Bei Dong Xiang, Quwo County, Linfen City, Shanxi Province

Beidong Township

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Beidong township is located in the southeast of Quwo County, Linfen City, Shanxi Province, with Zijin Mountain in the South and Huihe River in the north. There are 34 administrative villages, 38000 people and 65000 mu of cultivated land in the township. The river is crisscross, with beautiful mountains and rivers, rich products and outstanding people. It is the largest agricultural township in Quwo County. Qu Jiang highway passes through the countryside with convenient transportation and rich water resources. It has the history and experience of planting vegetables.

Beidong township has abundant water resources, fertile land, pleasant climate, beautiful natural scenery and forest coverage rate of 41.9%, which is the best living environment Township in Quwo County. The township governs 34 administrative villages, 8981 households and 35054 people (2017), with cultivated land area of 65000 Mu and per capita cultivated land of 1.7 mu. It is the largest agricultural township in Quwo County.

Beidong township was selected into the list of demonstration construction of strong agricultural towns in 2018.

Historical evolution

In the 26th year of the Republic of China, the system of village arrangement was implemented. Beidong was the Second District, which had jurisdiction over seven villages, namely, Shicun, beidong, Yimen, nanlinjiao, Xiyang, Dongyan and xijibi.

In April of the 36th year of the Republic of China, Quwo County was liberated, with Chengguan City, one district (Fengcheng), two districts (beidong), three districts (Houma), four districts (Gaoxian) and five districts (Qucun).

In April 1956, the district was removed and the township was built. Quwo County has jurisdiction over Chengguan town and seven townships including Houma, Shidian, Qucun, Anju, Gaoxian, Xiyang and Yingli (later changed to beidong).

In November 1958, villages and towns were withdrawn and people's communes were established. Quwo County has five people's communes: Weixing (Chengguan), Dongfeng (beidong), Feiyue (Shicun), Xingfu (Qucun) and Jianshe (Houma). In 1959, Dongfeng (beidong) people's commune was changed into beidong people's commune.

In July 1984, the township system was restored and beidong people's commune was converted into beidong township. In 2001, XIAPEI Township and beidong Township were merged into beidong Township with 34 villagers' committees under its jurisdiction.

Beidong township has jurisdiction over beidong, Yimen, Dongzhou, Jizhuang, beijisi, nanjisi, nanxiaying, beixiaying, dongxiaying, Xiyan, Dongyan, Liye, Baishui, Jingming, dongmingde, ximingde, Dongbao, Xibao, nanlinjiao, beilinjiao, Xizhou, Yingli, xujiabao, Hexi, shangpeizhuang, xiapeizhuang, Jiaoli, Renzhuang, peinanzhuang, Shandi, Anhu, Xuezhuang, etc Kiln yard.

A brief account of place names

According to Quwo's master · poem · Tang Pu, "the great grandson of Shuyu, Jincheng Hou, moved to Quwo.". According to Qianlong's newly revised Quwo County annals, Quwo is named after wo. In Erya, woquan is hanging, hanging and falling. The state of Jin is based on Jiangshan mountain. Jiangshui (boiling spring) flows from the south of Jiangshan mountain to the East. In the northwest, it flows through Qingyu gorge to the East, then flows to Baishi mountain to the East, and then hangs to woquan (Jingming waterfall). It also turns into Baishui village in the East, enters into Hui in the north, and flows into Fen in the West. Quwo and Xintian are the two capital lapels, which are the place where the water is flowing. It is the reason why Quwo is named.

geographical environment

Location context

Beidong township of Quwo County is located 10 kilometers southeast of Quwo County, Zijin Mountain in the south, Huihe River in the north, Jiangxian County in the East and Houma in the west, covering an area of 89.15 square kilometers. Zijin Mountain has beautiful scenery, rippling river water, Jingming waterfall, Jiaoli bridge, Millennium ginkgo tree, sanxianding, Renzhuang fan drum, Jindian ice and other natural landscape and historical and cultural heritage are very rich. Five reservoirs, including Huihe, Tianhe, Yigou, Feiquan reservoir 1 and reservoir 2, are well arranged. Heihe, Tianhe and Huihe rivers meet here. The farmland artesian irrigation network crisscrosses and connects the fields. Tongpu in the west, Houyue line in the north, Qujiang highway across the East and West, every village oil road, traffic is very convenient. The Zijinshan uplift in the south of beidong township has exposed bedrock and fissure water gushing out. In the valley between YaoYuan mountain and Houma Zhangjiashan mountain, fissure water gushes out. In winter and spring, the temperature is low and the Nanshan Mountain is shaded to form ice hanging. In April next year, it will be called "Jin palace hanging ice" in ancient times. Several springs gushed out from xuezhuangyu under the top of the three counties, forming a small flow and converging in Xuezhuang reservoir. Farmers Gao Hejiang and Chai Lingxia of Shandi village built a rolling dam and irrigation station in xuezhuangyu to block the water up to Zijin Mountain, and planted 8000 mu of barren hills in the north of the top of the three counties. Spring is full of flowers and autumn is full of fruits. The scenery is charming and infinite. The "boiling spring" in Jingming mountain gushes out with a flow of 0.46 m3 / s. Quwo County has set up a management committee of boiling spring irrigation area in Jingming village. The irrigation area has built the first reservoir and the second reservoir of boiling spring, three main canals, 25.75 km long, 98 branch canals, 84.47 km long, 122 bridges and culverts, 75 gates, 404 water drops and 2 inverted siphons. By 2007, 23 villages in beidong Township and 4 villages in Lechang town have been irrigated, with an irrigation area of 30000 mu, and water is delivered to the overflow ditch and Huihe river. The alluvial plain in front of Zijin Mountain is high in the South and low in the north, and it is gully area to Tianhe and Huihe faults. The eastern part is relatively flat, while the western part of Henan, peinanzhuang, Anhu, Xuezhuang and YaoYuan are gully areas.

