The slip gradually increases in magnitude during the rise period, attains its maximum speed during the high-speed period, and gradually decreases its speed during the deceleration period.
The high-speed period of the 2010 event corresponds to a marked increase in the activity of low-frequency earthquakes, similar to that of the 2003 event.
The Bungo channel slow slip events can be divided into three periods: a rise period, a high-speed period, and a deceleration period.
Then, during the high-speed period (Fig. 5(g)), the center of the slip area moved westward by approximately 30 km (relative to its position in Fig. 5(f)).
The rate of stress change appears to have a strong effect on the occurrence of low-frequency earthquakes, which become more active during the high-speed period of a long-term slow slip.
Then, during the high-speed period and deceleration period (Figs. 5 k)–(m)), the center of the slip area moved westward by approximately 15 km (relative to its position in Fig. 5 j)) while the slip magnitude in the central Bungo Channel area increased over time.
volume discharge of the pump at any wind speed V. period or time.
Single-factor optimization was used to confirm the effects of temperature, pH, inoculum quantity, rotational speed, fermentation period, methanol content, and SVH concentration on CA production (Fig. 1).
The horizontal wavelength, speed, and period of the GWs were measured as ~25 km, 2.5 km/min (150 km/h or ~40 m/s), and 10 min, respectively.
