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PRINCIPLES AND PRACTICES OF WATER
MANAGEMENT
(AAL102)
Mr. Rohitashv Nagar
Assistant Professor & HOD
Department of Agronomy
School of Agricultural Sciences
Career Point University, Kota (Raj.)
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Lecture-1
Water and its role in plants
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Water: Water is indispensable for human, animal and plant life. It is a
part of all organisms some of which contain more than 90%.Water is
an essential part of protoplasm. It is an important ingredient in
photosynthesis. About 400 to 500 liter of water is necessary for the
production of a kilo of plant dry matter. Water is also required for
translocation of nutrients and dissipation of heat.
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Role of water in plant
1. Water is essential for the germination of seeds and growth of plants.
2. During the process of photosynthesis, plants synthesize carbohydrates
from carbon dioxide and water
3. Water act as a solvent for fertilizers and other minerals, which are
taken up by the plant roots in the from of solution.
4. Water serves as medium for transport of chemicals to and from cell.
5. Aquatic life is possible in water only.
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Water resources of India
Total
Precipitation
400 Mha-m
Infiltration
into the soil
215 Mha-m
Evaporation
70 Mha-m
Surface flow
115 Mha-m
Rain
105 Mha-m
Snow
10 Mha-m
Soil moisture
165 Mha-m
Ground water
50 Mha-m
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Lecture-2
Soil water movement in soil and plants
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Transpiration: Transpiration is the process of water movement
through a plant and its evaporation from aerial parts, such as leaves,
stems and flowers. Water is necessary for plants but only a small
amount of water taken up by the roots is used for growth and
metabolism.
Factors affecting transpiration: Temperature, Water, Wind. The
environmental factors affecting transpiration in plants include light,
relative humidity, temperature, availability of water, and wind.
Specifically, these are climatic elements which
also affect photosynthesis and other plant growth and development
processes.
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Purpose of transpiration in plants: Transpiration serves three
essential roles: Movement of water and nutrients – Moves minerals
up from the root (in the xylem) and sugars (products of
photosynthesis) throughout the plant (in the phloem). Cooling –
80% of the cooling effect of a shade tree is from the evaporative
cooling effects of transpiration.
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Soil Moisture Constants
• Water contents under certain standard conditions are referred to as soil
moisture constants.
1. Saturation capacity: Saturation capacity refers to the condition of soil
at which all the macro and micro pores are filled with water and the soil
is at maximum water retention capacity.
2. Field capacity: At field capacity, the soil moisture tension depending on
the soil texture ranges from 0.10 to 0.33 bars (or −10 to −33 kPa). field
capacity is considered as the upper limit of available soil moisture.
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Physical Classification of Water
1. Gravitational water: Water held between 0.0 to 0.33 bars (0 to −33 kPa)
soil moisture tension, free and in excess of field capacity, which moves
rapidly down towards the water table under the influence of gravity is
termed as gravitational water.
2. Capillary water: As the name suggests capillary water is held in the
pores of capillary size i.e., micro pores around the soil particles by
adhesion (attraction of water molecules for soil particles), cohesion
(attraction between water molecules) and surface tension phenomena. It
includes available form of liquid water extracted by growing plants and is
held between field capacity (0.33 bars or −33 kPa) and hygroscopic
coefficient (31 bars or −3100 kPa).
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3. Hygroscopic water: The water held tightly in thin films of 4 – 5 milli
microns thickness on the surface of soil colloidal particles at 31 bars
tension (−3100 kPa) and above is termed as hygroscopic water.
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Soil – Plant and Plant – Water Relations
• To design a successful irrigation system, it is essential to know the plant
rooting characteristics, effective root zone depth, moisture extraction
pattern and moisture sensitive periods of crops.
• Rooting characteristic of plants: The purpose of irrigation is to
provide adequate soil moisture in the immediate vicinity of the plant
roots. All plants do not have the similar rooting pattern i.e., root
penetration and proliferation. Some plants have relatively shallow root
system (for example annual crops), while others develop several meters
under favorable conditions (for example tree crops).
