Kerala’s Dwindling Freshwater Resources
Published: Jul 31, 2015
The Banasura Sagar Dam, impounds the Karamanathodu tributary of the Kabini River. Despite abundant rainfall and availability of reservoirs the freshwater availability in Kerala is less than that in neighbouring Tamil Nadu and Karnataka.
Abstract: Water related problems are acute in many parts of Kerala during summer. The situation could worsen further as rapid urbanisation, indiscriminate sand mining and salinity intrusion into groundwater reservoirs gradually transform the State’s environmental scenario for the worst.
TO READ THE FULL ARTICLE
Already have an account? Log In
Keep reading with one of these options :
OR
MORE ARTICLES
Maitri II - India's New Antarctic Research Station
India is set to embark on a new chapter in its Polar exploration journey with the construction of Maitri II. The Indian government plans to establish a new research station near the existing Maitri ba...
Innovation INC : Deep Ocean-weather Smart
The Deep Ocean Mission (DOM), approved by the Government of India in 2021 under the Ministry of Earth Sciences (MoES), represents a strategic step in realizing Sustainable Development Goal 14 (SDG 14:...
Rare Earth Elements (REE)-China’s Grip, India’s Strategy, and the Arctic Frontier
China recently announced restrictions on the export of seven rare earth elements (REEs), soon after US President Donald Trump decided to impose tariffs. As the world's dominant supplier—responsible fo...
India First to Secure Dual Deep-Sea Exploration Contracts as the Global Regulations Remain in Flux
The International Seabed Authority (ISA) marked a watershed moment on September 15, 2025, signing a 15-year contract with the Indian government, revolutionising deep-sea exploration. India has been gr...
Term Power
What is ...
It depicts the rate of flow (discharge) versus time elapsed at a specific point in a river, or other channel. These graphs are generally employed to understand the influence of climate such as seasonal rainfall, flood, drought and climate change on groundwater levels. In addition, hydrographs are also utilised to understand the response of aquifers to pumping and irrigation.
These are wells dug into aquifers under positive pressure. The water in artesian wells rises to a point where hydrostatic equilibrium has been reached naturally, without any artificial aid.
Bed flow is the sustained flow in a stream that comes from groundwater discharge or seepage.
Hydraulic conductivity refers to the permeability of water through a medium. It describes the ease with which water flows through the pores or fractures of an aquifer.
Recharge is the addition of water to an aquifer to replenish it. It may occur naturally through rain, runoff or through artificial measures like spreading basins and recharge wells/irrigation.
These processes are aimed to mitigate the effects of global warming. It involves a multitude of global climate modification programmes that function to tackle climate change by removing CO2 from the air.
Also called paleo-water, the term refers to ancient freshwater reservoirs created millions of years ago and trapped underground in deep aquifers.
Runoff is the water that flows over the surface of earth. The flowing water mostly is a result of storms, glacial melt, floods or other sources. Runoffs are crucial for aquifer recharge.
The term refers to the comparatively dry soil or rock located between the ground surface and the
top of the water table. The pores of the soil/rock of this zone contain both water and air.
These are sedimentary beds through which zero flow occurs because of lack of porosity. Aquicludes generally underlie or overlie an aquifer. In case of the latter, the pressure could metamorphose it into a confined aquifer.