Impact of Coal Mining on the Moisture Movement in a Vadose Zone in Open-Pit Mine Areas

被引:13
作者
Lian, Huiqin [1 ]
Yi, Haiyang [2 ]
Yang, Yi [1 ]
Wu, Bin [3 ]
Wang, Rui [3 ]
机构
[1] North China Inst Sci & Technol, Sch Safety Engn, Langfang 065201, Peoples R China
[2] North China Inst Sci & Technol, Sch Safety Supervis, Langfang 065201, Peoples R China
[3] Heibei Coal Sci Res Inst, Xingtai 054099, Peoples R China
基金
国家重点研发计划; 美国国家科学基金会;
关键词
open-pit coal mine; dewatering; groundwater level; vadose zone; moisture movement; capillary water; ECOLOGICAL RESTORATION; HYDRAULIC CONDUCTIVITY; ENVIRONMENTAL-IMPACT; SOIL; MODEL; OPTIMIZATION; GROUNDWATER; PARAMETERS; TRANSPORT; DYNAMICS;
D O I
10.3390/su13084125
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Long-term dewatering of groundwater is a necessary operation for mining safety in open-pit coal mines, as extensive dewatering might cause ecological problems due to dramatic changes in moisture movement in the soil, especially in ecologically fragile areas. In order to evaluate the impact of the coal mining operation on moisture movement in the vadose zone and vegetation, this paper presents a quantitative methodology and takes the Baorixile open-pit coal mine as a study example. A long-term in situ experiment (from 2004 to 2018), laboratory analysis, and numerical modelling were conducted to analyze the mechanisms and relationship among the dropping groundwater level, the vadose-zone moisture, and the ecological responses in the grassland area. The experiment data and modelling results suggest that groundwater level dropping during open-pit mining operation has limited influence on the vadose zone, exhibiting a variation of capillary water zone within a depth of 3 m while the vadose zone and soil water zone were at least 16 m deep. The critical evaporation depth of ground water is 8 m. The long-term influence radius of groundwater dewatering is about 2.72 km during the Baorixile mining operation, and the groundwater level change mainly influences the lower part of the intermediate vadose zone and the capillary water zone below 16 m, with little influence on the moisture contents in the soil water zone where the roots of shallow vegetation grow. The results from this study provide useful insight for sustainable development of coal mining in ecologically fragile areas.
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页数:16
相关论文
共 69 条
[31]  
Niswonger R.G., 2011, MODFLOW NWT NEWTON F, DOI DOI 10.3133/TM6A37
[32]  
Oldenburg CM, 2004, VADOSE ZONE J, V3, P848, DOI 10.2113/3.3.848
[33]  
Pan G., 2016, THESIS CHANGAN U XIA
[34]   Environmental Sustainability of Open-Pit Coal Mining Practices at Baganuur, Mongolia [J].
Park, Jonghoon ;
Kwon, Eunhye ;
Chung, Euijin ;
Kim, Ha ;
Battogtokh, Batbold ;
Woo, Nam C. .
SUSTAINABILITY, 2020, 12 (01)
[35]  
PHILIP J. R., 1957, TRANS AMER GEOPHYS UNION, V38, P222
[36]  
Radcliffe D.E., 2018, SOIL PHYS HYDRUS MOD, DOI 10.1201/9781315275666
[37]  
Rahman S, 2014, THESIS U NEW MEXICO
[38]   Estimating the water retention curve from soil properties: comparison of linear, nonlinear and concomitant variable methods [J].
Rajkai, K ;
Kabos, S ;
van Genuchten, MT .
SOIL & TILLAGE RESEARCH, 2004, 79 (02) :145-152
[39]  
Rapantova N., 2007, Mine Water and the Environment, V26, P264, DOI DOI 10.1007/S10230-007-0017-1
[40]   ROOT-GROWTH RESPONSE TO DEFOLIATION IN 2 AGROPYRON BUNCHGRASSES - FIELD OBSERVATIONS WITH AN IMPROVED ROOT PERISCOPE [J].
RICHARDS, JH .
OECOLOGIA, 1984, 64 (01) :21-25