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Soil properties influencing root development
1. Hard pan: Root penetration is seriously affected by presence of a hard
pan or compacted layer in the soil profile. Thus roots cannot penetrate a
hard layer except through cracks.
2. Soil moisture: Since roots cannot grow in soil that is depleted in
moisture down to and below the permanent wilting point, a layer of dry
soil below the surface in the profile can restrict root penetration.
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3. Water table: A high water table limits root growth, and a rising water
table may kill roots that have previously grown below the new water
level.
4. Toxic substances: Presence of toxic substances in the sub-soil also
limits root growth and development. Saline layers or patches in the soil
profile therefore inhibit or prevent root penetration and proliferation.
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Types of water movement
• Generally three types of water movement within the soil are
recognized –saturated flow, unsaturated flow and water vapour flow.
1. Saturated water movement: The condition of the soil when all the
macro and micro pores are filled with water the soil is said to be at
saturation, and any water flow under this soil condition is referred to
as saturated flow.
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2. Unsaturated water movement: The soil is said to be under
unsaturated condition when the soil macro pores are mostly filled
with air and the micro pores (capillary pores) with water and some
air, and any water movement or flow taking place under this soil
condition is referred to as unsaturated flow.
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Water absorption by plants
Mechanism of Absorption of Water: In higher plants water is
absorbed through root hairs which are in contact with soil water and
form a root hair zone a little behind the root tips.
Mechanism of water absorption is of two types:
1. Active Absorption of Water: In this process the root cells play
active role in the absorption of water and metabolic energy released
through respiration is consumed.
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2. Passive Absorption of Water: It is mainly due to transpiration, the
root cells do not play active role and remain passive.
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Water stress: Water stress occurs when the demand for water exceeds
the available amount during a certain period or when poor quality
restricts its use. Water stress causes deterioration of fresh water
resources in terms of quantity (aquifer over-exploitation, dry rivers,
etc.).
Moisture stress: Moisture stress occurs when the water in a plant's cells
is reduced to less than normal levels.
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Crop plant adaptation to moisture stress condition
Effect on cereals:
1. On floral initiation, anthesis (wheat and rice)
2. At ripening stage (reduction in test wt.)
3. Plant height, leaf area.
4. leaf rolling, drying, premature death of leaf.
5. Reduction in photosynthesis and dry matter production.
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Effects on pulses and fruit crops:
• Flower abortion.
• Stress during pod filling reduces test wt.
• In some cases, drought prevails causes premature flowering which
results in reduced yield, size of pods, seeds and fruits.
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The Effect of Water Stress on Plants
• Wilting: As wilting increases, plant cells fully deflate, causing their
deaths. Partially wilted plants that are still green may recover if watering
is quickly initiated -- the addition of mulch helps to keep soil moisture
even.
• Reduced Photosynthesis: Photosynthesis is the process through which
plants create their own food. The amount of water, sunlight and carbon
dioxide available to the plant directly influences the amount of food a
plant can produce. When water levels are low due to water stress,
photosynthesis can slow or even stop, causing internal food supplies
vital to other processes to diminish or disappear -- yellowing may also
occur if photosynthesis stops completely.
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• Reduced Respiration: Respiration is the process through which
plants break down their food supply for energy to power system
processes. When plants are actively growing, they respirator heavily,
using up food stores quickly. With low water levels reducing the
plant's ability to photosynthesize, the plant's system processes slow
down, causing reduced or delayed growth and discoloration of
leaves, as well as flower or fruit drop.
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• Reduced Transpiration: Water taken up by a plant's roots is slowly
drawn up to openings in its leaves called stomas. The stomas release
waste products such as oxygen into the environment and bring in
carbon dioxide. This release also helps cool plant tissues. In
addition, transpiration maintains turgor in plants, keeping cells
evenly filled with water. When transpiration is stopped or slowed,
the plant begins to die from lack of nutrients, usually from the top
down.
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Role of water in plants

  • 1. Career Point Cares PRINCIPLES AND PRACTICES OF WATER MANAGEMENT (AAL102) Mr. Rohitashv Nagar Assistant Professor & HOD Department of Agronomy School of Agricultural Sciences Career Point University, Kota (Raj.)
