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
f = frictional 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 …
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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 lunar–derived 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… …
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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:
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:
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
f = frictional 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.
- The normal force (N) exerted on the body by the plane due to the force of gravity i.e. mg cos θ
- the force due to gravity (mg, acting vertically downwards) and
- 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.