Ijraset Journal For Research in Applied Science and Engineering Technology
Authors: Shruti Yerpude, Tushar Kodwate, Vijaya Banafar, Radha Deshkar, Rushikesh Chavan, Prof. Abhilasha Deshmukh
DOI Link: https://doi.org/10.22214/ijraset.2023.53673
Certificate: View Certificate
The technique of ground water recharge involves the process of enhancing the natural replenishment of groundwater by artificial means. This technique is often employed in areas where the groundwater level has depleted due to overexploitation or other factors such as climate change. Various methods are used to recharge groundwater, including surface water spreading, injection wells, recharge trenches, and recharge pits. These methods involve diverting water from streams, canals, or storm water drains to recharge areas. The water then percolates through the soil, replenishing the groundwater reservoir. In addition to artificial methods, natural processes such as infiltration, seepage, and percolation also contribute to groundwater recharge. However, the effectiveness of these natural processes is limited in areas with impermeable soil, low rainfall, or high evaporation rates. Groundwater recharge techniques have numerous benefits, including increasing water availability, improving water quality, reducing soil erosion, and enhancing vegetation growth. Recharge also helps in mitigating the effects of droughts and climate change by maintaining the water table level. Implementation of groundwater recharge techniques requires proper planning and monitoring to ensure the sustainability of the process. Factors such as the source of recharge water, the type of soil, and the depth of the water table need to be considered. In addition, appropriate technology and infrastructure must be in place to facilitate the recharge process. Overall, groundwater recharge techniques offer an effective and sustainable solution to the problem of depleting groundwater resources. By enhancing the natural replenishment process, these techniques provide a reliable source of water for various purposes, including domestic, industrial, and agricultural use.
I. INTRODUCTION
A. Overview
1) Systems For Harvesting Rainwater And Their Features
2) Introduction
Groundwater, as a vital source of freshwater, plays a crucial role in supporting human societies, agriculture, and ecosystems. However, unsustainable groundwater extraction practices and increasing water demands have led to widespread groundwater depletion and degradation of aquifers worldwide. Groundwater recharge, the process of replenishing groundwater through artificial or natural means, has emerged as a promising solution to restore groundwater levels and improve aquifer health. In this thesis, we review the current techniques of groundwater recharge, including both artificial and natural methods, and highlight their advantages, limitations, and challenges. We also discuss the socio-economic, environmental, and hydrogeological factors that influence the selection and implementation of groundwater recharge techniques. Finally, we identify the research gaps and future directions for sustainable groundwater recharge practices.
Importance of groundwater as a freshwater source.
3) Defination
Groundwater recharge can be defined as water added to the aquifer through the unsaturated zone after infiltration and percolation following any storm rainfall event.
B. Problem Statement
Due to unsustainable groundwater extraction methods and rising water demands, groundwater depletion and degradation have emerged as major global issues.
Aquifers are thus experiencing dropping water levels, decreased storage capacity, and diminishing water quality. Significant socioeconomic and environmental repercussions result from these problems, including decreased freshwater availability for human societies, agriculture, and ecosystems, higher energy costs for pumping groundwater from deeper depths, land subsidence, and ecological effects on ecosystems that depend on groundwater.
Groundwater recharge has been identified as a potential remedy to address these problems, restoring groundwater levels and enhancing aquifer health. But there are a number of issues with groundwater recharge methods that must be resolved, such as:
Technical difficulties: Groundwater recharge procedures, whether man-made or natural, are complicated and call for technical hydrogeological competence.
???????C. Objectives
II. LITERATURE SURVEY & REVIEW
A. Review of Literature
Rapid industrial development, urbanization and increase in agricultural production have led to increased groundwater withdrawals, resulting in freshwater shortages in many parts of the world. In view of this, greater emphasis is needed on the studies focusing on the sources and impact of groundwater recharge. The present study was taken up with the objective of assessing the groundwater recharge and its impact on the groundwater quality of Roorkee town, with a special consideration of the portion of the Upper Ganga Canal (UGC) passing through the town area.
2. Amartya Kumar Bhattacharya (2010)
Artificial groundwater recharge is a process by which the groundwater reservoir is augmented at a rate exceeding the augmentation rate under natural conditions of replenishment.
