natural body comprised of solids (minerals and organic matter), liquid, and gases
pedalogy
science dealing with the study of soils
pedogenesis
deals with soil formation or soil origin
supports plant growth
contains nitrogen, phosphorus, potassium, and other bio elements
habitat for animals and microorganisms
essential for water filtration
Soil forms through the accumulation and decay of organic matter and through physical, biological, and chemical weathering processes
process that breaks down rocks and minerals into smaller pieces
mechanical breakdown of rocks without changing their chemical composition
examples:
involved the chemical alteration of minerals within the rock
ex: Chocolate Hills, Philippines
involves the breakdown of rocks by living organisms
parent material
rocks from which the soil derived
climate
temperature and rainfall impact soil formation
time/age
time of formation
topography
differences in land elevation and slipe
high elevations = dry and thin soil
biota
plants, animals, and microorganisms contribute to soil structure and nutrient cycling
distinct horizontal layers of soil
O-Horizon: humans or organic matter
A-Horizon: topsoil, rich in minerals and organic matter
B-Horizon: subsoil, contains leached materials
C-Horizon: weathered parent material
R-Horizon: regolith, bedrock
soil profile: cross-sections, showing soil horizons
sand: 40%, silt: 40%, clay: 20%
good drainage: allows water to drain well
fertility: holds nutrients better than other soil but also provides better drainage
structure: loose texture: important for root development
pH: neutral to slightly acidic
percentage of a material’s volume that is pore space
more porous = more water it can hold
measures how easily fluids can flow through a material
black-brown: high organic matter
red-orange: oxidized; high iron content
yellowish-white: rich in clay minerals
gray: high moisture
determines the type and growth of plants that can thrive in it
solubility of some minerals needed for plant growth are pH dependent
common soils: 4 to 2
ideal pH: 6.5-7.5
nitrogen
needed by plants for cell-formation
nitrogen deficiency
yellowish brown colors along veins and tips of leaves, stunted growth, pale color of older leaves
phosphorus
essential for seed and root development
low P: stunted growth, late maturity of plants; weak plants with purple streaks in the stems
potassium
essential for strong and sturdy stems and advances root growth, resists diseases
low K: stunted growth, weak stem
decline in the quality and health of soil → loss of its ability to support healthy plant growth and perform essential ecological functions
causes
intensive farming practices (excessive tilling, overuse of chemical fertilizers)
inadequate soil conservation measures
characterized by the intense weathering of rocks and minerals
forms laterites: high in iron and aluminum oxides but low in nutrients
cause: deforestation (exposes the soil, minerals are washed away)
removal of topsoil → leads to thinning of soil, loss of nutrients and fertility → use of more fertilizers
causes
deforestation
human mismanagement of soil
conversion of agricultural croplands to deserts (cropland abandonment)
causes
drought
deforestation
over cropping
mining
poor agricultural practices
decomposition of organic waste by microorganisms into CO2, water and humans
compost - good soil conditioner
crop rotation and mixed crop cultivation to distrust life cycles of pests
biological controls (ex: wasps, mantis)
biogenetics (pest-resistant plants)
use of biopesticides
monoculture leads to soil infertility
depletes the natural nutrients of the soil faster
multi-cropping
various crops in one field
crop rotation
different crops in the same field over a period of time
prevent soil erosion
contour plowing
plowing and planting across the slope of the land, following its natural contours
terracing
creating flat areas or “steps” on a slope to create level platforms for planting
reforestation
replanting of trees in a previously forested area
afforestation
establishing a forest in an area where there was no forest before