The recovery of soil biochemical properties under grazed, grass-clover pasture, after simulated lignite mining, was studied over a 5-year period in a mesic Typic Dystrochrept soil at Waimumu, Southland, New Zealand. The restoration procedures involved four replacement treatments, after A, B, and C horizon materials had been separately removed, from all except the control, and stockpiled for 2-3 weeks . In each replacement treatment, the effects of ripping to 1 .8 m depth, mole drainage, and the use of fertilizer nitrogen were also investigated .Replacement treatment markedly influenced the recovery of herbage production and soil organic C and total N contents, N mineralization, microbial biomass (as indicated by mineral-N flush) and invertase and sulphatase activities . The effectiveness of replacement treatments decreased in the order : 1 . control (no stripping or replacement) . 2 . A, B, and C horizon materials replaced in the same order . 3. A, B, and C horizon materials each mixed with an equal amount of siltstone overburden and replaced in order, 4 . A and B horizon materials mixed before replacing over C horizon material.Ripping increased herbage production, net N mineralization, and to some extent microbial biomass . Drainage had little, if any, effect .Fertilizer N also stimulated herbage production, but depressed clover growth . Over 2 .5 years, it had little detectable effect on the soil properties .Increases in soil invertase and, to a lesser extent, sulphatase activity during the trial were closely related to changes in herbage production . Microbial biomass increased more rapidly than did soil organic C in the early stages of the trial .Rates of net N mineralization strongly suggest that N availability would have limited pasture growth, especially in the treatments with mixed soil materials .