[C2] Chapter 2: River and Coast


Characteristics of Sections in Rivers

Upper

Middle

Lower

River mouth

Altitude

High

Medium

Low

Very low

Gradient

Steep

Medium

Gentle

Very gentle

Water amount

Small

Medium

Large

/

Roughness

Very rough

Rough

Smooth

/

Shape

Narrow → v-shaped

Wider → v-shaped

Very wide

/

Overall energy

Little

Medium

High

Very little


Erosion

Types of Erosion

Headward

Strength slope of bank of river source → overhanging rocks fall down → lengthen river channel / river valley → river source extend backward

Vertical

River removes rock from its bed in upper course → deepen river channel / river valley

Lateral

River removes rock along the bank in middle + lower courses → widen river channel / river valley

Factors Affecting Rate of Erosion

Load

- Higher load → more erosion

- Heavier / angular load → higher potential for erosion

River energy

- Steep gradient → higher velocity / more water → higher energy → more erosive power

Water quality

Acidic water → more corrosion

Rock

More cracks / soluble materials → more erosion

Deforestation

Less vegetation cover → higher overland flow → more rocks / stones washed into river

Urbanization

- More surfaces covered with cement → less infiltration → more river discharge → higher energy

- Slope cutting → steeper slope gradient → higher overland flow → more channel water → higher energy

Industralization

Sewage pollute river water → more corrosion


Transportation

Types of Transportation

Suspension

Fine / light materials carried along → does not touch river bed

Traction

Large / heavy boulders / rocks → rolled → dragged along river bed

Saltation

Small stones / pebbles → bounce along river bed

Solution

Soluble materials → dissolved → carried downstream

Factors Affecting Rate of Transportation

Load

Larger size → higher energy → more transportation

River energy

Higher energy → larger amount of heavier load → more transportation

Erosion

Higher rate of erosion → more eroded materials

Rock Resistance

Higher resistance → more eroded / weathered materials

Climate

Hot / wet climate → more weathered materials

Gradient

Steep → more surface runoff // more soil erosion

Vegetation

Less vegetation → bare surface → more soil erosion

Lakes

Fewer lakes → sediments cannot be trapped


Deposition

Factors Affecting Rate of Transportation

Water amount

Less water // more water leaves basin // high evaporation rate → less deposition

Velocity

River flows into a large body of water // high channel friction // high amount of load // gentle channel gradient → lower water flow speed → less deposition

Sorting of Sediments

Top layer

Lightest / finest load → last to deposit

Bottom layer

Heaviest load → first to deposit


Factors Affecting Fluvial Processes and Downstream

Upper Course

Energy

Small amount of channel water // rough channel bed or banks // large or angular rock fragments → higher channel friction → lower water flow speed → less discharge → lower river energy

Erosion

- High elevation → high potential energy

- Vertical erosion being dominant → lateral erosion // headward erosion at river source

Transportation

Less energy for transportation // less discharge → insufficient energy to remove large rock fragments

Deposition

- Insufficient energy → deposition

- Sudden decrease in river energy → deposition

- Less discharge after rainstorms → river cannot transport large fragments → deposit on river bed

Middle Course

Energy

More channel water // smoother channel bed // smaller and rounder rock fragments → more discharge → greater river energy

Erosion

Steeper channel gradient → more lateral erosion than vertical erosion

Transportation

- Larger load → transported by traction / saltation

Deposition

- After flooding → river deposits sediments on valley floor

- Decrease in energy → deposition

Lower Course

Energy

- Large amount of channel water → more discharge

- Smoother channel bed and banks // fine and rounded rock debris → smaller channel friction → higher water flow speed → greater river energy

Erosion

Outer bank → lateral erosion → less vertical erosion

Transportation

Mainly transported by suspension

Deposition

Occurs in river mouth // inner banks // river bed during dry season // on valley floor during flooding


Landforms

Upper Course

V-shaped valleys

Upper course → active vertical erosion → river valley becomes deeper → v-shaped valleys

Interlocking spurs

Little energy in upper course → river cannot go through obstacles → forced to zigzag from side to side around obstacles → vertical erosion → less river channel → distinct spurs

Rapids

/

Waterfall

/

Gorges

River flows over more resistant rocks and less resistant rocks → erode the less resistant rocks

→ small = rapids

→ large = waterfall

→ continued undercutting of less resistant rocks → overhanging resistant rocks lose support → collapse → waterfall retreat → gorges

