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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Institut für Meereskunde, Universität Hamburg
    Publication Date: 2023-01-30
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Event label; Latitude of event; Longitude of event; Norwegian Sea; Pressure, water; Salinity; SFB 318; Temperature, water; UniHH_CTD; VA100; VA100_profile-1; VA100_profile-100; VA100_profile-101; VA100_profile-102; VA100_profile-103; VA100_profile-104; VA100_profile-105; VA100_profile-106; VA100_profile-107; VA100_profile-108; VA100_profile-109; VA100_profile-110; VA100_profile-111; VA100_profile-112; VA100_profile-113; VA100_profile-114; VA100_profile-115; VA100_profile-116; VA100_profile-117; VA100_profile-12; VA100_profile-122; VA100_profile-127; VA100_profile-13; VA100_profile-132; VA100_profile-137; VA100_profile-142; VA100_profile-143; VA100_profile-144; VA100_profile-145; VA100_profile-146; VA100_profile-147; VA100_profile-148; VA100_profile-149; VA100_profile-15; VA100_profile-150; VA100_profile-151; VA100_profile-152; VA100_profile-153; VA100_profile-154; VA100_profile-155; VA100_profile-156; VA100_profile-157; VA100_profile-158; VA100_profile-159; VA100_profile-16; VA100_profile-160; VA100_profile-161; VA100_profile-162; VA100_profile-163; VA100_profile-164; VA100_profile-165; VA100_profile-166; VA100_profile-167; VA100_profile-168; VA100_profile-169; VA100_profile-17; VA100_profile-170; VA100_profile-171; VA100_profile-172; VA100_profile-177; VA100_profile-182; VA100_profile-187; VA100_profile-19; VA100_profile-192; VA100_profile-197; VA100_profile-2; VA100_profile-206; VA100_profile-21; VA100_profile-22; VA100_profile-23; VA100_profile-24; VA100_profile-25; VA100_profile-26; VA100_profile-27; VA100_profile-28; VA100_profile-29; VA100_profile-3; VA100_profile-30; VA100_profile-31; VA100_profile-32; VA100_profile-33; VA100_profile-34; VA100_profile-35; VA100_profile-4; VA100_profile-45; VA100_profile-46; VA100_profile-47; VA100_profile-49; VA100_profile-5; VA100_profile-50; VA100_profile-51; VA100_profile-52; VA100_profile-53; VA100_profile-54; VA100_profile-55; VA100_profile-56; VA100_profile-57; VA100_profile-58; VA100_profile-59; VA100_profile-60; VA100_profile-61; VA100_profile-62; VA100_profile-63; VA100_profile-64; VA100_profile-65; VA100_profile-66; VA100_profile-67; VA100_profile-7; VA100_profile-70; VA100_profile-71; VA100_profile-72; VA100_profile-73; VA100_profile-74; VA100_profile-75; VA100_profile-76; VA100_profile-77; VA100_profile-78; VA100_profile-79; VA100_profile-8; VA100_profile-80; VA100_profile-81; VA100_profile-82; VA100_profile-83; VA100_profile-84; VA100_profile-85; VA100_profile-86; VA100_profile-87; VA100_profile-88; VA100_profile-89; VA100_profile-9; VA100_profile-90; VA100_profile-91; VA100_profile-92; VA100_profile-93; VA100_profile-94; VA100_profile-95; VA100_profile-96; VA100_profile-97; VA100_profile-98; VA100_profile-99; Valdivia (1961)
    Type: Dataset
    Format: text/tab-separated-values, 280602 data points
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  • 2
    Electronic Resource
    Electronic Resource
    New York, NY : American Institute of Physics (AIP)
    Physics of Fluids 1 (1989), S. 1460-1466 
    ISSN: 1089-7666
    Source: AIP Digital Archive
    Topics: Physics
    Notes: The thermocapillary migration of single water droplets in butyl benzoate was investigated using the Plateau configuration. The droplets were injected below the level of equal density in the stably stratified butyl benzoate. Because of buoyancy and Marangoni force, the droplets rise until these forces balance each other. For seven different temperature gradients the final position of four to eight single droplets was determined. The reciprocal diameter was found to be a linear function of the deflection from the height of equal density. A systematic deviation from the theory of Young, Goldstein, and Block [J. Fluid Mech. 6, 350 (1959)] was observed. This deviation was attributed to the convective heat transport inside and outside the droplet not covered by the theory. The experimental data could be fitted by introducing an effective temperature gradient that decreases with the square of the applied gradient.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 1989-09-01
    Print ISSN: 0899-8213
    Topics: Physics
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  • 4
    Publication Date: 1995-01-01
    Print ISSN: 0148-0227
    Electronic ISSN: 2156-2202
    Topics: Geosciences
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