The plasma composition of the solar corona is characterised by a varying overabundance of elements with a low first ionization potential (FIP) compared to those with a high FIP – this is called the FIP effect. Typically, the strongest enhancement is observed in active regions, as well as in situ in the slow solar wind. The FIP effect is not observed in the solar photosphere, suggesting that the enhancement of low-FIP elements must take place in the chromosphere. The ponderomotive force model (Laming, 2004) suggests that the FIP effect is driven by Alfvén waves depositing their energy in the chromosphere and, in doing so, applying an upwards ponderomotive force on low-FIP elements which preferentially transports them to the corona. This seminar will focus on discussing how waves with different properties can deposit their energy at varying heights in the chromosphere and affect the plasma composition pattern, i.e. the relative abundance of different elements, observed in the corona. This work highlights the potential for using plasma composition measurement to obtain information about wave activity in the solar atmosphere and estimate the chromospheric height at which wave energy is deposited.