Click on image to view larger version.


Figure 4


Fig. 4. Effective porosity,{theta}C0, calculated using the minimum equivalent pore radius (C0) for a given tension range (Eq. [8], dark points) and effective porosity, {theta}{Delta}{Psi}, computed from the representative mean pore radius for two consecutive soil water tensions, {lambda}{Delta}{Psi}, (Eq. [11], white points) measured under conventional tillage (CT), reduced tillage (RT), and no-tillage (NT). Macropores are defined as those pores that drain at {Psi} > –4 cm and mesopores as those pores draining at {Psi} between –4 and –14 cm. Asterisks indicate significant difference between {theta}C0 and {theta}{Delta}{Psi} (P < 0.05, t-test).