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WorksheetsPrinciples of soil science
Total questions: 60
Worksheet time: 30mins
Chemical properties of soil that set of chemical activities or reactions in the soil
Soil texture
Soil colloid
Soil structure
Soil profile
Soil component with extreme small size and large area, capable of absorbing cations and water
Colloid
Quartz
Feldspar
Carbonates
A type of soil colloid that is not crystalline and the negative charges of humus are associated with partially dissociated enolic (-OH), carboxyl (-COOH) and phenolic (-OH) groups.
Inorganic colloid
Organic colloid
Humus
Clay
A type of soil colloid that composed of silicate clays and oxide clays, amorphous clays.
Inorganic colloid
Organic colloid
Clay
Humus
Type of silicate clay minerals that is when saturated with water, basal spacing between layers can approach 20 degrees Amper.
Vermiculite
Illite
Montmorillonite
Kaolinite
A type of silicate clay minerals that capable only of limited expansion ; swells less than montmorillonite because of higher layer charge.
Vermiculite
Illite
Montmorillonite
Kaolinite
The El Nino phenomenon created a global problem on agriculture. This problem is manifested by wide cracks in soil. The cracks are due to be predominance of
Kaolinite
Montmorillonite
Vermiculite
Illite
Which has the highest pH dependent negative charges?
Organic Matter
Illite
Kaolinite
Montmorillonite
This consists of living organisms, dead plants and animal residues and other organic materials in various phases of decomposition.
Humus
Topsoil
Soil organic matter
Clays
A dark, complex mixture of organic substances modified from original organic tissue. Not biologically active and is pool responsible for many of the soil chemical and physical properties associated with soil organic matter and soil quality.
Humus
Topsoil
Soil organic matter
Clays
The cation exchange capacity of soil is a mixture of
The force of bonding between the soil and exchangeable cation
The negative charge of the soil neutralized by easily replaceable cations
The speed which ions added to the soil solution become adsorbed on soil particle surfaces
Acidity
The process whereby ions adsorbed on the surface of the soil colloids are exchanged from ions in the soil solution
Anion exchange
Cation exchange
Ion exchange
Isomorphous substitution
Soil acidity is due to the presence of these both elements in the soil.
CA and S
H and Al
MG and N
P and K
A form of soil acidity due to H+ ion in the soil solution.
Active acidity
Reserved acidity
Reduced acidity
Increase acidity
A form of soil acidity due to H+ and Al3+ in the solid phase, measure of the buffering capacity of the soil.
Active acidity
Reserved acidity
Reduced acidity
Increase acidity
The ability of the soil to resist sudden or drastic changes in pH.
pH dependent
Liming
Buffering capacity
Acid tolerant
A soil chemical property which largely controls nutrient availability and microbial activities.
Buffering capacity
CEC
Soil pH
Soil conductivity
It is considered as one of the causes of soil acidity.
Crop rotation
Irrigation
Leaching of bases
Liming
In order to correct the acidity of the soil, farmer must apply
Humus
Manure
Fertilizer
Lime
These are the effects of lime into the soil EXCEPT.
increase granulation
Neutralization of hydrogen ions
Increase availability of P, MO, CA and K
Inhibit the activity of micro-organisms
To be more effective, a liming material should be applied at the proper time. This is usually done at
Plowing
Planting
3-4 weeks before planting
Harvesting
The most common form of agricultural lime available in the market
CaCo3
CaMg (CO3)2
CaO
MgCO3
In sodic soils, because of the extreme alkalinity resulting from the high sodium content, the surface soil is usually discolored by the dispersed humus that can be carried upward by the capillary water and deposited when it evaporates, hence, the name.
White alkali
Black alkali
Brown alkali
Yellow alkali
It is a kind of salt-affected soils that has high exchangeable sodium percentage causing the soil to be dispersed,thus, making it slowly permeable or impermeable to water.
Sodic soil
Saline-sodic soil
Medium quality
Non-saline non-sodic
In the reclamation of salt-affected soil, the salt content of Saline soils must be lowered and one way is through leaching. In this method, it is desirable to use water of ____________ for leaching out soils.
Good quality
Poor-quality
Medium quality
No quality
Flooding of most rice fields causes the PH to move towards neutrality and as a consequence the availability of nutrients increases, hence, they do not need lime if they are flooded and puddle for rice production.
True
False
It depends
The PH remained unaffected
Deficiency indicates low level of nutrient elements while, this term indicates excessive level of nutrient elements in the plant or soil.
Sufficiency
Toxicity
Hidden hunger
Poverty adjustment
The deficiency of element makes it impossible for the plant to complete its life cycle.
True
False
Probably true
Probably false
The hydrolytic decomposition of proteins and the released of amines and amino acids.
