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Mixed layer

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MIXED LAYER MONTMORILLONITE-CHLORITE

by G. Brown, P. Bourguignon, J. Thorez , 1973
"... ABSTRACT: A bluish-green clay found in veins cutting across brecciated slates of the Llanvirnian stage at Huy, Belgium, is shown by X-ray diffraction and chemical analysis to be a lithium-bearing, aluminium-rich, regular mixed layer montmorillonite-chlorite with associated pyrophyltite, nacrite and ..."
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ABSTRACT: A bluish-green clay found in veins cutting across brecciated slates of the Llanvirnian stage at Huy, Belgium, is shown by X-ray diffraction and chemical analysis to be a lithium-bearing, aluminium-rich, regular mixed layer montmorillonite-chlorite with associated pyrophyltite, nacrite

stoichiometry of mixed layer export

by A. N. Antia , 2005
"... Abstract. Sinking particles, once caught in sediment trap jars, release dissolved elements into the surrounding medium through leaching from their pore fluids, chemical dissolution and the activity of free exoenzymes. This results in an increase in dissolved elements in the trap jar supernatant. Ele ..."
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and corrections applied for samples from sediment traps in the North Atlantic based on measurements of excess dissolved carbon, nitrogen, phosphorus, silica and calcium in the supernatant of the collection cups. At the base of the winter mixed layer, on average 90±6 % of phosphorus fluxes

A priori test of large eddy simulation of the compressible plane mixing layer

by Bert Vreman, Bernard Geurts, Hans Kuerten - J. Eng. Math , 1995
"... plane mixing layer ..."
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plane mixing layer

2007: Mixed layer instabilities and restratification

by Giulio Boccaletti, Raffaele Ferrari, Baylor Fox-kemper - J. Phys. Oceanogr
"... The restratification of the oceanic surface mixed layer that results from lateral gradients in the surface density field is studied. The lateral gradients are shown to be unstable to ageostrophic baroclinic instabilities and slump from the horizontal to the vertical. These instabilities, which are r ..."
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The restratification of the oceanic surface mixed layer that results from lateral gradients in the surface density field is studied. The lateral gradients are shown to be unstable to ageostrophic baroclinic instabilities and slump from the horizontal to the vertical. These instabilities, which

Sound generation in a mixing layer

by Tim Colonius, et al. , 1997
"... The sound generated by vortex pairing in a two-dimensional compressible mixing layer is investigated. Direct numerical simulations (DNS) of the Navier{Stokes equations are used to compute both the near-eld region and a portion of the acoustic eld. The acoustic analogy due to Lilley (1974) is also so ..."
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The sound generated by vortex pairing in a two-dimensional compressible mixing layer is investigated. Direct numerical simulations (DNS) of the Navier{Stokes equations are used to compute both the near-eld region and a portion of the acoustic eld. The acoustic analogy due to Lilley (1974) is also

The temperature-salinity relationship in the mixed layer

by Raffaele Ferrari
"... In the surface mixed layer (ML) of the ocean there is a remarkable correlation between the horizontal temperature and salinity gradients. The goals of this project are (1) to investigate if these correlations are the result of processes at work within the ML, (2) to develop ..."
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In the surface mixed layer (ML) of the ocean there is a remarkable correlation between the horizontal temperature and salinity gradients. The goals of this project are (1) to investigate if these correlations are the result of processes at work within the ML, (2) to develop

Winds for Ocean Mixed Layer Modeling

by Coolbaugh Eric J, Ou X Library, Eric J. Coolbaugh, Eric J. Coolbaugh , 1984
"... FNOC and SASS Wind Comparison SASS Wind Utilization 20. ABSTRACT (Continue on reverse aide II necaaaary and Identity by block number) A study of the feasibility of using SEASAT Scatterometer wind measurements as the surface wind stress forcing for an ocean mixed layer model. Comparisons are made of ..."
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FNOC and SASS Wind Comparison SASS Wind Utilization 20. ABSTRACT (Continue on reverse aide II necaaaary and Identity by block number) A study of the feasibility of using SEASAT Scatterometer wind measurements as the surface wind stress forcing for an ocean mixed layer model. Comparisons are made

On the stratification of turbulent mixed layers

by L. Mahrt, Jean-claude Andri - J. Geophys. Res , 1983
"... The vertical distribution of density or temperature is studied in turbulent boundary layers stratified by either salt or temperature and driven in an annulus by a rotating screen. With rapidly growing boundary layers the buoyancy flux due to entrainment becomes suf•ciently large that the boundary la ..."
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layer is no longer well mixed. Stratification in the boundary layer is largest near the entrainment interface, corresponding to extension of the density transition into the turbulent boundary layer. The stratification in the rest of the boundary layer is smaller and nearly independent of height

On the structure of turbulence in compressible mixing layer

by M. Menaa
"... The study of turbulent compressible flow is the object of a particular interest in this last decade. The striking attract is that many phenomena become very important with the effect of compressibility. Indeed, the structure of turbulence changes drastically and depends essentially on the convective ..."
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on the convective Mach number Mc, i.e. the Mach number based on the velocity difference between the large eddies and the external flows. One flow where the effect of compressibility on turbulence appears at relatively low Mach number is the plane mixing layer. The study of a supersonic mixing layer on self
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