List of aquifer parameter variations for well double-aquifer system simulation. ∆P1 and ∆P2 are pore pressure change in the upper and lower aquifers, respectively. ∆k1 and ∆k2 are permeability changes in the upper and lower aquifers. ∆T1 and ∆T2 are changes in recharge groundwater temperature of the upper and lower aquifer. Negative indicates a decrease.
No. . | ∆P1 (kPa) . | ∆P2 (kPa) . | ∆k1 (×10−15 m2) . | ∆k2 (×10−15 m2) . | ∆T1 (°C) . | ∆T2 (°C) . |
---|---|---|---|---|---|---|
1 | 10 | 10 | 0 | 0 | 0 | 0 |
2 | 50 | 50 | 0 | 0 | 0 | 0 |
3 | 100 | 100 | 0 | 0 | 0 | 0 |
4 | 200 | 200 | 0 | 0 | 0 | 0 |
5 | 500 | 500 | 0 | 0 | 0 | 0 |
6 | 1 000 | 1 000 | 0 | 0 | 0 | 0 |
7 | 1 000 | 1 000 | −0.8 | −0.8 | 0 | 0 |
8 | 1 000 | 1 000 | −0.5 | −0.5 | 0 | 0 |
9 | 1 000 | 1 000 | 1 | 1 | 0 | 0 |
10 | 1 000 | 1 000 | 4 | 4 | 0 | 0 |
11 | 1 000 | 1 000 | 1 | 1 | 0.2 | 0.2 |
12 | 1 000 | 1 000 | 1 | 1 | −0.2 | −0.2 |
13 | 1 000 | 500 | 1 | 1 | 0 | 0 |
14 | 500 | 1 000 | 1 | 1 | 0 | 0 |
15 | 1 000 | −1 000 | 0 | 0 | 0 | 0 |
16 | −1 000 | 1 000 | 0 | 0 | 0 | 0 |
17 | 1 000 | 1 000 | 1 | −0.5 | 0 | 0 |
18 | 1 000 | 1 000 | −0.5 | 1 | 0 | 0 |
19 | 1 000 | 1 000 | 1 | 1 | 0.2 | −0.2 |
20 | 1 000 | 1 000 | 1 | 1 | −0.2 | 0.2 |
No. . | ∆P1 (kPa) . | ∆P2 (kPa) . | ∆k1 (×10−15 m2) . | ∆k2 (×10−15 m2) . | ∆T1 (°C) . | ∆T2 (°C) . |
---|---|---|---|---|---|---|
1 | 10 | 10 | 0 | 0 | 0 | 0 |
2 | 50 | 50 | 0 | 0 | 0 | 0 |
3 | 100 | 100 | 0 | 0 | 0 | 0 |
4 | 200 | 200 | 0 | 0 | 0 | 0 |
5 | 500 | 500 | 0 | 0 | 0 | 0 |
6 | 1 000 | 1 000 | 0 | 0 | 0 | 0 |
7 | 1 000 | 1 000 | −0.8 | −0.8 | 0 | 0 |
8 | 1 000 | 1 000 | −0.5 | −0.5 | 0 | 0 |
9 | 1 000 | 1 000 | 1 | 1 | 0 | 0 |
10 | 1 000 | 1 000 | 4 | 4 | 0 | 0 |
11 | 1 000 | 1 000 | 1 | 1 | 0.2 | 0.2 |
12 | 1 000 | 1 000 | 1 | 1 | −0.2 | −0.2 |
13 | 1 000 | 500 | 1 | 1 | 0 | 0 |
14 | 500 | 1 000 | 1 | 1 | 0 | 0 |
15 | 1 000 | −1 000 | 0 | 0 | 0 | 0 |
16 | −1 000 | 1 000 | 0 | 0 | 0 | 0 |
17 | 1 000 | 1 000 | 1 | −0.5 | 0 | 0 |
18 | 1 000 | 1 000 | −0.5 | 1 | 0 | 0 |
19 | 1 000 | 1 000 | 1 | 1 | 0.2 | −0.2 |
20 | 1 000 | 1 000 | 1 | 1 | −0.2 | 0.2 |
List of aquifer parameter variations for well double-aquifer system simulation. ∆P1 and ∆P2 are pore pressure change in the upper and lower aquifers, respectively. ∆k1 and ∆k2 are permeability changes in the upper and lower aquifers. ∆T1 and ∆T2 are changes in recharge groundwater temperature of the upper and lower aquifer. Negative indicates a decrease.
