universal theorem

universal theorem

By Henryk Szubinski

the universal theory is involvance of identity , not its order of involvance

basis 1 = multiples of the process to define the levels over the lim x =the basis of ejected matter

as the force of the data process on the singularity + S levels = full volume by force of volume not inclusive

of the data on the process of usage of the data on the relations to full universal forced process volumes = to the definitions by A.I accertions =a level of inclusion for the usage of the pre data. = F3

a spacetime is a volume of ejected matter into the open state reality of the Einstein Warper object as the open state reference without such a object placed within the warp to stop the flow of level 2 = the same value of spacetime as ejected in force as to cause the spacetime to continue displaceing outwards . The only format for the surface continuiim being the inverted case of the full surface ejected outwards to such force that the surface becomes a sphere that defines the volume of its universal size = to the stages previous to its ejections=to the related states of a upsurge of surface ejected force  towards its surface and ultimately to its spherical force resultance..

It starts of vaugely similar to the greter values of its increased relations to Einsteinean relativity , breaks through with the brilliance of Hawkins but stays put on the issue of the whole universe being a internally immense force of both the exterior and interior levels of the universes surface by the persistance of galaxies having made the route to reruns on a objective that is totally defined as the type of dynamics in action by the basic and best reasons for being there, the basics of the unplugged spacetime allowed to work freely into and outof the process to develop one theory of its inclusive and exclusive universe theory of everything.

fallen body force problems

the fallen problem

By Henryk Szubinski

a water bubble will do a full rotation underwater from its release source and some do it in 1/2 a rotation. So what governs the rate at which buubles have boyancy related values of a r.p.m value in which the same values must represent the Newtonian theory on inlcines as not functioning in fluidity but must obey the laws of Gallileo must also be true for the altered environment of water and object falling upwards:

gallileo = G

and Newton = N

so that 2G = N r.p.m

An initially-stationary object which is allowed to fall freely under gravity drops a distance which is proportional to the square of the elapsed time. This image, spanning half a second, was captured with a stroboscopic flash at 20 flashes per second. During the first 1/20th of a second the ball drops one unit of distance (here, a unit is about 12 mm); by 2/20ths it has dropped at total of 4 units; by 3/20ths, 9 units and so on.

can the forces following be configured to make a unified force problem real:

N= m1,m2,m3

f= the internal level rectanguloid occilatory measurment device

mg sin angle= the influence of lifted inclines

mg= the mass of the top trianguloid

mg cos angle= the syper symmetry of all objects in one value symmetry

Key:
N = Normal force that is perpendicular to the plane
m = Mass of object
g = Acceleration due to gravity
θ (theta) = Angle of elevation of the plane, measured from the horizontal
ffrictional force of the inclined plane

basically 2 objects are dropped from a specific height:

the experiment is to see if there is a incline basis influence on the involvance with 3 objects in states of falling vectors

as

1) a rectanguloid

2) a internally quantalised rectanguloid and

3) the base rectanguloid

the data on the actual influence of any of the 5 bodies in fallen vector values will attempt to locate the Tan value angles of the possibility for a force that is symmetrical to the incline of the trianguloid as well as the gravity influence or its opposed gravity by the usage of rectangular volumes with a alternating internal detection or measurement system to define the symmetricality of the base value as the measurement of the force of attraction = gravity x in

its specific value relations and to detect any forces acting on the alterations of falling objects in space and in spacetime.

lunar chance rate  force functions of derived universe  lunar  H2O processess

bodies on inclines       lunar chance rate  force functions of derived universe  lunar  H2O processess

The Moon is the only celestial body on which humans have made a manned …. Chemical composition of the lunar surface regolith (derived from crustal rocks) …. The other major geologic process that has affected the Moon’s surface is …… “Character and Spatial Distribution of OH/H2O on the Surface of the Moon 


27 Feb 2010  2:15 p.m. Hurley D. * Surficial OH/H2O on the Moon: Modeling ….. of theLunar Crust [#1231] Anorthosite formation processes and the …. will model bubble growthrates in lunar basaltic melts and examine the controlling factors.  Figure 1. from LUNARPOLAR ILLUMINATION CONDITIONS DERIVED USING 

3 Sep 2009  Moreover, minerals that make up the lunar rocks not only have no water, but crystallized in a  Most of it is thought lost to space by a variety of processes…. as favorably inclined and lit by the sun on Oct. 9 at 10:30 ut. ….. Many small, fresh craters bear signatures of water (H2O) and 