Middle Course

Meanders

- Outer bank → erosion → higher water velocity → lateral erosion → undercut outer bank

- Inner bank → deposition → higher water velocity → deposited load → slip-off slope

→ meander

Lower Course

Oxbow lakes

Meanders → lateral erosion → meander bends → grow closer → flood → river cuts through bends to join → new channel → oxbow lakes = abandoned channel sealed by deposition

Floodplains

/

Levees

Flood water carry load in river → form valley floor → repeated flooding / deposition → build up floodplain →

flood water overflow from channel → lower water flow speed → larger and heavier load deposited close to river bank → levees (ridge-line)

Braided streams

- Dry season → lower water level → deposition → more river bed becomes low ridges

- Wet season → river water returns to previous levels → river flow blocked by ridges → braided streams = river forced to split into several separated channels → flow around ridges

River Mouth

Deltas

/

Lagoons

River enters the sea → lower speed of flow → river deposits its load layer upon layer → gently sloping platform of sediment builds up → extends into sea → delta →

sediments block river channel → river split into small channels → lagoons


Human Activities

Conservation of Reservoirs and Catchwaters

- Catchwaters → divert water from streams to reservoirs

- Examples: Upper Shing Mun Reservoir / Tam Lam Chun Reservoir

Positive Impact

Negative Impact

More freshwater for consumption / farming at lower course

- Less channel water amount at lower course

- Dry season → more cutoff → pollutants difficult to disperse → more water pollution → degrade fish habitats

- Less salt amount and nutrients → degrade farmlands

Farming and Fisheries

Some wetlands on floodplains are reclaimed → become ponds / farmlands

Positive Impact

Negative Impact

- More farming / freshwater fisheries

- Attract more migratory birds → fish bonds become feeding ground

- Higher risk of flooding: wetlands originally absorb water → conversion of wetland into fish bonds / farmland → less floodwater will be absorbed

Development of New Towns / Infrastructure

New towns need more land → large-scale reclamation at river mouth / floodplains → low-lying areas of river valleys become roads / railway networks

Positive Impact

Negative Impact

- Provided land for development

- Old urban areas have less over-concentration of population

- Higher risk of flooding → natural land surface become impermeable → more overland flow → higher amount of channel water

- Destroy natural habitats


Strategies Against Flooding

Hard Strategies

Channelization

Positive

- Deepen and widen river channel → higher water-holding capacity

- Straightening river channel → higher river velocity

- Cover with concrete → less bed / bank erosion → less deposition / friction

Negative

- Expensive to build

- Concrete lining destroys river habitats

- Less natural river banks

Dredging

Positive

- Deepen river channel → higher water-holding capacity

- Less channel roughness → higher river velocity

Negative

- Suitable for small section of river only → costly and time consuming for large-scale implementation

- Needs to carry out maintenance periodically

- Stirs up sediments → disturb aquatic lives

- Not effective against large-scale flooding

Dykes

/

Embankments

Positive

- Larger height of river banks → higher water-holding capacity

- More recreational space → cycling / walking trails

Negative

- Expensive to build

- Dykes collapse → flooding occurs

- Look unnatural

Bypass floodway

Positive

Catch runoff → divert water → less threat of flooding in populated areas

Negative

- Expensive to build

- Large area of land is needed → suitable area is not always available

- Damage original natural habitats

- More chance of flooding in areas in the floodway

Village flood pumping scheme

Positive

- Embankments surround village → less flood water flows into villages

- Stormwater drainage system → store stormwater runoff → increase time lag → more time to regulate discharge → less risk of flooding

Negative

- Expensive to build and maintenance

- Requires a large area of land

Soft Strategies

Land use planning

Positive

- Less casualties and property losses

- Store flood water

- Less worsening drainage during heavy rainstorms

Negative

- Difficult to restrict development

- Difficult to enforce: complex land ownership

Afforestation

Positive

- More interception → less overland flow

- Less soil erosion → less supply of load / silting

- Creates natural habitats

- More recreational grounds

Negative

- Requires a lot of time to grow trees

- Trees cannot intercept all rainwater → cannot prevent serious flooding

- Requires a lot of space

- High money cost for management and afforestation

Flood warning systems

Positive

- Give flood warnings → more time to evacuate / take precautionary measures

- Raise people's awareness of flooding

- Less casualties / property loss

Negative

- Cannot prevent flooding

- Some people without communication devices cannot receive flood warning in time


Waves

Types of Waves

Constructive waves

Destructive waves

Properties

Swash > backwash

Backwash > swash

Formation

- Calm weather condition → weak wind

Strong winds / storms

Energy

Dispersed / weak

Concentrated / strong

Work

Wave deposition (with shore materials)