In some parts of India, due to over-exploitation of groundwater, decline in groundwater levels resulting in shortage of supply of water, and intrusion of saline water in coastal areas have been observed. In such areas, there is need for artificial recharge of groundwater by augmenting the natural infiltration of precipitation or surface-water into underground formations by methods such as water spreading, recharge through pits, shafts, wells et cetera.
3. Rakh Usha M (2020)
Artificial recharge of groundwater is accomplished through placing surface water in basins, furrows, ditches, or different centers wherein it infiltrates into the soil and actions downward to recharge aquifers. synthetic recharge is an increasing
Number of used for short- or lengthy-term underground garage, where it has several blessings over floor storage, and in water reuse. artificial recharge requires permeable surface soils. in which these are not available, trenches or shafts in the unsaturated sector can be used, or water can be at once injected into aquifers via wells.
To design a machine for artificial recharge of groundwater, infiltration rates of the soil have to be determined and the unsaturated area among land floor and the aquifer ought to be checked for good enough permeability and lack of polluted regions.
4. Ahsen Maqsoom (2020)
Globally the researchers are identifying the new ways for better urban sustainability. One major issue in the current world is the lack of fresh water availability in cities due to rapid increase in the population. To meet water requirement, scientist are exploring different ways to enhance the groundwater recharge capacity. One such solution is the use of building information modelling (BIM) technology to identify multiple structures that can be constructed to provide the potential recharge. This research aims to develop multiple structures which can provide ground water recharge capability.
5. Lonkar Swapnil Suni (2019)
At the rate in which Indian population is increasing, it is said that India will surely replace China from most densely populated country in the world after 2020-2030. These will lead to high rate of consumption of most valuable resource ‘water’. In order to conserve and meet our daily demands of water requirements, we need to think for alternative cost effective and relatively easier method of conversing water. During monsoons lots of water goes waste into gutters, drains.
6. Roohul Khan (2016)
Estimates of groundwater recharge constitute fundamental input for most approaches used to evaluate and manage groundwater resources. Most approaches for quantifying groundwater recharge measure recharge directly or indirectly over a limited area (point or small-basin scale) and for short periods of time. Estimation of recharge, by any method is normally subject to large uncertainties and errors. In this paper, various methods of estimating ground water recharge are outlined and critically reviewed with regard to their limitations.
B. Patent Search
III. WORKDONE
A. Methodology
A law determining the rate of flow through soils was established in 1865 by the French scientist Mr. H. Darcy on the basis of experimental data. He claimed that this discharge was inversely proportional to the length of the soil sample (L) and directly related to head loss (H) and the area of the soil's cross-section (A). Q is therefore equal to runoff (m3/s). Head loss (m) = H
L is the soil sample's length in metres.
A = Area of the soil's cross-section (m2)
Here, H/L stands for the head loss or hydraulic gradient (I), and K is the permeability co-efficient. hence, finally
IJERTV8IS090021 (This work is licenced under a Creative Commons Attribution Licence) International Journal of Engineering Research & Technology (IJERT) http://www.ijert.org ISSN: 2278-0181
2. Calculation of Rainwater Collection
The total volume of the water rainwater available from any rooftop survey is a product of total rainfall and the surface area of collection. Runoff coefficient is usually applied to account for infiltration, evaporation and other losses and it varies from 0.8 to0.95. in order to estimate the average annual monsoon rainfall data for location needed to be used and using table 1 of IS 15797:2008 (Roof Top Rainwater Harvesting-Guidelines.)
Station |
Temperature (in C)
|
Relative Humidity (%) |
Rainfall (in mm)
|
Rainfall (in cm)
|
|||||||||
Nagpur |
Maximum |
Departure
|
Minimum
|
Departur
|
At 8:30 Hrs |
Departure |
Last 24 Hrs
|
Since 1/10/22 |
Departure |
Annual Total
|
Annual Normal
|
|
|
29 |
-2 |
11 |
-4 |
67 |
2 |
0 |
146 |
73 |
165.25 |
115 |
|
||
Table No. 1 Rainwater Collection
Source- Regional Meteorological center mumbai
E. Percolation Test
This test is used to figure out how well the soil can absorb water. The design of the septic system depends on the results of this test. In order to comprehend how soil behaves when there is moisture present, this test is also performed while purchasing land. As per test is another name for this test. For the precise computation of line length, pit depth, etc., each contour may have a different set of rules. The percolation test, however, follows the same technique. According to IS2470-part-2, this test is conducted in India.
