LESSON 5 Flashcards

1
Q

It’s the water returned to the air, from a liquid to gaseous state

A

Evaporation

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2
Q

Evaporation from plants

A

Transpiration

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3
Q

Combination of evaporation and transpiration

A

Evapotranspiration

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4
Q

Used interchangeably with evapotranspiration

A

Consumptive Use

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5
Q

It refers to the sum of evapotranspiration and water used by the plants for tissue building processes

A

Consumptive Use

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6
Q

Importance of Evapotranspiration

A

For water conservation
For determining irrigation requirements for crops
For determining water storage in reservoir

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7
Q

Factors affecting Evaporation

A
  1. Meteorological Factors
  2. Nature of the evaporating surface
  3. Effects of water quality
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8
Q

Meteorological Factors

A

Solar radiation directly affects temperature.

Evaporation is directly proportional to air temperature.

Vapor pressure affects the degree of air saturation.

Evaporation is fast in dry air.

Evaporation is directly proportional to wind speed.

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9
Q

TRUE OR FALSE

All surface exposed to precipitation are
potentially evaporating surfaces

A

True

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10
Q

TRUE OR FALSE

The larger the area exposed to evaporation, the slower the rate of evaporation.

A

False; Faster

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11
Q

Evaporation varies ____________ with salinity of water

A

Inversely

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12
Q

TRUE OR FALSE

Evaporation rate is faster in fresh water due to low vapor pressure.

A

False; High vapor pressure

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13
Q

For saturated soils, evaporation may be similar to that from an ____________. As soil moisture decreases, the rate of evaporation ___________.

A

open free-water surface,
also decreases

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14
Q

Helps in moisture conservation
because they decrease the rate of
evaporation.

A

Mulches

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15
Q

Measurement of Evaporation

A

Evaporation pan
Lysimeter or Evapotranspirimeters

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16
Q

In order to make a measurement that takes these factors into account, it is possible to physically isolate a portion of land from its surroundings and continuously weigh it to monitor changes in water content.

A

Lysimeter or Evapotranspirimeters

17
Q

Methods of Determining ET

A
  1. Field Experimental Plots
  2. Soil Water Studies
  3. Integration Method
  4. Inflow-outflow method
18
Q

the quantity of water applied in these plots is kept small to avoid deep percolation losses and surface runoff is measured

A

Field Experimental Plots

19
Q

samples are taken at various depths in the root zone

A

Soil Water Studies

20
Q

the water used by plants and evaporation from the water and soil surfaces are combined for the entire area involved

A

Integration Method

21
Q

inflow into the area (precipitation), outflow from the area and change in groundwater level are evaluated

A

Inflow-outflow method

22
Q

Categories of Methods of Predicting Evaporation and Evapotranspiration

A
  1. Mass transfer
    2 Energy of Balance
  2. Empirica Methods
23
Q

water moves away from evaporating and transpiring surfaces in response to the combined phenomena of turbulent mixing of the air and the vapor pressure gradient

A

Mass transfer

24
Q

requires measurements of wind and humidity at two or more elevations

A

Mass transfer

25
Q

heat is required for evaporation of water,
so if there is no change in water
temperature, the net radiation or heat
supplied is a measure of evaporation

A

Energy balance

26
Q

developed from experience and field research based on assumption that the energy available for evaporation is proportional to temperature

A

Empirical Methods