Soil porosity changes in orchards with subsurface irrigation: quantification and interpretation

  1. Rosa M. Poch
  2. Josep M. Villar 1
  3. Miquel Pascual 1
  4. Josep Rufat 2
  1. 1 Universitat de Lleida
    info

    Universitat de Lleida

    Lleida, España

    ROR https://ror.org/050c3cw24

  2. 2 Parc Científic i Tecnològic Agroalimentari de Lleida
Revue:
Boletín de la Sociedad Geológica Mexicana

ISSN: 1405-3322

Année de publication: 2019

Tomo: 71

Número: 1

Pages: 1-10

Type: Article

DOI: 10.18268/BSGM2019V71N1A1 DIALNET GOOGLE SCHOLAR

D'autres publications dans: Boletín de la Sociedad Geológica Mexicana

Résumé

In order to assess the irrigation efficiency under water-limiting conditions, four different treat-ments of subsurface irrigation of peach trees in a semi-arid Mediterranean climate near Lleida (NE Iberian Peninsula) were tested. The treatments included pressurized air injection, deficit irriga-tion, full irrigation (as control) and an addition of rice husk around the pipe to improve porosity. Because the latter treatment improved physical conditions and resulted in better tree growth, a micromorphological study was conducted in order to understand the reason for this behaviour. The experiment was carried out in a commercial peach orchard (Prunus persica L.). The soil was a Xeric Torriorthent, with a loam texture, affected by salinity and with low organic matter content. One undisturbed block (30 cm each side) was taken from each treatment, and two vertical thin sections, 5 × 13 cm, including the subsurface pipe, were made. A fluorescent dye was added to the polyester resin to obtain UV light images of the porosity. The pore parameters and the pore size distribution were obtained for each treatment. Strong changes in the pore types of the four treat-ments are evident in the thin sections. Full and deficit irrigation treatments are characterised by a weakly developed subangular blocky structure, with a vesicular intra-aggregate structure. Deficit irrigation with air injection produced, in its upper part, a structure similar to the full and deficit irri-gation treatments. In the surroundings and below the pipe, where the effect of pressurized air was higher, the soil structure is apedal, with vesicles (bubbles), 200 – 500 μm in size. Porosity of the soil modified with rice husk is greater than that of the other three treatments: the 15 – 30 μm porosity fraction is double, and the larger fractions three times that of the other treatments. It contains many oval excrements of mites (probably Oribati-dae), 50 – 100 μm in size, associated with moder-ately decomposed rice husk tissues. We conclude that the modifications around the irrigation pipes that promoted faunal activity are very effective in conveying water to the soil in comparison to that of pressurized air, which only increases vesicular (non connected) porosity.