  • 2. Career Point Cares Lecture-1 Water and its role in plants
  • 3. Career Point Cares Water: Water is indispensable for human, animal and plant life. It is a part of all organisms some of which contain more than 90%.Water is an essential part of protoplasm. It is an important ingredient in photosynthesis. About 400 to 500 liter of water is necessary for the production of a kilo of plant dry matter. Water is also required for translocation of nutrients and dissipation of heat.
  • 4. Career Point Cares Role of water in plant 1. Water is essential for the germination of seeds and growth of plants. 2. During the process of photosynthesis, plants synthesize carbohydrates from carbon dioxide and water 3. Water act as a solvent for fertilizers and other minerals, which are taken up by the plant roots in the from of solution. 4. Water serves as medium for transport of chemicals to and from cell. 5. Aquatic life is possible in water only.
  • 5. Career Point Cares Water resources of India Total Precipitation 400 Mha-m Infiltration into the soil 215 Mha-m Evaporation 70 Mha-m Surface flow 115 Mha-m Rain 105 Mha-m Snow 10 Mha-m Soil moisture 165 Mha-m Ground water 50 Mha-m
  • 6. Career Point Cares Lecture-2 Soil water movement in soil and plants
  • 7. Career Point Cares Transpiration: Transpiration is the process of water movement through a plant and its evaporation from aerial parts, such as leaves, stems and flowers. Water is necessary for plants but only a small amount of water taken up by the roots is used for growth and metabolism. Factors affecting transpiration: Temperature, Water, Wind. The environmental factors affecting transpiration in plants include light, relative humidity, temperature, availability of water, and wind. Specifically, these are climatic elements which also affect photosynthesis and other plant growth and development processes.
  • 8. Career Point Cares Purpose of transpiration in plants: Transpiration serves three essential roles: Movement of water and nutrients – Moves minerals up from the root (in the xylem) and sugars (products of photosynthesis) throughout the plant (in the phloem). Cooling – 80% of the cooling effect of a shade tree is from the evaporative cooling effects of transpiration.
  • 10. Career Point Cares Soil Moisture Constants • Water contents under certain standard conditions are referred to as soil moisture constants. 1. Saturation capacity: Saturation capacity refers to the condition of soil at which all the macro and micro pores are filled with water and the soil is at maximum water retention capacity. 2. Field capacity: At field capacity, the soil moisture tension depending on the soil texture ranges from 0.10 to 0.33 bars (or −10 to −33 kPa). field capacity is considered as the upper limit of available soil moisture.
  • 12. Career Point Cares Physical Classification of Water 1. Gravitational water: Water held between 0.0 to 0.33 bars (0 to −33 kPa) soil moisture tension, free and in excess of field capacity, which moves rapidly down towards the water table under the influence of gravity is termed as gravitational water. 2. Capillary water: As the name suggests capillary water is held in the pores of capillary size i.e., micro pores around the soil particles by adhesion (attraction of water molecules for soil particles), cohesion (attraction between water molecules) and surface tension phenomena. It includes available form of liquid water extracted by growing plants and is held between field capacity (0.33 bars or −33 kPa) and hygroscopic coefficient (31 bars or −3100 kPa).
  • 13. Career Point Cares 3. Hygroscopic water: The water held tightly in thin films of 4 – 5 milli microns thickness on the surface of soil colloidal particles at 31 bars tension (−3100 kPa) and above is termed as hygroscopic water.
  • 14. Career Point Cares Soil – Plant and Plant – Water Relations • To design a successful irrigation system, it is essential to know the plant rooting characteristics, effective root zone depth, moisture extraction pattern and moisture sensitive periods of crops. • Rooting characteristic of plants: The purpose of irrigation is to provide adequate soil moisture in the immediate vicinity of the plant roots. All plants do not have the similar rooting pattern i.e., root penetration and proliferation. Some plants have relatively shallow root system (for example annual crops), while others develop several meters under favorable conditions (for example tree crops).
