Who is the richest man in Taihe County, Anhui Province?

What is known is Zhang Hesheng, with assets of 400 million.

Taihe county, alias Xiyang, is located in the northwest of Anhui province and belongs to Fuyang city. It has successively won the titles of China's hometown of folk culture and art, China's advanced grain production county and China's green model county.

Taihe county has a temperate monsoon climate and fertile land. Grain crops are mainly wheat, soybean, corn, sorghum and taro, while cash crops are mainly sesame, rape, cotton, tobacco, mint and Chinese herbal medicines, especially mint, which is known as "China's Asian mint and Taihe's China mint". There are mineral resources such as oil, nitrate, sand and clay in Taihe County, and there are scenic spots such as Jinghu Park, Taihe Hot Spring Resort and cherry orchard. Taihe County has two passenger stations, Taihe North (Pukuai Railway Station) and Taihe East (High-speed Railway), with convenient transportation.

In May, 20021,the Rural Work Leading Group of Anhui Provincial Party Committee reported the results of the performance evaluation of the rural revitalization strategy in 2020, and Taihe County, as an outstanding unit in the performance evaluation of the rural revitalization strategy in 2020, reported and praised it.

Location context

Taihe County is located in the northwest of Anhui Province, bordering Yang Guo and Lixin in the east, Fuyang in the south, Jieshou in the west, Linquan in the southwest, Qiaocheng District in Bozhou City in the north and dancheng in Henan Province in the northwest. The county is located between east longitude11525'-1555' and north latitude 3304'-3335', with a total area of 1822 square kilometers. It is 224 kilometers from Fengtai and Huainan to Hefei in the southeast and 307 kilometers from Huaiyang and Xihua to Zhengzhou in the northwest. It is 209 kilometers from Jinpu Road to Bengbu in the east and 2 10 kilometers from Pinghan Road to Luohe in the west. Taihe county is 52 kilometers long from north to south and 60 kilometers wide from east to west.

geologic structure

The strata in Taihe county are Holocene in the depth of 0-40 meters, and Pleistocene below 40 meters. The lithology at the top of Upper Pleistocene is bluish yellow variegated sub-clay, which is messy and hard in color, hard after drying, smooth in section, with iron-manganese nodules and calcareous nodules and cracks, but not developed. The new system is divided into three parts: upper, middle and lower. The buried depth of the lower Holocene roof is 18-24m, and the thickness is about 20m. The top is gray-black, purple-gray loam, dense, hard after drying, with fine particles, slightly slippery feeling, undeveloped cracks, containing more humus, which may be weathering crust. This layer is the symbol layer of the lower member of Holocene. The thickness of single layer is 4-8m, which is greater than 10m in some areas, and it is thinner to the southeast, only about 2m. The middle part becomes grayish yellow clayey silt or silty sand, with a thickness of about 4m and a thickness of 6-8m to the south. Generally, there are many layers, and the deposition is unstable. Most of them are thin layers of silt, loam and loam. Poor sorting, containing calcareous nodules in clayey silt, which is the boundary marker layer between Holocene and Pleistocene.

topography

Taihe County is located in the northwest of Huaibei warping plain. Since the third year of Yuanguang (BC 132), the Yellow River has flooded and silted to the west for many times, with the Yellow River beach as the main landform type. The territory is flat, high in the northwest (36.05 meters above sea level) and low in the southeast (30.5 meters above sea level), with a height difference of 5.55 meters and a natural slope of110000 to 1/7000. According to the classification of geomorphological causes, it can be divided into denudation and accumulation river plain and the latest flood plain. The eroded and accumulated Hejian plain is widely distributed in Hejian area, which is composed of bluish yellow variegated loam with a black weathering crust of about 50 cm at the top. The surface is flat and the terrain is gently inclined from northwest to southeast. The bluish-yellow variegated loam is obviously eroded and falls off in a prismatic shape along the cracks. The eroded loam fragments are piled up nearby or moved to other places again.

Climatic characteristics

Taihe county is located in the eastern part of the Asian continent. According to the natural division of China, the climate is divided into east monsoon temperate zone and semi-humid zone, which is close to the tropical climate in North Asia and is essentially a buffer zone for the two climates. It is characterized by obvious monsoon climate, four distinct seasons, abundant sunshine, mild climate, moderate rainfall and long frost-free period. However, due to the buffer zone of two climates, the weather is often changeable, and natural disasters such as low temperature, continuous rain, drought, waterlogging, hail, frost and strong wind often appear, which has adverse effects on agricultural production. Temperature: annual average 14.9℃. 65438+ 10 is the coldest in October, with an average of 0.7℃, and the hottest in July, with an average of 27.9℃, with an annual temperature difference of 27.2℃. The extreme maximum temperature of 1959 to 1985 is 40.8℃. The extreme minimum temperature is -2 1.3℃, and the maximum and minimum temperature difference is 62. 1℃. Taihe county 1959 to 1985, the lowest temperature is below -20℃ for five consecutive years, and the highest temperature is above 40℃ for five consecutive years.