Which soil texture is easier to change pH?

Sandy soils are easier to change pH because of their larger particle size and lower nutrient and organic matter retention compared to other types of soil. The structure of sandy soil allows for rapid drainage and the leaching of nutrients and ions, which means that amendments such as lime or sulfur can be applied more effectively and will react quicker within this soil texture.

In sandy soils, there’s a greater potential for adjusting the pH because the soil has a lower buffering capacity. This means it doesn't resist changes to pH as much as soils with finer textures, like clay or silty soils, which have higher cation exchange capacities and can retain nutrients and pH-altering elements. With loamy soils, which combine sand, silt, and clay, the pH change would also be slower than in sandy soils due to their balanced textures.

Therefore, the rapid response of sandy soils to pH-altering practices makes them easier to change in comparison to other soil types.