Across
- 4. helps you determine classifications for soil textures.
- 7. Flat peds that lie horizontally in the soil.
- 12. the strength of the ped.
- 13. how much water is retained by soil particles.
- 14. When soil particles cling together in an arrangement known as a ped.
Down
- 1. Roughly spherical, like grape nuts. Plant roots, microorganisms, and sticky products of organic matter decomposition bind soil grains into granular aggregates.
- 2. how quickly water moves through soil.
- 3. pores in the soil created by: Roots and other organic matter (i.e., decaying substances) Animals, such as worms and rodents. Soil particle size and "fit"
- 5. the zone, which plant roots can
- 6. the shape of the ped.
- 7. Larger, vertically elongated blocks, often with five sides.
- 8. Every grain acts independently. No binding agent holding grains together. Permeability is rapid.
- 9. Roughly cube-shaped, with more or less flat surfaces. Blocky structures are typical of B horizons.
- 10. Compact, coherent soil not separated into peds. Small pores, slow permeability, and poor aeration.
- 11. grow.
