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    기술보고서 게시판 내용
    타이틀 Ballistics Model for Particles on a Horizontal Plane in a Vacuum Propelled by a Vertically Impinging Gas Jet
    저자 Lane, J. E.;; Metzger, P. T.
    Keyword BALLISTIC TRAJECTORIES;; COMPUTATIONAL FLUID DYNAMICS;; DIFFERENTIAL EQUATIONS;; EQUATIONS OF MOTION;; GAS JETS;; JET IMPINGEMENT;; LUNAR DUST;; LUNAR SURFACE;; MATHEMATICAL MODELS;; SIMULATION;; TRAJECTORY ANALYSIS;; TRAJECTORY MEASUREMENT;; VACUUM
    URL http://hdl.handle.net/2060/20100031187
    보고서번호 KSC-2010-164
    발행년도 2010
    출처 NTRS (NASA Technical Report Server)
    ABSTRACT A simple trajectory model has been developed and is presented. The particle trajectory path is estimated by computing the vertical position as a function of the horizontal position using a constant horizontal velocity and a vertical acceleration approximated as a power law. The vertical particle position is then found by solving the differential equation of motion using a double integral of vertical acceleration divided by the square of the horizontal velocity, integrated over the horizontal position. The input parameters are: x(sub 0) and y(sub 0), the initial particle starting point;; the derivative of the trajectory at x(sub 0) and y(sub 0), s(sub 0) = s(x(sub 0))= dx(y)/dy conditional expectation y = y((sub 0); and b where bx(sub 0)/y(sub 0) is the final trajectory angle before gravity pulls the particle down. The final parameter v(sub 0) is an approximation to a constant horizontal velocity. This model is time independent, providing vertical position x as a function of horizontal distance y: x(y) = (x(sub 0) + s(sub 0) (y-y(sub 0))) + bx(sub 0) -(s(sub 0)y(sub 0) ((y - y(sub 0)/y(sub 0) - ln((y/y(sub 0)))-((g(y-y(sub 0)(exp 2))/ 2((v(sub 0)(exp 2). The first term on the right in the above equation is due to simple ballistics and a spherically expanding gas so that the trajectory is a straight line intersecting Ɛ,0), which is the point at the center of the gas impingement on the surface. The second term on the right is due to vertical acceleration, which may be positive or negative. The last term on the right is the gravity term, which for a particle with velocities less than escape velocity will eventually bring the particle back to the ground. The parameters b, s(sub 0), and in some cases v(sub 0), are taken from an interpolation of similar parameters determined from a CFD simulation matrix, coupled with complete particle trajectory simulations.

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