It is demonstrated that nitroaromatic compounds (NACs) may adsorb specifically and reversibly to natural clay minerals in aqueous suspension. Adsorption of NACs to clays is high when the exchangeable cations at the clays include K+ or NH4+ but is negligibly small for homoionic Na+-, Ca2+-, Mg2+-, and Al3+-clays. Highest adsorption coefficients (Kd values up to 60 000 L kg(-1)) are found for polynitroaromatic compounds including some important contaminants such as explosives (e.g., trinitrotoluene, trinitrobenzene, dinitrotoluidines) and dinitrophenol herbicides (e.g., DNOC, DINOSEB). Nonaromatic nitro compounds (e.g., RDX) generally exhibit very low K-d values. The specific adsorption of NACs can be rationalized by electron donor-acceptor (EDA) complex formation with oxygens present at the external siloxane surface(s) of clay minerals. K-d values of a given NAC and clay mineral can be estimated from known K-d values of other NACs, even when measured at other clay minerals. The affinity and the adsorption capacity of the clays for NACs increase in the order kaolinite ( illite < montmorillonite. Thus, clay minerals, depending on their abundance and degree of K+- (or NH4+) saturation, may control the phase distribution and thus the mobility and (bio)availability of NACs in soils and aquifers. Implications of the results with respect to remediation measures at contaminated sites are discussed.