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Overview of Study Area in Bangladesh
            in context of
    Regional and Local Settings
                  M. Shahjahan Mondal
                   Associate Professor
        Institute of Water & Flood Management
   Bangladesh University of Engineering & Technology
      Email: mshahjahanmondal@iwfm.buet.ac.bd

                    Workshop on
      Water Security in Peri-Urban South Asia:
     Adapting to Climate Change & Urbanization
                 16-19 August 2010
                 Kathmandu, Nepal
GBM Basins
• Bangladesh is the lower
  riparian of the GBM
  basins
• 91% flows
• Ganges contribution is
  37%
• SW part of Bangladesh is
  totally dependent on the
  Ganges water
• Gorai
SW Bangladesh
• Sundarbans – largest
  continuous mangrove
  ecosystem & a
  ramsar world heritage
  site
• Mongla Port – second
  sea port
• Khulna – third largest
  city
• Khulna has a strong
  industrial base
Existing Problems
• 28% of the population live in the coastal area
• Water logging
• Coastal Embankment Project (CEP) was implemented
  in the 1960s
• A series of polders were constructed to control the
  intrusion of saline water
• The intervention simplified the drainage network from a
  very large number of tidal creeks & rivers to a small
  number of large rivers.
• This reduced the tidal volume and increased the tidal
  range.
Existing Problems
• The occurrence of cyclone,
  storm surge and flood
• The 1991 cyclone left 150
  thousand people dead
• Salinity in both SW & GW
• Arsenic
• Reduction in fresh water inflow
  due to u/s withdrawal & siltation
• Land use change due to shrimp
  farming
• Vulnerable to tsunami & SLR
Existing Problems
• Coastal zone is low lying with 62% of the land below 3
  m & 86% below 5 m above msl.
• Due to 88 cm SLR, 11% more coastal area will be
  inundated
• 5 ppt saline front will penetrate 40 km inland
• The whole of Sundarbans will be lost
• Increased salt water intrusion is considered as one of
  the causes of top dying of Sundari trees
• Salinity level recorded near Khulna in 2007 was the
  highest in the past 32 years
Khulna City
• 3rd largest city
• Located on the right bank
  of the Bhairab-Rupsha,
  one of the most important
  distributaries of the
  Ganges in the Southwest
  Coastal Region of
  Bangladesh
• Area: 46 km2
• Population: > 1.5 million;
  growth rate 5%
History
• Declared as Pourashava in 1884
• Until partition of India in 1947, Khulna was a sleepy little
  district town, overshadowed by the huge metropolis of
  Kolkata.
• After partition, Khulna began to seek its own identity. It
  had a sudden influx of population, which necessitated
  the development of a satellite town at Khalishpur under
  Daulatpur thana, which was about 8 km from the zero
  point at the Circuit House Maidan.
• By 1960, the intervening space had filled out and it
  became a divisional headquarter.
• The central location and proximity to Sundarban and
  seaport prompted the government to develop the jute
  industry in and around Khulna after the partition in 1947.
• During late 1950s & 1960s, it became an important
  center for industrial development
History (con…)
• Newsprint mills, shipyard, jute mills, match factories,
  hardboard mills were established
• Khulna was given a metropolitan status in 1984 when
  its population exceeded one million.
• But since the 1980's, the decreasing popularity of jute
  and jute goods in the international market, in spite of
  its value as a biodegradable packaging material, put a
  brake on further expansion of the jute industry.
• But at present there are signs of a revival through new
  products and processes, as well as environmental
  compulsions.
• The city is regaining impetus for growth, following the
  export processing activities centering on shrimp
  cultivation
• Academic & training institutions
Strategic Importance of Khulna
• The location of Khulna in the heart of the SW coastal
  region has given it many advantages.
• The linkages of the city with regional towns and growth
  centres have made it the most important city in the
  region
• provides links to the Mongla sea port, which is only 40
  km d/s
• is a major river port of the country for inland water
  transport
• Sundarban attracts tourist from home and abroad
• has a strong industrial base after Dhaka and Chittagong
• This has come into focus specially after the completion
  of Lalon Shah Bridge and Khanjahan Ali Bridge which
  will facilitate Nepal and seven sister states of India to
  use Mongla port facilities if agreement can be made at
  the govt level
Khulna City Corporation
• in 1990 with 5 thanas &
  31 wards
• one-fourth is city core
• Densely populated;
  contains multi-storied
  buildings
• The rest is a mixture of
  urban & peri-urban areas
• There are several low-
  income areas and slums
  throughout the city
Urban Drainage Problem


