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Prepared By
MD. ASADUZZAMAN
Department of Soil, Water and Environment
University of Dhaka
 About 2.8 million hectares of land in Bangladesh is
within the grip of salinity which is equal to about one
fifth of the total area.
 Out of these coastal areas about 0.833 million hectares
of the arable lands, which constitutes about 52.85% of
the net cultivable area in 64 upazillas of 13 districts
are affected by varying degrees of soil salinity.
 A considerable success in boosting up of food production
could be achieved by the efficient utilization of this vast
area of land.
 The salinity prevalent in Noakhali, Khulna, Comilla,
Barisal and Patuakhali districts has penetrated upto
about 151.4 km and 46.3 km inland from coasts of Khulna
and Barisal, respectively.
 It is the view to the experts, that with the introduction of
high yielding varieties of different crops these lands may
become suitable for crop lands following proper planned
cultivation.
District Salinity Categories
(thousand hectares)
District
Total
S1 S2 S3 S4
1. Satkhira 16.50 85.60 33.35 10.90 146.35
2. Khulna 3.90 92.54 13.80 9.80 120.04
3. Patuakhali 68.50 46.60 0.00 0.00 115.10
4. Bagerhat 28.30 77.08 2.60 0.00 107.98
5. Barguna 96.39 7.20 0.00 0.00 103.35
6. Cox’s Bazar 7.20 16.20 17.30 14.00 54.70
Source: Soils Publication No. 33, BARC (1990)
Intensity of Soil Salinity: S1>S2>S3>S4.
District Salinity Categories
(thousand hectares)
District
Total
S1 S2 S3 S4
7. Noakhali 6.30 39.90 3.40 0.00 49.60
8. Bhola 9.52 30.81 0.00 0.00 40.33
9. Pirojpur 18.40 1.90 0.00 0.00 20.30
10. Laxmi
pur
10.90 6.80 1.60 0.00 19.30
11. Feni 1.60 6.70 0.70 0.00 9.00
12. Chand
pur
1.50 0.00 0.00 0.00 1.50
Country total 287.37 426.43 79.75 39.90 833.45
Figure : The coastal area soil in Bangladesh
 The soils which contain sufficient water-soluble salts
in the root zone affect or impair plant growth in
general, may be termed as saline soil.
 According to Biswas and Mukherjee (1987), saline soils
are soils containing excess of nutral soluble salts
dominated by chlorides and sulfates that affect plant
growth.
Definition of saline soil
Formation of Saline Soil
According to Boyer (1970) the most important sources of
salts in the formation of saline soils are
•Intrusion of sea water
•Marine sediments
•Saline ground water
•Saline irrigation water
•Poor drainage
•Seepage from canals, and
•Arid climate
 In areas of low rainfall, salts formed during the
weathering of soil minerals are not fully leached.
 The salinity sources in Bangladesh are quite different
from the other saline areas of arid and semi arid
regions of the world. Here, the main cause of salinity is
marine origin. Sea water salinity surrounding the
coastal areas of Bangladesh is induced by
1) salt water intrusion during cyclone or typhoon,
2) direct inundation by saline or brackish water,
3) heavy withdrawal of water upstream by neighboring
country, which results saline water movement along
the main rivers and tributaries,
4) upward or lateral movement of saline ground water
during the dry season and
5) withdrawal of ground water in the northwest for
irrigation which encourages saline water movement in
the aquifers, and since fresh water is costly and rare,
farmers have tendency to irrigate land with saline
water flowing through rivers.
 Patchy stand and stunted growth are the most obvious
features observed in plants due to salinity. No yield
enhancement at any salinity level.
 Sodium chloride and sodium sulphate salinities
suppressed the growth of peanut. High concentration
of both NaCl and Na2SO4 greatly reduced the shoot
growth, biomass and dry weight of all plant parts.
Shoot length was also reduced at all concentrations of
both salts
 Salt tolerance of plants is associated with salt
exclusion, which is the ability of plants to restrict the
uptake and/or transport of salt between roots & shoots.
