breaker
By Henryk Szubinski
how a 4 x level of energetic interactions and a connection to 10 Dimensional planes of particle interactions towards a 3 rd level of 6 particle planes in their similar values but on alterant height planarity as being used by a type sector 1 to sector 2 to sector 3 by the usage of breaking the interactive space time and to use the type pole vaulting inbetween the formats to gain lift on the
level break value = to the lift gravity mass of the vechicle value mass
Particle image velocimetry (PIV) is an optical method of fluid visualization. It is used to obtain instantaneous velocity measurements and related properties in fluids. The fluid is seeded with tracer particles which, for the purposes of PIV, are generally assumed to faithfully follow the flow dynamics. It is the motion of these seeding particles that is used to calculate velocity information of the flow being studied. Other techniques used to measure flows are Laser Doppler velocimetry and Hot-wire anemometry. The main difference between PIV and those techniques is that PIV produces two dimensional vector fields, while the other techniques measure the velocity at a point.
During PIV, the particle concentration is such that it is possible to identify individual particles in an image, but not with certainty to track it between images. When the particle concentration is so low that it is possible to follow an individual particle it is called Particle tracking velocimetry, while Laser speckle velocimetry is used for cases where the particle concentration is so high that it is difficult to observe individual particles in an image.
Typical PIV apparatus consists of a camera (normally a digital camera with a CCD chip in modern systems), a high power laser, for example a double-pulsed Nd:YAG laser or a copper vapor laser, an optical arrangement to convert the laser output light to a thin light sheet (normally using a cylindrical lens and a spherical lens), a synchronizer to act as an external trigger for control of the camera and laser, the seeding particles and the fluid under investigation. A fiber optic cable or liquid light guide often connects the laser to the lens setup.
1———————— 2—————— 3—————-
each level might look like this:
3 4 6
—– —————– ———–
—– —————– ———–
—– —————– ———–
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what occurs between is the sectional break up of the horizon into angles such as:
1———20 degrees 2……….56 degrees 3—–170 degrees
data on the basics inputted and below the horizon for the multi staged sections of the turn about in data concerned with the process of reversing any vector problem in the astrophysics of data by process of actualised verticality in the sections by the usage of the vechicle structure cage in the mid section of the side view as the basic controll of the vector intercies caused by altering the angles of the qauntal transformers and the subsequent sections of the main vector controll of the inverted and rooted sections into x type formats for vertical control.
inner outer motion
By using the sections of the breaks in 3 sections ,the data on the formats of available scatter particle zobnes used for breaks = differencial inputs of the broken sections = to the enthopy of the height and angle of access of zones with planar characteristics for continued vertical roweing:
Stereoscopic PIV utilises two cameras with separate viewing angles to extract the z-axis displacement. Both cameras must be focused on the same spot in the flow and must be properly calibrated to have the same point in focus.
In fundamental fluid mechanics, displacement within a unit time in the X, Y and Z directions are commonly defined by the variables U, V and W. As was previously described, basic PIV extracts the U and V displacements as functions of the in-plane X and Y directions. This enables calculations of the Ux, Vy, Uy and Vx velocity gradients. However, the other 5 terms of the velocity gradient tensor are unable to be found from this information. The stereoscopic PIV analysis also grants the Z-axis displacement component, W, within that plane. Not only does this grant the Z-axis velocity of the fluid at the plane of interest, but two more velocity gradient terms can be determined: Wx and Wy. The velocity gradient components Uz, Vz, and Wz can not be determined. The velocity gradient components form the tensor: