Table 7.

Overview of low-frequency and ultrasonic velocity changes due to the presence of |$\mathrm{CO_2}$|⁠. All results are shown as deviations to the test at 100 per cent water saturation in percentage. Negative values indicate velocity reduction, positive values a velocity increase. For US velocity data (US) at 12 per cent free |$\mathrm{CO_2}$| data got lost and could be only derived from elastic properties at seismic frequencies (LF).

SaturationP-wave LFP-wave USS-wave LFS-wave US
100 per cent water+ |$\mathrm{CO_2}$|−3−3−1−3
12 per cent free |$\mathrm{CO_2}$|−72
31 per cent free |$\mathrm{CO_2}$|−6−6−1−4
1 per cent free |$\mathrm{CO_2}$|−301−1
SaturationP-wave LFP-wave USS-wave LFS-wave US
100 per cent water+ |$\mathrm{CO_2}$|−3−3−1−3
12 per cent free |$\mathrm{CO_2}$|−72
31 per cent free |$\mathrm{CO_2}$|−6−6−1−4
1 per cent free |$\mathrm{CO_2}$|−301−1
Table 7.

Overview of low-frequency and ultrasonic velocity changes due to the presence of |$\mathrm{CO_2}$|⁠. All results are shown as deviations to the test at 100 per cent water saturation in percentage. Negative values indicate velocity reduction, positive values a velocity increase. For US velocity data (US) at 12 per cent free |$\mathrm{CO_2}$| data got lost and could be only derived from elastic properties at seismic frequencies (LF).

SaturationP-wave LFP-wave USS-wave LFS-wave US
100 per cent water+ |$\mathrm{CO_2}$|−3−3−1−3
12 per cent free |$\mathrm{CO_2}$|−72
31 per cent free |$\mathrm{CO_2}$|−6−6−1−4
1 per cent free |$\mathrm{CO_2}$|−301−1
SaturationP-wave LFP-wave USS-wave LFS-wave US
100 per cent water+ |$\mathrm{CO_2}$|−3−3−1−3
12 per cent free |$\mathrm{CO_2}$|−72
31 per cent free |$\mathrm{CO_2}$|−6−6−1−4
1 per cent free |$\mathrm{CO_2}$|−301−1
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