Evidence has shown that shoot growth of Etrog citron
and Kharna khatta was reduced significantly by 50mm
NaCl, but growth of Ranpur lime plants showed a
marked reduction only at 100ml NaCl
 Salinity treatment with 48 mM NaCl in solution culture
reduced dry matter production by 65% in shoots and
43% in roots of sunflower plants.
 The aim of reclamation is to remove salinity from the root
zone within permissible limits, so as to restore the
productivity of salt-affected soil.
 Before starting the reclamation of saline soil knowledge
of the following is essential.
1. Quality of irrigation water.
2. Nature and distribution of salt in the coastal zone.
3. Level of sub-soil water.
4. Drainage condition.
Reclamation of Saline Soil
Eradication or
removal of the salts
-Leaching
-Irrigation
management
-Drainage
management
-Beneficial use of
multiple water
resources
Conversion of some
of the salts to less
injurious forms
-By using gypsum
-By using elemental
sulfur and sulfuric
acid
Designated
control
-Mulching
-Crop choice
-Pre-plant
irrigation
 The most common method used to the free soil of
excess salts is installation of drainage systems and
leaching or flushing.
 A combination of two, flooding after field drainage
ditches have been installed, is the most through and
satisfactory.
 The salts that dissolve are leached from the solum and
drained away.
Eradication or Removal of the Salts
 Application of excess water, above evapotranspiration
requirements to leach salts from the root zone of soils
may effectively control salinity.
 The most common method by which salt is removed is
by leaching it out of the root zone with water.
 An equation for this is
DiCi – DdCd = 0
 Di (the volume of water per unit area of land is
expressed by its depth),
 Ci , initial salt concentration,
 Dd, the volume of water drained out of the soil,
 Cd the salt concentration which drained out by water.
Leaching
Salinity Control during Irrigation
 While it is difficult to forecast accurately the tolerance of
crops, the comparative data presented in the following
table may be helpful.
 Table : Relative tolerance of certain plants to salty soils:
Tolerant Moderately
tolerant
Moderately
sensitive
Sensitive
Barley, grain
Bermuda grass
Bougainvillea
Cotton
Date
Barley, forage
Beet, garden
Broccoli
Brome grass
Clover, berseem
Alfalfa
Broad bean
Cauliflower
Cabbage
Clover
Apple
Apricot
Bean
Blackberry
Carrot celery
Source: Cited by Nyle C. Brady (1990) in
“The Nature and Properties of Soil” as
modified from Carter (1981).
Tolerant Moderately
tolerant
Moderately
sensitive
Sensitive
Natal plum
Mutall alkali grass
Rescue grass
Rosemary
Sugar beet
Salt grass
Wheat grass
Wild rye
Wheat grass, tall
Fig
Orchard grass
Oats
Rye, hay
Sorghum
Sudan grass
Wheat
What grass, western
Trefoil, birds foot
Corn
Cowpea
Cucumber
Lettuce
Pea
Peanut
Rice, paddy
Soya-bean
Sweet clover,
timothy
Grape fruit
Lemon
Onion
Orange
Peach
Pineapple, Guava
Potato
Rose
Strawberry,
Tomato
 Bangladesh is a vast delta having 14.2 million ha, of which
roughly coastal brackish waters cover 17%.
 At present only 5% of the coastal brackish water region is
under coastal aquaculture mainly for shrimp farming.
 Gradually shrimp production is increasing through horizontal
expansion of the farming area.
 So that, coastal aquaculture would develop as a good source
of animal protein for the growing population.
 A foreign currency earner and as well as maintainer of
ecological balances in the brackish-water region.
 Correct planning, regulation and motivation are needed to
develop an environment friendly coastal aquaculture
program to avoid ecological disasters in a land scarce and
densely populated like Bangladesh.
 Development of coastal area soils for agricultural purposes
is of great importance for a small country like Bangladesh.
 The reclamation of saline soils and practicing cultivation
of salinity resistant crop varieties should be emphasized.
 Another potentiality of our coastal soils is the shrimp
production and export of which can earn substantial
foreign currency.