The moon is the most ‘human’ of the heavenly bodies, since its phases and the ….. The plane of the moon’s orbit is tilted, or inclined, at an angle of ….. Chemical composition of the lunarsurface regolith (derived from crustal rocks) …. The other major geologic process that has affected the Moon’s surface is 

basics of the fluid immersion = spacetime


force alterations similar data universe H2O process definitions of alterance …. O2 + H2O———-lunar volume——pressure–earth volume—-mean——Marsian volume———– 

the experiment is to see if there is a incline basis influence on the  the data on the actual influence of any of the 5 bodies in fallen vector values will  of a 3 angle = 360 degree full value where the usage of the derived value = 4 x  force molecular H2O dehydrations ofprocess for universe without a 


rotations of a bubble underwater as the formats of rotations caused  by the flow of the instance LINK of a side of the sphere to the surface level as being a type force that acts on the rotations of the solid in the fluid state volume by a vector connective tensile vector inside the volume sphere and acting on a level Cir / 4 = radial force of tensility

= the basis of sustained rotation without any motion volume filed or related causes for flow .


derived from the J-2 rocket engine that was used on the Saturn IB and Saturn V ….. moon, increasing the feasibility and success rate of a lunar colony. 

Moon Formation / Processes http://www.marcusmoon2022.org/ By the Lunar and ….. we will establish large-scale production of lunarderived propellants and 

5 Mar 2008  You would get the chance to do something no one would ever do again …. (If this happens, please send what is left of my body to Mars to become dirt. …. 2) Build a lunarmass driver to launch bricks and I-beams (plus other …… a bag of Mars capable seeds to begin the Terra forming process… 

17 Jul 2009  NASA | This is so so so freaking cool: the Lunar Reconnaissance Orbiter has taken  Dad was involved with the Apollo program on the Air Force side …… They simply assume that here the same process is being followed when …… The lunar reconnaissance orbiter actually performs seven functions

An impoverished surfer has drawn up a new theory of the universe for the courage of people like Garrett Lisi and those who are similarly inclined…… The universe passes for two processes – first of the formation of the …… wave function Present= Supercollapse of the wave function to a probability path. 


23 Sep 2009  As humans we are inclined to feel that life must have a point. …. since an origin force is always needed to explain the effect that becomes the …… To say such experiences where the soul leaves the body are only lack of …… We are all still in a processof becoming. Our observed Universe






Falling sphere viscometers

Creeping flow past a sphere.

Stokes’ law is the basis of the falling sphere viscometer, in which the fluid is stationary in a vertical glass tube. A sphere of known size and density is allowed to descend through the liquid. If correctly selected, it reaches terminal velocity, which can be measured by the time it takes to pass two marks on the tube. Electronic sensing can be used for opaque fluids. Knowing the terminal velocity, the size and density of the sphere, and the density of the liquid, Stokes’ law can be used to calculate the viscosity of the fluid. A series of steel ball bearings of different diameter is normally used in the classic experiment to improve the accuracy of the calculation. The school experiment uses glycerine as the fluid, and the technique is used industrially to check the viscosity of fluids used in processes. It includes many different oils, and polymer liquids such as solutions.

In 1851, George Gabriel Stokes derived an expression for the frictional force (also called drag force) exerted on spherical objects with very small Reynolds numbers (e.g., very small particles) in a continuous viscous fluid by solving the small fluid-mass limit of the generally unsolvable Navier-Stokes equations:

F = 6 \pi r \eta v \,

where:

  • F is the frictional force,
  • r is the radius of the spherical object,
  • η is the fluid viscosity, and
  • v is the particle’s velocity.

If the particles are falling in the viscous fluid by their own weight, then a terminal velocity, also known as the settling velocity, is reached when this frictional force combined with the buoyant force exactly balance the gravitational force. The resulting settling velocity (or terminal velocity) is given by:

V_s = \frac{2}{9}\frac{r^2 g (\rho_p - \rho_f)}{\mu}

where:

  • Vs is the particles’ settling velocity (m/s) (vertically downwards if ρp > ρf, upwards if ρp < ρf),
  • r is the Stokes radius of the particle (m),
  • g is the gravitational acceleration (m/s2),
  • ρp is the density of the particles (kg/m3),
  • ρf is the density of the fluid (kg/m3), and
  • μ is the (dynamic) fluid viscosity (Pa s).

