We study field-induced incommensurate–commensurate transitions (ICTs) in classical spin chains with Dzyaloshinskii-Moriya interaction (DMI) , strong easy-plane anisotropy, and weak easy-axis anisotropy within the easy plane. This model describes systems with ferromagnetic layers coupled by exchange interaction with DMI. The magnetic field is applied in the easy plane at an arbitrary angle to the easy axis stabilizing a soliton lattice in the ground state. We consider ferromagnetic and antiferromagnetic in-chain exchange interactions within the continuum limit and show that the easy-axis anisotropy leads to qualitatively different effects in these two cases: the ferromagnetic chain is described by a double-sine-Gordon-type equation with phase-shifted harmonics, whereas the antiferromagnetic chain reduces to a sine-Gordon equation. For the latter case, phase boundaries between incommensurate and commensurate states are found analytically in space and confirmed by numerical calculations for certain and values. Close to all ICTs, results of the continuum consideration become invalid due to a stochastic destruction of near-separatrix solutions which either make an ICT a first-order transition or stabilize states with spatially irregular soliton and antisoliton arrangements.

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