A new approach to increase land reclamation rate in coal mining subsidence area: A case study of Guqiao Coal Mine, China
coal mining, mining subsidence, high groundwater table, mine reclamation, sustainable land use
Environmental Science and Engineering > 3. Land Reclamation and Ecology Rehabilitation
Abstract Accepted
Gensheng LI / 中国矿业大学
Zhenqi Hu / 中国矿业大学
Dongzu Yuan / 中国矿业大学(北京)
Pengyu Li / 中国矿业大学(北京)
Zhanjie Feng / 中国矿业大学
Yibo He / 中国矿业大学(北京)
Wenjuan Wang / 圣彼得大学
Underground coal mining inevitably causes land ponding in the region with high groundwater tables, which will affect sustainable land development. However, the traditional reclamation (TR) method has a low land reclamation rate. Thus, finding a suitable reclamation approach is crucial to alleviate the conflicts between coal exploitation and land protection. In this paper, the Guqiao Coal Mine of China, used as a typical case study, was seriously affected by mining-induced ponding. First, the dynamic distributions of surface subsidence and land damage from 2007 to 2017 were revealed based on concurrent mining and reclamation (CMR). Second, the land-water layout of five reclamation schemes (e.g., no reclamation, TR, CMR I, CMR II, and CMR III) were simulated. Then, a dynamic filling elevation model and filling thickness model were constructed. Finally, the earthwork allocation sequence was optimized. Results revealed that: 1) reclaimed land area: CMR III > CMR II > CMR I > TR > no reclamation. 2) Digging depths are directly proportional to the earthwork volumes and land area and are inversely proportional to the water areas, but with an increase in digging depths, the reclaimed land area is relatively lower. 3) CMR schemes had reclaimed 426.31~637.82 ha and 259.62~471.13 ha more land than no reclamation and TR scheme, respectively. Compared with no reclamation and TR scheme, CMR schemes can increase the proportion of reclaimed land by 33.77~50.52% and 20.57~37.32%, respectively. Research results provide a reference for increasing the mine reclamation rates in areas with high phreatic tables.