No. . | ∆P1 (kPa) . | ∆P2 (kPa) . | ∆k1 (×10−15 m2) . | ∆k2 (×10−15 m2) . | ∆T1 (°C) . | ∆T2 (°C) . |
---|---|---|---|---|---|---|
1 | 10 | 10 | 0 | 0 | 0 | 0 |
2 | 50 | 50 | 0 | 0 | 0 | 0 |
3 | 100 | 100 | 0 | 0 | 0 | 0 |
4 | 200 | 200 | 0 | 0 | 0 | 0 |
5 | 500 | 500 | 0 | 0 | 0 | 0 |
6 | 1 000 | 1 000 | 0 | 0 | 0 | 0 |
7 | 1 000 | 1 000 | −0.8 | −0.8 | 0 | 0 |
8 | 1 000 | 1 000 | −0.5 | −0.5 | 0 | 0 |
9 | 1 000 | 1 000 | 1 | 1 | 0 | 0 |
10 | 1 000 | 1 000 | 4 | 4 | 0 | 0 |
11 | 1 000 | 1 000 | 1 | 1 | 0.2 | 0.2 |
12 | 1 000 | 1 000 | 1 | 1 | −0.2 | −0.2 |
13 | 1 000 | 500 | 1 | 1 | 0 | 0 |
14 | 500 | 1 000 | 1 | 1 | 0 | 0 |
15 | 1 000 | −1 000 | 0 | 0 | 0 | 0 |
16 | −1 000 | 1 000 | 0 | 0 | 0 | 0 |
17 | 1 000 | 1 000 | 1 | −0.5 | 0 | 0 |
18 | 1 000 | 1 000 | −0.5 | 1 | 0 | 0 |
19 | 1 000 | 1 000 | 1 | 1 | 0.2 | −0.2 |
20 | 1 000 | 1 000 | 1 | 1 | −0.2 | 0.2 |
No. . | ∆P1 (kPa) . | ∆P2 (kPa) . | ∆k1 (×10−15 m2) . | ∆k2 (×10−15 m2) . | ∆T1 (°C) . | ∆T2 (°C) . |
---|---|---|---|---|---|---|
1 | 10 | 10 | 0 | 0 | 0 | 0 |
2 | 50 | 50 | 0 | 0 | 0 | 0 |
3 | 100 | 100 | 0 | 0 | 0 | 0 |
4 | 200 | 200 | 0 | 0 | 0 | 0 |
5 | 500 | 500 | 0 | 0 | 0 | 0 |
6 | 1 000 | 1 000 | 0 | 0 | 0 | 0 |
7 | 1 000 | 1 000 | −0.8 | −0.8 | 0 | 0 |
8 | 1 000 | 1 000 | −0.5 | −0.5 | 0 | 0 |
9 | 1 000 | 1 000 | 1 | 1 | 0 | 0 |
10 | 1 000 | 1 000 | 4 | 4 | 0 | 0 |
11 | 1 000 | 1 000 | 1 | 1 | 0.2 | 0.2 |
12 | 1 000 | 1 000 | 1 | 1 | −0.2 | −0.2 |
13 | 1 000 | 500 | 1 | 1 | 0 | 0 |
14 | 500 | 1 000 | 1 | 1 | 0 | 0 |
15 | 1 000 | −1 000 | 0 | 0 | 0 | 0 |
16 | −1 000 | 1 000 | 0 | 0 | 0 | 0 |
17 | 1 000 | 1 000 | 1 | −0.5 | 0 | 0 |
18 | 1 000 | 1 000 | −0.5 | 1 | 0 | 0 |
19 | 1 000 | 1 000 | 1 | 1 | 0.2 | −0.2 |
20 | 1 000 | 1 000 | 1 | 1 | −0.2 | 0.2 |
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