river watershed floodplain

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    RIVER Nur Aisyah Putri Yella Apriliana

    sadiyah

    Dwi RahayuSetyawati Rani Fitriani Karina Noveandra Hilma Muthiah Windi Novita Rizky

    Erisa MarettaSilaban

    Alifa Istiyani

    Nurul Annisa Zikri Danar Aji Rizki Tri

    Elis Listiani

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    Type And Characteristics

    River

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    Based on the source of the river water canbe divided into three kinds

    Rainy River Glacier River Mixed River

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    Based on the water discharge according tothe river is divided into three kinds

    Permanent River Periodic River Episodic River

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    Based on the origin of events (genetics)the river is divided into 5 types

    Consequent River Subsequent or strike the river valley Obsekuen River Resekuen River

    Insekuen River

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    Based on the geological structure of theriver is divided into two kinds

    Antecedents River Superposed River

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    Based on the flow pattern of theriver is divided into 6 types

    Radial or menjari Dendritic Trellis Rectangular

    Pinate Annular

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    Watershed

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    Definition

    A watershed, also called a "drainagebasin" in North America, is an area in

    which all water flowing into it goes to acommon outlet, such as the same estuary

    or reservoir.

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    The water in a watershed originatesvia precipitation that is collected on the

    surface and groundwater.The area of watershed can be determined

    with measure that area in topography

    map. The area of watershed is reallyinfluence to river discharge.

    http://geography.about.com/od/physicalgeography/a/hydrologiccycle.htmhttp://geography.about.com/od/physicalgeography/a/hydrologiccycle.htm
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    Types of Watersheds

    Gemuk Watershed

    Kurus Watershed

    http://3.bp.blogspot.com/-ZS1yu8Q-7xQ/T9Q-QDjFQoI/AAAAAAAAAEw/Uvq2Uda-J5s/s1600/Untitled-7.gifhttp://3.bp.blogspot.com/-xXzB3eg-w-s/T9Q94yUU9cI/AAAAAAAAAEo/-rT176Bte8Q/s1600/Untitled-6Z.gif
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    Component of watershed

    Physical Condition Human

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    Human Impacts on Watersheds

    Polution Reduce the amount of water flowing to

    it

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    Preventing of damaged watershed

    Do not deforesting / plants in thewatershed areas

    Do not building in the area of thewatershed as a residential or otherpurposes.

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    Watershed Management andRestoration

    Watershed management is the organization andplanning of human activities on a watershed andrecognizes the links between these activities and

    the watershed's health.Watershed restoration on the other hand is

    aimed at restoring already impacted watershedsto their natural state through the monitoring of

    pollution and regulations to reduce further

    pollution.

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    FLOODPLAIN

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    Definition

    Floodplain is the area around the river which hasa surface elevation of land under flood water

    level in the 50 year return period.Condition of the land in the region is generally

    fertile flood plains and store a variety of potential

    and accessibility, so as to have a high power ofdance to be cultivated and shelter, business

    center and other economic activities.

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    Flood and sedimentation

    Generally floodplainsediment is dominatedby sediments such as

    silt and mudsuspension, although

    sometimes appears finesandstones deposited

    by strong currents

    during the flood peak.

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    Point bar deposits

    The precipitate which occurred at the peakof the curve called a point bar.

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    Here are some of the functions ofthe river for human life, including:

    Sources of Drinking Water and Water Supply As an Electrical As Transport Line As The Fresh water Fish Farming, Shrimp, and

    Crab As aplace of recreation and tourism As the Sports Turf

    As Exploration Place Science and Research

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    Measuring Flow Velocity andDischarge

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    The discharge measurementQ=AV

    Which,Discharge (Q)

    Area (A)Mean flow velocity (V).

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    Flow velocity is measuredwith a current meter .

    A plot of flow velocity versus depth offlow is called the velocity

    profile. Velocity varies with depth in anon-line armanner so the averagevelocity for the subsection is not atmid-

    depth (0.5d) but rather at 0.6 d fromthe water surface

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    So if you want to determine theaverage velocity at a vertical, a single

    measurement can be taken at 3/5 ofthe depth from the water surface