Research Article
Evaluation of the Influence Caused by Tunnel Construction on Groundwater Environment: A Case Study of Tongluoshan Tunnel, China
Table 5
Membership of each indictor at every level calculated from quantification of Tongluoshan tunnel and the evaluation criteria.
| Indicator | Grades | Very weak | Weak | Moderate | Strong | Very strong |
|
[C11] average annual rainfall (mm) | 0 | 0 | 0.211 | 0.789 | 0 |
[C12] average annual evaporation (mm) | 0.288 | 0.712 | 0 | 0 | 0 |
[C13] area of catchment zone (km2) | 0 | 0 | 0.080 | 0.920 | 0 |
[C14] coefficient of rainfall infiltration | 0.158 | 0.146 | 0.256 | 0.330 | 0.110 |
[C15] spatial relationship between the tunnel and geomorphology | 0.600 | 0 | 0 | 0.400 | 0 |
[C16] capacities of reservoirs and lakes on the ground (m3) | 0 | 0 | 1.000 | 0 | 0 |
[C17] flow of surface rivers (m3/s) | 0 | 1.000 | 0 | 0 | 0 |
[C21] carbonate rocks exposure ratio (%) | 0 | 0.800 | 0.200 | 0 | 0 |
[C22] water yield property of aquifers | 0.624 | 0 | 0.301 | 0 | 0.075 |
[C23] water pressure on the tunnel (Mpa) | 0 | 0.800 | 0.200 | 0 | 0 |
[C24] development of folds | 0 | 0 | 0 | 1.000 | 0 |
[C25] development of fracture zones | 0 | 0 | 1.000 | 0 | 0 |
[C26] formation lithology | 0.210 | 0.350 | 0 | 0 | 0.440 |
[C27] location of tunnel in horizontal and vertical hydrodynamic zoning of groundwater | 0 | 0 | 0 | 1.000 | 0 |
[C31] length of tunnel (km) | 0 | 0.289 | 0.711 | 0 | 0 |
[C32] area of disturbed range (m2) | 0 | 0 | 1.000 | 0 | 0 |
[C33] construction method | 0 | 0 | 0 | 0.200 | 0.800 |
[C34] burial depth of tunnel (m) | 0 | 0 | 1.000 | 0 | 0 |
[C35] measures for prevention of groundwater flowing into tunnel | 0.200 | 0 | 0.800 | 0 | 0 |
|
|