    Drainage system in KCC
 is towards the Mayur River
  Drainage system is
 open
  Total length : 652 km
  Paved drain: 291 km
  Semi-paved : 56 km
  Earthen drain: 305 km
Geological & Hydrological Setting
• Topographically, the city slopes towards west
  but regionally towards south.
• The average height is 3.3 m above msl
• The city lies on the Ganges deltaic plain in
  north and Ganges tidal plain in south and
  consists of late Holocene to recent Alluvium
• Lithologically, the area is composed of coarse
  to very fine sand, silt and silty clay up to a
  depth of 300 m with peaty soil and calcareous
  as well as non-calcareous soil at the top
Urban Geomorphology of Khulna City
                                     LAND FORMS AND INFERRED SEDIMENTARY ENVIRONMENT AND
                                                            EVENTS.

                                     NL, FB, ML and AC form peatlands in some parts of the inactive
                                     area of the Ganges delta and coastal plain.

                                     Flood plain, channels and peat lands within the Ganges delta in
                                     progradational phase with intermittent deposition of fine silt of
                                     transgrassive sea.
                                     Shallow marine shelf, estuarine and tidal flat under transgressive
                                     sea




                                     Deposits of rivers flowing in the Ganges delta during Late
                                     Pleistocene to Holocene epoch. The lower is erosive and
                                     unconformable.




                                     Tidal creeks, tidal channel and estuarine plain deposition in the
                                     coastal area in the Bengal Basin during early Quaternary epoch,
                                     which may be equivalent to upper part of the Dupi Tila
                                     Formation. The lower contact is sharp to gradational
                                     Deposition of sand in large channels in the KCC area of the
                                     southern part of the present inactive Ganges delta which may be
                                     equivalent to the Lower Dupi Tila Formation and or Upper part of
                                     the Tipam Formation.       The lower contact is erosive and
                                     unconformable.
                                     Marshy area and small channels in flood plain.

Note: NL= Natural Levee, FB= Flood Basin, ML= Marshy Land and AC = Abandoned Channel
Contemporary Water Management Issues in Khulna
                    City

•   Drinking water crisis
•   Lowering of GWT
•   Poor drainage
•   Water logging
•   Water quality
•   Solid waste management
•   Climate change vulnerability
•   Urban planning
•   Dying of Mayur River
Drinking Water Crisis

• Present water supply is mainly from groundwater
  sources drawn from both DTW & STW
• Water supply is 13 MG per day
• The coverage is only 30% of households with piped
  water supply
• The rest is self-managed and many of the people face
  water crisis
• To cope with this insufficient supply and increasing
  demand, KWASA was established in March 2008
Lowering of GWT

During the dry season, 50% of DTWs become
inoperative.
Poor Drainage System

• Drainage system is not good
   – Improper slope, inadequate sections & inadequate outlets
   – Lack of maintenance
   – Disposal of wastes into drains
   – Encroachments & settlements on drainage paths
   – River and water pollution
   – Corruption
   – No study
   – Water insecurity in urban & peri-urban areas
• There were natural drains, but widths were reduced
• KWASA is responsible
• KWASA needs to return back to the original drains
Water Logging due to Poor Drainage System

In Khulna city, 38% of households regularly experience
short-duration logging.