  • 15. Career Point Cares Soil properties influencing root development 1. Hard pan: Root penetration is seriously affected by presence of a hard pan or compacted layer in the soil profile. Thus roots cannot penetrate a hard layer except through cracks. 2. Soil moisture: Since roots cannot grow in soil that is depleted in moisture down to and below the permanent wilting point, a layer of dry soil below the surface in the profile can restrict root penetration.
  • 16. Career Point Cares 3. Water table: A high water table limits root growth, and a rising water table may kill roots that have previously grown below the new water level. 4. Toxic substances: Presence of toxic substances in the sub-soil also limits root growth and development. Saline layers or patches in the soil profile therefore inhibit or prevent root penetration and proliferation.
  • 17. Career Point Cares Types of water movement • Generally three types of water movement within the soil are recognized –saturated flow, unsaturated flow and water vapour flow. 1. Saturated water movement: The condition of the soil when all the macro and micro pores are filled with water the soil is said to be at saturation, and any water flow under this soil condition is referred to as saturated flow.
  • 18. Career Point Cares 2. Unsaturated water movement: The soil is said to be under unsaturated condition when the soil macro pores are mostly filled with air and the micro pores (capillary pores) with water and some air, and any water movement or flow taking place under this soil condition is referred to as unsaturated flow.
  • 20. Career Point Cares Water absorption by plants Mechanism of Absorption of Water: In higher plants water is absorbed through root hairs which are in contact with soil water and form a root hair zone a little behind the root tips. Mechanism of water absorption is of two types: 1. Active Absorption of Water: In this process the root cells play active role in the absorption of water and metabolic energy released through respiration is consumed.
  • 21. Career Point Cares 2. Passive Absorption of Water: It is mainly due to transpiration, the root cells do not play active role and remain passive.
  • 23. Career Point Cares Water stress: Water stress occurs when the demand for water exceeds the available amount during a certain period or when poor quality restricts its use. Water stress causes deterioration of fresh water resources in terms of quantity (aquifer over-exploitation, dry rivers, etc.). Moisture stress: Moisture stress occurs when the water in a plant's cells is reduced to less than normal levels.
  • 24. Career Point Cares Crop plant adaptation to moisture stress condition Effect on cereals: 1. On floral initiation, anthesis (wheat and rice) 2. At ripening stage (reduction in test wt.) 3. Plant height, leaf area. 4. leaf rolling, drying, premature death of leaf. 5. Reduction in photosynthesis and dry matter production.
  • 25. Career Point Cares Effects on pulses and fruit crops: • Flower abortion. • Stress during pod filling reduces test wt. • In some cases, drought prevails causes premature flowering which results in reduced yield, size of pods, seeds and fruits.
  • 26. Career Point Cares The Effect of Water Stress on Plants • Wilting: As wilting increases, plant cells fully deflate, causing their deaths. Partially wilted plants that are still green may recover if watering is quickly initiated -- the addition of mulch helps to keep soil moisture even. • Reduced Photosynthesis: Photosynthesis is the process through which plants create their own food. The amount of water, sunlight and carbon dioxide available to the plant directly influences the amount of food a plant can produce. When water levels are low due to water stress, photosynthesis can slow or even stop, causing internal food supplies vital to other processes to diminish or disappear -- yellowing may also occur if photosynthesis stops completely.
  • 27. Career Point Cares • Reduced Respiration: Respiration is the process through which plants break down their food supply for energy to power system processes. When plants are actively growing, they respirator heavily, using up food stores quickly. With low water levels reducing the plant's ability to photosynthesize, the plant's system processes slow down, causing reduced or delayed growth and discoloration of leaves, as well as flower or fruit drop.
  • 28. Career Point Cares • Reduced Transpiration: Water taken up by a plant's roots is slowly drawn up to openings in its leaves called stomas. The stomas release waste products such as oxygen into the environment and bring in carbon dioxide. This release also helps cool plant tissues. In addition, transpiration maintains turgor in plants, keeping cells evenly filled with water. When transpiration is stopped or slowed, the plant begins to die from lack of nutrients, usually from the top down.