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Soil physics

Water retention characteristics of coarse porous materials to construct purpose-designed plant growing media

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Pages 181-189 | Received 25 Jul 2017, Accepted 27 Feb 2018, Published online: 21 Mar 2018
 

ABSTRACT

Among potential components to construct Technosols for urban greening purposes, the commercially available geogenic coarse porous materials (CPMs) are mainly used in practice because of their high porosity. However, the knowledge of the hydraulic behavior of CPMs as well as of their mixtures with other substrates is limited, provoking their suboptimal usage. Therefore, we determined the water retention characteristics, including the available water capacity (AWC) of six geogenic CPMs: porlith, expanded shale, expanded clay, tuff, pumice, and lava. In order to obtain the water retention characteristics of the CPMs as well as of their mixture with sand (1:4 per volume), the following methods adapted from soil physics were applied over a wide range of pressure heads: Equi-pF apparatus, ceramic tension plates, pressure plate extractors, WP4C apparatus, and water vapor adsorption. The results were used to parametrize the modified Kosugi model (using SHYPFIT 2.0). Porlith and tuff have the highest AWC (0.37 m3 m−3 and 0.17 m3 m−3, respectively) and are the only ones which can be recommended as effective water-retaining materials. Further materials exhibit an AWC less than 0.10 m3 m−3. The CPMs exhibit a bimodal pore size distribution, which can be well described by the applied model, except for pumice and expanded shale. The mixtures present overall low AWCs up to 0.07 m3 m−3, with the pure sand having less than 0.03 m3 m−3. For practical application a quite high ratio of CPM is needed, and the mixing material must be adapted to the hydraulic properties of the CPMs. The water inside the CPMs may be easily available for plant roots able to penetrate in the CPMs’ coarse pores.

Acknowledgments

This work was supported by the Deutscher Akademische Austauschdienst (DAAD, German Academic Exchange Service) under Grant A/10/80575. We thank Dr. Peter Dominik for his contribution of ideas and for the constructive discussion.

Notes

Additional information

Funding

This work was supported by the Deutscher Akademischer Austauschdienst (DAAD, German Academic Exchange Service) under Grant A/10/80575.

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