HYDRAULIC-PROPERTIES OF SPHAGNUM PEAT MOSS AND TUFF (SCORIA) AND THEIR POTENTIAL EFFECTS ON WATER AVAILABILITY

Citation
Ff. Dasilva et al., HYDRAULIC-PROPERTIES OF SPHAGNUM PEAT MOSS AND TUFF (SCORIA) AND THEIR POTENTIAL EFFECTS ON WATER AVAILABILITY, Plant and soil, 154(1), 1993, pp. 119-126
Citations number
29
Categorie Soggetti
Agriculture Soil Science","Plant Sciences",Agriculture
Journal title
ISSN journal
0032079X
Volume
154
Issue
1
Year of publication
1993
Pages
119 - 126
Database
ISI
SICI code
0032-079X(1993)154:1<119:HOSPMA>2.0.ZU;2-E
Abstract
The potential rate of water and nutrient supply to plant roots depends on the hydraulic properties of the container medium (growth medium, s ubstrate), primarily on its unsaturated hydraulic conductivity, which is a measure of the medium's resistance to water flow. Water availabil ity to plants grown in containers is usually being evaluated using cri teria based exclusively on water characteristic curves of the medium i n which the plant is grown. This approach is challenged in the present paper. We hypothise that the coarse structure of peat moss as well as of other container media may result in a sharp decrease in hydraulic conductivity, as the water content of peat is reduced. Transient chang es in unsaturated hydraulic conductivity may result in reduced water u ptake by plant roots. The objectives of this research were to determin e the hydraulic properties of sphagnum peat moss and to evaluate their potential effects on water availability. Tuff (granulated volcanic as h) and its mix with peat were also tested for comparison. Water charac teristic curves (drying and wetting cycles) and saturated hydraulic co nductivity were measured. A predictive mathematical model was used to calculate the unsaturated hydraulic conductivity of the media. Measure d water retention and saturated hydraulic conductivity data were used to estimate model parameters by a nonlinear least-squares curve-fittin g technique. Model predictions of unsaturated hydraulic conductivity w ere validated by direct measurements. Results showed that,sharp variat ions in hydraulic conductivity occur in a very narrow suction range (0 -2.5 kPa). In this range a decrease of more than three orders of magni tude in the unsaturated hydraulic conductivity was observed for peat. A similar trend was observed for the other media tested. This suggests that the approach that has been commonly used for determinations of w ater availability and for irrigation scheduling in container media may provide inaccurate predictions as to potential plant response.