R unoff from agricultural land carries sediment and nutrients that can harm receiving water quality and degrade land productivity. Infiltration capacity and surface hydraulic conductivity of the soil is a principal factor in determining the amount of runoff resulting from a rainfall or irrigation event. Surface application of livestock manures alters surface hydraulic conductivity by forming a short-term soil-plugging effect, which reduces infiltration capacity and by acting as a longterm soil conditioner which improves the infiltration capacity. Hydrologic models are valuable tools in determining the effects of land-use practices on hydrology and water quality. To successfully model hydrologic responses and thus identify best management practices, a complete understanding of the infiltration process is necessary. This understanding must include the effects of agricultural practices such as tillage, manure application, etc., on infiltration. The hydrologic models must be adapted to changing soil surface conditions that are affected by altered agricultural practices and changing environmental conditions. The goal of this study was to determine the effect of livestock manure application on surface-seal formation. The specific objective was to review existing infiltration models that have been adapted for surface sealing or crust formation and to modify these models to predict water infiltration through the surface seal formed by manure application. The scope of this study required a nondestructive method for determining surface-seal properties of manure-amended soils. Modifications of these models will aid consultants and regulators dealing with manure application and water-quality issues in decisionmaking processes. LITERATURE REVIEW Many researchers have observed that a thin layer of reduced permeability forms on the surface of soil exposed to rainfall (Duley, 1939; McIntyre, 1958; Tackett and Pearson, 1965). This distinct layer is characterized by higher bulk density and lower porosity than the underlying soil. The term "surface seal" is commonly used to describe the effect this layer of reduced permeability has on limiting infiltration. Upon drying, the seal shrinks to form a hard crust that impedes seedling emergence and tears seedling roots as the seal cracks (Hillel, 1980). Knowledge of surface-sealing properties is required to model infiltration through a surface seal. Prediction of surface-seal characteristics is difficult, since surface-seal development is a function of several factors, including texture, initial bulk density, aggregate stability, initial shear strength, organic matter, tillage, and land-use practices (Sharma, 1980; Rawls et al., 1990), as well as rainfall intensity, second moment of drop-size density distribution, and maximal drop diameter (Assouline and Mualem, 1997). Little data has been published regarding surfacesealing characteristics in manure-amended soils. Many approaches have been proposed to describe infiltration through a stable surface seal. Hillel and Gardner (1970) conclude...