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WorksheetsSample Questions in Soil Science — Section 1: Soil Microbiology
Total questions: 150
Worksheet time: 1hrs 15mins
Net nitrogen immobilization in soil occurs if the C/N is
Less than 20:1
Greater than 20:1
Greater than 35:1
Less than 15:1
None of the above
Individually, which among the following soil organisms have the least biomass?
Actinomycetes
Fungi
Bacteria
Protozoa
Earthworm
Which among the following soil organisms are acid-loving?
Fungi
Protozoa
Bacteria
Actinomycetes
A and B above
Ammonia volatilization from NH4+-bearing fertilizers is not favored by which of the following?
High pH
High Temperature
High CEC
a and b above
b and c above
Soil microorganisms degrade organic residues primarily for
Phosphorus and ATP
Carbon and energy
Nitrogen and energy
Phosphorus and energy
Nitrogen and phosphorus
The root-nodule bacteria belong to the genus
Clostridium
Azotobacter
Rhizobium
Agrobacterium
None of the above
The anaerobic non-symbiotic nitrogen fixing bacteria belong to the genus
Derxia
Clostridium
Azotobacter
Bradyrhizobium
Nitrobacter
Algae are considered as
Autotrophs
Photoautotrophs
Chemoautotrophs
Both a and b above
None of the above
The source of energy for blue-green algae is
Sunlight
Metabolism of glucose
Organic matter decomposition
Oxidation of inorganic compounds
None of the above
The predominant available form of N under flooded soil condition is
NO3-N
Organic-N
NH4-N
NO2-N
None of the above
The available form of nitrogen which predominates under upland condition is
Ammonium
Nitrite
Nitrate
Microbial biomass N
Fixed N
The conversion of NO3 to N2 is referred to as
Nitrogen fixation
Denitrification
Immobilization
Volatilization
None of the above
The percentage of organic N in the soil is approximately
95-96%
80-85%
68-75%
50-60%
60-70%
Nitrogen is added to the soil system by which of the following processes?
Leaching
Nitrogen fixation
Ammonia volatilization
a and b above
b and c above
The conversion of organic N to inorganic or mineral N is termed as
Immobilization
Nitrification
Mineralization
Ammonification
None of the above
The conversion of N2 to NH3 is referred to as
Denitrification
Nitrate reduction
Nitrogen fixation
Volatilization
None of the above
Microorganisms which do not require oxygen are called
Aerobes
Anaerobes
Obligate aerobes
Microaerophillic
None of the above
The fixation and regeneration of CO2 in the biosphere is referred to as
Carbon cycle
CO2 evolution
Respiration
Nutrient cycle
None of the above
The optimum temperature requirement of thermophiles is
Greater than 45°C
Less than 45°C
Greater than 30°C
Less than 30°C
30-40°C
Microorganisms which require organic compounds as sources of carbon and energy are
Autotrophs
Heterotrophs
Chemoautotrophs
Photoautotrophs
None of the above
It refers to the entrapment of ammonium ions in-between crystal lattices of clays thus rendering them unavailable for plant use. This process is called
Nitrogen fixation
Microbial fixation
Ammonium fixation
Nutrient fixation
None of the above
Rhizobia are generally associated with nitrogen fixation in
Rice
Peanut
Corn
Sorghum
Sugarcane
Bacteria belonging to this genus are non-symbiotic nitrogen fixers
Nitrobacter
Aerobacter
Azotobacter
Arthrobacter
Nitrosomonas
If a crop residue contains 60% organic carbon and 5% total nitrogen, its C/N ratio is
10:1
12:1
15:1
20:1
25:1
The C/N ratio of soil microbial biomass is about
5-8:1
12-15:1
15-20:1
20-25:1
None of the above
The most abundant microorganisms found in the soil are generally the
Fungi
Bacteria
Actinomycetes
Algae
Protozoa
The incorporation of inorganic nitrogen into microbial tissues is
Mineralization
Immobilization
Nitrification
Denitrification
Ammonification
Which of the following microorganisms is very sensitive to potassium levels in soil and therefore useful in diagnosing potassium deficiency?