In some areas, more than 90% people are affected by water
logging.
Groundwater Quality

• The aquifer system is hydraulically connected to the
  Bay of the Bengal & the surrounding rivers.
• 85, 35 & 50% of the wells had Na+, K+ & Cl-
  concentrations exceeding the WHO limit.
• Excess in Na+ and Cl- concentration is due to the
  seawater intrusion which forces the abandonment of
  water wells in many instances.
• High TDS values in about half of the borewells may
  be attributed to hydraulic connection with the river.
Groundwater Quality of KCC area
                                           Bangladesh
                    Parameters   Average
                                            standard
                pH                 7.87       6-8.5
                EC (µs/cm)       1405.83
                TDS (ppm)        1011.17     1000
    Cations




                Na+              209.42      200
                K+                 5.58       12
                Ca+              102.50       75
                Mg2+              28.00     30-35
                Cl-              292.08    150-600*
                CO32-             44.33
    Anions




                HCO3-            631.92
                H4SiO42-          51.17
                PO43-              0.56        6
                SO42-             20.92       400
Source: Shahinujjaman, 2004
Surface Water Quality
                Seasonal variation of the Bhairab Water Quality
   SL No.                         Pre                    Post
                Parameter                  Monsoon
                              Monsoon                 Monsoon
       1       pH                 6.8         7.69        6.9
       2       Temp (C)          31.6         28.9       22.3
       4       CO2               0.15         0.15        0.2
       5       DO (ppm)           7.8          6.9       6.92
       6       TDS (mg)         10380       195000       6520
       7       HCO3-              180         135        142
       8       H4SiO4              5           2.5       2.82
       9       Na+               2300        2150        1750
      10       K+                 78           72         61
      11       Ca+                96           15         84
      12       Mg2+               150         140        145
      13       Cl-               4653        4330        4510
      14       SO42               700         658        682
      15       NO3-                3           2.8        2.9
      16       PO43-               2          0.08       1.09
Khanom, 2009
Solid Waste Management

• Solid waste generation in Khulna City is 450 tons a day.
• KCC is responsible (33%)
• NGOs, CBOs & private organizations are also involved
  (17%)
• Half is collected & reaches the final disposal site which is
  about 8 km from the city
• The uncollected waste is often dumped in an
  uncontrolled manner throughout the city clogging drains,
  blocking roads & occupying vacant plots
• This causes flooding, increases traffic congestion &
  presents health risk
Climate Change Vulnerability

• International Institute for Development and Environment
  on "Climate Change and the Urban Poor: Risk and
  resilience in 15 of the world's most vulnerable cities"
• It identified Khulna as one of the most vulnerable cities
• The report says that the major concerns for Khulna are
  frequent and increased level of floods, storm surges,
  intensity of cyclones, water logging, saline intrusion,
  sedimentation and river erosion.
• Climate refuges in Khulna after Sidr and Aila
Urban Planning

• KDA was created as a semi-autonomous body in 1961
• under the Ministry of Housing and Public Works
• Planned development and expansion of Khulna City and
  its suburb areas
• A new and revised master plan comprising of 451 km2
  was prepared and approved by the govt in 2001
• A further expansion of the master plan extending upto
  the Mongla port is underway
• Unlike Dhaka, Khulna is the city, which is still virgin and
  can be made a planned city
Mayur River
• Derelict river
• It flows to the NW side of the
  Khulna city
• It separates Dumuria thana
  from the city
• 9.5 km long; falls into the
  Rupsha River near Badamtala,
  Batiaghata
• Subsistence uses
• Few hundred fisher families
• There was abundance of fish
  until 1983
Mayur River
• It receives all types of
  municipal & industrial
  wastes
• 18 canals & drains to
  drain out effluents
• Slums around this river
• Dumping (domestic &
  urban sewage, industrial
  effluents, agricultural
  wastes) at various sites of
  the river
Other Water Related Issues of KCC

  Tropical cyclone and storm surge

  Inundation of freshwater sources during
cyclonic event and storm surge

  Increased salinity in rivers and aquifers –
power plant was closed due to salinity

