[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] NOC of Groundwater withdrawal from CGWA or State Groundwater Authority is mandatory for all Industries and Infrastructure projects. CGWA has made a panel of Accredited Consultants who understand the
[vc_row][vc_column][vc_column_text] Detailed Guidelines for Abstraction of Saline Ground Water Water having above EC above 5000 µ siemens/cm at 250C is Saline Water. Any user desirous of utilizing saline groundwater is
[vc_row][vc_column][vc_column_text] Guidelines for Ground Water abstraction for bulk water supply As per the new guidelines, all those users abstracting ground water and using it for supply as bulk water supplies
[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