Mineralization
Immobilization
Ammonification
Aminization
A process of converting nitrogen form inorganic to organic forms rendering it available to plants.
Mineralization
Immobilization
Ammonification
Aminization
A process of converting nitrogen from organic to inorganic forms rendering it available to plants.
Mineralization
Immobilization
Ammonification
Aminization
This type of organism derives their food from light (photosynthesis) or from inorganic oxidation reaction.
Heterotrphs
Autotrophs
Semi-heterotrophs
Parasitic plants
Thus type of micro-organism mostly present in moist, sandy soils as they have large pores to accommodate the swimming activities of these highly mobile in the soil. This is commonly called thread worms as eel worms.
Protozoa
Nematodes
Fungi
Algae
It is a single celled prokaryotic organism having no distinct nucleus.
Algae
Bacteria
Fungi
Nematodes
The most efficient organic matter decomposer under acidic soil conditions.
Bacteria
Actinomycetes
Fungi
Protozoa
This refers to the inherent capacity of the soil to provide nutrients to plants in the right and correct proportion.
Soil management
Soil productivity
Soil fertility
Soil condition
Is a capacity of the soil for producing plants or sequence of plants under a specified system of management.
Soil management
Soil productivity
Soil fertility
Soil condition
This process is largely dependent on the growth of roots in a soil
Mass flow
Root interception
Diffusion
Adhesion
Is a movement of ions with soil water. It occurs when solute are transported with the convective flow of water from soil to plant roots.
Mass flow
Root interception
Diffusion
Adhesion
These are common methods of cropping system that can conserved soil and water EXCEPT.
Crop rotation
Contour farming
Green manuring
Irrigation
A type of soil fertility evaluation usually done in the farmers' field to assess the effect of fertilizers and their interactions with all existing factors of growth and development in any given location.
Soil chemical test
Plant analysis
Observation of nutrient deficiency and toxicity symptoms
Field fertilizer experiment
A method of soil fertility evaluation whereby soil nutritional status is known before crop is planted.
Soil chemical test
Plant analysis
Observation of nutrient deficiency and toxicity symptoms
Field fertilizer experiment
This is the minimum guarantee of plant nutrient contents in fertilizer materials in terms of percentage of total N, P2O5 and K2O. Example 14-14-14
Fertilizer materials
Fertilizer grade
Fertilizer content
Fertilizer requirements
A type of inorganic fertilizer that contains the three(3) major elements (N, P2O5 and K2O)
Single
Incomplete
Complete
Compound
It is a method of fertilizer application that farmers dissolve the solid fertilizer materials in water and then apply it as spray to the plants.
Broadcasting
Foliar
Side dressing
Banding
In buying organic fertilizers, it is best to know the following EXCEPT.
Standard weight of 50kg
The moisture content which should be below 35%
The item should not a foul odor
The item should have at least 100% fertilizer grade
A comprehensive soil classification system developed by the soil survey staff of the USA.
Soil classification
Soil taxonomy
Soil survey
Soil diagnostic
The lowest category in the soil taxonomy is
Order
Sub-order
Great group
Series
The most detailed category in soil taxonomy is
Soil series
Soil family
Soil order
Soil great group
A term related to the soil moisture regime That is sufficient moisture during the growing season only.
Aquic
Udic
Xeric
Ustic
A term related to the soil moisture regime That is dry at least half of the growing season.
Aquic
Udic
Aridic
Ustic
Soil order with no diagnostic horizons
Entisols
Inceptisols
Alfisols
Vertisols
A well-developed soil with low base status (acidic) in forest and upland areas in the warm tropics
Entisols
Ultisols
Oxisols
Mollisols
A type of soil survey that it's main concern is the management of the soil scale of maps produced a range from 1:5,000 to 1:15, 000.
Explanatory survey
Reconnaissance survey
Semi-detailed survey
Detailed survey
A type of soil survey that its main purpose is to obtain a rapid general appraisal of an area to determine possible studies to conduct or to locate suitable sites for a development project.
Explanatory survey
Reconnaissance survey
Semi-detailed survey
Detailed survey
It is the ability of the rain to cause soil erosion.
Erosivity
Erodibilty
Erosion control
Erosion measures
The soils'inherent susceptibility to erosion.
Erosivity
Erodibilty
Erosion control
Erosion measures
Water is one of the agents in soil erosion, which of the following did water belong?
Erosivity
Erodibilty
Erosion control
Erosion measures
This refers to any erosion control practices such as contouring, strip cropping, terracing, mulching etc?
Erosivity
Erodibilty
Erosion control
Erosion measures
These are ways of controlling soil erosion EXCEPT.
Reforestation
Contouring
Deforestation
Terracing
