WorksheetsSample Questions (1–20) soil science
Total questions: 100
Worksheet time: 53mins
Which of the following is NOT a component of Soil
Mineral particles
Air
Water
Each choice is a of soil
Which term refers to the void spaces in soil which can be filled by water or air?
Permeability
Soil texture
Soil structure
porosity
Which of the following best describes leaching?
Water brings nutrients from below plant roots so they are available to plants
Nutrients come from groundwater and streams and appear in the soil for plant use
Nutrients accumulate in water then are supplied to plants through the soil
Water carries nutrients
Which of the following is a true statement?
Soil tests are most useful during the growing season to monitor plant nutrient uptake
Plant tissue analysis is the best assessment of nutrient levels in soil
Using a soil test and plant tissue analysis in combination will provide the best results for nutrient availability and the best corrective action
Soil tests are most useful during the growing season to predict lime and fertilizer needs
Which of the following is NOT a soil texture?
Sand
Clay
Smooth
silt
Which type of nutrients is needed in large amounts by plants?
Macronutrients
Micronutrients
Secondary nutrients
Non-mineral nutrients
Which of the following is another name for micronutrients
Small nutrients
Major nutrients
Trace elements
Non-mineral nutrients
Soil consists of four major components. Which of the following is NOT one of them?
Mineral material
Organic matter
Water
Rock fragments
The three size-classes of mineral soil particles (that determine texture) are:
Sand, loam, clay
Sand, silt, clay
Gravel, sand, silt
Clay, silt, loam
Which size range corresponds to sand particles?
0.002 – 0.05 mm
0.05 – 2.0 mm
< 0.002 mm
2.0 – 5.0 mm
What percentage (approximately) of a typical soil’s volume is mineral material?
25%
45%
55%
70%
Which soil texture class is the only one that is chemically active and capable of adsorbing plant nutrients?
Sand
Silt
Clay
Loam
Why is soil texture important for soil health?
It affects the soil’s ability to resist erosion only
It determines mineral composition exclusively
It influences pore space available for water, air, and nutrients
It decides the soil’s color
Which of the following statements about soil texture is true?
Soil texture can be easily changed by human addition of compost
Soil texture is mainly determined by geology and climate
Soil texture is unrelated to water holding capacity
Soil texture determines organic matter content
The term “pore space” or voids in soil refers to:
The proportion of sand particles
The air spaces left between soil particles or aggregates
The total volume of mineral particles
The amount of organic matter
What is the significance of pore space (voids) in soils?
It reduces soil fertility
It provides sites for water, air, roots, and organisms
It increases soil compaction
It removes nutrients
Which of the following best defines soil “health,” per the lesson plan’s key concepts?
The ability of soil to produce high crop yields only
The capacity of soil to function as a living ecosystem sustaining plants, animals, and humans
The chemical fertility of soil alone
The amount of sand in the soil
Soil health encompasses which components?
Physical only
Chemical only
Biological only
Physical, chemical, and biological
Which factor(s) can influence soil health (as per the lesson plan)?
Parent material and climate only
Human activities (like cropping and fertilization) only
Both environmental conditions and human activities
None — soil health is fixed
In a soil with high clay content, you would expect:
High permeability and rapid drainage
Low chemical activity
High nutrient-holding capacity due to adsorption
Very coarse texture
If a soil has about 45% mineral material, 5% organic matter, ~25% water and ~25% air by volume, this represents:
A. A sandy soil
B. A typical well-balanced soil
C. Poor quality soil
D. Only topsoil
Which of following is a biological component of soil health (even if the textbook calls out physical/chemical/biological)?
Clay particles
Air-filled pore space
Soil microorganisms (bacteria, fungi) and organic matter decomposition
Water saturation
The mineral particles in soil originated from:
Decomposed plant matter
Parent rock material weathered over time
Animal waste
Added fertilizers
In the context of soil texture, “loam” refers to:
Soil composed entirely of clay
Soil high in organic matter only
A balanced mixture of sand, silt, and clay
Soil with no pore space
Which of the following soil textures would generally have the fastest drainage and lowest water-holding capacity?
Clay
Loam
Sand
Silt loam
What role does organic matter play in soil structure and health?
