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Desalinisation :
Ocean Thermal Energy Conversion (OTEC) is a process that can produce electricity by using the temperature difference between deep cold ocean water and warm tropical surface waters.
Denaturation :
1) Primary structure: the linear structure of amino acids in the polypeptide chain
2) Secondary structure: hydrogen bonds between peptide group chains in an alpha helix or beta sheet
3) Tertiary structure: three-dimensional structure of alpha helixes and beta helixes folded
4) Quaternary structure: three-dimensional structure of multiple polypeptides and how they fit together.
Desalinisation :
- Process that extracts mineral components from saline water , the removal of salts and minerals from a target substance as in soil desalination, which is an issue for agriculture.
- Methods :
- Vacuum distillation or Thermal — boiling to leave impurities behind.
- LTTD Technique Low temparature thermal Distillation without membranes in Kavarati , minikoy by NIOT because of (easy , less expensive , many sources for energy availability )
- Reverse Osmosis RO at the Largest desalinisation plant in India at Minjur of Chennai , It needs Membrane for filtration which is costly because of high cost of electricity per se.
- multi-stage flash distillation :
- Multiple-effect distillation (MED) :
- Vapor-compression evaporation :
- Freeze thaw :
- Solar Evaporation :
- Electrodialysis reversal :
- Membrane distillation :
- Wave powered distillation :
- After distillation Calcium , Magnesium and other healthy minerals are added in purified water to make it pure drinking water.
- Concerns in RO process :
- High cost of electricity consumption
- Remaining by-products elements (include 40% waste saline water contains Brine ) are thrown in oceans which can cause pollution and can affect marine life.
- Hence discharge of Brine into oceans by keeping the marine life in mind.
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Ocean Thermal Energy Conversion (OTEC) is a process that can produce electricity by using the temperature difference between deep cold ocean water and warm tropical surface waters.
Denaturation :
- is a process in which proteins or nucleic acids lose the quaternary structure, tertiary structure & secondary structure which is present in their native state, by application of some external stress or compound such as a strong acid or base, a concentrated inorganic salt, an organic solvent (e.g., alcohol or chloroform), radiation or heat.
- Protein denaturation is also a consequence of cell death. Denatured proteins lose their 3D structure and therefore cannot function.
1) Primary structure: the linear structure of amino acids in the polypeptide chain
2) Secondary structure: hydrogen bonds between peptide group chains in an alpha helix or beta sheet
3) Tertiary structure: three-dimensional structure of alpha helixes and beta helixes folded
4) Quaternary structure: three-dimensional structure of multiple polypeptides and how they fit together.
Process of denaturation:
1) Functional protein showing a quaternary structure
2) When heat is applied it alters the intramolecular bonds of the protein
3) Unfolding of the polypeptides (amino acids)
Kelp Forest
WINDS across the World : map is here ----> Winds of World Region wise
Mistral : Southern Europe
Blizzard : Northern America
Sirrocco : (originates in North Africa) --> passes through Mediterenean Sea ---> blows in South Europe
Harmattan : Central Africa
The islands of Arabian Sea include Lakshadweep and Minicoy.
-> 9 Degree Channel divides Lakshadweep and Minicoy islands.
-> While, the goup of Lakshadweep islands is itself divided by 11 Degree Channel, as I told above. [Source: 11th NCERT 'India: Physical Environment' Chapter 2]
Coastline :
In India, Coastline are in order
Gujarat > Tamilnadu >Andhra
Coastal Regulation Zone :
Rill erosion occurs when runoff water forms small channels as it concentrates down a slope. These rills can be up to 0.3m deep. If they become any deeper than 0.3m they are referred to as gully erosion.
1) Functional protein showing a quaternary structure
2) When heat is applied it alters the intramolecular bonds of the protein
3) Unfolding of the polypeptides (amino acids)
Kelp Forest
WINDS across the World : map is here ----> Winds of World Region wise
Mistral : Southern Europe
Blizzard : Northern America
Sirrocco : (originates in North Africa) --> passes through Mediterenean Sea ---> blows in South Europe
Harmattan : Central Africa
The islands of Arabian Sea include Lakshadweep and Minicoy.
-> 9 Degree Channel divides Lakshadweep and Minicoy islands.
-> While, the goup of Lakshadweep islands is itself divided by 11 Degree Channel, as I told above. [Source: 11th NCERT 'India: Physical Environment' Chapter 2]
Coastline :
- Canada has the longest coastline in the world.
- Norway has the second longest coastline in the World, and the longest in Europe.
In India, Coastline are in order
Gujarat > Tamilnadu >Andhra
Coastal Regulation Zone :
- Under the Environment Protection Act, 1986 of India, notification was issued in February 1991, for regulation of activities in the coastal area by the Ministry of Environment and Forests (MoEF).
- As per the notification, the coastal land up to 500m from the High Tide Line (HTL) and a stage of 100m along banks of creeks, estuaries, backwater and rivers subject to tidal fluctuations, is called the Coastal Regulation Zone(CRZ).
- CRZ-1:
- are ecologically sensitive areas ,
- essential in maintaining the ecosystem of the coast ,
- lie between low and high tide line.
- Exploration of natural gas and extraction of salt are permitted.
- CRZ-2:
- The areas form up to the shoreline of the coast.
- Unauthorised structures are not allowed to construct in this zone.
- CRZ-3:
- rural and urban localities which fall outside the 1 and 2.
- Only certain activities related to agriculture even some public facilities are allowed in this zone
- CRZ-4:
- Lies in the aquatic area up to territorial limits.
- Fishing and allied activities are permitted in this zone.
- Solid waste should be let off in this zone.
- This zone covered coastal stretches in islands of Andaman & Nicobar and Lakshdweep
Rill erosion occurs when runoff water forms small channels as it concentrates down a slope. These rills can be up to 0.3m deep. If they become any deeper than 0.3m they are referred to as gully erosion.