[vc_row][vc_column][vc_column_text] Groundwater impact assessment (GWIA) is a tool that is used to assess the potential impacts of a proposed development on groundwater resources. GWIA looks at how proposed activities might
[vc_row][vc_column][vc_column_text]As per the new guidelines notified on 24.09.2020, all industries extracting/proposing to extract ground water in excess of 100 m3/day in Over-exploited, Critical and Semicritical areas shall have to mandatorily
[vc_row][vc_column][vc_column_text]RWH can be done in homes, apartments, societies, schools, institutions, commercial premises and any other space as long as there is a catchment area in the form of a roof
[vc_row][vc_column][vc_column_text]Rainwater harvesting techniques have already been devised and used since ancient times. These were implemented at the community level in areas where rainfall is the only major source of fresh
[vc_row][vc_column][vc_column_text]1. Safe area: Area categorized as SAFE from the groundwater resources point of view, based on the latest groundwater resources assessment carried out jointly by CGWB and State groundwater organizations. 2.
[vc_row][vc_column][vc_column_text]1. Brief about the proposed project giving location details, coordinates, google/ toposheet maps, etc. demarcating the project area. 2. Groundwater situation in and around the project area, including water level,
[vc_row][vc_column][vc_column_text]Piezometer is a borewell/tubewell used only for measuring the water level by lowering a tape/sounder or automatic/digital water level measuring equipment. It also takes a water sample for water quality
[vc_row][vc_column][vc_column_text]Water audit is a systematic process of objectively obtaining a water balance by measuring water flow from the site of water withdrawal or treatment, through the distribution system, and into
[vc_row][vc_column][vc_column_text] The occurrence and distribution of groundwater are controlled primarily by the geology of the area and the quantum of recharge received by the existing aquifer formations. Thus the alluvial
[vc_row][vc_column][vc_column_text] Water first enters an aquifer through gravity-induced downward movement (percolation), but it also flows in a lateral direction within an aquifer. This flow can occur due to the dip
