The soil type Dystrophic Red
Latosol of B horizon was used with the following chemical characteristics: pH in water = 4.7, pH Ca[Cl.sub.2]= 4.2, organic matter = 8.2 g [kg.sup.-1]; P = 1.0 mg [dm.sup.-3]; K = 0.5 [mmol.sub.c] [dm.sup.-3]; Ca = 4.0 [mmol.sub.c] [dm.sup.-3]; Mg = 2.0 [mmol.sub.c] [dm.sup.-3]; Al = 14.1 [mmol.sub.c] [dm.sup.-3]; H+Al = 76.0 [mmol.sub.c] [dm.sup.-3]; sum of bases = 6.5 [mmol.sub.c] [dm.sup.-3]; cation exchange capacity = 82.5 [mmol.sub.c] [dm.sup.-3] and base saturation = 7.9%, it was determined using the methodology described by Claessen (1997).
The experimental area 1,552 mm annual average length and Dark Red
Latosol soil.
Clay-rich yellow
latosol predominates, and the topography varies from flat to smooth wavy.
Oxidizable carbon fractions in Red
Latosol under different management systems.
The soil was classified as Dystrophic Red - Yellow
Latosol (EMBRAPA, 2013).
Seedlings of soybean and purple nutsedge were planted at the same time in plastic pots with a diameter of 25 cm which were filled with 3 kg of
latosol soil and base fertilizer i.e.
A clayey soil geotechnically classified as mature residual gneiss soil and pedologically as Red-Yellow
Latosol of expressive occurrence in the brazilian territory and, especially, in the Zona da Mata of the state of Minas Gerais was used thoroughly in this study.
Impact of simulated acid rain on trace metals and aluminum leaching in
Latosol from Guangdong Province, China.
Castro Filho C, Lourenf o A, Guimaraes MF, Fonseca ICB (2002) Aggregate stability under different soil management systems in a red
latosol in the state of Parana, Brazil.
Soil has a clay texture, classified as Eutroferric Red
latosol (Embrapa, 2006).