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Flashcards covering vocabulary terms for soil fertility.
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Soil
Weathered upper surface of the Earth's crust that supports plant growth
Soil Forming Factors
Parent Material, Climate, Topography, Organisms, Time, Humans
Aeolian
Wind blown sediment
Soil Forming Processes
Additions, Losses, Translocations (up and down), Transformations (chemical change)
Soil Physical Processes
Color, Texture, Structure, Profile, Density, Pore Space, Aggregation, Water-Holding Capacity
Sand
Gritty
Silt
Smooth
Clay
Sticky
Soil Textural Classes
Sand - 50%, Silt - 15%, Clay - 35%
Soil Structure
Granular < 0.5 cm, Platy, Blocky 1.5-5cm, Columnar, Single-grained
Particle Density
mp/vp
Bulk Density
mp/vb
Low pore space
High Db implies…
Water Potentials
Force that causes water to move or not
Gravitational Water Potential
Acceleration due to gravity x soil height
Matric Water Potential
Adhesion and Capillarity
Osmotic Water Potential
Water movement across a semipermeable membrane to equalize concentration of solutes
Plant Water Use
Evapotranspiration
Types of Water Movement in Soil
Saturated Flow, Unsaturated Flow, Vapor Movement
Types of Irrigation
Surface (Flood), Sprinkler, Drip
What is pH?
Concentration of H+ ions in a solution
5 Sources of H+
Carbonic Acid, SOM, Fertilizers, Cation Uptake, Precipitation
Liming Materials
CaCO3 - Calcium Carbonate (Limestone), CaO - Calcium Oxide (Quick Lime), Ca(OH)2 - Calcium Hydroxide, CaMg(CO3)2 - Dolomite, CaSO4 - Gypsum
Liming Methods
Slow Reaction, Few weeks: Quick Lime and Slaked Lime, Year: Finely ground limestone
Salinity
Recharge - where H2O comes from, Discharge - where H2O evaporates, Seep - whole network of recharge-discharge
What Causes Saline Seepage?
Contact/Slope, Depression Bottom, Slough Ring, Hydraulic Discharge, Outcrop Mechanism, Canal Seepage
Crops for Discharge Area
Salt-tolerant species, Wheatgrasses, wild rye, sweet clover, alfalfa, bromegrass, Sugar beets, barley, safflower, sunflower, wheat
Types of Erosion
Splash Erosion, Sheet Erosion, Rill Erosion, Gully Erosion
Solutions for Water Erosion
No till and plant different, Grass waterway, Contour cropping, Strip cropping, Terraces
Solutions for Wind Erosion
Stabilize soil aggregates, Cover crops, No till, Rotate entrance, Manure, Reduce wind velocity at soil surface, Shelterbelt
WIND EROSION EQUATION
E = ICKLV
Management for Sodic Soil
Good drainage, Fertilizer, Irrigation, SOM, Deep-tillage
SOM and Soil Organisms
Raw residues and microorganisms- 1-10% of soil composition, usually vegetation
Active fraction
10-40% of soil composition
Stable fraction
40-60% of soil composition
Decomposition rates of organic compounds
Sugars, starches, simple proteins decompose fastest, while lignins and phenolics decompose slowest
Cellulose
A polymer consisting of 7000-15000 sugar units
Lipids
Hydrophobic compounds found in soil
C-C bonds
The main energy source for microorganisms in soil
Mineralization
The process by which soil organic matter decomposes and releases inorganic nutrient forms
Immobilization
Microbial uptake of mineral nutrients, making them temporarily unavailable
Leaching
The influence of soil organic matter chelates and micronutrient cations
Nutrient capture by plants
The process by which plants access nutrients from the soil
Carbon:nutrient ratio
A metric that powers microbial growth and reproduction, with C:N ratios of 25:1, 20:1 favoring plants, and 30:1 favoring microbes
Soil Organism Roles
Includes plants, shredders, decomposers, and nutrient transformers
Earthworms
Soil organisms that stimulate microbial activity, mix and aggregate soil, and improve water -holding capacity
Factors promoting earthworms
Presence of fresh undecomposed organic matter, pH > 5.8, moisture, and temperature of 50°F
Factors depressing earthworm populations
Droughty soils, anhydrous ammonia, and tillage
Dung Beetles
Insects that feed on animal waste, which serves as a nutrient source
Soil Health
The ability of soil to carry out essential functions such as water regulation and nutrient cycling
Soil health indicators
Metrics that include infiltration rate, soil respiration, earthworm counts, and plant diversity
Functional Diversity
The ability of soil organisms to utilize a wide range of substrates and carry out many processes
Functional Redundancy
The overlap of different species roles, leading to stability and resilience in ecosystems
Keystone species
Species whose presence contributes to the diversity of life, and whose extinction would ruin the ecosystem
Mycorrhizal fungi
Fungi that help roots grow to nutrients and water
Mass Flow
The movement of nutrients through soil due to concentration gradients
Leaching
Influence of SOM chelates and micronutrient cations
What is Functional Diversity?
