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Na+, K+, Cs+ and Ca2+ are common exogenous cations that could be introduced into soils either via long‐term tillage with inorganic fertilizers or the leakage of nuclear waste. However, the manner in which they co‐adsorb and compete with the intrinsic potassium ions in illite, the response of intrinsic potassium (K′+), as well as the underlying mechanisms of these interactions, remain unclear. These...