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Article << Previous     |     Next >>   Contents Vol 43(3)

Temporal dynamics of water repellency and soil moisture in eucalypt plantations, Portugal

Gemma Leighton-Boyce A D, Stefan H. Doerr A, Richard A. Shakesby A, Rory P. D. Walsh A, António J. D. Ferreira B C, Anne-Karine Boulet B, Celeste O. A. Coelho B

A Department of Geography, University of Wales Swansea, Singleton Park, Swansea SA2 8PP, UK.
B Centro das Zonas Costeiras e do Mar, Departamento de Ambiente e Ordenamento, Universidade de Aveiro, P-3810-193 Aveiro, Portugal.
C Environmental Technologies Sector, Department of Pure and Environmental Sciences, ESAC, IPC, Bencanta, P-3040-316 Coimbra, Portugal.
D Corresponding author. Current address: Komex International Ltd., 4500 16 Avenue NW, Calgary, Alberta T3B OM6, Canada. Email: gleightonboyce@calgary.komex.com
 
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Abstract

This paper investigates water repellency and soil moisture under 4 different Eucalyptus globulus plantations in Portugal. On 8 occasions over a 16-month period, measurements were made at 3 depths (surface, 0.10 and 0.20 m) at 60 points on four 10 by 18 m grids. The main results are: (i) at all sites and depths, spatial frequency of repellency (defined as percentage of repellent grid points) followed a moisture-related seasonal cycle, its amplitude being greatest for the longest established site, where surface repellency was contiguous in dry late-summer conditions, but was entirely absent after wet winter conditions; (ii) at a few points at 2 sites, repellency persisted during winter; (iii) repellency severity was dichotomously distributed regardless of season (i.e. soils were generally either wettable or highly repellent); and (iv) at the longest established site, when soil moisture was <14% soils were repellent, and when soil moisture was >27% soils were wettable. This may either support the existence of a ‘transition zone’, or be an artefact of the different scales of repellency and soil moisture assessments. Reasons for the observed changes in repellency and their relationship with soil moisture and antecedent rainfall are explored and soil hydrological implications discussed.

Keywords: water repellence, repellency severity, %Ethanol method, hydrophobicity, Eucalyptus globulus, overland flow, time domain reflectometry, transition zone.


   
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