 So, the soils’ potentialities should be explored as well as
managed for agricultural sustainability of future
Bangladesh.
Presentation

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Presentation

  • 1. Prepared By MD. ASADUZZAMAN Department of Soil, Water and Environment University of Dhaka
  • 2.  About 2.8 million hectares of land in Bangladesh is within the grip of salinity which is equal to about one fifth of the total area.  Out of these coastal areas about 0.833 million hectares of the arable lands, which constitutes about 52.85% of the net cultivable area in 64 upazillas of 13 districts are affected by varying degrees of soil salinity.
  • 3.  A considerable success in boosting up of food production could be achieved by the efficient utilization of this vast area of land.  The salinity prevalent in Noakhali, Khulna, Comilla, Barisal and Patuakhali districts has penetrated upto about 151.4 km and 46.3 km inland from coasts of Khulna and Barisal, respectively.  It is the view to the experts, that with the introduction of high yielding varieties of different crops these lands may become suitable for crop lands following proper planned cultivation.
  • 4. District Salinity Categories (thousand hectares) District Total S1 S2 S3 S4 1. Satkhira 16.50 85.60 33.35 10.90 146.35 2. Khulna 3.90 92.54 13.80 9.80 120.04 3. Patuakhali 68.50 46.60 0.00 0.00 115.10 4. Bagerhat 28.30 77.08 2.60 0.00 107.98 5. Barguna 96.39 7.20 0.00 0.00 103.35 6. Cox’s Bazar 7.20 16.20 17.30 14.00 54.70
  • 5. Source: Soils Publication No. 33, BARC (1990) Intensity of Soil Salinity: S1>S2>S3>S4. District Salinity Categories (thousand hectares) District Total S1 S2 S3 S4 7. Noakhali 6.30 39.90 3.40 0.00 49.60 8. Bhola 9.52 30.81 0.00 0.00 40.33 9. Pirojpur 18.40 1.90 0.00 0.00 20.30 10. Laxmi pur 10.90 6.80 1.60 0.00 19.30 11. Feni 1.60 6.70 0.70 0.00 9.00 12. Chand pur 1.50 0.00 0.00 0.00 1.50 Country total 287.37 426.43 79.75 39.90 833.45
  • 6. Figure : The coastal area soil in Bangladesh
  • 7.  The soils which contain sufficient water-soluble salts in the root zone affect or impair plant growth in general, may be termed as saline soil.  According to Biswas and Mukherjee (1987), saline soils are soils containing excess of nutral soluble salts dominated by chlorides and sulfates that affect plant growth. Definition of saline soil
  • 8. Formation of Saline Soil According to Boyer (1970) the most important sources of salts in the formation of saline soils are •Intrusion of sea water •Marine sediments •Saline ground water •Saline irrigation water •Poor drainage •Seepage from canals, and •Arid climate
  • 9.  In areas of low rainfall, salts formed during the weathering of soil minerals are not fully leached.  The salinity sources in Bangladesh are quite different from the other saline areas of arid and semi arid regions of the world. Here, the main cause of salinity is marine origin. Sea water salinity surrounding the coastal areas of Bangladesh is induced by 1) salt water intrusion during cyclone or typhoon, 2) direct inundation by saline or brackish water,
  • 10. 3) heavy withdrawal of water upstream by neighboring country, which results saline water movement along the main rivers and tributaries, 4) upward or lateral movement of saline ground water during the dry season and 5) withdrawal of ground water in the northwest for irrigation which encourages saline water movement in the aquifers, and since fresh water is costly and rare, farmers have tendency to irrigate land with saline water flowing through rivers.
