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SOLID PHASE
Consists of minerals (gravel,
sand and silt) and organics
(humus, plant and crop
residues)
LIQUID PHASE
It is called as soil solution. It
consists of water with dissolved
minerals and nutrients.
Oxygen and carbon dioxide can
also dissolved in the soil
solution.
GASEOUS PHASE
It occupies the pore space that
is not filled with water.
Nitrogen, oxygen, water
vapor, and carbon dioxide are
the primary gases from the air
and living organisms.
Filtration
It is the capture and subsequent
degradation of manure solids in the soil
matrix.
Biological degradation
The physical properties of the soil such as
temperature, moisture oxygen supply,
pH, and nutrients affects the microbial
growth and metabolism.
ION EXCHANGE
ADSOPRTION
PRECIPITATION
COMPLEXATION
Chemical reactions
Ion exchange
includes cations and anions
wherein the positivelty/negatively
charged particles of waste is exchanged
with soil particles and organic materials.
Adsorption
occurs when the ions are
attached to soil surface
precipitation
occurs when soluble
compounds is deposited in soil voids.
Complexation
is the interaction of
metals with soil organic matter and
some oxides and carbonates, resulting
in the formation of large, stable
molecules.
Mineralization
occurs through physical, chemical
and biological conversion of waste into inorganic
forms making them available to plants.
Organic waste mineralization
a process where
microbes digest organic waste to convert into
inorganic or more stable organic materials.
Cation Exchange
Capacity (CEC)
The ability of the soil to hold nutrients and release
them through chemical reactions for plant uptake.
pH
A measure of the level of acidity or alkalinity in the
soil. It is essential for plant nutrition, growth and soil’s
biological and chemical activity.
Bulk Density
Amount of solid particle weight per volume of such
mass of soil. It reflects the level of porosity (void
space in the soil that can be filled by air or water) and
compaction of the soil. Compacted soils (higher bulk
density) have less porosity, lower air content, lower
water infiltration, and poor plant growth.
Soil Aggregate
Stability
Amount of solid particle weight per volume of such
mass of soil. It reflects the level of porosity (void
space in the soil that can be filled by air or water) and
compaction of the soil. Compacted soils (higher bulk
density) have less porosity, lower air content, lower
water infiltration, and poor plant growth.
Earthworms
Population
Earthworms help accelerate biomass decomposition,
nutrient cycling and building a better pores system for
water infiltration and retention.
MICROBIAL BIOMASS Carbon and
Microbial
Respiration
Laboratory measurement used as an indicator of the
microbial abundance in the soil. Both are directly
related to the general biological activity, which
influences the nutrients availability for crops and the
generation of the substances that act as a “glue” to
help build more stable soil aggregates.
Macronutrients
are the building blocks
for plant growth which is required in
large quantities. It includes nitrogen,
phosphorus, magnesium, and
potassium. Nitrogen, phosphorus,
magnesium, and potassium are non-
mineral class of macronutrients.
phosphorus
magnesium
potassium
Nitrogen
MACRONUTRIENTS
Micronutrients
elements required
for balance growth of plants which
constitute in less than 1% of its dry
weight. Essential micronutrients
includes boron (B), zinc (Zn),
manganese (Mn), iron (Fe), copper
(Cu), molybdenum (Mo), chlorine (Cl).
boron
ZINC
MANGANESE
IRON
COPPER
MOLYBDENUM
CHLORINE
MICRONUTRIENTS
Groundwater
recharged naturally by rain
through infiltration and deep percolation.
NITRATE
Excessive ____ consumption can cause
methemoglobinemia (“blue baby syndrome”),
PHOSPHORUS
Excessive
_____ consumption can cause problems with bones.
PATHOGENS
contaminates groundwater such as various
bacteria, viruses, and protozoa causes different outbreaks.
HEAVY METALS
agricultural wastes such as arsenic,
fluoride, mercury, and lead, also contaminates groundwater.