Across
- 1. Percentage of soil volume made up of pore space.
- 3. Downward movement of water through soil layers.
- 4. Clumps of soil particles; improve structure and water retention.
- 6. Large pores that drain freely and allow air movement; poor water retention.
- 8. Compression of soil reducing pore space and limiting root development.
- 9. Describes soil by particle size; affects drainage and workability.
- 11. Soil type with balanced proportions of sand, silt, and clay; ideal for plant growth.
- 12. How well soil removes excess water; influenced by texture and slope.
- 14. Measure of soil acidity or alkalinity; affects nutrient availability.
- 16. Small pores that hold water too tightly for plant uptake; help resist compaction.
- 17. Entry of water into soil from the surface.
- 18. Medium pores that retain water available to plants.
Down
- 2. Arrangement of soil particles into aggregates; affects porosity and root growth.
- 5. A distinct layer in the soil profile, such as topsoil (A) or subsoil (B).
- 7. Mass of dry soil per volume; high values indicate compaction and poor root penetration (two words, no space).
- 10. Upward movement of water through pores; supports plant hydration.
- 11. Nutrient loss due to water movement through soil.
- 13. Air-filled pore space in soil; essential for root and microbial respiration; reduced by compaction.
- 15. Stable organic matter from decomposition; improves structure, nutrient retention, and water holding.
