A method of evaluating stabilization fluids for use in a subterranean formation having a clay composition is disclosed. The method features providing a plurality of replicant core samples representative of the composition of a subterranean formation. A plurality of stabilization fluids are introduced to the plurality of replicant core sample such that an eluted mixture is extracted from a second end of each replicant core sample. Afterwards, at least one property of the eluted mixture from each replicant core sample is determined.