Pseudomonas denitrificans
Aspergillus flavus
Aspergillus niger
Azotobacter chroococcum
Nitrobacter agilis
A deficiency of this element will not enable a legume and its bacterial partner to perform nitrogen fixation. This element is
Boron
Phosphorus
Molybdenum
Zinc
Magnesium
The group of soil microorganisms which is responsible for decomposing organic matter is the
Heterotrophs
Autotrophs
Phototrophs
Chemoautotrophs
None of the above
Organic materials with wide C/N ratios are not ready sources of available nitrogen because the nitrogen that they contain is subject to
Nitrification
Volatilization
Immobilization
Fixation
None of the above
The soil microbial population is generally highest in the
A horizon
B horizon
C horizon
B2 horizon
A0 horizon
Chemoautotrophs are those organisms which derive their energy from
Sunlight
Oxidation of organic materials
Fermentation
Oxidation of inorganic substances
None of the above
For soil bacteria, growth results in an increase in the
Size of the individuals
Number of the individuals
Form of the individuals
Size and number of the individuals
None of the above
The most efficient organic matter decomposers under acidic soil conditions are the
Bacteria
Actinomycetes
Fungi
Protozoa
Algae
Pesticides will be retained much longer in soils with
Low organic matter
High moisture content
2:1 dominant clay type
Low pH
1:1 dominant clay type
Net mineralization of organic nitrogen in the soil will occur if the C/N ratio is less than
20:1
30:1
40:1
50:1
60:1
The initial substrate for nitrification is
Nitrite
Nitrate
Ammonium
Amine
None of the above
The ultimate end-product of denitrification is
N2
NO
N2O
NH3
None of the above
A gas which can be used as an indicator of the level of microbial activity in the soil is
Nitrogen
Oxygen
Hydrogen
Carbon dioxide
Methane
Associative nitrogen fixation is undertaken by bacteria in association with
Rice
Corn
Sugar cane
Pasture grasses
All of the above
Frankia spp. are soil microorganisms which are responsible for the nodulation in
Casuarina
Alnus
Eleagnus
Coriaria
All of the above
The number and activity of bacteria in the soil are affected by
pH
Moisture
Oxygen supply
Salinity
All of the above
A type of microscope which provides a 3-dimensional view of the soil microorganisms is called
Light microscope
Scanning electron microscope
Transmission electron microscope
Immuno-fluorescent microscope
None of the above
A 1:1000 soil-water dilution means that one part of soil is suspended in
9 parts of sterile H2O
99 parts of sterile H2O
999 parts of sterile H2O
1000 parts of sterile H2O
None of the above
In a legume biological nitrogen fixing system, the microsymbiont is
Bacteria
Actinomycete
Algae
Fungi
None of the above
CO2 evolution in soil is a function of
Microbial population
Aeration
pH
Temperature
All of the above
The amount of molecular nitrogen (N2) in the atmosphere is about
88%
78%
68%
58%
48%
When NO3 is denitrified all the way to N2, there is a shift in the valence of N from +5 to
+4
+3
+2
+1
0
Which of the following bacterial genera had been known to be capable of denitrification?
Agrobacterium
Azospirillum
Pseudomonas
Thiobacillus
All of the above
A soil consist of the three components; namely: solid, liquid and gas
The solid is composed of inorganic matter and organic matter
The liquid is a solution with dissolved ions in it
The gas component is about 80% nitrogen gas (N2)
None of the above
All of the above
A soil consist of three components; namely: solid liquid and gas
The solid is composed of inorganic matter
The liquid is a solution with dissolved ions in it
The gas is 80% oxygen gas
None of the above
All of the above
A soil consist of three components; namely: solid, liquid and gas.
The solid is composed of inorganic matter and organic matter
The liquid is a pure water
The gas is 80% oxygen gas
None of the above
All of the above
Under its natural occurrence a soil is aggregated and porous.
An aggregate is composed of millions of individual particles
Water and air occupy the pores
The pores are interconnected channels to other pores
None of the above
All of the above
The solid particles of a soil vary in composition, size and shape.
The solid is composed of inorganic and organic matter
The solid is composed of soil separates called sand, silt and clay
The solids stick or cluster together to form soil aggregate
None of the above
All of the above
The inorganic solid particles vary in size which are classified as soil separates.
