Passive absorption of mineral salts occurs through simple diffusion down a concentration gradient without expending metabolic energy. Several theories have been proposed to explain the mechanism of passive absorption, including diffusion, ion exchange, Donnan equilibrium, and mass flow. Diffusion involves the net movement of minerals from high to low concentration until equilibrium is reached. Ion exchange involves replacing ions on the surface of cell walls. Donnan equilibrium describes the balance of ions across a selectively permeable membrane. Mass flow theory states that minerals are absorbed with water flow into roots during transpiration. However, some objections to purely passive absorption have been raised, as metabolic activities and accumulation against gradients have been observed.