Formation Mechanism and Sustainable Utilization of Ningwu Ice Cave in China | Chapter 5 | Novel Perspectives of Geography, Environment and Earth Sciences Vol. 4

 The present study examined the energy exchange of Ningwu Ice Cave and before quantitatively interprets the formation and preservation system of the ice deposit. Heat strength is conducted inefficiently into the iceberg cave from outside and divider rock in spring, summer, and fall. While in winter, heat energy is moved very efficiently on account of the air natural change of possession, thus cooling it unhappy. Wherever the annual average air temperature is above 0 °C, ice caves can be raise. The largest hailstone cave in China, Ningwu Ice Cave in Shanxi Province, serves as an exemplification. We simulate the heat transfer process at this ice grotto using the Finite Element Method in consideration of quantitatively investigate the mechanism of establishment and preservation of the glaze cave. The estimation aids in assessing the belongings of global toasting, tourists, coloured lights, important conditions, and other determinants on the long-term growth of the ice cave as a touristry resource. Other icicle caves in China had sealed doors installed at the entrances in an effort to "cover" them, but this obviated cooling in the winter, and the iceberg in these caves will completely yield within tens of age. Rare natural landscapes usually have a very high advantage in terms of exercise. The benefit extends beyond erudition to include commerce. Like ice caves, particularly those in the direction of temperate domains like Ningwu Ice Cave. On the one help, ice bodies maybe used to study small-scale temperature changes over the past few decades. On the other hand, on the base of scientific protection and growth, ice caves maybe opened to tourists as a travel resource to advance the development of the local touristry market and drive the development of green saving with local traits. Details of sustainable utilization of Ningwu Ice Cave in China were resolved.

Author(s) Details:

Shaohua Yang,
Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China.

Yaolin Shi,
Key Laboratory of Computational Geodynamics, College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China.

Please see the link here: https://stm.bookpi.org/NPGEES-V4/article/view/9644