The size range of soil particle is equal to or less than 5 mm
Sand is medium size soil separate
Clay is the smallest or the finest soil separate
None of the above
All of the above
The relative distribution of soil separates in a soil mass is called soil texture.
Sand, silt and clay are soil separates
Soil texture changes easily with poor methods of cultivation
Soil texture is improved by adding organic fertilizer
None of the above
All of the above
Soil texture refers to the coarseness or fineness of a soil.
Sand is gritty
Silt is sticky and plastic
Clay is smooth
None of the above
All of the above
Soil texture refers to the coarseness or fineness of a soil.
Sand is coarse and gritty
Silt is powdery and smooth
Clay is sticky and plastic
None of the above
All of the above
Many soil properties and characteristics are affected by soil texture.
Sandy soil is more porous than clay soil
Loamy soil are rich in silt
Clay soil is chemically more reactive than sandy soil
None of the above
All of the above
In relation to crop production sandy soils are known to be:
Droughty
Easy to be cultivated
Easy to drain
None of the above
All of the above
In relation to crop production clayey soils are known to be:
Sticky to cultivate
Fertile than sand
High water holding capacity than sand
None of the above
All of the above
Many soil properties and characteristics are affected by soil texture.
Clayey soils are more porous than sandy soil
Silt texture is associated to poor physical properties
Sandy soil is chemically more reactive than clay soil
None of the above
All of the above
Soil texture could be determined by:
"Feel" method
Pipette method
Hydrometer method
None of the above
All of the above
Soil texture could be determined in the laboratory by:
Ammonium acetate method
Buoyancy method
Hydrometer method
None of the above
All of the above
The upper diameter size limit of clay particles is:
2.0 mm
0.2 mm
0.02 mm
0.002 mm
0.0002 mm
The upper diameter size limit of silt particles is:
2.0 mm
0.2 mm
0.02 mm
0.002 mm
0.0002 mm
The upper diameter size limit of sand particles is:
2.0 mm
0.2 mm
0.02 mm
0.002 mm
0.0002 mm
Soil textural class wherein the coarseness of sand, the smoothness feel of silt and the stickiness of clay are manifested in almost equal proportion in a soil mass.
Sand
Silt
Clay
Loam
None of the above
Soil texture that would be best for growing lowland rice.
Sandy loam
Silty loam
Clay loam
All of the above
None of the above
Characteristic feel of sand separates when rubbed in between the finger is:
Coarse
Smooth
Sticky when moist
All of the above
None of the above
Characteristic feel of clay separates when rubbed in between the finger is:
Coarse
Smooth
Sticky when moist
All of the above
None of the above
Characteristic feel of silt separates when rubbed in between the finger is:
Coarse
Smooth
Sticky when moist
All of the above
None of the above
Many soil properties and characteristics are affected by soil structure.
Loam is the soil structure that most crops prefer
Dispersed clay soil possesses good soil structure
Compacted soil structure allows fast movement of air in the soil
None of the above
All of the above
Many soil properties and characteristics are affected by soil structure.
Crumb is the best structure that most crops prefer
Dispersed clay soil possesses poor soil structure
Poor water movement in platy soil structure
None of the above
All of the above
Which among the following is not a soil structure?
Loam
Crumb
Platy
Sub-angular blocky
Prismatic
Soil densities and porosities are affected by soil texture and soil structure.
Porosity increases with increasing bulk density
Soil compaction increases bulk density
Soil aggregation increases bulk density
None of the above
All of the above
Soil densities and porosities are affected by soil texture and soil structure.
Porosity increases with decreasing bulk density
Soil compaction decreases bulk density
Soil aggregation improves porosity
None of the above
All of the above
Pore-size distribution affects movement and retention of water and air in the soil.
Macro-pores retain water
Macro-pores are important in root respiration
Micro-pores are more important than macro-pores
None of the above
All of the above
Pore-size distribution affects movement and retention of water and air in the soil.
Micro-pores retain water
Macro-pores are important in drainage and root respiration
Micro-pores and macro-pores are equally important to root growth
None of the above
All of the above
A soil with a bulk density of 1.3 g/cm3 and a particle density of 2.60 g/cm3 will have a porosity of:
5%
25%
50%
75%
Bulk density is a good indicator of soil degradation.