  Shortage of freshwater for agriculture
Other Water Related Issues of KCC

  Pollution of rivers and ponds from untreated
urban and industrial effluents

  Hanging latrines on ponds and river canals

  Unplanned urban settlements on the river banks
Peri-Urban Areas in & around KCC

                           Peri-urban areas

                           Urban areas
Peri-Urban area:
               Identification & issues
• KWASA coverage is one-
  third of the area
• DTWs were not sunk in a
  planned way
• KWASA is not permitting
  DTW installation
• No DTW in Ward No. 1, 2
  & 3 of Daulatpur; STW is
  not safe
• No water infrastructure in
  Phultala, Batiaghata,
  Rupsha & Dighalia
• Self managed STW/DTW
• No NGO is working in
  WSS in peri-urban area
Peri-Urban area
• Khals are water logged, leased out
• Some are polluted
• Siltation & encroachment
Peri-Urban area
• KCC planned to lift 9 MG
  of GW from Phultala area
  with 40 DTWs
• The project came to a
  halt in 2007 in the face of
  people's agitation
• Madhumati water with
  treatment
• Poddo Beel as a reservoir
  – farmers’ agitation
• Mayur as reservoir –
  NGO
Visited area
• Rupsha F. Ghat
Visited area
•   Md. Nagar
•   Agricultural until 2000
•   Not many people
•   Rainfed agriculture
•   Land value
    – Tk. 3-10 thousand
    – Tk. 150-400 thousand
• 1 DTW per 10-100 h/h
• No drainage congestion
Visited area
• 10-vent regulator at
  Tetultala
• To prevent salt water
  intrusion
• No coordination between
  BWDB & local people
• Gate operation &
  management
Visited area
•   KWASA is looking for alternative source of water
•   Natural drainage is towards the Mayur River
•   Siltation, pollution & encroachment
•   Subsistence uses & use as a reservoir
•   ETP – cost, regulation!!!
•   Capacity is adequate!!!

• BWDB, LGED, KCC, KDA, KWASA, DPHE,
  Fisheries, DC

• Software!!!
Visited area
• Sea level rise could delay discharge from the
  drainage system in low-lying areas
• Flooding by contaminated wastewater could cause
  serious health risks
• Changes in salinity regime from sea level rise may
  affect the availability of fresh surface and
  groundwater

• Still in the process of selecting the exact field site!!!
Thank you
• At every section of an estuary, salinity varies with the
  state of tide and also with the up land flow. Bangladesh
  has a monsoonic climate. The upland river flow has a
  distinct seasonal pattern. The upland flow increases from
  June to reach the peak in August/September and
  decreases from October. With this variation of fresh
  water flow salinity varies inversely. Salinity front of a
  particular concentration starts moving upstreams from
  October and starts moving towards sea during June.
• The Ocean water has salinity of 35 parts per thousand
  whereas in the Bay of Bengal close to Bangladesh coast
  it is 30–32 parts per thousand. This is due to discharge
  of sweet water by the three big rivers.
• Rajbond Trenching Ground Site: It is at
  present the only official dumping site, 25
  acres in area situated at a distance of
  about 10 kms to the west of KCC
  Headquarter
Problem of Solid Waste Management

On-payment door to door collection of household
garbage covers about 17% households by local NGOs.

33% of the households throw waste into nearby drains,
on low lands, or elsewhere.

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Bangladesh Research Site_ Dr. M Shahjahan Mondal

