SWCE PT.1 Flashcards
- The factor that affects adoption of soil
and water conservation measures
a. land tenure
b. high initial investment cost
c. construction skills
d. both a and
e. all of the above
Answer: e. all of the above
- A wet area, periodically inundated with standing or
slow moving water, that has grassy or herbaceous
vegetation and often little peat accumulation; the
water may be salt, brackish or fresh
a. karst
b. Marsh
c. Peat
d. Valley
Answer: b. Marsh
- Regions that are characterized by formations
underlain by carbonate rock typified by the
presence of limestone caverns and sinkholes
a. Karst
b. Marsh
c. Peat
d. Wetland
Answer: a. Karst
- Which of the following is not a soil structure?
a. Loam
b. Crumb
c. Platy
d. Sub-angular blocky
e. Prismatic
Answer: a. Loam
- Soil productivity is the ability of the soil
a. To produce the desired amount of plant yield
b. Supply nutrients in sufficient and balanced
amounts
c. Store and resist leaching nutrients
d. All of the above
Answer: a. To produce the desired amount of plant yield
- When a sickly yellowish green color was found,
the plant was possibly suffering from what
major element deficiency?
a. Nitrogen
b. Boron
c. Phosphorus
d. Zinc
e. Potassium
Answer: a. Nitrogen
- Refers to the manifestation of physical forces of
cohesion and adhesion acting within the soil at
various moisture contents.
a. Soil consistency
b. Soil aggregate
c. Soil cohesion
d. Soil structure
e. Soil texture
Answer: a. Soil consistency
- It has the property of soil which enables clay
to change slope without cracking when it is
subjected to deforming stress.
a. Puddlability
b. Permeability
c. Friability
d. Consistency
e. Plasticity
Answer: e. Plasticity
- Refers to the relative proportion of various size
groups of individual soil grains:
a. Soil texture
b. Soil consistency
c. Soil colloid
d. Soil profile
e. Soil structure
Answer: a. Soil texture
- Water which has been absorbed from an
atmosphere of water vapor as a result of
attractive forces in the surface of the particles.
a. Capillary water
b. Hygroscopic water
c. Rainwater
d. Gravitational water
e. Mineral water
Answer: b. Hygroscopic water
Kinds of Soil Water
Hygroscopic water – water held tightly to the surface of soil particles by adsorption forces
Capillary water – water held by forces of surface tension and continuous film around soil particle and
capillary spaces
Gravitational water – water that moves freely in
response to gravity and drains out of the soil
- It is refer to the ease of crumbling of soils.
a. Plasticity
b. Soil colloid
c. Soil consistency
d. Friability
Answer: d. Friability
- A natural body composed of a variable mixture of
broken and weathered minerals and decaying
organic matter and when containing the proper
amount of air and water, supplies sustenance
and gives mechanical support of plants:
a. Fertilizer
b. Soil
c. Humus
d. Rock
e. Mineral
Answer: b. Soil
- The study of soil which puts more emphasis
on the origin, characteristics, classification
and description:
a. Pedology
b. Pathology
c. Agronomy
d. Soil science
Answer: a. Pedology
- The percentage of moisture on dry weight basis that
is held against the pull of gravity, after drainage has
ceased in a soil that has been saturated:
a. Wilting point
b. Hygroscopic coefficient
c. Air dry
d. Field capacity
e. Oven dry weight
Answer: d. Field capacity
Soil Moisture constants:
1. Saturation Capacity – all pores of the soil are filled
with water - Maximum water-holding capacity
2. Field Capacity (FC) – is the moisture content after
drainage of gravitational water has become very slow and the moisture content has become relatively stable
3. Permanent Wilting Point/Percentage (PWP) – moisture content at which plants can no longer obtain enough moisture to meet transpiration requirement and remain wilted (and eventually dies) unless water is added
4. Moisture equivalent – amount of water retained by a sample of initially saturated soil material
5. Wilting Range – range in soil moisture content which plants undergo progressive degree of permanent or irreversible wilting
6. Available Water – soil moisture between field capacity and permanent wilting
point
- The capacity of water bodies to cleanse
themselves of pollutants over a period of time
and/or stretch
a. Stress capacity
b. Driving capacity
c. Assimilative capacity
d. Water holding capacity
Answer: c. Assimilative capacity
- Are natural drainage areas within the
boundary defined by the divide
a. Watershed
b. Catchment
c. Basin
d. All of the above
Answer: d. All of the above
The following are watershed descriptors,
except
a. Drainage density
b. Basin shape
c. Relief ratio
d. Stream order
e. Flood routing
Answer: e. Flood routing
- A watershed descriptor that describes the
dissection of a basin and determines its
response to a rainfall input
a. Drainage density
b. Circulatory ratio
c. Relief ratio
d. Stream order
e. Stream gradient
Answer: a. Drainage density
- The area of a drainage basin is approximately
10000 acre with an average length of 2500m. The
elevation of the remote place of the basin from the
outlet stream is 1000m. What is the estimated
time where the flow reaches the outlet stream.
a. 0.191
b. 0.155
c. 0.595
d. 0.115
Answer: a. 0.191
The ratio of the circumference of a circle, of
the same area as the basin, to the basin
perimeter
a. Circulatory ratio
b. Elongation ratio
c. Relief ratio
d. Circumferential ratio
Answer: a. Circulatory ratio
The capacity of rainfall (precipitation) to effect
the detachment and transport of soil particles.
a. Erodibility
b. Erosivity
c. Effectivity
d. Conductivity
Answer: b. Erosivity
Soil Erosion –is the detachment and transport of soil particles by natural (i.e. water and wind) or anthropogenic (man-induced or man-related) causes.
Soil Erodibility – the susceptibility of the soil to be
eroded
Rainfall Erosivity – the capacity of rainfall to cause
erosion
Eroding agents – rainfall/raindrop, runoff, wind
Which of the following is not a purpose of
terracing?
a. To reduce soil erosion
b. For water conservation
c. For flood control
d. For soil fertility rejuvenation
e. None of the above
Answer: d. For soil fertility rejuvenation
Soil erosion is the _______ of soil particles
by natural or anthropogenic causes.
a. Detachment
b. Detachment and transport
c. Detachment, transport and deposition
d. Detachment and entrainment
e. Detachment, transport and entrainment
Answer: b. Detachment and transport
The following are on-site effects of erosion,
except
a. Reduced crop productivity
b. Reduced infiltration
c. Increased of direct runoff
d. Damaged biodiversity
e. None of the above
Answer: e. None of the above