Xiahuayuan

Although unconfirmed elsewhere a dispatch published in the Eastern Times (Shanghai) on July 24 stated that a clash already had occurred between Feng’s troops and the Government forces in the vicinity of Hsiahuayuan on the railway south, of Kalgan.

[1933 July 29, “Will Feng-Japanese Crisis in Chahar Precipitate New Civil Warfare?”, in The China Weekly Review, volume 65, number 9, Shanghai, →OCLC, page 354, column 1

The eastern counties of the Datong- and Huairen-type (Xiahuayuan District, Zhangjiakou District and Yanqing County) have no access to the water transfer, but have relatively water-rich basins without significant competing surface water users.

2017, Jacob Möhring, Ilona M. Otto, Xiaoxi Wang, “Impacts and adaptation”, in Frank Wechsung, Stefan Kaden, Markus Venohr, Jürgen Hofmann, Jens Meisel, Zhenci Xu, editors, Sustainable Water and Agricultural Land Use in the Guanting Basin under Limited Water Resources, Schweizerbart Science Publishers, →ISBN, →ISSN, →OCLC, page 331

The selected study area, the Xiahuayuan District (Figure 1) in Zhangjiakou City, Hebei Province, is located at 115°16′ E and 40°29′ N. This region has a temperate continental monsoon climate, with four distinct seasons, and hosts abundant mineral resources, including reserves of coal, shale, granite and other resources used throughout the territory. The region also hosts ample symbiotic mineral resources, including hematite and multi-metals. By March 2009, the Xiahuayuan District, owing to its long-time singular industrial structure, inadequate economic aggregates and serious resource shortages, was classified by the State Council of China as a second batch resource-exhausted city.

2022, Qiang Fan et al., “Evolution Analysis of the Coupling Coordination of Microclimate and Landscape Ecological Risk Degree in the Xiahuayuan District in Recent 20 Years”, in Sustainability, volume 14, number 3, →DOI, →ISSN, page 2