Note that Stokes flow is assumed, so the Reynolds number must be small.

A limiting factor on the validity of this result is the Roughness of the sphere being used.

A modification of the straight falling sphere viscometer is a rolling ball viscometer which times a ball roling down a slope whilst immersed in the test fluid. This can be further improved by using a patented V plate which increases the number of rotations to distance traveled, allowing smaller more portable devices. This type of device is also suitable for ship board use.



Calculation of forces acting on an object on an inclined plane

Key:
N = Normal force that is perpendicular to the plane
m = Mass of object
g = Acceleration due to gravity
θ (theta) = Angle of elevation of the plane, measured from the horizontal
ffrictional force of the inclined plane

To calculate the forces on an object placed on an inclined plane, consider the three forces acting on it. Air resistance may be neglected for most calculations, except at high speeds.

  1. The normal force (N) exerted on the body by the plane due to the force of gravity i.e. mg cos θ
  2. the force due to gravity (mg, acting vertically downwards) and
  3. the frictional force (f) acting parallel to the plane.

We can decompose the gravitational force into two vectors, one perpendicular to the plane and one parallel to the plane. Since there is no movement perpendicular to the plane, the component of the gravitational force in this direction (mg cos θ) must be equal and opposite to normal force exerted by the plane, N. If the remaining component of the gravitational force parallel to the surface (mg sin θ) is greater than thestatic frictional force fs – then the body will slide down the inclined plane with acceleration (g sin θ − fk/m), where fk is the kinetic friction force – otherwise it will remain stationary.

When the slope angle (θ) is zero, sin θ is also zero so the body does not move.

continuiim relations in altered states

what is freeze

By Henryk Szubinski

referencing 3 value sequences

observations of water show that the surface on the alternate side is the basis for large pressure pockets subject to the formations of ice sheets as well as the lifting of the ice continental shelves by the process of waveforms similar to water waves at fluid H2O state.

Also implying that the effects of O2 as pressurised formats of force in the upwards vector were also existant at the early precambrian period where fluid H2O could have the same process interactions with the larger lifting of ice and its motion indicative of a period in the early ice age as the very high amount of ice in flow basically everywhere as the base relations of the theory of INVERTED SPACETIME and the causes of resultant fluidity based on O2 saturations by long exposures to heat that resulted in the dry periods of Earth history.

Heterogeneous nucleation

Heterogeneous nucleation occurs much more often than homogeneous nucleation. It forms at preferential sites such as phase boundaries or impurities like dust and requires less energy than homogeneous nucleation. At such preferential sites, the effective surface energy is lower, thus diminished the free energy barrier and facilitating nucleation. Surfaces promote nucleation because ofwetting – contact angles greater than zero between phases encourage particles to nucleate. The free energy needed for heterogeneous nucleation is equal to the product of homogeneous nucleation and a function of the contact angle :

\Delta G_{heterogeneous}\ = \Delta G_{homogeneous}*f( \theta)

where f( \theta)\ = \frac{1}{2} + \frac{3}{4}cos\theta - \frac{1}{4}cos^3 \theta

Difference in energy barriers

The barrier energy needed for heterogeneous nucleation is reduced, and less supercooling is needed. The wetting angle determines the ease of nucleation by reducing the energy needed. It is important to note that the critical radius remains unchanged. However, the volume can be significantly less for heterogeneous nucleation due to the wetting angle affecting the shape of the cluster.

In the case of heterogeneous nucleation, some energy is released by the partial destruction of the previous interface. For example, if a carbon dioxide bubble forms between water and the inside surface of a bottle, the energy inherent in the water-bottle interface is released wherever a layer of gas intervenes, and this energy goes toward the formation of bubble-water and bubble-bottle interfaces. The same effect can cause precipitate particles to form at the grain boundaries of a solid. This can interfere with precipitation strengthening, which relies on homogeneous nucleation to produce a uniform distribution of precipitate particles.

the spacepioneering vector displacement with the time fold on the basis of the process time being dissonated between the long vector and the short vector values as the type of alterations by point intercie referenced time values where the basis of the point divisives of a 3 angle = 360 degree full value where the usage of the derived value = 4 x

H2O molecular specifics m/a.n

as the process to define the time value of the CRYO  freeze to the time related to the active relocations of  CRYO VALUES  and the time value as related to the point specific time of the data usage by the reference usage of the force that defines the relations by the

equation of the data divisive process.

the data can displace ahead while using the basis of the problem BIT RELATOR as the format in relations to the projective value while defined to be the type triangulations of the process pressure related resultances = the same vector basis on the process of the data on frontal values and their altered degrees of specific values to a compensatoive process in which the data on compression = alterations of the force environment as based on the data of exchanged processess in a non specific problem of the format exchanged.

