Influence of arbuscular mycorrhizae on heavy metal (Zn and Pb) uptake and growth of Lygeum spartum and Anthyllis cytisoides

The hypothesis tested in this paper is that, because the freshest water occurs in the largest soil pores (macropores), plants of low to moderate transpiration rate can survive in salinized soil because they preferentially extract water from macropores. The hypothesis predicts that a plant growing in a macroporous soil should have greater growth under a given salinity treatment than a similar plant growing in a soil with the same mineralogy but without macropores. This hypothesis was tested by growing bell pepper (Capsicum annuum) in the greenhouse in pots filled with either a commercial fritted clay (a highly macroporous soil) or the same clay ground to a finer texture and sieved to remove macropores and produce a microporous soil. The pots sat in pans filled with salt water. Half of the pots were irrigated once a day with fresh water and the other half received no fresh water. Plants growing in the macroporous soil had greater growth for a given salinity treatment than the plants growing in the microporous soil under both the irrigated and non-irrigated conditions. Under the irrigated condition for the highest salinity treatment, the non-reproductive fresh weight per plant, total dry weight per plant and fruit fresh weight per plant was 114 g, 12 g and 50 g, respectively, for the macroporous soil and 47 g, 4.5 g and 5 g, respectively, for the microporous soil. The results of this study provide evidence to suggest that a better understanding of what constitutes a good structure in a saline soil may aid us in our efforts to improve the management of saline soils. We suggest that it may be possible to increase the agricultural production on salinized land by no-tillage agriculture which preserves macroporosity. Possible obstacles could be the tendency of field saline-sodic soils to swell and the unavailability of relatively fresh irrigation water in areas with saline soils.