“…Still another theory suggests that lime reacts directly with clay edges, forming a network of cementatious materials (Stocker, 1972). Optical studies show evidence that all of these processes may occur in clay-limewater systems (Ormsby and Bolz, 1966;Ford et aI., 1982). Some of the major factors that influence soil's ability to react with lime are soil pH; organic carbon content; natural drainage; presence of excessive quantities of exchangeable sodium; clay mineralogy; degree of weathering; presence of carbonates, sulfates, or both; extractable iron; sesquioxide ratio; and silica-alumina ratio.…”