", which was "the largest town in Wuzhong". It is said that when Emperor Qianlong went down to Jiangnan, he mistakenly pronounced the word "Hu (H Jie)" as "Xu (x Jie)", so it has been called "Hu (x Jie) Shuguan".

During the Liangzhu culture period (5000 years ago), there were tribes living in Hushuguan area. Cultural relics of Jiangsu Province, 1956

In the cultural relic survey of the management committee, the "zengwa site" in Hushuguan was excavated, which was "judged to be from the Shang and Zhou dynasties BC to the middle and late spring and Autumn Period", and the lower level "overlapped with Liangzhu Cultural Relics". In 1986, the site was designated as a county (city) cultural relics protection unit.

At the end of Shang Dynasty (about 3100 years ago), it belonged to Gouwu state.

In the first year of King Zhou Jian (585 BC), Shoumeng, the 19th grandson of Taibo, was called King (the first year of Shoumeng). There was a chronology of the state of Wu. Hushuguan belonged to the state of Wu. During the spring and Autumn period and the Warring States period, it was also under the jurisdiction of the Wu, Yue and Chu princes.

Qin set up a county, which belonged to Wu County. It is said that the first emperor of Qin asked the king of Wu to send the tomb to Helu. The white tiger squatted on the hill and disappeared after more than 20 Li. Because the place was named "huwan", it was the earliest name of Hushuguan.

In 696 ad, Wu County was divided into Wu County and Changzhou county.

In the first year of Kaiping in Houliang Dynasty (907 AD), Qian Xun was granted the title of king of Wu and Yue, and Hu Xun was an important place in the northwest of Su city of Wu and Yue State. During this period, the place names of "Xushi" and "Hushu" were changed.

In the fourth year of Xuande in the Ming Dynasty (1429 AD), Hu Shu Chao was set up, which was about Hu Shu town in Erdu, Changzhou county.

In June of the tenth year of Xianfeng in the Qing Dynasty (1860 AD), the Taiping army captured Hushuguan and occupied Suzhou City, and built "Sufu province". Hushuguan was the base of Taiping barracks in the northwest of Sufu provincial capital of Taiping army.

In December of the second year of Tongzhi reign (1863 AD), the Qing army recaptured Suzhou and still restored the old system.

In 1906, Hushuguan railway station was built, which became one of the early towns in China.

In January of the first year of the Republic of China (1912 A.D.), the governor of Jiangsu issued an order to abolish the prefectures and prefectures, and set up the County Hall. In the same month, Suzhou was renamed Wu County. Hushuguan is the first town of Wu County.

In December of 1928, the city of Wu County was divided into Suzhou City, city and county, and Hushuguan town was subordinate to Wu County. In May of 19, Suzhou city was abolished and returned to Wu County. The town is the same.

In December 1937, the local self-government Committee of the puppet Suzhou was established, and the counties and towns were under its jurisdiction. Hushuguan town was one of the 26 Township offices designated by the magistrate's office of the puppet Wu County.

In September 1940, the people's Anti Japanese Self Defense Association of Weihuang (Weitang, Huangdai) District in Northwest Wu County was established. Hushuguan was governed by Caonan, Dongqiao (established in March and April) and Caonan, Dongqiao and Huangqiao (established in February and June) in the following year.

In the 33rd year of the Republic of China (1944 AD), the Hushuguan area was under the control of the Japanese puppet army, and the vast rural areas were led by the administrative offices of Yangshan and Pengshan districts in Suxi county to carry out Anti Japanese guerrilla activities until the victory of Anti Japanese war in August 34.

In September 1945, Wu County Government of KMT took over Wu County and was subordinate to Jiangnan administrative office. Hushuguan was also subordinate before the war.

On April 25, 1949, Hushuguan was liberated and Suzhou was liberated on April 27. On May 1, Wu County designated Chengxiang District as the city of Suzhou, where the city and county were divided. Hushuguan is the first town of Wu County, until 1983, the city managed the county system.

In the winter of 1958, the townships around Hushuguan were merged into Baoan people's commune, which was a combination of government and society. The office is located in Siqiao lane.

