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					Linear Kinematics: x = (vf + vi)/2 V t vectors: never mix x and y dx 1 v x  v 0t  at 2 , dt 2 1 x  v f t  at 2 2  v , a t  1 x  v 0  v f t note: this is just average speed x time 2   x( or distance traveled) = ∫ v dt = area under a speed vs time graph dv = slope of a velocity vs time graph a dt   Dynamics Σ F  ma, Ff  FN     v 2f  v 02  2ax Range equation: R = 2V o 2 (sin 2φ)/g = horizontal distance traveled if shot at angle   d2x a 2  dt Fg   G vectors: never mix x and y ixj=k w  mg but against circle j x i = -k ( s is a maximum therefore can be less than calculated, and k is constant) m1m2 r2 Fc  mac , Fc  m v2 , r Fs  kx      scalars. Direction is less important….easier……very little trig. Dot product yields scalar projections: i∙i = 1, i∙j = 0 Energy: W  F  d  Fd cos , W   Fdxcos = area under an F vs distance graph W  K , W  U U g  mgh on a planet, mm Ug  G 1 2 between objects (like Earth and Sun, apple and moon)   r 1 2 K   mv 2 Total Mechanical Energy E = K + U For satellites in circular orbit Fc =Fg to find orbital velocity U = K to find escape velocity K = -U/2 and E = -GMm/2r where are is the separation between centers U i  Ki  U f  K f if gravity is the only force in play 1 Us  kx2 2 F = -dU/dx = negative of slope on a U vs x graph.  Know shapes of stable, unstable and neutral equilibrium. W = dU/dt t P  Fv used mainly when sliding an object against friction at constant speed P Momentum vectors again; separate x and y  dp = slope of a momentum vs time graph p  mv , pi  p f , F  dt J  mv , J  Ft , J   Fdt = area under an F vs t graph     & Oscillation Rotation   2π radians = 360°  ,  t  1    0 t  t 2 2      , t  v  r s  r d dt  at  r d  dt  1    i   f t 2  Fc  m 2 r CM calculation: Pick a convenient origin then do  z Xcm = Σmx/Σm. Next do y and   If there is no outside force acting, the motion of the CM will remain unchanged. If an outside force is acting, F =ma find the acceleration of the CM. If you are rotating about the CM Other shapes us I   r dm, 2 I   mr 2 Ihoop = mr2 I disk = ½ mr2 I   r 2dV (called a volume integral if you did it in calculus) If you are rotating about any axis a distance d from the center of mass  I p  Icm   Md 2  1 K r  I 2 2 L  I ,        I ,   rF sin  = rxF (RHR for direction) L  mvrsin    Kepler: for any satellite about a central star 4 2 T , (k goes to 1 when AU’s and Years are used) 2  ksa 3 , k s  Gms l m Tp  2 Ts  2 g k  I for the rocking oscillation of any shape of known I mgd  2r 2 x  Acost    where A is the amplitude. (or use sine) v  T T d2x a   A 2 cost    , a  2 , a   2 x v  dx / dt   A sin t    , dt   Tcp  2