The central part and the northern part are high in the East and low in the West. The three rivers of Huihe, Heihe and Tianhe flow from east to west and intersect in the areas of shangpeizhuang and xiapeizhuang. Due to the river cutting, the northern part of beidong, Dongzhou, Pingle, Yimen and the northern part belong to the dry highland gully area of Si; the central part belongs to the dry highland gully area of Liye, Dongpu, Xipu and Yingli.

Context

Beidong township is located in the southeast of Quwo County. Its geographical coordinates are 35 ° 33 ′ n to 35 ° 51 ′ N and 110 ° 24 ′ e to 110 ° 37 ′ E. Zijin Mountain in Nanping is adjacent to Huihe River in the north, Jiangxian County in the East and Houma County in the West. It is 6 kilometers long from north to South and 15 kilometers wide from east to west, with a total area of 89.15 square kilometers.

geology

Zijin Mountain front fault, located in Baishui, Renzhuang, YaoYuan line, east-west trend, 12 km. The fault inclines to the northeast, the south wall rises relatively, and the north wall falls relatively. It is a normal fault. It is speculated that the fault distance is more than 1000 meters. The landform has obvious fault triangle. The fault extends from southeast to Jiangxian.

landforms

Zijin East West winding, the main peak of three counties, 1118 meters above sea level. Bare rock, steep geothermal, deep valley, rare vegetation, earth rock mountain. Hilly terrace area is distributed in the edge of the inclined plain in front of Zijin Mountain, the South Bank of Huihe River and the North Bank of Heihe River, with an altitude of 500-600 meters. It has undulating hills, vertical and horizontal gullies, U-shaped and V-shaped gullies, and deep cutting. During the Cenozoic, the Zijinshan uplift was relatively strong. The west end of Zijinshan was close to the Aikou area of Houma City. The tertiary and Quaternary, semi cemented sandy conglomerate, and the sand layer was uplifted to about 520 meters above sea level. There is a clear planation plane distribution in the front of Zijin Mountain, which reflects that the neotectonic movement has the characteristics of intermittent rise, and the footstones in the front of Zijin Mountain are deeply buried.

climate

The whole township has a warm temperate continental monsoon climate with four distinct seasons. It is warm in spring, hot in summer, cool in autumn and cold in winter, slightly longer in winter and summer, and slightly shorter in spring and autumn. The annual average temperature is 12 ℃, and the temperature difference between winter and summer is large. January is the coldest with an average temperature of - 3.3 ℃; July is the hottest with an average temperature of 26.4 ℃; the temperature difference between winter and summer is 29.7 ℃. Generally, the low gas temperature drops to 0 ℃ or below in late October and rises to above 0 ℃ in early April of the next year. The annual accumulated temperature above 10 ℃ is 4395 ℃.

ground temperature

According to the records from 1977 to 1978, the annual average surface temperature is 15.3 ℃, the average surface temperature in January is - 2.3 ℃, and the average surface temperature in July is 30.4 ℃. The extreme maximum surface temperature was 70.7 ℃, which occurred on July 1, 1977. The extreme minimum temperature of - 25.3 ℃ occurred on December 18, 1984. Generally, there is frozen soil on the ground in the middle of November. The depth of frozen soil is 10 cm. Generally, it is thawed in the middle of December and in the middle of February next year. In 1977, the maximum frozen soil depth was 52 cm, and the dates were January 8-23 and February 4-8.

precipitation

According to the 35 year records from 1954 to 1988, the annual average precipitation is 525.7mm. The precipitation in 1964 was the most (825.5 mm) and that in 1957 was the least (310.4 mm). The difference between wet and dry is 515.1 mm. The annual precipitation is mainly concentrated from July to September, accounting for half of the annual precipitation, during which there are many rainstorms.

evaporation

The annual average evaporation is 1722.8 mm, the largest in 1957, 2969 mm, and the smallest in 1964, 1344.2 mm.

wind

It is windy in spring and winter, with southeast wind in spring and northwest wind in winter. The average wind speed is 1.8 m / s, with inner wind level 2 and maximum wind level 8. Jingming mountain pass is windy all the year round, with an average wind force of 6.

sunshine

The annual average sunshine duration is 2474 hours, the longest in 1965, 2703 hours, and the shortest in 1964, 2050 hours; the sunshine duration is the longest in June, 265 hours, and the shortest in February, 164 hours; the cumulative sunshine duration from March to October is 1778 hours. The sunshine duration in 1988 was 2143 hours, which was less than the average annual 330.7 hours.

Frost free period

The average annual frost free period is 189 days, and the longest is 228 days in 1988. In 1970, the shortest time was 169 days. The first frost usually occurs in the middle and late October, the earliest in the late September, and the last frost in the middle and late April.

hydrology

There are Huihe River, Heihe River and Tianhe River in the territory, all of which flow into Fenhe River from east to west, belonging to Fenhe River System in the Yellow River Basin. There are two sources of Huihe River: one is sangwangmiao in Fushan County, and the other is Daling in Qinshui County, which is called Huihe River after confluence at the estuary of Yicheng. It flows through Pingle, Dongzhou, beidong, Shangpei, XIAPEI and Jiaoli and enters Lechang. There is a tributary of Heihe River flowing in from XIAPEI. Heihe River, originated in Jiangxian County, flows from Nanji temple,

Chinese PinYin : Shan Xi Sheng Lin Fen Shi Qu Wo Xian Bei Dong Xiang