ENVIRONMENTAL LAW ppt on laws of environmental law
Sand Minning
1.
2. • Sand mining is a practice that is used to extract sand,
mainly through an open pit. However, sand is also mined
from beaches, inland dunes and dredged from ocean beds
and river beds. It is often used in manufacturing as an
abrasive, for example, and it is used to make concrete.
• Sand dredged from the mouths of rivers can also be used to
replace eroded coastline.
• Another reason for sand mining is the extraction of minerals
such as rutile, ilmenite and zircon, which contain the
industrially useful elements titanium and zirconium. These
minerals typically occur combined with ordinary sand.
• Short term benefits
3. • Direct impact on the stream’s physical habitat characteristics
Channel geometry
Bed elevation
Substrate composition and stability
Instream roughness elements
Depth
Velocity
Turbidity
Sediment transport
Stream discharge
Temperature
4. 1. Alteration of the flow patterns resulting from
modification of the river bed
2. An excess of suspended sediment
3. Damage to riparian vegetation and instream
habitat
7. • Kinds of instream sand mining
Dry-pit
Wet pit mining
Bar skimming or "scalping."
Pits on the adjacent floodplain or river terraces
• Types of instream habitats
a) Log structures
b) Log jams
c) Cover structures
d) Boulders structures etc.
8. a. Extraction of bed material in excess of natural replenishment by
upstream transport
o This causes bed degradation, increases suspended sediment,
sediment transport, water turbidity and sand/gravel siltation
o Becomes unsuitable for many aquatic organisms
o Gravel removal not only impacts for the extraction site
9.
10. b. Bed degradation, changes themorphology of thechannel
o Potential for diversion of flow through
o Migration blockages for fish during low flows
oIf the gravel extraction activity is conducted away from the active
river channel during low water periods
o As active channels naturally meander, the channel may migrate
into
11. c. Operation of heavy equipmentin thechannelbed
o Can directly destroy spawning habitat for fish and
macroinvertebrate habitat, and produce increased turbidity
and suspended sediment downstream.
Figure 2.2: Turbid water due to sand mining
12. d. Alteringchannel hydraulics
o Stockpiles and overburden in the floodplain can alter channel hydraulics
during high flows.
e. Removalor disturbanceof instreamroughnesselements
o It negatively affects both quality and quantity of instream habitat.
o Instream roughness elements - particularly large woody debris, play a
major role in providing structural integrity to the stream ecosystem.
13. • Many hectares of fertile streamside land are lost annually
• Degraded stream habitats result in lost of fisheries productivity,
biodiversity, and recreational potential.
• Severely degraded channels may reduce land and aesthetic values.
• All species require specific habitat conditions to ensure long-term
survival
• Unstable stream channels are inhospitable to most aquatic species
• The complete removal of vegetation and destruction of the soil
profile destroys
14. A.Destructionofthe riparianzone
It serves as buffer to pollutants entering a stream from runoff, controls
erosion, and provides habitat and nutrient input into the stream.
B. Loweredfloodplaingroundwater
o Riparian vegetation reliant on the groundwater will subsequently be
stressed
C. Permanentflooding
o Subsequently causes annual or frequent flooding into the disturbed site.
D. Destructionof riparianvegetation
o This is caused by heavy equipment, processing plants at or near the
extraction site
E.Disturbingthenaturalhydraulicsoftheriparianzone
o Generation of recruitment may be lost
F. Removaloflargewoodydebrisfromtheriparianzone
o It negatively affects the plant community.
G. Reducedvegetative bankcover
o Resulting in reduced shading and increased water temperatures.
15. Impacts for groundwater
Bed degradation from instream mining lowers the elevation of stream flow
Saline water may intrude into the fresh water body
Impacts for Water Quality
Increased riverbed and bank erosion
Increased short-term turbidity
Suspended solids can increase water treatment costs
17. • Bed degradation and consequent effects on channel and
bank stability
• Increased sediment loads, decreased water clarity
• Changes in channel morphology and disturbance of
ecologically important roughness elements in the river bed
• Ecological effects on bird nesting, fish migration etc.
• Modification of the riparian zone including bank erosion
• Direct destruction from heavy equipment operation
• Discharges from equipment and refueling
• Impacts on structures and access
• Biosecurity and pest risks
• Impacts on coastal processes
18. Figure 2.4 : Extensive Modification to Stream Channel Caused by sand mining
19. Acid Mine Drainage-Threat to water resources
Acid mine drainage also dissolves toxic metals
such as copper, aluminum, cadmium, arsenic,
lead and mercury from the surrounding rock
Yellow boy
The impacts to aquatic life may range from
immediate fish kills to sub lethal, impact affecting
growth, behavior or ability to reproduce
21. • 1. Sand mining sites should be situated outside the
active floodplain and excavation should not take place
from below the water table.
• 2. Larger rivers and streams should be used
preferentially than small rivers and streams.
• 3. Pit excavations located on adjacent floodplain or
terraces should be separated from the active channel.
• 4. The removal or disturbance of instream roughness
elements during gravel extraction activities should be
avoided.
• 5. Turbidity levels should be monitored
• 6. Operation and storage of heavy equipment within
riparian habitat should be restricted.
An instream flow is a water right for the stream and the resources that depend on it. It has a priority date like any other water right. Instream flows are the stream flow levels that will protect and preserve instream resources and values.
The term “instream flow” identifies a specific stream flow level (measured in cubic feet per second, cfs) at a specific location on a given stream. The weather causes natural flow variations throughout the year so an instream flow is a range (a “regime”), usually changing month-to-month, instead of a single number.
Instream flows do not affect existing (senior) water rights, rather, they protect the river from future withdrawals.
Setting instream flows does not put water in streams.
In state law, the terms “base flow” and “minimum instream flow” have the same meaning as “instream flow.”
A riparian zone or riparian area is the interface between land and a river or stream. Riparian is also the proper nomenclature for one of the fifteen terrestrial biomes of the earth. Plant habitats and communities along the river margins and banks are called riparian vegetation, characterized by hydrophilic plants.
The riparian zone includes stream banks, riparian vegetation and vegetative cover.
Destruction of the riparian zone during sand / gravel extraction operations can have multiple deleterious effects on instream habitat.
Damaging any one of these elements can cause stream bank destabilization, resulting in increased erosion, sediment and nutrient inputs, and reduced shading and bank cover leading to increased stream temperature.