  • 1. Overview of Study Area in Bangladesh in context of Regional and Local Settings M. Shahjahan Mondal Associate Professor Institute of Water & Flood Management Bangladesh University of Engineering & Technology Email: mshahjahanmondal@iwfm.buet.ac.bd Workshop on Water Security in Peri-Urban South Asia: Adapting to Climate Change & Urbanization 16-19 August 2010 Kathmandu, Nepal
  • 2.
  • 3. GBM Basins • Bangladesh is the lower riparian of the GBM basins • 91% flows • Ganges contribution is 37% • SW part of Bangladesh is totally dependent on the Ganges water • Gorai
  • 4. SW Bangladesh • Sundarbans – largest continuous mangrove ecosystem & a ramsar world heritage site • Mongla Port – second sea port • Khulna – third largest city • Khulna has a strong industrial base
  • 5.
  • 6. Existing Problems • 28% of the population live in the coastal area • Water logging • Coastal Embankment Project (CEP) was implemented in the 1960s • A series of polders were constructed to control the intrusion of saline water • The intervention simplified the drainage network from a very large number of tidal creeks & rivers to a small number of large rivers. • This reduced the tidal volume and increased the tidal range.
  • 7. Existing Problems • The occurrence of cyclone, storm surge and flood • The 1991 cyclone left 150 thousand people dead • Salinity in both SW & GW • Arsenic • Reduction in fresh water inflow due to u/s withdrawal & siltation • Land use change due to shrimp farming • Vulnerable to tsunami & SLR
  • 8. Existing Problems • Coastal zone is low lying with 62% of the land below 3 m & 86% below 5 m above msl. • Due to 88 cm SLR, 11% more coastal area will be inundated • 5 ppt saline front will penetrate 40 km inland • The whole of Sundarbans will be lost • Increased salt water intrusion is considered as one of the causes of top dying of Sundari trees • Salinity level recorded near Khulna in 2007 was the highest in the past 32 years
  • 9. Khulna City • 3rd largest city • Located on the right bank of the Bhairab-Rupsha, one of the most important distributaries of the Ganges in the Southwest Coastal Region of Bangladesh • Area: 46 km2 • Population: > 1.5 million; growth rate 5%
  • 10. History • Declared as Pourashava in 1884 • Until partition of India in 1947, Khulna was a sleepy little district town, overshadowed by the huge metropolis of Kolkata. • After partition, Khulna began to seek its own identity. It had a sudden influx of population, which necessitated the development of a satellite town at Khalishpur under Daulatpur thana, which was about 8 km from the zero point at the Circuit House Maidan. • By 1960, the intervening space had filled out and it became a divisional headquarter. • The central location and proximity to Sundarban and seaport prompted the government to develop the jute industry in and around Khulna after the partition in 1947. • During late 1950s & 1960s, it became an important center for industrial development
  • 11. History (con…) • Newsprint mills, shipyard, jute mills, match factories, hardboard mills were established • Khulna was given a metropolitan status in 1984 when its population exceeded one million. • But since the 1980's, the decreasing popularity of jute and jute goods in the international market, in spite of its value as a biodegradable packaging material, put a brake on further expansion of the jute industry. • But at present there are signs of a revival through new products and processes, as well as environmental compulsions. • The city is regaining impetus for growth, following the export processing activities centering on shrimp cultivation • Academic & training institutions
  • 12.
  • 13. Strategic Importance of Khulna • The location of Khulna in the heart of the SW coastal region has given it many advantages. • The linkages of the city with regional towns and growth centres have made it the most important city in the region • provides links to the Mongla sea port, which is only 40 km d/s • is a major river port of the country for inland water transport • Sundarban attracts tourist from home and abroad • has a strong industrial base after Dhaka and Chittagong • This has come into focus specially after the completion of Lalon Shah Bridge and Khanjahan Ali Bridge which will facilitate Nepal and seven sister states of India to use Mongla port facilities if agreement can be made at the govt level
  • 14. Khulna City Corporation • in 1990 with 5 thanas & 31 wards • one-fourth is city core • Densely populated; contains multi-storied buildings • The rest is a mixture of urban & peri-urban areas • There are several low- income areas and slums throughout the city
  • 15.
  • 16.
  • 17. Urban Drainage Problem Drainage system in KCC is towards the Mayur River Drainage system is open Total length : 652 km Paved drain: 291 km Semi-paved : 56 km Earthen drain: 305 km