  • 11.  Patchy stand and stunted growth are the most obvious features observed in plants due to salinity. No yield enhancement at any salinity level.  Sodium chloride and sodium sulphate salinities suppressed the growth of peanut. High concentration of both NaCl and Na2SO4 greatly reduced the shoot growth, biomass and dry weight of all plant parts. Shoot length was also reduced at all concentrations of both salts
  • 12.  Salt tolerance of plants is associated with salt exclusion, which is the ability of plants to restrict the uptake and/or transport of salt between roots & shoots. Evidence has shown that shoot growth of Etrog citron and Kharna khatta was reduced significantly by 50mm NaCl, but growth of Ranpur lime plants showed a marked reduction only at 100ml NaCl  Salinity treatment with 48 mM NaCl in solution culture reduced dry matter production by 65% in shoots and 43% in roots of sunflower plants.
  • 13.  The aim of reclamation is to remove salinity from the root zone within permissible limits, so as to restore the productivity of salt-affected soil.  Before starting the reclamation of saline soil knowledge of the following is essential. 1. Quality of irrigation water. 2. Nature and distribution of salt in the coastal zone. 3. Level of sub-soil water. 4. Drainage condition.
  • 14. Reclamation of Saline Soil Eradication or removal of the salts -Leaching -Irrigation management -Drainage management -Beneficial use of multiple water resources Conversion of some of the salts to less injurious forms -By using gypsum -By using elemental sulfur and sulfuric acid Designated control -Mulching -Crop choice -Pre-plant irrigation
  • 15.  The most common method used to the free soil of excess salts is installation of drainage systems and leaching or flushing.  A combination of two, flooding after field drainage ditches have been installed, is the most through and satisfactory.  The salts that dissolve are leached from the solum and drained away. Eradication or Removal of the Salts
  • 16.  Application of excess water, above evapotranspiration requirements to leach salts from the root zone of soils may effectively control salinity.  The most common method by which salt is removed is by leaching it out of the root zone with water.  An equation for this is DiCi – DdCd = 0  Di (the volume of water per unit area of land is expressed by its depth),  Ci , initial salt concentration,  Dd, the volume of water drained out of the soil,  Cd the salt concentration which drained out by water. Leaching Salinity Control during Irrigation
  • 17.  While it is difficult to forecast accurately the tolerance of crops, the comparative data presented in the following table may be helpful.  Table : Relative tolerance of certain plants to salty soils: Tolerant Moderately tolerant Moderately sensitive Sensitive Barley, grain Bermuda grass Bougainvillea Cotton Date Barley, forage Beet, garden Broccoli Brome grass Clover, berseem Alfalfa Broad bean Cauliflower Cabbage Clover Apple Apricot Bean Blackberry Carrot celery
  • 18. Source: Cited by Nyle C. Brady (1990) in “The Nature and Properties of Soil” as modified from Carter (1981). Tolerant Moderately tolerant Moderately sensitive Sensitive Natal plum Mutall alkali grass Rescue grass Rosemary Sugar beet Salt grass Wheat grass Wild rye Wheat grass, tall Fig Orchard grass Oats Rye, hay Sorghum Sudan grass Wheat What grass, western Trefoil, birds foot Corn Cowpea Cucumber Lettuce Pea Peanut Rice, paddy Soya-bean Sweet clover, timothy Grape fruit Lemon Onion Orange Peach Pineapple, Guava Potato Rose Strawberry, Tomato
  • 19.  Bangladesh is a vast delta having 14.2 million ha, of which roughly coastal brackish waters cover 17%.  At present only 5% of the coastal brackish water region is under coastal aquaculture mainly for shrimp farming.  Gradually shrimp production is increasing through horizontal expansion of the farming area.  So that, coastal aquaculture would develop as a good source of animal protein for the growing population.  A foreign currency earner and as well as maintainer of ecological balances in the brackish-water region.  Correct planning, regulation and motivation are needed to develop an environment friendly coastal aquaculture program to avoid ecological disasters in a land scarce and densely populated like Bangladesh.
  • 20.  Development of coastal area soils for agricultural purposes is of great importance for a small country like Bangladesh.  The reclamation of saline soils and practicing cultivation of salinity resistant crop varieties should be emphasized.  Another potentiality of our coastal soils is the shrimp production and export of which can earn substantial foreign currency.  So, the soils’ potentialities should be explored as well as managed for agricultural sustainability of future Bangladesh.