We have investigated two original hydrated cobalt arsenates based on Co 2+ octahedral edgesharing chains. Their different magnetocrystalline anisotropies induce different types of metamagnetic transition, spin-flop versus spin-flip. In both compounds, a strong local anisotropy (Ising spins) is favored by the spin-orbit coupling present in the CoO6 octahedra while ferromagnetic (FM) exchanges predominate in the chains. Co2(As2O7), 2H2O (1) orders antiferromagnetically below TN = 6.7 K. The magnetic structure is a non-collinear antiferromagnetic spin arrangement along the zigzag chains with DFT calculations imply frustrated chains and weakened anisotropy. A metamagnetic transition suggests a spin-flop process above 0H = 3.2 T. On the contrary, BaCo2As2O8.2H2O (2) linear chains are arranged in disconnected layers, with only inter-chain ferromagnetic exchanges and therefore increasing its magnetocrystalline anisotropy. The magnetic structure is collinear with a magnetic easy axis that allows a spin-flop to a sharp spin-flip transition below TN= 15.1 K and above 0H = 6.2 T.