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  • https://math.libretexts.org/Bookshelves/Analysis/Complex_Variables_with_Applications_(Orloff)/07%3A_Two_Dimensional_Hydrodynamics_and_Complex_Potentials/7.06%3A_More_Examples_with_Pretty_Pictures
    Φ(z)=log(z1)+log(z+1)=log((z1)(z+1))=log(z21). Now, as z approaches the y-axis from one side or the other, the argument of log(z21) a...Φ(z)=log(z1)+log(z+1)=log((z1)(z+1))=log(z21). Now, as z approaches the y-axis from one side or the other, the argument of log(z21) approaches either π or π. Farther away from the origin the flow stops being radial and is pushed to the right by the uniform flow. It is the point on the x-axis where the flow from the source exactly balances that from the uniform flow.

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