It decreases pore space
It acts like “glue,” helping mineral particles form aggregates and improving water and nutrient holding capacity
It reduces the chemical activity of the soil
It makes soil purely sandy
Which of the following describes a shift in paradigm that soil health represents (compared to traditional “soil fertility”)?
Viewing soil as a nonliving system focused only on chemical fertility
Considering soil as a living ecosystem — physical, chemical, and biological components integrated
Ignoring organic matter as insignificant
Focusing only on mineral content
Which of the following is not one of the four major soil components?
Soil organic matter is primarily derived from:
Weathered rock
Decomposed plant and animal residues
Industrial fertilizers
Groundwater
Which soil particle is the smallest?
Sand
Silt
Clay
Gravel
Which particle controls much of a soil's chemical reactivity?
Sand
Gravel
Clay
Silt
The soil texture triangle is used to determine:
Soil pH
Soil color
Soil mineral chemical composition
Relative proportions of sand, silt, and clay
Which texture generally has highest water-holding capacity?
Sand
Silt
Loam
Clay
Which soil texture drains the fastest?
Silty clay
Sand
Loam
Clay loam
Soil structure refers to:
The size of mineral grains
How particles are arranged into aggregates
The chemical composition of soil
The pH level of soil
Good soil aggregation increases:
Compaction
Evaporation
Infiltration
Acidity
A “platy” soil structure most often restricts:
Root penetration
Color development
pH buffering
Organic matter decomposition
Porosity refers to:
Nutrients in the soil
Air and water spaces between particles
Plant residue on the surface
Mineral particle hardness
High porosity usually means:
High density
Low root growth
More water can be stored
Lower infiltration
Permeability describes the soil’s ability to:
Hold nutrients
Resist temperature change
Allow water to pass through
Generate organic matter
Compaction generally causes:
Increased aeration
Reduced porosity
More microbial activity
Lower bulk density
A perched water table forms when:
A. Water cannot infiltrate through a restrictive layer
B. Soil is too dry
C. Plants remove too much water
D. Soils have high sand content
Which factor most strongly influences infiltration?
Soil color
Soil structure
Soil temperature
Soil salinity
Saturated soil means:
All pores are filled with water
Water is moving upward
Water is evaporating
No water remains
Key property affecting both infiltration and runoff is:
Soil pH
Soil temperature
Soil texture
Soil color
Water movement through large pores is mostly controlled by:
Gravity
Osmosis
Capillarity
Root pressure
Capillary rise occurs when:
Water moves downward only
Fine pores draw water upward
Water evaporates from roots
Soil freezes
Soil color is most commonly measured with the:
Soil factor guide
Munsell color chart
Hydrometer chart
Porosity index
Dark-colored soil usually indicates high:
Salt
Sand
Organic matter
Clay
Red or yellow soils usually indicate presence of:
Iron oxides
Aluminum
Calcium carbonate
Sodium
Parent material affects:
Only soil color
Only soil nutrients
Soil texture, chemistry, and mineralogy
Only biological activity
All are forms of physical weathering except:
Freeze–thaw
Root wedging
Abrasion
Acid dissolution
Chemical weathering includes:
Rusting of iron minerals
Frost cracking
Biological tunneling
Mechanical breakup
Loess is:
River-deposited sand
Wind-blown silt
Volcanic ash
Glacial till
Glacial till is best described as:
Uniform silt
Poorly sorted material left by glaciers
Organic-rich sediment
Calcareous bedrock only
Soils rich in calcium carbonate often show:
High acidity
White or light-colored accumulations
Dark black color
Strong red iron staining
Parent material derived from volcanic ash typically has:
Low nutrient content
Excellent water-holding capacity
The O horizon consists mainly of:
Weathered bedrock
Organic residues
Clay deposits
Leached minerals
The A horizon is typically the:
Subsoil
Topsoil
Parent material
Hardpan
Leaching most often occurs in the:
O horizon
A horizon
E horizon
C horizon
The B horizon is known for:
Organic matter accumulation
Clay and iron accumulation
No soil formation
Bedrock exposure
The C horizon represents:
Fully weathered soil
Parent material with little alteration
Strongly leached soil
