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PHYSICAL-HYDRAULIC PROPERTIES OF A SANDY LOAM TYPIC PALEUDALF SOIL UNDER ORGANIC CULTIVATION OF 'MONTENEGRINA' MANDARIN (Citrus deliciosa TENORE)

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Academic year: 2019

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Table 1. Particle-size distribution, particle density (PD) and organic matter content (OM) in the Sandy Loam Typic Paleudalf
Table 2. Bulk density ( BD ), macroporosity ( Ma ), microporosity ( Mi ), and total porosity ( TP ) in the 0.00-0.15, 0.15-0.30, 0.30-0.45, and 0.45-0.60 m layers, in the interrows under disk harrowing, knocking down weeds using logs in “V”, mechanical mow
Figure 1. Water infiltration rate and accumulated water infiltration in three sampling sites: between the wheel tracks of the tractor (BWT), in the wheel tracks (WT), and under the projection of the canopy (CPL).

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