Forest water balance model
- Silva Joint Research Unit
Drainage is the water output, lateral or vertical, from a plot of soil. Biljou© is a mono-dimensional model in which water flows move vertically. This model adapts perfectly to sites with no slope or those for which it is assumed that lateral water inputs and water outputs are equal but reproduces poorly for other conditions, such as sites where water accumulates. These particular topographic situations require mobilizing 2D or 3D models based on different designs and are considerably more difficult to parameterize.
Vertical drainage is difficult to measure accurately and is not routinely performed on experimental sites. Tools such as lysimeter plates (which collect free water using gravity) or porous tubes (water extraction via vacuum) exist for measuring drainage water and are used to collect samples at different depths in the soil for chemical analysis.
Collection of soil water through porous tubes (left) and lysimeter plates being installed in the soil (right). The soil solutions are collected in bottles (below)
However, these devices do not provide quantitative measurements of drainage flow, mainly because the magnitude of the collection area is unknown: in a given soil horizon, this area may be larger or smaller than the surface of the plate. Our approach is to calculate drainage by the difference (see the page Water Balance) between incident rainfall and actual evapotranspiration. Like the other water fluxes, the flow of drainage water is expressed in mm (1 mm = 1 L / m²).
Water flow or drainage flow corresponds to varying rates of displacement of free water in the soil.
Two situations are possible :
Drainage can occur throughout the year through the processes described above. Drainage is naturally higher during periods of heavy rainfall. At its maximum, drainage will equal incident rainfall (when the soil is at field capacity and when there is no transpiration). Refer to the page Water balance modelling for more information on calculating drainage in the soil layers.
Little quantitative information is available on this issue to date, but we do know that from the decimetre scale, significant spatial variability in drainage exists relative to soil texture, structure, bulk density heterogeneities and as such, variability in soil porosity.
We performed simulations in a temperate climate over the course of a wet year and a dry year, in three forest types: coniferous, deciduous with high leaf index and deciduous with low leaf area index:
|drainage (in mm)|
(2002, 1158 mm)
drainage (in mm)|
(1996, 676 mm)
|deciduous high LAI||557||237|
|deciduous low LAI||586||247|
Ballif JL, Dutil P (1983) Lysimétrie en sol de craie non remanié. I - Drainage, évaporation et rôle du couvert végétal. Résultats 1973-1980. Agronomie, 3, 857-866.
Badeau V, Ulrich E (2008) RENECOFOR - Etude critique de faisabilité sur : la comparabilité des données météorologiques « RENECOFOR » avec celles de Météo France, l’estimation de la réserve utile en eau du sol et le calcul des volumes d’eau drainée en vue du calcul de bilans minéraux sur les placettes du sous-réseau CATAENAT. Editeur : Office National des Forêts, Direction Technique et Commercial Bois, ISBN 978 – 2 – 84207 – 323 – 7, 108 p. et 166 pages annexes.
Beven K, Germann P (1982) Macropores and Water Flow in Soils. Water Resources Research, 18 (5), 1311-1325.
Klinge R, Schmidt J, Fölster H (2001) Simulation of water drainage of a rain forest and forest conversion plots using a soil water model. Journal of Hydrology, 246, 82-95.
Minderman G, Leeflang K W F (1968) The amount of drainage water and solutes from lysimeters planted with either oak, pine or natural dune vegetation, or without any vegetation cover. Plant and Soil, XXVIII, n°1 February 1968, 61-80.