In October 1960, the Xingxian and Xiangqiao brigades of Hushuguan and Baoan people's commune were assigned to Suzhou. In October 1962, it was transferred to Wu County. During the period, it was Suzhou Huguan people's commune. After returning to Wu County in 1963, the "commune" was removed as a town. The town government is in Zhuqing bridge.

On August 17, 1987, Hushuguan was approved by the provincial people's government and implemented the system of town governing village.

On November 19, 1988, Hushuguan was put under the jurisdiction of Suzhou suburb by Wu County.

In July 1992, the Management Committee of Hushuguan economic development zone was located in Gonghe village.

administrative division

As of May 2015, there are 5 administrative villages and 8 communities in Hushuguan town.

population

The total population of Hushuguan town was 62873 (in 2017).

geographical environment

Location context

Hushuguan is located in the northwest of Suzhou City and on the Bank of the canal. The center of the town is 120 ° 29'e and 31 ° 23'n, with Wangting in the north and Tongan town and Cangshu town in the West. Beijing Hangzhou Grand Canal runs through the north and south of the town, and longhuatang and zhuqingtang run through the East and West.

climate

Hushu pass is located in the middle subtropical to the north subtropical transition humid monsoon climate type. The climate is characterized by four distinct seasons, warm climate, abundant rain, sufficient sunshine and long frost free period, with obvious alternation of wind direction. The annual average temperature is 15.8 ℃, the annual average precipitation days is 134 days, the average relative humidity is 79%, the actual average sunshine hours is 2178 hours, the sunshine percentage is 49.3%, and the average atmospheric pressure is 1016.8 MB.

Geology and geomorphology

The upper Paleozoic is Devonian, Carboniferous, Mesozoic and middle lower Triassic strata. The Jurassic volcano * Iwade is exposed to the north of Yangshan, the east to the Hu Guan area and the tan mountain Huqiu, and so on, and to the north of the tile mountain and the Bai Shi mountain. Devonian is a stratum composed of siltstone and block sandstone of continental and delta facies, which was land from 400 to 350 million years ago. The Paleozoic climate was dry and hot, which made the Devonian strata tight and hard, not easy to be weathered and denuded. Yangshan hill is the whole or most part of the area. The Carboniferous is the early sea land replacement from 350 million to 290 million years ago. It is mainly composed of siltstone, fine sandstone and mudstone. From Jurassic to Cretaceous, influenced by the Yanshan movement, the strata formed in the town produced many fold and fault layers. The magma in the deep crust was broken up along the fault and frequently updip (intruded). Some of them rushed out of the surface, and some intruded into different depths below the surface and condensed and consolidated to form various kinds of intrusive rocks. In the northeast of Yangshan mountain, Hushuguan, Huqiu, Cao, Chenghu and other places, the volcanic rocks formed at that time are all under the Quaternary soil layer. Later, due to the rising of the crust and the weathering and denudation of the upper cover, the underground granite was exposed or close to the surface of the earth, which became today's grotesque granite landform. The animal shape of "lion dragon" in Guanshan Mountain is a typical granite hill.

natural resources

water resource

Huguan town is rich in groundwater resources, which is located in the edge zone of the water rich area of loose rock confined pore water. There are 4-5 confined aquifers in the depth range of 150-250 meters underground. The phreatic aquifer usually communicates with the surface water. The water quality is mostly polluted (shallow surface water). The water quality of deep aquifer is better. In addition, the sub region of carbonate fissure karst water area in the west of Yunhe River also constitutes the groundwater rich area of the whole area.

1、 Water rich area of confined pore water in loose rock

The water rich areas are distributed in Huqiu, Baiyangwan and Changqing areas, with the first confined water group as the main and the second confined water group in some areas. The boundary of Huajing, Baofeng and Changqing in Hushuguan is also at the edge of the confined pore water rich area of loose rocks. The lithology is mainly composed of medium and fine sand, partially mixed with medium coarse sand, 15-25m thick, 80-115m buried depth of roof, 1500-2000m water inflow per day of single well, but excluding the water area near the river. The middle rich water area is distributed in the east of Huguan xijinqiao line. Most of them are the second confined water group. The lithology of the aquifer is composed of fine sand and silty fine sand, mixed with sub sandy fine sand, 10-13m thick, 110-120m deep roof, single well

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