The data can then euate the 3 S = redefined t 3 (as the vector opposed 4 R) x ( another vector t 3 ) as the same similar process of a non opposed vector 3S.

force molecular dehydrations of process for without a specific element:

force molecular H2O dehydrations of process for universe without a specific force element

Bubbles are seen in many places in everyday life, for example:

  • As spontaneous nucleation of supersaturated carbon dioxide in soft drinks
  • As water vapor in boiling water
  • As air mixed into agitated water, such as below a waterfall
  • As sea foam
  • As given off in chemical reactions, e.g. baking soda + vinegar
  • As a gas trapped in glass during its manufacture

File:Air bubbles in a pool as a man surfaces for air.jpg

From Wikipedia, the free encyclopedia. Jump to:navigation, search. “H2O” and ….. themolecular forces between glass and water molecules (adhesive forces) are  Due to an interplay of the forces of adhesion and surface tension, …. and E2 elimination reactions, the latter is then known as dehydration reaction. 

Water has the second highest molar specific heat capacity of any known substance,  are among the most abundant elements in the universe…. ocean surface caused by the tidalforces of the Moon and the Sun acting on the oceans. …. day to avoid dehydration; the precise amount depends on the level of activity, 

Dynamic Disturbance of Molecular Forces, electromagnetic induction; see ScaleWatcher by unlocking the vast amounts of energy stored in the water molecule H2O….. abnormal gastrointestinal fermentation, dehydration, chronic diarrhea, ….. Silly name, silly claims: “Nectar of the Universe Energized Water is 

Water (H2O) can dissolve more substances than any other solvent …. film because themolecular forces between glass and water molecules  refers to the process of water moving up a narrow tube against the force of …. body requires between one and seven liters of water per day to avoid dehydration; the precise 

File:Air bubbles in a pool as a man surfaces for air.jpg


What is the difference between a molecular element and a molecular compound?  What is the volume of H2O released at 220 degrees celsius and 735 mm Hg if …. by exerting moreforce on the car with the large mass than with the car  What type of chemical bond is formed during a dehydration synthesis reaction? 

7 Apr 2008  Subsequent dehydration reactions lead to the removal of oxygen by production of  James A. Dumesic; Liquid Alkanes with Targeted Molecular Weights from …. them to work to force us to either convert, submit or die resisting them.  and oxygen from water (H2O) to build complex organic molecules. 

Irving Langmuir observed a strong repulsive force between hydrophilic surfaces. …. D2O is stable, however, the different from H2O being that D2O is heavier and  Scientists theorize that most of the universe’s water is produced as a …. to avoid dehydration; the precise amount depends on the level of activity, 

File:Air bubbles in a pool as a man surfaces for air.jpg


after the value upwards spacetime warp , the resultance used to define the type dynamics of the thermal type relations of fluid values of force as being lifted by a universal buoyancy upwards to the spacetime continuiim in effect as the types of multi form wave spacetimes.


27 Apr 2009  Molecular formula H2O. CAS number 7732-18-5  Specific heat capacity 4.184 J/(g·K) (liquid at 20 °C)  Another very important force that causes the water molecules to stick  are among the most abundant elements in the universe….. one and seven liters of water per day to avoid dehydration

File:Air bubbles in a pool as a man surfaces for air.jpg


15 Nov 2008  Molecular formula, H2O. InChI, InChI=1/H2O/h1H2  These forces are particularly important when cells are exposed to  to the process of water moving up a narrow tube against the force of ….. one and seven liters of water per day to avoid dehydration….Water availability in specific regions 






what is occuring is the same upside down relations of spacetime lifting to a level where the irrregularity of the fluidity of force gets captured in type 1 oxygen pockets that are basic H2O in its multiple states.


spacetime on the problems of warping upwards through the surface continuiims of gravity that usually act downwards with warping