The percolation rate is the amount of time in minutes needed for water to fall 25 mm into the test hole, according to IS2470 part 2. To allow generating results, a test in trial pits should be conducted in more than one location in the area.
F. Percolation Test Procedure
The permeability of the soil at the depth where the effluent needs to be disposed of is assessed using a percolation test.
A circular or square hole that is boarded to the necessary depth for the planned absorption test has a diameter of 100 to 300mm. To eliminate any smeared soil surface and create a natural soil interface into which water may percolate, the bottom of the hole is carefully scratched. To prevent the bottom of the hole from scouring, all loose debris is removed, and course or fine sand with a 50mm thickness is added.Then, water is poured over gravel to a minimum depth of 30holes 6 to 10 inches in diameter with vertical sides should be dug or bored. Intensity of the projected absorption trenches' approximate depth, usually 24 inches below the surface, must be reached by the holes. Place a plug in the hole if it is greater than 6 to 8 inches. Put a 4-inch-diameter perforated pipe piece into the hole, and then add drain rock to fill the area between the pipe and the hole's walls. It is advised that the reviewing authority receive a sketch or photo of the hole. Scratch or roughen the sides and bottoms of the holes to create smooth, natural surfaces. Take out any extra material. Fill holes with about 2 inches of washed gravel of a 3/4-inch thickness to prevent scouring caused by water.0mm. The wettest time of year will be used to conduct this test.
IV. RESULT AND DISCUSSION
The use of artificial recharge at GHRIET campus (site consider for this case study) can raise the groundwater table and make more groundwater available. It is crucial for reducing surface runoff, increasing water availability for campus use and industrial use, improving drainage, reviving springs, and improving the quality of groundwater, among other things. Additionally, it is thought to lessen the effects of changing rainfall patterns caused by various meteorological conditions. Meeting the demand for spatial water productivity and availability at a regional and global level is also crucial.
V. ACKNOWLEDGEMENT
We are extremely thankful to our guide Prof. Abhilasha Deshmukh under whom our project took the shape of reality from mere idea. We are thankful to our guide for enlightening us with his/her precious guidance and constant encouragement. We thank our guide for providing us with ample support and valuable time. We are indebted to our guide who constantly provided a stimulus to reach our goals.
We are grateful to Dr. Mahesh Raut, HOD, Civil Engineering, GHRIET, for kind co-operation and timely help.
We express our gratitude towards Dr. Swati Dixit, Dean Academics, GHRIET, for his never-ending support, planning and motivation.
We are blessed to have Dr. Vivek Kapur, our beloved Director Sir as our mentor who is an immense source of motivation and encouragement.
Lastly, we would like to thank all those who were directly or indirectly related to our project and extended their support to make the project successful.
In order to manage and maintain water resources, groundwater recharge technique design is quite important. Groundwater recharge techniques are efficient tools for recharging depleted aquifers and sustaining a sustainable water supply, it can be determined after examining various techniques and strategies. The following are some important findings about how groundwater recharge strategies are designed: 1) Site-specific design: The hydrogeological characteristics of each site should be taken into consideration while designing groundwater recharge strategies. To guarantee maximum efficacy, factors such soil type, aquifer characteristics, land use, and rainfall patterns should be carefully studied. 2) Multiple methods: To increase the recharge potential, a variety of recharge methods should be used in conjunction. Techniques like recharge wells, recharge trenches, infiltration basins, and percolation ponds can be used, depending on the site\'s features. 3) Maintenance: It\'s critical to regularly check on recharge sites to gauge their effectiveness and spot any modifications that may be required. To guarantee optimal performance, maintenance procedures such as desilting, vegetation control, and periodic cleaning should be carried out. 4) Integration with land use planning: To maximise their efficiency, groundwater recharge techniques should be combined with land use planning. For long-term success, it is essential to locate suitable recharge regions, take runoff patterns into account, and control possible pollution sources. 5) Participation of local stakeholders and communities in the planning and execution process generates a sense of ownership and guarantees long-term sustainability. Communities must be informed about the value of groundwater recharge, and prudent water use must be encouraged. 6) Scalability and adaptability: The plan should be scalable and able to adjust to changing hydrological conditions, such as shifting patterns of rainfall or rising water demand. Scalability is crucial because recharge methods could need to be multiplied or increased in response to escalating water stress. 7) Considerations for Water Quality: The plan should take them into account. To get rid of impurities and make sure the recharged water fulfils quality standards, pre-treatment procedures like sedimentation basins or filtration systems could be required. In conclusion, it should be kept in mind that the design of groundwater recharge techniques should be site-specific, take into account a variety of options, address water quality issues, connect with land use planning, entail monitoring and maintenance, involve communities, and guarantee adaptability and cost-effectiveness. Groundwater recharge techniques can greatly support sustainable water management by taking these factors into account, as well as help to lessen the difficulties brought on by water scarcity.