Ability of soil organisms to utilize a wide range of substrates and carry out many processes
Functional Redundancy
Different species roles overlap, leading to stability and resilience
What is a keystone species?
Species presence contributes to diversity of life; extinction would ruin the ecosystem
What do earthworms do?
Stimulate microbial activity, mix and aggregate soil, increase nutrient availability
Dung Beetles
Animal waste that serves as a nutrient source and decomposer food source
Soil health
Ability to carry out essential functions like water regulation and nutrient cycling
Soil health indicators
Include infiltration rate, soil respiration, earthworm counts, and plant diversity
Water regulation
Measured by infiltration rate, surface crusting, and water-holding capacity
Sustaining plant and animal life
Indicators include soil cover, earthworm counts, and plant diversity
Filtering and buffering
Measured by pH, buffer pH, and groundwater quality
Physical stability and support
Indicators include soil aggregates, soil density, and evidence of erosion
Saline soils
Soils that require leaching to remove excess salt
Subsurface drainage water quality concerns
Loss of Nitrogen and other nutrients, pesticide/herbicide contamination, canal seepage
Saturated Buffer
Diverts a portion of drain tile water into a vegetated buffer strip where plants remove nitrogen
Bioreactor
An underground trench filled with wood chips where microbial activity breaks down nitrogen in water
Constructed Wetlands
Water is diverted through a wetland with microbes and vegetation that slows water movement and causes denitrification
Components of Soil Organic Matter (SOM)
Raw residues and microorganisms (1-10%), Active Fraction (10-40%), Stable Fraction (40- 60%)
SOM as a revolving bank account
You get out what you put in; deposit organic materials to maintain a healthy SOM balance
Required SOM for suitable soil physical properties
3-5% SOM is necessary for optimal soil structure and stability
Purpose of maintaining SOM above 3-5%
Improves soil structure, stability, water-holding capacity, nutrient supply, and biodiversity
Impacts of tillage on soil physical properties
Degrades soil structure, compacts soil, and increases risk for wind and water erosion
Tillage effects on SOM cycles
Accelerates decomposition of SOM and disrupts soil microbial communities, altering nutrient cycling
Soil erosion
The process by which soil is removed from the land surface, often exacerbated by poor management practices
Nutrient cycling
The process of nutrients being reused and recycled in the ecosystem
Soil Aggregation
The clustering of soil particles into aggregates, improving soil structure and function
Decomposition
The breakdown of organic matter by microorganisms, releasing nutrients back into the soil
Biodiversity in soil
The variety of life forms in the soil, contributing to ecosystem resilience and function
Water-holding capacity
The ability of soil to retain water for use by plants
Buffering pH
The ability of soil to resist changes in pH, maintaining a stable environment for organisms
Soil structure
The arrangement of soil particles and the pore spaces between them, affecting water movement and root growth
Microbial activity in soil
The actions of microorganisms that contribute to nutrient cycling and organic matter decomposition