Liquid hog manure (LHM) is a valuable source of nutrients for farm production. Long-term experimental plots that had received LHM applications of 0, 50, and 100 m(3) ha(-1) annually for 20 years were analyzed for total soil C, N and P storage. Applications increased total soil N and P by 1,200 kg N ha(-1) and 850 kg P ha(-1) at 100 m(-3) LHM year(-1), compared to the control treatment. However, C storage did not increase with LHM rates and was lower in the 50 m(3) ha(-1) LHM treatment (86 Mg C ha(-1)) than in the 0 or 100 m(3) ha(-1) treatments (100 Mg C ha(-1)). In addition to the limited quantities and high decomposability of the C supplied by LHM, it is hypothesized that LHM stimulated the mineralization of both native soil C and fresh root-derived material. This priming effect was particularly apparent in deeper soil horizons where the decomposability of native C may be limited by the supply of fresh C. This study indicates that while LHM can be a significant source of crop nutrients, it has limited capacity for maintaining or increasing soil C.