記憶度
11問
28問
0問
0問
0問
アカウント登録して、解答結果を保存しよう
問題一覧
1
sometimes, this is considered negligible and are not included in the estimation process.
Evaporation losses
2
assures the transport of water within the fields
field application system
3
portion of the perimeter of the canal that is in contact with the flowing water.
Wetted perimeter
4
Types of Aquifer
Unconfined Aquifer , Confined Aquifer, Perched Aquifer
5
ratio of the bulk density of the soil with the density of water; it is the ratio of the weight of soil to the weight of water with volume equal to the total soil volume
Apparent specific gravity
6
any water bearing, permeable geological formation that stores and transmits water
Aquifer
7
The measure of the amount of water in the soil. It can be expressed as a dry mass basis or volume basis.
Moisture content
8
are used all over the world as sources of irrigation water
Rivers
9
water flow that is conveyed in such a manner that top surface is exposed to the atmosphere such as flow in canals, ditches, drainage channels, culverts, and pipes under partially full flow conditions.
Open channel flow
10
Refers to the water that is above the Earth’s surface. Includes lakes, rivers, and man-made reservoir such as dams. It is highly prone to pollution.
Surface water
11
canals with impermeable material for channel stabilization and/or reduced seepage.
Lined channel
12
the arrangements of primary particles in the soil into units or peds
Soil structure
13
grade line of the water surface profile plus the velocity head in open channels.
Energy grade line
14
are due to operator or technician skill, which may affect the volume delivered to the farm
Operation losses
15
kinds of runoff
Surface Runoff, Interflow – subsurface runoff , Baseflow
16
usually a reservoir, surface water such as swamps, rivers, or lakes, or a pumping station with either a surface or groundwater source. It directs water into the irrigation system.
Main intake structure
17
the ratio of the volume of water to the total soil volume
Volume Basis
18
water is directly diverted from the river without any structures, dams or other devices. The off-take canal is directly excavated through the river bank and no gate is provided
Direct River Diversion
19
are supplied with water by rainfall that falls directly on the surface of the lake, by water run-off from the adjacent landand small streams, or by groundwater that seeps through the soil to the lowest point which is the lake.
Lakes
20
describes any liquid or solid water that falls to Earth as a result of condensation in the atmosphere.
Precipitation
21
Water Sources for Irrigation
Surface water, Groundwater
22
transports water from the main intake structure or main pumping station up to the farm ditches.
The conveyance system
23
provides the moisture needed by the crop that is not satisfied by rainfall.
Irrigation
24
is a process in all plants that normally takes place during the day, giving off water vapor from the leaves openings.
Transpiration
25
an impermeable body of rock which contains no interconnected openings or interstices and therefore neither absorbs nor transmits water
Aquifuge
26
the amount of water the soil profile will hold when all its pore spaces are filled up with water
Saturation Point
27
the difference in moisture content of the soil between field capacity and the permanent wilting point.
Available Moisture
28
an important source of irrigation water, especially for small-scale irrigation projects. Because it is only available below ground level, it must be lifted, or pumped before it can be used
groundwater
29
slope of the water surface profile plus the velocity head in open channels
Slope of the energy grade line
30
this is the most significant loss that should be considered for efficiency improvement. It is defined as the downward and lateral movement of water into the soil.
Seepage losses
31
vertical line from the top of the channel to the water surface at the design condition.
Free board
32
a body that does not allow transmission of a significant amount of water, such as clay, a till, or a poorly fractured igneous or metamorphic rocks.
Aquitard
33
depth of water in the channel cross section
Depth
34
An aquifer that is exposed at the ground surface that is the aquifer formation extends essentially to the land surface.
Unconfined Aquifer
35
the process of a liquid's surface changing to a gas.
Evaporation
36
is the application of water to create a condition in the soil that is favorable for plant growth.
Irrigation
37
width of the channel cross-section at the free surface
Top width
38
that portion of the available moisture that is most easily extracted by plants; this is approximately 75% of the available moisture
Readily Available Moisture
39
Special type of unconfined aquifer and occurs when the ground water body is separated from the main ground water by a relatively impermeable stratum of small aerial extend and by the zone of aeration above the main body of groundwater.
Perched Aquifer
40
Water used for irrigation comes from?
surface water or groundwater
41
is the removal of excess water in the soil to create conditions suitable for plant growth.
Drainage
42
removes the excess water from the fields.
drainage system
43
as the portion of rainfall, snowmelt, and/or irrigation water that runs over the soil surface toward the stream rather than infiltrating into the soil.
Runoff
44
cross sectional area of a conveyance channel measured perpendicular to the direction of flow
Area
45
constant flow depth along a longitudinal section of a channel under a uniform flow condition
Normal depth
46
impermeable formation which contains water
Aquiclude
47
occurs when flow has a constant water area, depth, discharge, and average velocity through a reach of channel.
Uniform flow
48
The ratio of the weight of water to the dry weight of the soil
Dry Mass Basis
49
is the movement of irrigation water from a source. It is usually done using a simple earth canal or a network of control structures,channels, and distribution system
Water conveyance
50
the ratio of the void volume to the total soil volume. It is denoted by the letter “n”.
porosity
51
takes place when the water is absorbed by vegetation cover and trees, absorbed into the ground, or stored in puddles and land formations such as furrows and streamlets.
Interception
52
physical process involving the slow passage of water through the soil.
Infiltration
53
the process of a gas changing to a liquid.
Condensation
54
the soil moisture content when plants permanently wilt. The soil moisture tension at this point is about 15 atmospheres
Permanent Wilting Point
55
A well that brings groundwater to the surface without pumping because it is under pressure within a body of rock and/or sediments known as an aquifer.
Artesian Wells
56
are very common in the construction of concrete-lined canals
Rectangular channels
57
It is the one in which groundwater is confined under pressure greater than the atmospheric pressure by overlying and underlying impervious layers.
Confined Aquifer
58
elevation drop per unit length of the channel bottom
Channel bed slope
59
the amount of water a soil profile will hold against drainage by gravity at a specified time (usually from 24 to 48 hours) after a thorough wetting. (2) the moisture content of the soil when gravitational water has been removed (after irrigation by flooding). It is usually determined few days after irrigation. The soil moisture tension at this point is normally between 1/10 to 1/3 atmosphere.
Field Capacity
60
is an artificial lake. It can be formed by building a dam across a valley, by excavating the land or by surrounding apiece of land with dykes
Reservoir
61
To avoid the problems caused by fluctuating water levels in a river, a weir can be built across the river.
River diversion using weir
62
refers to the controlled application of water from agriculture through man-made systems.
Irrigation
63
ratio of the particle density of the soil with the density of water; it is the ratio of the weight of soil to the weight of water with volume equal to the volume of the soil particles alone
Real specific gravity
64
Refers to the water that is below the Earth’s surface. Less prone to pollution
Groundwater
65
ratio of flow area to the wetted top width
Hydraulic depth
66
ratio of the horizontal to vertical dimension of the channel wall
Side slope
67
is on the transport of water through field ditches to the fields to be irrigated
distribution system
68
refers to the relative proportion of various size groups of individual soil grains. It is determined by the relative proportion of sand, silt, and clay fractions present in the soil.
Soil texture
69
slope of the free water surface
Slope of the hydraulic grade line
70
the ratio of the dry weight of the soil to the volume of the soil particles
Particle density
71
cross sectional area of flow divided by the wetted perimeter
Hydraulic radius
72
methods in measuring soil moisture
Gravimetric Method , Soil Moisture Sensors, Remote Sensing