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[AGE31-04] Effects of changes in viscosity under low gravity on infiltration rate
Keywords:viscosity, low gravity, infiltration rate
It is important to clarify water behavior in the porous media to realize cultivation of crops in spacecraft, on Mars or on the Moon. However, Jones et al. (1999) revealed that infiltration rate in porous media under microgravity (µG) is lower than that under 1G. In addition, Maruo (2018) revealed that infiltration rate in the capillary tube under µG is lower than that under 1G. Infiltration in porous media under µG depends on capillary force, so that the decrease infiltration rate in the capillary tube might be a cause of the decrease in infiltration rate in the porous media under µG. It is thought that the decrease of infiltration rate in capillary tube under µG was caused by a decrease in surface tension, an increase in contact angle, and/or an increase in viscosity. Naganuma et al. (2019) reported that the surface tension of water does not vary with gravity. In addition, it was revealed that the contact angle of water droplets under µG does not change compared to under 1G (Naganuma et al., 2018). However, there are few studies that evaluated the gravitational dependence of the viscosity of water. In this research, we evaluated the gravity dependence of the viscosity of water and estimated the influence of viscosity change on infiltration rate. In this experiment, low gravity experiment using parabolic flight was carried out for 2 days using MU-300 (Diamond Air Service Inc., Nagoya, Japan) as an aircraft. The gravity condition was µG (1st day: 3 times, 2nd day: 3 times), 1/6G (1st day: 3 times, 2nd day: 6 times), 1/3G (1st day: 5 times, 2nd: 3 times), and each low gravity duration was 20 to 30 seconds. Changes in gravity were acquired from the accelerometer installed in the aircraft. For the acrylic column with an inner diameter of 64 mm and a height of 41 mm used for the experiment, water repellent treatment was performed on the upper 14 mm of the inner wall of the column, and the water level was adjusted so that the boundary between the processed part and the unprocessed part became the water surface. Degassed water was used as the sample to be filled in the column. For measurement of viscosity, a viscometer (Tuning Fork Vibro Viscometers SV-10, A & D Co., Ltd.) was used. The water temperature was measured by a temperature sensor built in the viscometer. The measurement interval of viscosity and temperature was 2 seconds on the 1st day and 1 second at the 2nd day. I photographed the state of the surface with a video camera (GoPro Hero 4, GoPro Inc.). Experimental results showed a negative correlation between viscosity and gravity in the range of 0G to 1G (Fig. 1). In the range of 1 G to 2 G, the measured values varied due to vibration, and reliable data could not be obtained. Since it is known that the surface tension and the contact angle do not change under µG, it is considered that the decrease infiltration rate in the capillary tube was brought about only by the increase in viscosity. From this, we consider the effect of increase in viscosity under µG on decrease of capillary invasion rate. Maruo (2018) defines the rate of change of infiltration rate in the capillary tube under µG compared to under 1G as a coefficient of delay αand is expressed by equation (1) (Fig. 2). Postulate that values other than viscosity do not change with 1G and µG in equation (1), it is considered that equation (2) holds. Therefore, 1/α2in capillary infiltration experiment by Maruo (2018) is compared with ημG/η1Gin this experiment. 1/α2is 2.49 at the capillary diameter of 0.8 mm, 2.78 at 2.37 mm, 3.19 at 5.5 mm, ημG/η1Gis at 2.66 on the 1st day and 2.70 on the 2nd day, 1/α2and ημG/η1Gare nearly the same value. From this, it is considered that the decrease infiltration rate in the capillary tube under µG was caused by the increase in viscosity.