Geomorphic Engineering

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    Devashis Chatterjee

    Geomorphic EngineeringIssues For Research,

    And Some Awkward Questions

    Devashis Chatterjee

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    Devashis Chatterjee

    Water as resource

    Water for human use comes from rivers,ponds, wells

    All ultimately derived from rain

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    Devashis Chatterjee The Water Cycle

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    Devashis Chatterjee

    Four questions

    Renewable?

    Sharing silt? Affect area

    Geomorphology involved?

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    Devashis Chatterjee

    Renewable

    Renewable or perennial?

    Boundary conditions of replenishment

    Thresholds of behaviour

    Decision

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    Rivers ofIndia

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    Artificial

    lake

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    Devashis Chatterjee lake

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    Devashis Chatterjee

    ?

    Discharge changes

    Slope stays

    Braiding/ meandering switch

    Vulnerable to shift

    Who is affected?

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    Patterns

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    Braided

    Spiti

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    Devashis Chatterjee Braid to meander

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    equilibrium

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    Devashis Chatterjee Ganga bankline

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    Threshold

    Discharge

    vs

    slope

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    Colorado

    water

    sediment

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    River changes

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    Channel reduction

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    Above

    dam

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    Degradation below dams

    Yellow R

    Sanmexia

    4.0m/66km

    4yrs

    South SaskatchewanDiefenbaker

    2.4 m/8 km

    12 yrs

    ColoradoHoover

    7.1 m/111 km

    14 yrs

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    Devashis Chatterjee

    alluviation

    Flood plains are built by alluviation

    This happens during floods

    In tamer rivers of Europe and NAmerica floods at 80% bank height in50 years

    In monsoon Himalayan rivers?

    Indus estimate 10 m. silt in 5000 yrs.

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    Response

    time

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    Devashis Chatterjee Delta dynamics

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    Devashis Chatterjee Brahmaputra

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    Nile Delta

    Accretion stopped after Delta Barrage1868

    Western side of Rosetta promontoryretreated 6 km 1900-1991

    Before Aswan rate of retreat 20m/yr

    By 1991 rate was 240m/yr

    From 1984-2001 120 m/yr

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    IGCP 475

    Conceptual model for the behaviour of low-latitude, high-load Monsoon Asia Pacificrivers and deltas (compared to better-studied'type' systems from North America andEurope)

    Better constraints on sediments fluxes toAsian margins and the world ocean Capacity-building and scientific advancement fordeveloping nations of the region Identifyfuture threats and possible mitigation ofgeohazards in deltaic setting

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    delta

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    Impact Analysis

    Concerned with biota

    Effects of process modification would

    cascade

    Area affected is defined by river basin,notmeasurable in kilometres

    Cost/Benefit is asymmetric

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    Research ideas

    Lessons of experience

    Monitoring of geomorphic change

    Network of information

    Application of new tools of observation

    analysis

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    Information

    Not available in the public domain

    Restrictions on topographic data

    Red tape on river, climate and otherthematic data

    No window

    Bigger budget, more hurry

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    Geomorphologists

    Whether from geology or geographyapproach

    Have these as low priority

    Role of academics

    Role of professional agencies

    Still talking only to each other