Hydrogeology in Strategic Water Conservation
Published: Aug 15, 2018
.jpg )
Photo: Prasad
Reports from India’s mountainous regions find that springs are drying up. Conservation strategies need to factor in the occurence of groundwater in these regions, particularly in the Himalaya; Tunganath, Uttarakhand.
Abstract: Conventional approaches to conservation of groundwater have not considered the need to involve an understanding of aquifer measurement and hydrogeology. Considering India’s diverse geography, it is pertinent to develop a scientific understanding of underlying geology of groundwater resources and how aquifers work.
TO READ THE FULL ARTICLE
Already have an account? Log In
Keep reading with one of these options :
OR
MORE ARTICLES
Hope or Hurdle? NEP 2020 and the Education of the Marginalized
The National Education Policy (NEP) 2020 aims to transform India's education system with a focus on inclusivity and access. However, for marginalized communities, the effectiveness of these reforms re...
Vanishing Grants: The Fate of Higher Education in India
The foundational principle upon which our education systems rest is fundamentally based on the democratic values of: secularism, federalism, liberty, and equality. The New Education Policy (NEP), 2020...
NEP and Rising Salaries
The National Education Policy (NEP) 2020 has been hailed as a transformative framework for Indian education, introducing sweeping reforms aimed at structural change and improving access, quality, and...
Hazy Ridge Boundaries: In Conversation with Chetan Agarwal on Encroachments, Forest Governance, and Conservation Policies.
The Delhi Ridge, an extension of the Aravalli Hills, is the last remaining natural forest in the capital and a crucial ecological barrier that shields the Indo-Gangetic Plains from desertification. It...
Term Power
What is ...
Non-revenue water is the water that has been produced but is lost before it reaches the customer. It is one of the biggest problems as it increases the water stress.
An aquifer is an underground layer of permeable rock, sediment, or soil that yields water. The aquifers near the surface are usually used for water supply and irrigation.
Drip irrigation is a micro-irrigation system where water drips slowly into the roots of the plants from pipes buried below the surface.
Groundwater recharge is a hydrologic process where water moves downwards from surface water to groundwater. Groundwater recharge occurs through wetlands, rainfall and more.
A floodplain is a strip of relatively flat and normally dry land alongside a stream, river, or lake that is covered by water during a flood. Floodplains are produced by lateral movement of a stream and by overbank deposition.
Hardness of water is the quality indication of salts in water. Water hardness can cause costly industrial problems, such as breakdowns in boilers and cooling towers, and may even cause irreplaceable corrosion. The temporary hardness of water can be removed by boiling, while permanent hardness removal require a water softener or an ion exchange column.
A settling pond is an open lagoon into which wastewater contaminated with solid pollutants is placed and allowed to stand. The basins are used to control water pollution in industries such as agriculture,aquaculture, and mining.