GRAVEL MULCHING IN VINEYARDS OF SOUTHERN SWITZERLAND

Citation
J. Nachtergaele et al., GRAVEL MULCHING IN VINEYARDS OF SOUTHERN SWITZERLAND, Soil & tillage research, 46(1-2), 1998, pp. 51-59
Citations number
13
Categorie Soggetti
Agriculture Soil Science
Journal title
ISSN journal
01671987
Volume
46
Issue
1-2
Year of publication
1998
Pages
51 - 59
Database
ISI
SICI code
0167-1987(1998)46:1-2<51:GMIVOS>2.0.ZU;2-U
Abstract
The growing awareness of the potential of traditional agricultural tec hniques has resulted in a recent scientific interest in these techniqu es. As modernisation and mechanisation often lead to the abandonment o f these measures, it is vital to document them. Gravel mulching is suc h a traditional technique that is still practised in Chamoson (souther n Switzerland). As no written information about this technique in Cham oson was found, an inquiry was set up amongst the wine-growers of Cham oson. The main objective of this inquiry is to document gravel mulchin g, based on the experiences of the wine-growers themselves. The result s of the inquiry showed that these practitioners in Chamoson consider the effects of the gravel mulch on the thermal (temperature) and hydra ulic (infiltration and evaporation) characteristics of the soil, to be the most important for wine-growing. In addition to the inquiry, fiel d experiments were set up to investigate the effects of a gravel mulch on soil temperature and evaporation during summer. The results of the se experiments show that a gravel mulch causes a significant increase in the soil temperature at two measured depths (mean increase of 0.97 degrees C at 3-cm depth and 1.5 degrees C at 10 cm; measuring period: 21/07/94-14/08/94) and at the surface (mean increase of 2.2 degrees C; measuring period: 24 h). As for the effect on evaporation, field expe riments show an increase of the cumulative evaporation depth, due to t he presence of a gravel mulch. This unexpected result can be explained when considering the soil characteristics of the mulched field (i.e., a very stony topsoil with a discontinuous mulch) and the rainfall reg ime during the measuring period (limited amounts of rainfall; non-satu rated soils). The results of the evaporation experiment in the field, agree with the results from similar laboratory experiments reported in the literature. (C) 1998 Elsevier Science B.V. All rights reserved.