The mathematics of such phrases as “instantaneous impulse”, “in the direction of orbital motion”, and “perpendicular to the plane of the ellipse” should be mentioned.
Most objects separated from spacecraft were put in a convenient spot with respect to an astronaut, not thrown. But, they were not put perfectly at rest with respect to the astronaut, or the vehicle. When noticed, most were within a few meters of the astronaut, and not drifting at a visible rate. They were still lost irretrievably, because you can’t just go fetch it.
The thing is, the vector was very close to random in magnitude and direction. While not specifically impossible to solve, it’s not something you can do on a mission, because to do so you have to change the orbit of the spacecraft, and then calculate a new orbit to return to your mission rendezvous. Then you have to risk an astronaut’s life, and waste atmosphere, to go EVA to fetch it. Not really within reasonable parameters for most current mission capabilities.
On the other end of the range of problems, nuking an object as it moves toward Earth, the object will not break up into even sized pieces, but will rather break along its existing structural weak points, into objects of highly variable size. It is a necessary consequence of the same mathematics that the largest fragments will change vectors the least, barring some extraordinary coincidence of blast parameters, and object geometry. While the gut level expectation is for it to be a cone of objects blasting to one side or another, the blast characteristics in space will be very dependent on shape, surface characteristics, and tensile and compression strength of the object, which are pretty well unknowable.
Example: The object has a layer of accreted ice, and rock material several meters in depth. The bulk of it’s mass, however is iron, and relatively solid. The nearby nuke blast will not move the central mass nearly as much as it will the portions of the accreted material close inside the tangent cone from the blast center to the radial edges of the object. Even accreted material in the center surface (with respect to the blast center) would be moved from their current trajectory less than the edges. Computing how much blast, and just where to place it is an enormous engineering problem, and necessarily ends up being best guesses, and approximations.
Each fragment has a unique orbit after the first blast. Second attempts must involve immediate recalculation for each significant sized piece, and that requires observations of the new orbits for each as well. Then new calculations must be made for blast size, and placement for each piece that still represents a danger on the current orbital pass, and none of that tells you what happens when the detritus comes around again.
By the way, you have to have your second salvo in orbit, and ready, unless you start on the object several months before impact at a minimum. In the case of Comet Shoemaker-Levy 9, estimates made in six days or less before actual observed impacts were within a range of 1 - 7 minutes for impact with Jupiter. These objects had been under frequent observation by multiple astronomical instruments for more than two years. Three of the objects were later characterized as “missing” since there was no data on impacts for them, or observations showing where they were, if they missed Jupiter.
The math isn’t beyond us theoretically, but pragmatically, it’s too big a problem to solve in the time we would have to solve it by several orders of magnitude.
Tris