Data from: Coral tentacle elasticity promotes an out-of-phase motion that improves mass transfer
Data files
Jul 22, 2020 version files 5.05 KB
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Table_S2A.csv
981 B
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Table_S2B.csv
1.17 KB
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Table_S3.csv
2.71 KB
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Table_S4.csv
191 B
Abstract
Usage notes
Table S2. Flow conditions and the measured phase difference in the field experiments on individuals of A. diaphana (A) and colonies of D. favus (B). uc is the horizontal current velocity, A
is the average amplitude of the horizontal wave-induced velocity uw,
SD is its standard deviation, f
is wave frequency calculated as the inverse of the period, and Δφ
is the phase difference between the water and tentacle velocities.
Table S3. Conditions of the D. favus laboratory experiments. DT and LT
are the tentacle's diameter and length, uc
the horizontal current velocity, A
the amplitude of the wave-induced horizontal velocity uw
, f
the wave frequency calculated as the inverse of the period f=1/T
, and Δφ
the phase difference calculated as the difference between the phase in the sine-fitted horizontal water and the tentacle velocities. The Reynolds number, Re=UmDT/ν
, and the Keulegan–Carpenter number, KC=UmT/DT
where calculated using the maximal velocity of the horizontal phase-averaged period, Um=max(u)
, and the kinematic viscosity of sea-water ν
.
Table S4. Flow conditions during the G. fascicularis laboratory experiments. uc is the current velocity, A
is the wave amplitude of the wave-induced horizontal velocity uw
, f
is the wave frequency calculated as the inverse of the period f=1/T
, and Δφ
is the phase difference between the water and tentacle velocities.