Bulk density does not change with poor soil cultivation practices
Increasing bulk density indicates deteriorating soil physical condition
Decreasing bulk density indicates deteriorating soil physical condition
None of the above
All of the above
Particle density is a stable soil property. Most agricultural soils would have particle densities close to this value.
1.65 g/cm3
2.65 g/cm3
3.65 g/cm3
4.65 g/cm3
Type of soil structure that is best for growing upland crops.
Massive
Platy
Crumb
Loam
Single-grain
The soil structure of a compacted plow soil is:
Massive
Platy
Crumb
Loam
Single-grain
The color of a soil indicates some chemical conditions.
Dark or black color indicates high organic matter
Reddish color indicates that the soil is high in oxides of iron
Yellowish color indicates that the portion of lowland soil is at oxidized state
None of the above
All of the above
The color of a soil indicates some chemical conditions.
Dark or black color indicates high organic matter
Dark or black color indicates that the soil is high in oxides of iron
Dark or black color indicates that the soil is at oxidized state
None of the above
All of the above
The color of a soil indicates some chemical conditions.
Reddish color indicates high organic matter
Reddish color indicates that the soil is high in oxides of iron
Reddish color indicates that the soil is young
None of the above
All of the above
Plants depend on the water stored in the soil.
The upper limit of available water is saturated moisture content
The upper limit of available water is hygroscopic point
The upper limit of available water is field capacity
None of the above
All of the above
Plants depend on the water stored in the soil.
The upper limit of available water is field capacity
The lower limit of available water is permanent wilting point
Available water capacity is field capacity minus permanent wilting point
None of the above
All of the above
Available water capacity is calculated as
Saturation minus permanent wilting point
Field capacity minus permanent wilting point
Hygroscopic point minus permanent wilting point
None of the above
All of the above
Gravitational water capacity is equal to
Saturated moisture minus permanent wilting point
Saturated moisture minus field capacity
Saturated moisture minus hygroscopic point
None of the above
All of the above
The moisture content of an air dry soil is known as
Saturation
Field capacity
Permanent wilting point
Hygroscopic coefficient
Zero point
Movement of water in the soil is always from:
Higher to lower soil moisture content
Higher to lower total potential energy
Higher to lower soil moisture tension
None of the above
All of the above
If soil moisture content is 50%, field capacity is 40% and permanent wilting point is 20%, the amount of available water in the soil is:
10%
20%
30%
None of the above
All of the above
If soil moisture content is 35%, field capacity is 40% and permanent wilting point is 20%, the amount of available water in the soil is:
5%
10%
15%
None of the above
All of the above
Calculate the gravimetric moisture content of a soil sample if its fresh weight = 25 gm and oven dry weight = 20 gm.
25%
20%
15%
None of the above
All of the above
Calculate the volumetric moisture content of a soil sample if its fresh weight = 25 gm, oven dry weight = 20 gm and bulk density = 1.2 g/cm3 .
30%
24%
20%
None of the above
All of the above
Soil grown to corn is best cultivated when the soil consistency is:
Hard
Friable
Plastic
Viscous
Lowland rice land is prepared to have a soil consistency that is:
Hard
Friable
Plastic
Viscous
Bacteria belong to this factor of soil formation.
Climate
Living organisms
Time
Parent material
Horizontal layers of soil differentiation.
Concretions
Structure
Horizons
Hardpans
A square meter of land dug to a depth that nearly touches the bedrock.
Profile
Parent material
Pedon
Aquifer
Mature soil have the following horizons:
AB
ABC
BC
AC
Young soils have the following horizons:
AB
ABC
ABCD
AC
The solum is composed of these horizons:
ABC
BC
ABCR
AB
The regolith is composed of these horizons:
AB
BC
ABC
ABCR
The topsoil usually refers to this horizon:
AB
A
E
C
The subsoil usually refers to this horizon:
AB
A
B
C
Blocks of soil from each horizon pasted on a hard board.
Regolith
Monolith
Litolith
Pedon
The government agency in charge of the survey and classification of soils in the Philippines.
BPI
BSWM
NAFC
DPWH
Basis for mapping the distribution of Philippine soils.
Soil series/type
Soil order
Soil Family
Great Group
A group of soils which developed from the same parent material and whose profile characteristics are the same.
