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Ground Water

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Groundwater is the water located beneath the earth's surface in soil pore spaces and in the fractures of rock formations. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from, and eventually flows to, the surface naturally; natural discharge often occurs at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology. Typically, groundwater is thought of as liquid water flowing through shallow aquifers, but, in the technical sense, it can also include soil moisture, permafrost (frozen soil), immobile water in very low permeability bedrock, and deep geothermal or oil formation water. Groundwater is hypothesized to provide lubrication that can possibly influence the movement of faults. It is likely that much of the Earth's subsurface contains some water, which may be mixed with other fluids in some instances. Groundwater may not be confined only to the Earth.

Study of hydrographs indicates depletion in many places over the years: Poor rainfall, shrinking lakes, depleting water levels in reservoirs and drawing of excess water through borewells have had an impact on the groundwater levels in different areas of the city. A study of hydrographs indicates that over the years, water table has depleted in many places like Bowenpally, Aghapura, Erragadda, Basheerbagh, Langer Houz, Jubilee Hills, Begumpet, Koti, West Marredpally, Gudimalkapur, Musheerabad, Sanathnagar, Madhapur, said Dr. P.D. Sridevi, Principal Investigator of National Geophysical Research Institute (NGRI). Addressing a workshop on ‘Groundwater in Hyderabad: Issues of Access and Regulation’, she said that the groundwater being exploited through borewells from depths ranging up to 300 metres so much so that in the pre-monsoon, water level was plummeting between five metres to 20 metres Below Ground Level (BGL). There was slight improvement post-monsoon with the BGL being two to 15 metres. Hyderabad and its surrounding areas like Shamshabad, Shamirpet, Medchal and Keesara were under the ‘Over Exploited’ category as per the A.P. Groundwater Department’s 2010 report, she informed.

Related National symposium and workshops are
• National Workshop on Groundwater Governance and Regulation • NGWA Workshop — Groundwater Quality and Unconventional Gas Development • 3.Climate Change and Groundwater: Comparative and International Law and Policy Dimensions • IGWA CEC Workshop • 5 IGWA CEC Workshop • 6 IGWA CEC Workshop • 7 IGWA CEC Workshop
• 2014 Pennsylvania Groundwater Symposium • 2015 Pennsylvania Groundwater Symposium • The 3rd Remote Sensing and Hydrology Symposium (RSHS14) • British Hydrological Society Symposium 2014 • 2015 NGWA Groundwater Summit • International Conference of Hydrometeorological Risks and Climate Change • Emerging Contaminants Symposium
Relevant Conferences:
• AWRA’s 2014 GIS and Water Resources VIII – Data to Decisions Conference • Groundwater Issues and Water Management Conference • Course Groundwater in the Coastal zone • 2014 Spring Runoff Conference • Groundwater Management in India: Issues and Challenges • 42nd IAH International Congress AQUA2015 • American Water Works Association (AWWA) Conference • 9th Conference on Sustainable Development of Energy, Water and Environment Systems • Groundwater Issues and Water Management –Strategies Addressing Challenges of Sustainability and Drought in California

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This page was last updated on 07th Oct, 2014

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