h u m a n   s u s t a i n m en t s  f o r c e

By Henryk Szubinski

COMNPARATIVES OF GRAVITY IN ENTHROPY AND BOYANCY AS A HIGH VALUE COMPARATIVE

Buoyancy and gravity are actually the same thing. If something is in a fluid and gravity is exerting a greater pull on the fluid than the object in the fluid, that is what buoyancy is.
EARTHS GRAVITY

basically the difference between man and woman are derivable to their influence on a type 1 relationship with which a general volume of fluids in the course of sustainemnt of life on Earth = to the usage of a minimal value in enthropy of the general difference between the H2O involvement in the amnion sack and the basis of a entrhropic definition of H2O = about a metre.

When theese possibilities are comparatively made to hydroxyle on the lunar surface as a general löayer of what would appear to be a gravity value of a 1 /x.g = 10 F

The ability of human productivity in its general category of producing a level of gravity that is less to or equal to the boyancy level by similar volume amounts = to the general bexternality of stemmic relationships with the exterior world our Earth.

This implies or means that the values of projective interactions any value specified or non specified relationship of the values of g / boyancy = to any value 3D relational Volume .x

the values therein are the values of physicaly sustainable sci fi reality..based on accertions of involvant relationships of human to the value 3 x = to external g values / amount of involvancies ( in the process of boyancy) implying that boyancy is a charactristic of every level sustainemnets with a sufficient gravity division = to the stemmic basis of a process in action.

3 relations of bouyancy

1———————————————-2——————————————3

data on gravity 3x = 1/10 g

as a type hyperspace connection to O2OH and H2O

3x H2O =1/10 . O2OH

AS ATOMIC MASS RELATIONSHIPS OF ENTROPY IN A ONE SIDED EQUATION:

To derive a generalized entropy balanced equation, we start with the general balance equation for the change in any extensive quantity Θ in a thermodynamic system, a quantity that may be either conserved, such as energy, or non-conserved, such as entropy. The basic generic balance expression states that dΘ/dt, i.e. the rate of change of Θ in the system, equals the rate at which Θ enters the system at the boundaries, minus the rate at which Θ leaves the system across the system boundaries, plus the rate at which Θ is generated within the system. Using this generic balance equation, with respect to the rate of change with time of the extensive quantity entropy S, the entropy balance equation for an open thermodynamic system is:[16]

\frac{dS}{dt} = \sum_{k=1}^K \dot{M}_k \hat{S}_k + \frac{\dot{Q}}{T} + \dot{S}_{gen}

where

\sum_{k=1}^K \dot{M}_k \hat{S}_k = the net rate of entropy flow due to the flows of mass into and out of the system (where \hat{S} = entropy per unit mass).
\frac{\dot{Q}}{T} = the rate of entropy flow due to the flow of heat across the system boundary.
\dot{S}_{gen} = the rate of internal generation of entropy within the system.

Note, also, that if there are multiple heat flows, the term \dot{Q}/T is to be replaced by \sum \dot{Q}_j/T_j, where \dot{Q}_j is the heat flow and Tj is the temperature at the jth heat flow port into the system.

THE BOUYANCY OF COMPARATIVES WITH A HYDROXYLE VALUE AS SPACE TIME IN ITS h2o / o2 oh ATOMIC VALUE

3x H2O  SPACETIME =1/10 1/20 X . O2OH

A SPACETIME COMPARATIVE CAN USE THE VALUE 1/10 AS ANY INTERACTION WITH 1/10 GRAVITY BY EXCHANGEING THE h2o FORMAT AS BEING THE 1/10 SPACE TIME =HYDROXYLE IN ITS value..as a higher velocity exchange of data on the exchanges of boyancy..

This is the equation to calculate the pressure inside a fluid in equilibrium. The corresponding equilibrium equation is:

\mathbf{f}+\operatorname{div} \sigma=0

where f is the force density exerted by some outer field on the fluid, and σ is the stress tensor. In this case the stress tensor is proportional to the identity tensor:

\sigma_{ij}=-p\delta_{ij}.\,

Here \delta_{ij}\, is the Kronecker delta. Using this the above equation becomes:

\mathbf{f}=\nabla p.\,

Assume the outer force field is conservative, that is it can be written as the negative gradient of some scalar valued function:

\mathbf{f}=-\nabla\Phi.\,

Then we have:

\nabla(p+\Phi)=0 \Longrightarrow p+\Phi = \text{constant}.\,

Hence the shape of the open surface of a fluid equals the equipotential plane of the applied outer conservative force field. Let the z-axis point downward. In our case we have gravity, so Φ = −ρgz where g is the gravitational acceleration, ρ is the mass density of the fluid. Let the constant be zero, that is the pressure zero where z is zero. So the pressure inside the fluid, when it is subject to gravity, is

p=\rho g z.\,

So pressure increases with depth below the surface of a liquid, as z denotes the distance from the surface of the liquid into it. Any object with a non-zero vertical depth will have different pressures on its top and bottom, with the pressure on the bottom being greater. This difference in pressure causes the upward buoyancy forces.

The buoyant force exerted on a body can now be calculated easily, since we know the internal pressure of the fluid. We know that the force exerted on the body can be calculated by integrating the stress tensor over the surface of the body:

\mathbf{F}=\oint \sigma \, d\mathbf{A}

The surface integral can be transformed into a volume integral with the help of the Gauss–Ostrogradsky theorem:

\mathbf{F}=\int \operatorname{div}\sigma \, dV = -\int \mathbf{f}\, dV = -\rho \mathbf{g} \int\,dV=-\rho \mathbf{g} V

where V is the measure of the volume in contact with the fluid, that is the volume of the submerged part of the body. Since the fluid doesn’t exert force on the part of the body which is outside of it.