PEDOTRANSFER FUNCTIONS RELATED TO SPATIAL VARIABILITY OF WATER RETENTION ATTRIBUTES FOR LOWLAND SOILS

mães e bebés que tem lugar no que ele chama ((trocas rituais ou de rotina)).. facto, o que ele tem investigado são as tro- cas lúdicas que se dão na altura de

Keywords: Giuseppe Millico; La pietà d’amore; Ópera Nova; Ajuda; Antonio Lucchesi.. Giuseppe Millico e La pietà d’amore: de Nápoles a Lisboa ao Rio

Soybean and wheat grain yield as related to soil penetration resistance at a matric potential of -33 kPa in the 0.10-0.20 m layer under the tillage systems: CT- conventional

(2006) studied the combined effects of 1-MCP and CaCl 2 dips (1% for 2 min) and controlled atmosphere (3 kPa O 2 +10 kPa CO 2 ) on quality of fresh-cut strawberries, and observed

Water retention curves [soil water content (U, g g -1 ) as a function of matric potential (kPa)] cambisolic dystrophic Red-Yellow Latosol (LVAd), according to double van

As the soil water content for all dates presented parabolic trend, the parabolic trend surface parameters of equation (3) were plotted as a function of the date of sampling. The

ABSTRACT: Among the equations available to describe the relation between matric potential and soil water content, the soil water retention function, the most commonly used is