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( 1 ) As parameter k increases with parameters a and q kept constant , the displacement tends to damp out quickly . This result is anticipated . As q increa- ses with a and k remaining unchanged , the displacement tends to approach the ...
( 1 ) As parameter k increases with parameters a and q kept constant , the displacement tends to damp out quickly . This result is anticipated . As q increa- ses with a and k remaining unchanged , the displacement tends to approach the ...
Seite
... the integral along the perturber's classical straight - line path of the interaction energy V ( t ) divided by : Þ ( p , v ; ) = √ _`_V ( t ) / 1⁄2 dt = -S V ( vp2 + v ̧3ï3 ̄ ) di / K - ∞ where h / 2π ; h is the Planck constant .
... the integral along the perturber's classical straight - line path of the interaction energy V ( t ) divided by : Þ ( p , v ; ) = √ _`_V ( t ) / 1⁄2 dt = -S V ( vp2 + v ̧3ï3 ̄ ) di / K - ∞ where h / 2π ; h is the Planck constant .
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... along the perturber's classical straight - line path of the interaction energy V ( t ) divided by : ∞ • ( p , v ; ) = S_V ( t ) / 1⁄2 dt - ∞ ∞ = ƒ ___ V ( v / p2 + v ̧3ï3 ̄ ) dik - where = h / 2π ; h is the Planck constant .
... along the perturber's classical straight - line path of the interaction energy V ( t ) divided by : ∞ • ( p , v ; ) = S_V ( t ) / 1⁄2 dt - ∞ ∞ = ƒ ___ V ( v / p2 + v ̧3ï3 ̄ ) dik - where = h / 2π ; h is the Planck constant .
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