Table 4.
Important possible growing media (modified after Ter Berg, 2000).
| Substrate | Raw material | Characteristics | |||||
|---|---|---|---|---|---|---|---|
| AVa | WVb | OMc | Densityd | RDe | |||
| m3 m−3 | m3 m−3 | g g−1 | kg m−3 | kg m−3 | |||
| None | NFT | Nutrient film technique | – | 0.99 | 0 | – | – |
| DFT | Deep flow technique | – | 0.99 | 0 | – | – | |
| Aeroponic | Foggy nutrient solution | 0.99 | – | 0 | – | – | |
| Inert | Sand, gravel, or mixes | Granular material of fine divided rock and mineral particles | 0.20 depending on particle size | ||||
| Glass wool | Melted silica sand (1200°C) | f | |||||
| Foam | Phenolic foam granules based on mineral oil | f | |||||
| Rock wool | Melted basalt and lime stone after supply of coke (1600°C) | 0.04 | 0.94 | 0.02 | 1900 | 49 | |
| Lava | Brocken, sieved vulcanic stone | f | |||||
| Pumice | Porose, air filled vulcanic stone | 0.26 | 0.57 | 0.03 | 2000 | 431 | |
| Perlite | Morphous volcanic glass | 0.52 | 0.44 | 0.01 | 900 | 105 | |
| Vermiculit | Hydrous silicate mineral | f | 0.50 | 2500 | 70–100 | ||
| Vleece | Polyester, etc. | g | |||||
| Clay granules | Decompressed clay (1100°C) | 0 | 1870 | 489 | |||
| Polyurethan | Mix of mineral oil and di-isocyanat | 0.35 | 0.60 | 0.99 | 1190 | 78 | |
| Organic | Wood fiber | Pressed wood mill waste | 0.62 | 0.20 | 0.98 | 1440 | 87 |
| Saw dust | Different origins | g | |||||
| Peat | 0.14 | 0.79 | 0.96 | 1580 | 113 | ||
| Coco fiber | Different origins | 0.55 | 0.40 | 0.98 | 0.77 | ||
| Rice husks | Different origins | g | |||||
| Composts | Different origins | g | |||||
Suitability depends on availability, growing conditions, and experimental goal (Ter Berg, 2000).
Air volume;
water volume;
organic portion;
density of the solid matter;
bulk density;
physical and chemical characteristics insufficiently known;
depending on origin, produce characteristics may differ significantly.