A Laboratory Manual for X-Ray Powder Diffraction
It may be necessary to dissolve the carbonates in some limestones and sediments before the clay minerals can be identified. However, treatment with strong acids to remove carbonate can attack the structure of clay minerals (e.g. trioctahedral minerals are often destroyed by such treatment), and even dilute acid can attack the silicate layers via interlayer regions and exposed edges. Generally, dilute acetic acid is preferred over hydrochloric acid because it less likely to affect clay crystallinity.