Defining the "ideal" soil structure in surface soil of a typic fluvaquent in the Netherlands

Traditional soil structure descriptions are static and qualitative. However , measurement of basic physical and chemical characteristics of a given soi l structure followed by simulation modeling of crop yields and water and nu trient regimes results in a dynamic and quantitative soil structure charact erization. Within any given soil series, different types of structure may o ccur as a result of different manage ment practices, and each structure typ e can thus be characterized. This, however, is a reactive approach in which soil structures are presented as given fact. This paper explores a proacti ve approach in which measurement of basic soil characteristics on a series of standardized structure samples and exploratory simulation modeling are u sed to define an "ideal" structure, using plant growth and nutrient-use eff iciency as indicators. Management practices to realize such an "ideal" stru cture remain to be designed by others. Quantitative indica tors for the "id eal" structure in the 0- to 30-cm surface soil of a loamy, mixed, mesic Typ ic Fluvaquent (a prime agricultural soil in the Netherlands) were based on simulated yields and associated nitrate leaching. Simulations considered wa ter supply capacity, occurrence of bypass flow and internal catchment, leac hing of nitrates as a function of fertilization scenarios, accessibility of water to roots, and trafficability in spring. Exploratory simulations, usi ng a validated model for a period of 30 yr to express temporal variability for a complete soil profile with varying topsoil structures, showed a struc ture consisting of 0.5-cm aggregates and a bulk density of 1.6 g cm(-3) to be "ideal" for the agricultural land use being considered.