Soil Waste Management
Vermicomposting
- it is a process by which worms are used to convert organic materials into a humus like material known as vermin-compost.
What is a soil?
- according to natural resources conservation services (NRCS) soil is the unconsolidated mineral or organic material on the immediate surface of the earth that serves as a natural medium for the growth of land plants.
- Soil also forms in the PEDOSPHERE
What is pedosphere?
Pedosphere: is the foundation of terrestrial life/living skin of earth.
What does SOIL provides?
- water and nutrients to plants and microbes
- physical support system in which terrestrial vegetation is rooted.
- source and sink for the biogeochemical cycles of carbon, nitrogen, and sulfur.
- habitat for soil biota, mostly decomposers.
FACTORS AFFECTING SOIL FORMATION:
- parent material
- climate
- topography
- biological factors
- time
Soil texture: it refers to the composition of the soil in terms of the amounts of small (clays), medium (silts), and large (sands) particles.
Soil profile
- sequence of soil horizons from the surface down to the bedrock.
Regolith
- loose heterogenous and superficial material covering the bedrock.
SOILD ORDERS
- single dominant characteristics affecting soils in that location.
ORDERS:
- Alfisols: relatively high base saturation; not organic rich; evidence of clay transport.
- Andisols: derived major properties from volcanic parent material.
- Arid soils: low in organic matter
- Entisols: not well-developed even after long periods.
- Histosols: formed from organic matter
- Inceptisols: moderately weathered soils.
- Mollisols: high in organic matter, vermiculate or smectite.
- Oxisols: highly-weathered.
- Spodols: an organic matter transport
- Ultisols: low base saturation soils
- Vertisols: swelling days, frost, etc. cause lower horizons to mix with upper horizons.
- Gelisols: frozen soils.
Importance of soil
- arable land for agriculture
- regulating water and filtering potential pollutants
- nutrient cycling
- foundation and support
- mineral deposits