some stuff I found on the internet. AWC is available water capacity WRC is Water retention characteristics. Who knew crushed bricks held so much water ? And lava holds water like sand which is not much.
https://www.tandfonline.com/doi/full/10 ... 18.1447293
Porlith has a high AWC of 0.38 m3m−3, which is in a comparable magnitude with the one for bricks (up to 0.4 m3m−3; Blume and Runge 1978; Nehls et al. 2013). These comparable water retention characteristics can be attributed to similarities of the structure of these two materials.
For tuff, the measured FC (0.23 m3m−3) exceeds the reported values of 0.10 m3m−3 (Da Silva et al. 1993) and 0.12 m3m−3 (Wallach et al. 1992). The tuff studied in this work has, accordingly, more pores able to retain water in the range of the AWC.
Expanded clay, expanded shale, and pumice have similarly low FC and AWC compared to tuff and porlith. The expanded clay has a ceramic cover, which is likely to disrupt the capillary continuum and thus hinders the uptake of water (see the structure of the material in Fig. 2). Expanded shale shows a low and narrow amount of pores retaining water in between pF 1.8 and pF 3.0, draining almost completely at pF > 3.0.
Regarding pumice, previous research on its porosity shows that it has a wide pore size spectrum and that shape and connectivity of the pores depends on the origin of the pumice (Whitham and Sparks 1986; Lura et al. 2004). Gunnlaugsson and Adalsteinsson (1994) report that the majority of pumice is composed by closed, occluded, or dead-end pores not available for water storage. This particular porosity may also be present in our studied material, and it can be reflected in the high variance of the WRC (Fig. 2) at pF ≤ 2.5 (SD = 0.007 m3m−3), and pF 3.0, with a SD = 0.053 m3m−3. For higher suctions (pF > 4.0), the values are more consistent as the materials were crushed prior measurement.
Lava has a very low AWC. Its water retention characteristics are quite similar to the ones of the sand of our study. The low AWC is mainly attributed to its large pore sizes >50 μm, some of them clearly visible, as depicted in Fig. 2.