  • 18. Geological & Hydrological Setting • Topographically, the city slopes towards west but regionally towards south. • The average height is 3.3 m above msl • The city lies on the Ganges deltaic plain in north and Ganges tidal plain in south and consists of late Holocene to recent Alluvium • Lithologically, the area is composed of coarse to very fine sand, silt and silty clay up to a depth of 300 m with peaty soil and calcareous as well as non-calcareous soil at the top
  • 19.
  • 20.
  • 21. Urban Geomorphology of Khulna City LAND FORMS AND INFERRED SEDIMENTARY ENVIRONMENT AND EVENTS. NL, FB, ML and AC form peatlands in some parts of the inactive area of the Ganges delta and coastal plain. Flood plain, channels and peat lands within the Ganges delta in progradational phase with intermittent deposition of fine silt of transgrassive sea. Shallow marine shelf, estuarine and tidal flat under transgressive sea Deposits of rivers flowing in the Ganges delta during Late Pleistocene to Holocene epoch. The lower is erosive and unconformable. Tidal creeks, tidal channel and estuarine plain deposition in the coastal area in the Bengal Basin during early Quaternary epoch, which may be equivalent to upper part of the Dupi Tila Formation. The lower contact is sharp to gradational Deposition of sand in large channels in the KCC area of the southern part of the present inactive Ganges delta which may be equivalent to the Lower Dupi Tila Formation and or Upper part of the Tipam Formation. The lower contact is erosive and unconformable. Marshy area and small channels in flood plain. Note: NL= Natural Levee, FB= Flood Basin, ML= Marshy Land and AC = Abandoned Channel
  • 22. Contemporary Water Management Issues in Khulna City • Drinking water crisis • Lowering of GWT • Poor drainage • Water logging • Water quality • Solid waste management • Climate change vulnerability • Urban planning • Dying of Mayur River
  • 23. Drinking Water Crisis • Present water supply is mainly from groundwater sources drawn from both DTW & STW • Water supply is 13 MG per day • The coverage is only 30% of households with piped water supply • The rest is self-managed and many of the people face water crisis • To cope with this insufficient supply and increasing demand, KWASA was established in March 2008
  • 24. Lowering of GWT During the dry season, 50% of DTWs become inoperative.
  • 25. Poor Drainage System • Drainage system is not good – Improper slope, inadequate sections & inadequate outlets – Lack of maintenance – Disposal of wastes into drains – Encroachments & settlements on drainage paths – River and water pollution – Corruption – No study – Water insecurity in urban & peri-urban areas • There were natural drains, but widths were reduced • KWASA is responsible • KWASA needs to return back to the original drains
  • 26. Water Logging due to Poor Drainage System In Khulna city, 38% of households regularly experience short-duration logging. In some areas, more than 90% people are affected by water logging.
  • 27. Groundwater Quality • The aquifer system is hydraulically connected to the Bay of the Bengal & the surrounding rivers. • 85, 35 & 50% of the wells had Na+, K+ & Cl- concentrations exceeding the WHO limit. • Excess in Na+ and Cl- concentration is due to the seawater intrusion which forces the abandonment of water wells in many instances. • High TDS values in about half of the borewells may be attributed to hydraulic connection with the river.
  • 28. Groundwater Quality of KCC area Bangladesh Parameters Average standard pH 7.87 6-8.5 EC (µs/cm) 1405.83 TDS (ppm) 1011.17 1000 Cations Na+ 209.42 200 K+ 5.58 12 Ca+ 102.50 75 Mg2+ 28.00 30-35 Cl- 292.08 150-600* CO32- 44.33 Anions HCO3- 631.92 H4SiO42- 51.17 PO43- 0.56 6 SO42- 20.92 400 Source: Shahinujjaman, 2004
  • 29. Surface Water Quality Seasonal variation of the Bhairab Water Quality SL No. Pre Post Parameter Monsoon Monsoon Monsoon 1 pH 6.8 7.69 6.9 2 Temp (C) 31.6 28.9 22.3 4 CO2 0.15 0.15 0.2 5 DO (ppm) 7.8 6.9 6.92 6 TDS (mg) 10380 195000 6520 7 HCO3- 180 135 142 8 H4SiO4 5 2.5 2.82 9 Na+ 2300 2150 1750 10 K+ 78 72 61 11 Ca+ 96 15 84 12 Mg2+ 150 140 145 13 Cl- 4653 4330 4510 14 SO42 700 658 682 15 NO3- 3 2.8 2.9 16 PO43- 2 0.08 1.09 Khanom, 2009
  • 30. Solid Waste Management • Solid waste generation in Khulna City is 450 tons a day. • KCC is responsible (33%) • NGOs, CBOs & private organizations are also involved (17%) • Half is collected & reaches the final disposal site which is about 8 km from the city • The uncollected waste is often dumped in an uncontrolled manner throughout the city clogging drains, blocking roads & occupying vacant plots • This causes flooding, increases traffic congestion & presents health risk