[1] Allen, D. M., Mackie, D. C. & Wei, M. 2004. Ground-water and climate change: a sensitivity analysis for the Grand Forks aquifer, southern British Columbia, Canada. Hydrogeology Journal, 12(3), 270-290. [2] Allison, G. B. & Hughes, M. W. 1978. The use of environmental chloride and tritium to estimate total recharge to an unconfined aquifer. Australian Journal of Soil Research, 16, 181-195. [3] Anderson, L. J. & Sevel, T. 1974. Profiles in the unsa-turated and saturated zones, Gronhoj, Denmark. In: Isotope Techniques in Groundwater Hydrology, 1. IAEA, Vienna, 3-20. [4] Babklin, V. I. & Klige, R. K. 2004. The contemporary hydrosphere. In: Shiklomanov, I. A. & Rodda, J. C. (eds) World Water Resources at the Beginning of the 21st Century. International Hydrology Series, UNESCO, Cambridge University Press, Cambridge, 13-18. [5] Bala, G., Caldeira, K., Wickett, M., Phillips, T. J., Lobell, D. B., Delire, C. & Mirin, A. 2007. Combined climate and carbon-cycle effects of large-scale deforestation. PNAS (physical sciences/ environmental sciences), 104(16), 6550-6555. [6] Banks, S. B. & Banks, D. 2001. Abandoned mines drainage: impact assessment and mitigation of discharges from coal mines in the UK. Engineering Geology, 60 (1-4), June 2001, 31-37. [7] Bar-Matthews, M., Ayalon, A. & Kaufman, A. 1998. Middle to Late Holocene (6,500 yr period) paleoclimate in the Eastern Mediterranean region from stable isotopic composition of speleothems from Soreq Cave, Israel. In: Issar, A. S. & B rown, N. (eds) Water, Environment and Society in Times of Climate Change. Kluwer Academic Publishers, Dordrecht, 203-214. [8] Bar-Matthews, M., Ayalon, A., Gilmour, M., Matthews, A. & Hawkesworth, C. J. 2003. Sea-land oxygen isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implication for paleo-rainfall during interglacial intervals. Geochimica et Cosmochimica Acta, 67, 3181-3199. [9] Bell, J. L., Sloan, L. C., Revenaugh, J. & Duffy, P. B. 2003. Evaluation of Northern Hemisphere natural climate variability in multiple temperature reconstructions and global climate model simulations. Global and Planetary Change, 37(1-2), 19-32. [10] Bender, F. A-M., Rodhe, H., Charlson, R. J., Ekman, A. M. L. & Loeb, N. 2006. 22 views of the global albedo - comparison between 20 GCMs and two satellites. Tellus A, 58(3), 320-330. [11] Bouwer, L. M, Aerts, J. C. J. H, Droggers, P. & Dohman, A. J. 2006. Detecting the long- term impacts from climate variability and increasing water consumption on run off in the Krishna river basin (India). Hydrology and Earth System Sciences, 10, 703-713. [12] Brooks, N. 2006. Cultural responses to aridity in the Middele Holocene and increased social complexity. Quaternary International, 151, 29-46. [13] Brown, N. G. 2001. History and Climate Change: A Eurocentric Perspective. Routledge. [14] Buffoni, L., Brunetti, M., Mangianti, F., Maugeri, M. & Nanni, T. 2002. Variazioni [15] Climatiche in Italia Negli Ultimi 130 Anni. Bollettino Geofísico Anno XXIII. [16] Burke, S. P., Potter, H. A. B. & Jarvis, A. 2005. Groundwater Rebound in the South Yorkshire Coalfield: a review of initial modelling. In: Proceedings of the 9th International Mine Water Congress (IMWA 2005) September 5-7, 2005, Oviedo, 223-227. [17] Burnett, W. C., Aggarwal, P. K., Aureli, A. et al. 2006. Quantifying submarine groundwater discharge in the coastal zone via multiple methods. Science of the Total Environment, 367, 498-543. [18] Cambi, C. & Dragoni, W. 2000. Groundwater, recharge