Tribal
Village |
People's
Participation |
Program Implementation consists of
three phases:
Selection of the Villages
Drilling operations Maharashtra State is covered by nearly 90% of Mesozoic and early Tertiary volcanic rocks, characterised by a thick sequence of lava flows. Aquifers are generally shallow, represented by weathered and fractured basalt located mainly in depressions, river sides, flat areas. Deeper aquifers may also occur. They are, in most cases, represented by inter- lava flow materials, exceptionally by granular rock types. Some prospects to find groundwater is also along fault lines and dykes. As most boreholes struck water within the first 100 feet, it was found more appropriate to drill, for the same village, two boreholes of 100 feet each rather than to insist on going deeper in a dry hole and reach 200 feet as is usually done by other organizations; such a depth may be justified only in areas where previous drillings have proved the existence of a deep aquifer. The average yield of boreholes drilled by the project in volcanic rocks of Maharashtra is in the order of 1500 litres per hour; in a few cases borehole yield reached 10,000 litres or more per hour. Drilling is carried out by a contractor using a down-the-hole hammer drilling. Casing is inserted only in the soft and weathered upper section of the rock sequence. The average rate of success has been around 90% . The high rate of success is due to: a very accurate borehole site survey; a constant supervision of the drilling operations and flow measurements; the use of slotted casing, whenever appropriate; and the installation of the bucket pump in a number of low-yielding boreholes. Hand Pump Installation Two types of pumps are installed by the program: the Mark II hand-pump and the bucket pump described ahead . The Mark II pump is installed in boreholes having good yield (generally not less than 300 litres per hour) and in villages with at least 100 people. The bucket pump is designed for villages with less than 100 people or for villages located in remote areas inaccessible during the wet season for the regular maintenance of hand- pumps. Hand-pumps are installed at depths established in accordance with the: well yield: the lower the yield, the deeper the pump is installed; the depth of water level; the depth of water entries; the number of users; and the form of the village (if houses are close to each other or sparsely located; in the first case water withdrawal is more intense in certain hours as women like to collect water in company of their neighbors, thus creating a fast water level drop in low-yielding wells). |
| Back to Table of Contents | ..........Home............. | Go to Next Section |