  • 31. Climate Change Vulnerability • International Institute for Development and Environment on "Climate Change and the Urban Poor: Risk and resilience in 15 of the world's most vulnerable cities" • It identified Khulna as one of the most vulnerable cities • The report says that the major concerns for Khulna are frequent and increased level of floods, storm surges, intensity of cyclones, water logging, saline intrusion, sedimentation and river erosion. • Climate refuges in Khulna after Sidr and Aila
  • 32. Urban Planning • KDA was created as a semi-autonomous body in 1961 • under the Ministry of Housing and Public Works • Planned development and expansion of Khulna City and its suburb areas • A new and revised master plan comprising of 451 km2 was prepared and approved by the govt in 2001 • A further expansion of the master plan extending upto the Mongla port is underway • Unlike Dhaka, Khulna is the city, which is still virgin and can be made a planned city
  • 33. Mayur River • Derelict river • It flows to the NW side of the Khulna city • It separates Dumuria thana from the city • 9.5 km long; falls into the Rupsha River near Badamtala, Batiaghata • Subsistence uses • Few hundred fisher families • There was abundance of fish until 1983
  • 34. Mayur River • It receives all types of municipal & industrial wastes • 18 canals & drains to drain out effluents • Slums around this river • Dumping (domestic & urban sewage, industrial effluents, agricultural wastes) at various sites of the river
  • 35. Other Water Related Issues of KCC Tropical cyclone and storm surge Inundation of freshwater sources during cyclonic event and storm surge Increased salinity in rivers and aquifers – power plant was closed due to salinity Shortage of freshwater for agriculture
  • 36. Other Water Related Issues of KCC Pollution of rivers and ponds from untreated urban and industrial effluents Hanging latrines on ponds and river canals Unplanned urban settlements on the river banks
  • 37. Peri-Urban Areas in & around KCC Peri-urban areas Urban areas
  • 38. Peri-Urban area: Identification & issues • KWASA coverage is one- third of the area • DTWs were not sunk in a planned way • KWASA is not permitting DTW installation • No DTW in Ward No. 1, 2 & 3 of Daulatpur; STW is not safe • No water infrastructure in Phultala, Batiaghata, Rupsha & Dighalia • Self managed STW/DTW • No NGO is working in WSS in peri-urban area
  • 39. Peri-Urban area • Khals are water logged, leased out • Some are polluted • Siltation & encroachment
  • 40. Peri-Urban area • KCC planned to lift 9 MG of GW from Phultala area with 40 DTWs • The project came to a halt in 2007 in the face of people's agitation • Madhumati water with treatment • Poddo Beel as a reservoir – farmers’ agitation • Mayur as reservoir – NGO
  • 42. Visited area • Md. Nagar • Agricultural until 2000 • Not many people • Rainfed agriculture • Land value – Tk. 3-10 thousand – Tk. 150-400 thousand • 1 DTW per 10-100 h/h • No drainage congestion
  • 43. Visited area • 10-vent regulator at Tetultala • To prevent salt water intrusion • No coordination between BWDB & local people • Gate operation & management
  • 44. Visited area • KWASA is looking for alternative source of water • Natural drainage is towards the Mayur River • Siltation, pollution & encroachment • Subsistence uses & use as a reservoir • ETP – cost, regulation!!! • Capacity is adequate!!! • BWDB, LGED, KCC, KDA, KWASA, DPHE, Fisheries, DC • Software!!!
  • 45. Visited area • Sea level rise could delay discharge from the drainage system in low-lying areas • Flooding by contaminated wastewater could cause serious health risks • Changes in salinity regime from sea level rise may affect the availability of fresh surface and groundwater • Still in the process of selecting the exact field site!!!
  • 47. • At every section of an estuary, salinity varies with the state of tide and also with the up land flow. Bangladesh has a monsoonic climate. The upland river flow has a distinct seasonal pattern. The upland flow increases from June to reach the peak in August/September and decreases from October. With this variation of fresh water flow salinity varies inversely. Salinity front of a particular concentration starts moving upstreams from October and starts moving towards sea during June. • The Ocean water has salinity of 35 parts per thousand whereas in the Bay of Bengal close to Bangladesh coast it is 30–32 parts per thousand. This is due to discharge of sweet water by the three big rivers.
  • 48. • Rajbond Trenching Ground Site: It is at present the only official dumping site, 25 acres in area situated at a distance of about 10 kms to the west of KCC Headquarter
  • 49. Problem of Solid Waste Management On-payment door to door collection of household garbage covers about 17% households by local NGOs. 33% of the households throw waste into nearby drains, on low lands, or elsewhere.