Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Yinfei LUO"'
Publikováno v:
Zhongguo dizhi zaihai yu fangzhi xuebao, Vol 33, Iss 2, Pp 1-8 (2022)
The development characteristics and formation mechanism of landslides are the basis and premise for further research on landslide prevention and utilization. Therefore, it is necessary to thoroughly study on the development characteristics and format
Externí odkaz:
https://doaj.org/article/207ce146a0a14778855354c17d1ad2a8
Publikováno v:
Shuiwen dizhi gongcheng dizhi, Vol 48, Iss 5, Pp 193-204 (2021)
The Xining Basin in Qinghai Province is rich in geothermal resources of low to medium temperature, but the geothermal reservoir is dominated by weakly consolidated sandstone containing clay minerals, and the geothermal water has high salinity, which
Externí odkaz:
https://doaj.org/article/4c95834c35804ffa822393240888dc10
Autor:
Yong Xiao, Kui Liu, Yuqing Zhang, Hongjie Yang, Shengbin Wang, Zexue Qi, Qichen Hao, Liwei Wang, Yinfei Luo, Shiyang Yin
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Climate warming is the greatest future challenge to the hydrosphere and the human community, especially in arid and semiarid regions. This study took the Golmud river watershed on the Tibetan Plateau as an example to numerically identify the developm
Externí odkaz:
https://doaj.org/article/59dcd013de2e4fb7b9d5d21189ee5baf
Publikováno v:
Lithosphere, Vol 2021, Iss Special 5 (2022)
AbstractAdvances in the exploration of the geothermal resources with remarkably high temperatures in the Gonghe Basin, northeastern Tibetan Plateau, provide an enhanced understanding of the origin and emplacement of hot dry rock (HDR). Based on the i
Externí odkaz:
https://doaj.org/article/d8dfd176a9fb483ab2d05d40360163b9
Autor:
Yude Lei, Zhen Zhao, Baojian Zhang, Xianchun Tang, Yinfei Luo, Guiling Wang, Jun Gao, Dailei Zhang
Publikováno v:
Water, Vol 14, Iss 24, p 4058 (2022)
There are 30 carbonate hot springs in Yaoshuitan geothermal field, Xining Basin, China, with a temperature of 18~41.5 °C; and there are 10 carbonate hot springs in Qijiachuan geothermal field, with a temperature of 10~19.5 °C. Both geothermal field
Externí odkaz:
https://doaj.org/article/893d73d7a54b41a8bcc350936e04ef6e
Publikováno v:
Energy Reports, Vol 5, Iss , Pp 1025-1029 (2019)
It is important to have an accurate understanding of heat transfer process of water flowing through fractures for geothermal energy extraction and utilization. We designed an experiment to study the convective heat transfer characteristics of distill
Externí odkaz:
https://doaj.org/article/929ccce175a14c6295bbdf87ea4e99d9
Autor:
Zhen Zhao, Guangxiong Qin, Yinfei Luo, Songhe Geng, Linchao Yang, Ronghua Wen, Jiahao Chao, Liang Zhang
Publikováno v:
Energies, Vol 14, Iss 9, p 2671 (2021)
The Xining Basin in Qinghai Province, China, is rich in mid–low temperature geothermal resources, but the reinjection of geothermal water has not yet started. In this paper, the physical properties of rocks sampled from the newly drilled geothermal
Externí odkaz:
https://doaj.org/article/ff50c1689e2542f690b155cc2a61d600
Publikováno v:
Energy Reports, Vol 5, Iss, Pp 1025-1029 (2019)
It is important to have an accurate understanding of heat transfer process of water flowing through fractures for geothermal energy extraction and utilization. We designed an experiment to study the convective heat transfer characteristics of distill
Autor:
Honglei Lei, Yinfei Luo, Zhihong Lei, Yueqiang Ma, Yude Lei, Yanjun Zhang, Ziwang Yu, Zhongjun Hu, Ling Zhou
Publikováno v:
Energy and Buildings. 200:31-46
Understanding the sensitivity to different reservoir parameters can help optimize the use of a designated reservoir. Four key parameters, namely, fracture permeability, well spacing, injection temperature, and injection rate, are considered in this s
Publikováno v:
Arabian Journal of Geosciences. 14
The Zhacang thermal field has the highest temperature and the most typical characteristics among the 84 geothermal anomalies discovered in Qinghai Province, China. It is located 15 km southwest of Guide County and has a total area of 8.4 km2, where t