THE USE OF OLIVE MILL EFFLUENTS (MARGINES) AS SOIL CONDITIONER MULCH TO REDUCE EVAPORATION LOSSES

Citation
Hj. Mellouli et al., THE USE OF OLIVE MILL EFFLUENTS (MARGINES) AS SOIL CONDITIONER MULCH TO REDUCE EVAPORATION LOSSES, Soil & tillage research, 49(1-2), 1998, pp. 85-91
Citations number
20
Categorie Soggetti
Agriculture Soil Science
Journal title
ISSN journal
01671987
Volume
49
Issue
1-2
Year of publication
1998
Pages
85 - 91
Database
ISI
SICI code
0167-1987(1998)49:1-2<85:TUOOME>2.0.ZU;2-U
Abstract
This study evaluated the efficiency of waste by-products of olive oil extraction (called ''margines'') as a soil conditioner. Because of the adhesive, hydrophobic, and fertility properties of margines, their di rect effect on soil aggregation and on the changes of hydrodynamic soi l characteristics were assessed. The wet sieving technique and rainfal l simulation were used to determine the optimal application rate of th e soil conditioner on a loamy sand. The efficiency in reducing evapora tion losses of incorporation and surface application treatments with s traw mulch (450 g cm(-2)) and a bare untreated soil surface under labo ratory-controlled evaporativity of 10 mm day(-1) were compared. Moistu re content was determined by means of time domain reflectometry. It wa s concluded that the application of a straw mulch was very efficient i n controlling evaporation only during the initial stage of evaporation . A surface application of margines is not as effective in reducing ev aporation as incorporating them. The latter application reduced the ev aporation loss by almost 30%. When applying the models of Groenevelt e t al, [Soil Technol. 2 (1989) 279-285] and van Wesemael et al. [Phys. Chem. Earth. 20 (1995) 293-299] the two phases in the evaporation proc ess were identified. The drying coefficient k(d) introduced by Groenev elt et al. [ibid,] describes the second phase of the evaporation proce ss, and the proposed soil boundary condition coefficient k(b) by Groen evelt et al. [ibid.] and van Wesemael et al. [ibid,] describes the fir st phase as a function of the soil surface condition. (C) 1998 Elsevie r Science B.V. All rights reserved.