Help connecting vector fields in ODE and Vector Calc

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SUMMARY

The discussion centers on the relationship between vector fields in calculus and direction fields in ordinary differential equations (ODEs). The vector field F= corresponds directly to the system dY/dt = {dx/dt = y, dy/dt = x}, establishing that direction fields and vector fields are indeed the same. Additionally, it is confirmed that level curves of the potential function f=xy form hyperbolas, which align with the isoclines of the ODE, indicating that isoclines in conservative fields are represented by the level curves of their potential functions.

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  • Understanding of vector fields in calculus
  • Familiarity with ordinary differential equations (ODEs)
  • Knowledge of line integrals and their applications
  • Concept of conservative and non-conservative fields
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  • Study the relationship between vector fields and direction fields in ODEs
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musik132
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The vector field F=<y,x> looks exactly like the the direction field for the system
dY/dt = {dx/dt = y}
{dy/dt = x}
A few questions on this:
Are the direction field of a system of ODE's the same as a vector field of calculus?
In vector calc we take the line integral of a vector field over some trajectory to find something like work. So if the direction field and vector field are the same does it mean that if given initial values and the work I can find the trajectory?

One more question: Suppose the potential of F=<y,x> is f=xy. The level curves of this function f are hyperbolas. When plotted they look like the isoclines of the ODE. If they are then do all isoclines of an ODE which is in the form of a conservative field, have isoclines that are formed by level curves of the potential? Does this extend to non conservative fields in anyway?I had trouble phrasing this question in google to find some relevant sources, does anyone have a good source to read up on this connection, if there is one?Thanks ahead of time
 
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Yes, the "vectors" in ODEs are the same as "vectors" in Calculus. Yes, the level curves are curves of constant potential and so are "isoclines". You can also think of them as being the curves of constant altitude in a geodetic map.
 
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