Wave erosion (without shore materials)

Wave form

- Lower wave height

- Longer wavelength

- Lower wave frequency

- Higher wave height

- Shorter wave length

- Higher wave frequency

Beach shape

Wide / flat

Narrow / steep

Factors Affecting Wave Characteristics

Constructive Wave

Destructive Wave

Wind speed

Lower → lower energy

Higher → higher energy

Fetch

Shorter → obstructed by island

Longer → facing open sea

Wind duration

Shorter

Longer → prevailing wind

Offshore gradient

Gentler: widely-spaced submarine contour lines

Steeper: closely-spaced submarine contour lines

Location

Sheltered → at bays

Exposed → at headland

Seabed roughness

Rougher: mangrove

Smoother

Rock resistance

More

Less

Coastal process

Deposition

Erosion


Coastal Landforms

Constructive Waves

Beaches

Building up of sand in sheltered areas

Spits / Bars / Lagoons / Tombolos

Long and narrow deposits of sediments attached to land → extend out into sea → spits formed by longshore drift →

Ridges of sediments parallel to the coast → extension of spits → completely blocked off a bay / river mouth → bars //

Spits build up → join on island to mainland → 2 islands connected → 2 spits connected → tombolos

water trapped behind bars → lagoons

Destructive Waves

Notch

/

Sea cliffs

/

Wave-cut platforms

Wave erosion concentrated at area between high tide and low tide → land undercut to form notch →

undercutting continue → notch enlarged → overhanging parts collapse → steep rock face adjacent coast → sea cliff →

flat rock surface: wave-cut platform

 Sea cave / sea arches and stacks

Lines of weakness exposed to wave erosion → enlarged → form cracks → grow and develop into sea cave


Human Activities

Reclamation

More land for urban development and economic development

Positive Impact

Negative Impact

More land for development → increase quality of life

- Disturb marine ecosystem → bury marine habitats

- High cost

- Look unnatural and unattractive: straighter coastline

- Less safety of navigation: harbor → narrower // higher water velocity

- More water pollution: higher concentration of human activities → kill marine lives

Recreation

Beautiful coastal landscapes for development of recreation / tourism // more grounds for water sports

Positive Impact

Negative Impact

More place for people to relax

- Damage marine habitats: mangroves and coral reefs are removed

- Water and land pollution: more number of tourists and human activities along the coast


Strategies for Coastal Protection

Hard Strategies

Sea walls

Positive

- Reflect and deflect waves → protect coast from wave erosion

- Strong and durable

- Effective and efficient to reflect and dissipate wave energy

- More recreational areas

- Protect coastal structures from coastal flooding

Negative

- Expensive to build and maintain

- Walls are not durable → waves may undercut the wall → collapse

- Look unnatural

Breakwaters

Positive

- Break incoming waves → less erosion power

- Effective and efficient to reflect wave energy

- Safe for ships to anchor

Negative

- Expensive to build and maintain

- Visually unattractive

- Easily destroyed in storms

- Water pollution

- Cannot limit erosion elsewhere: waves are only deflected

Rock armor / rip-rap

Positive

- Easy to build

- Cheap and easy to maintain

- Local boulders can blend with local geology

- More place for fishing

Negative

- Looks unnatural / ugly

- Limits access to beaches

- Requires maintenance

Gabions

Positive

- Absorb energy of waves

- Cheap and flexible

- Can blend with local geology

- Can blend with environment → vegetation can grow

Negative

- Not as effective as sea walls

- Look unnatural

- Cages are easily corroded → require regular maintenance

- Risk of injury

- Shorter life span

Soft Strategies

Beach nourishment

Positive

- Looks natural

- Slows down removal of beach materials

- More recreational ground → favor development of tourism and economy

- Cheap and easy to carry out with local sand

Negative

- Ineffective against strong waves

- Short term solution only: beach erosion is a continuous process

- Imported sand: higher cost  // harmful to local species // contains toxic materials