1978
DOI: 10.1016/0029-8018(78)90062-8
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Artificial upwelling induced by ocean currents —Theory and experiment

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Cited by 18 publications
(2 citation statements)
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“…where h k is the kinetic head of horizontal current, h ρ is the density difference head, which can be calculated by integrating the relative density difference of the density profile along the length of the vertical tube [19], and h f is the total head loss of fluid motion.…”
Section: Theoretical Analysismentioning
confidence: 99%
“…where h k is the kinetic head of horizontal current, h ρ is the density difference head, which can be calculated by integrating the relative density difference of the density profile along the length of the vertical tube [19], and h f is the total head loss of fluid motion.…”
Section: Theoretical Analysismentioning
confidence: 99%
“…In the process of flow motion, a place in flow field may be filled by only liquid phase, or only gas phase and or the two phase interfaces, so it is the key point to solve the data coupling and parameters of switching in two phases [9]. At present, multiphase flow model uses the Euler method to depict and handle the numerical relationship in various phases, i.e.…”
Section: Governing Equationmentioning
confidence: 99%