Organic-rich material
An E horizon is characterized by:
Strong loss of clays and organic matter
High accumulation of salts
Parent rock
Excessive root biomass
Soil horizons collectively form the:
Soil base
Soil profile
Soil surface
Soil crust
A “root-limiting layer” in a soil profile is most often caused by:
Organic matter
Compaction or dense clay
Biological activity
Earthworm channels
The boundary between horizons is called:
A transition zone
A soil factor
A pedon
A contact
A soil pedon represents:
A color category
The smallest unit considered a soil body
Only the A horizon
A model profile with no variation
Soil health emphasizes soil as a:
Chemical storage tank
Mineral deposit
Living ecosystem
Nonliving medium
The MOST abundant soil organisms are:
Earthworms
Bacteria
Beetles
Fungi
Fungi are important because they:
Compact soil
Break down organic matter and form hyphal networks
Reduce soil fertility
Replace roots
Mycorrhizal fungi help plants by:
Removing nutrients
Enhancing nutrient and water uptake
Reducing root surface area
Increasing soil compaction
Earthworms improve soil by:
Decreasing macropores
Increasing aeration and aggregation
Raising soil temperature
Sealing surface pores
A key feature of biological soil crusts is:
Root networks
Mosses, cyanobacteria, and lichens
Gravel formation
Acid buildup
Soil respiration mainly measures:
Oxygen production
CO₂ released by microbes and roots
Water evaporation
Soil temperature
High biological activity usually indicates:
Poor soil health
Active nutrient cycling
No organic matter
Complete saturation
Soil organisms are adversely affected by:
Residue cover
High compaction
Good aggregation
Plant diversity
Which practice most enhances soil microbial diversity?
Monocropping
Frequent tillage
Minimal soil disturbance
Removing residues
Soil organic matter improves:
Bulk density
Water retention, structure, nutrient availability
Soil color only
Soil salinity
Organic matter is composed largely of:
Salts
Plant residues at various decomposition stages
Pesticides
Clay
Humus is:
Raw plant material
Fully decomposed organic matter
Mineral residue
Soil-dwelling insects
Increasing organic matter generally:
Increases compaction
Decreases infiltration
Improves aggregate stability
Reduces nutrient cycling
The majority of soil carbon is found in the:
O and A horizons
C horizon
E horizon
Bedrock
Carbon sequestration in soil is enhanced by:
Intensive tillage
Grazing mismanagement
Perennial vegetation
Removing residues
Which factor slows organic matter decomposition?
Warm temperatures
Aeration
Moist conditions
Cold temperatures
Soil microbes use carbon primarily as:
A. A nutrient sink
B. An energy source
SOM contributes to nutrient cycling by:
Fixing nitrogen
Slowly releasing nutrients as it decomposes
Filtering nutrients out of the soil
Eliminating minerals
60. Residue cover contributes to soil carbon by:
A. Blocking plant growth
B. Preventing microbial activity
C. Reducing erosion and feeding soil organisms
D. Hardening the soil surface
The three primary macronutrients are:
Fe, Zn, Cu
K, Ca, Mg
N, P, K
C, O, H
Nitrogen is important for:
Root hairs
Chlorophyll and vegetative growth
Wax formation
Soil porosity
Phosphorus mainly supports:
Root development and energy transfer
Disease resistance
Water uptake
Soil color
Potassium improves:
Leaf color only
Water regulation and stress tolerance
Soil structure
Organic matter formation
Soil pH affects nutrient:
(a)
A soil pH of 7 is considered:
Acidic
Neutral
Alkaline
Toxic
Acidic soils often require:
Sulfur
Lime
Iron
Sand
Nutrients are often lost by:
Leaching and erosion
Organic additions
Microbial activity
Root interception
Cation exchange capacity (CEC) measures soil’s ability to:
Hold water
Hold positively charged nutrients
Trap oxygen
Decompose minerals
High clay and organic matter generally mean:
Low CEC
High CEC
No exchange sites
Poor nutrient holding ability
Soil erosion is defined as:
Movement of soil by water or wind
Decomposition of organic matter
Chemical breakdown of minerals
Loss of soil color
Sheet erosion is:
Removal of soil in small channels
Even removal of thin layers
Sudden collapse of slopes
Erosion by freezing
Rill erosion differs from gully erosion because rills:
Are shallow and repairable
Are deep channels
Cannot be crossed by equipment
Form only in clay soils
