✍ Scribed by C. Grimaldi; Z. Thomas; M. Fossey; Y. Fauvel; P. Merot
No coin nor oath required. For personal study only.
Chloride is a major anion in soil water and its concentration rises essentially as a function of evapotranspiration. Compared to herbaceous vegetation, high transpiration rates are measured for isolated trees, shelterbelts or hedgerows. This article deals with the influence of a tree hedge on the soil and groundwater Cl^−^ concentrations and the possibility of using Cl^−^ as an indicator of transpiration and water movements near the tree rows. Cl^−^ concentrations were measured over 1 year at different depths in the unsaturated zone and in the groundwater along a transect intersecting a bottomland oak hedge. We observed a strong spatial heterogeneity of Cl^−^ concentrations, with very high values up to 2 g l^−1^ in the unsaturated zone and 1·2 g l^−1^ in the upper part of the groundwater. This contrasts with the low and homogeneous concentrations (60–70 mg l^−1^) in the deeper part of the groundwater. Cl^−^ accumulation in the unsaturated zone at the end of the vegetation season allows us to identify the active root zone extension of trees. In winter, upslope of the tree row, downwards leaching partly renews the soil solution in the root zone, while the slow water movement under the trees or farther downslope results in Cl^−^ accumulation and leads to a salinization of the soil and groundwater. This salinization is of the same order as experimental conditions produce negative effects on oak seedlings. The measurement of Cl^−^ concentrations in the unsaturated zone under tree rows at the end of the vegetation season would indicate whether certain topographic, pedological or climatic conditions are likely to favour a strong salinization of the soil, as observed in the present study. Copyright © 2009 John Wiley & Sons, Ltd.
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