Soil Order
Soil Series
Soil Family
Great Group
Soil profile characteristic important to a civil engineer:
Color
Structure
Texture
Microbial population
Soil profile characteristic important to a biologist:
Roots and faunal activity signs
Color
Texture
Bulk density
Standard reference system for soil color.
Soil Taxonomy
Soil map
Soil survey report
Munsell color chart
Soil color description.
Hue, value, chroma
Tint, lightness, mixture
Shade, reflection
Intensity
Describes darkness or lightness of a soil color.
Hue
Value
Chroma
Intensity
Sign of poor drainage
Yellowish mottles
Bluish gray mottles
Reddish concretion
Reddish orange mottles
Natural soil aggregates.
Crumbs
Clods
Peds
Pebbles
A simple test for limestone parent materials.
H2SO4 reaction
HCl reaction
Brittleness
Stickyness
Structureless soil:
Granular
Crumb
Prismatic
Massive/single-grained
Soils with no diagnostic horizons:
Entisols
Mollisols
Oxisols
Alfisols
Broadest category of soil taxonomy:
Great Group
Sub order
Order
Family
Soils which are predominantly montmorillonitic:
Vertisols
Entisols
Inceptisols
Histosols
The Haber Bosch process for making N fertilizer.
N2 + N2O → NH3
N2 + 3H2 → 2NH3
N2 + 2O2 → NO3
N2 + H2O → NO3
The highest analysis (grade) solid N fertilizer.
Ammonium sulfate
Anhydrous ammonia
Urea
Ammonium nitrate
The reaction during biological N fixation.
N2 → NH3
N2 + H2O → amino acid
N2 + H2O → protein
N2 + H2 → ammonium sulfate
The enzyme needed to transform urea to (NH4)2CO3 in soil.
Carboxylase
Anhydrase
Urease
Papase
The weak acid formed upon hydrolysis and subsequent reaction of urea in soils.
Acetic acid
Carbonic acid
Uric acid
Silicic acid
The other essential nutrient element present in ammonium sulfate but absent in urea.
Calcium
Sulfur
Iron
Magnesium
The percent N, P2O5, and K2O in a fertilizer is:
Fertilizer ratio
Fertilizer grade
Fertilizer recommendation
Fertilizer brand
A single-element or straight fertilizer.
Complete fertilizer (14-14-14)
Ammonium phosphate
Urea
All of the above
The fertilizer nutrients that are generally applied all at planting time (basal).
N and P
P and K
N and K
P and Ca
The fertilizer nutrients which are usually split applied.
N and K
P and K
N and P
N and S
The available form of nitrogen.
N2
N2O
NH4+
NH3
Enzyme in nitrogen transformation in legumes.
Nitrogenase
Dehydrogenase
Decarboxylase
Anhydrase
This ratio determines mineralization rate of organic matter.
N/S
C/N
P/N
N/K
Application of N fertilizer in alkaline soils causes.
NH3 volatilization
Nitrification
Denitrification
Mineralization
This is an acid forming reaction of NH4+.
Nitrification
Denitrification
Ammonification
Mineralization
This metal ion is usually present in toxic amounts in strongly acid soils.
Aluminum
Calcium
Potassium
Magnesium
Binding of an organic compound and a metal ion.
Coordination
Complexation
Chelation
Oxidation
Most micronutrients become less available at:
Decreasing soil pH
Increasing pH
Neutral pH
Strongly acid pH
When nutrients are immobile, deficiency first shows up in:
Youngest leaves
Oldest leaves
Senescent leaves
Stems
Deficiency of these elements causes chlorosis.
N and Ca
P and Ca
N and S
Fe and Cl
Deficiency of sulfur first shows up as chlorosis of:
Oldest leaves
Youngest leaves
Middle leaves
Stems
The suitable fertilizer for an alkaline N deficient soil.
Anhydrous NH3
Urea
Calcium nitrate
Ammonium sulfate
The appropriate N fertilizer for a sulfur deficient soil.
Urea
Ammonium nitrate
Potassium nitrate
Ammonium sulfate
Application of fertilizer at planting.
Topdressing
Foliar
Band
Basal
Application of fertilizer after plant emergence.
Basal
Topdressing
Foliar
Deep placement