variability and climatic changes: some consideration out of the modelling of an appenninic spring. Hydro-geology, 4, 39-53. [19] Castellani, V. & Dragoni, W. 1997. Ancient tunnels: from Roman outlets back to the early Greek civilization. Proceedings of the XII International Conference of Speleology, La Chaux-de-Fonds, Switzerland, August 12-14 1997, 3(2), 265-268. [20] Cook, P. G., Edmunds, W. M. & Gaye, C. B. 1992. Estimating paleorecharge and paleoclimate from unsaturated zone profiles. Water Resources Research, 28, 2721-2731. [21] Corsini, A., Soldati, M. & Pasuto, A. 2004. Landslides and climate change in the Italian Dolomites since the Late glacial. Catena, 55, 141-161. [22] Covey, C. 2003. Asteroids and comets; effects on Earth. In: MacCracken, M. C. & Perry, J. (eds) Encyclopedia of Global Environmental Change, Volume 1, John Wiley, 205-211. [23] Cremaschi, M. & Di Lernia, S. 1999. Holocene climatic changes and cultural dynamics in the Libyan Sahara. African Archaeological Review, 16, 211 -238. [24] Cremaschi, M., Pizzi,C. &Valsecchi, V. 2006. Water management and land use in the terramare and a possible climatic co-factor in their abandonment: The case study of the terramara of Poviglio santa Rosa (northern Italy). Quaternary International, 151, 87-98. [25] Davis, M. 2002. Late Victorian Holocausts: El Niño Famines and the Making of the Third World. Verso, London. [26] De Felice, A. M. & Dragoni, W. 1994. Considerazioni su variazioni climatiche e disponibilitci idriche in alcune localitii dell\'Italia Centrale. Il Quaternario, VII(1b), 357-364. [27] de Jager, C. & Usoskin, I. G. 2006. On possible drivers of Sun-induced climate changes. Journal of Atmospheric and Solar-Terrestrial Physics, 68, 2053 -2060. [28] Dearing, J. A. 2006. Climate-human-environment interactions: resolving our past. Climate of the Past, 2, 187-203. [29] Dehn, M. & Buma, J. 1999. Modelling future landslide activity based on general circulation models. Geomor-phology, 30, 175-187. [30] Dehn, M., Burger, G., Buma, J. & Gasparetto, P. 2000. Impact of climate change on slope stability using expanded downscaling. Engineering Geology, 55, 193-204. [31] Di Matteo, L. & Dragoni, W. 2006. Climate change and water resources in limestone and mountain areas: the case of Firenzuola Lake (Umbria, Italy). Proceedings of the 8th Conference on Limestone Hydrogeology, Neuchatel, Switzerland, 21-23 [32] September 2006. Presses universitaires de Franche-Comte (FRANCE), 83-88. [33] Dikau, R. & Schrott, L. 1999. The temporal stability and activity of landslides in Europe with respect to climatic change; TESLEC: main objectives and results. Geomorphology, 30, 1-12. [34] Dixon, N. & Brook, E. 2007. Impact of predicted climate change on landslide reactivation: case study of Mam Tor, UK. Landslides, 4, 137-147. [35] Drake, N., Wilson, A., Pelling, R., White, K., Mattingly, D. & Black, S. 2004. Water table decline, springline desiccation, and the early development of irrigated agriculture in the Wadi al-Ajal, Libyan Fezzan. Libyan Studies, 34, 95-112. [36] Dragoni, W. 1998. Some considerations on climatic changes, water resources and water needs in the Italian region south of the 43°N. In: Issar, A. S. & Brown, N. (eds) Water, Environment and Society in Times of Climatic Change. Kluwer, 241-271. [37] Edmunds, W. M. & Walton, N. R. G. 1980. A geo-chemical and isotopic approach to recharge evaluation in semi-arid zones, past and present. In: Arid Zone Hydrology, Investigations with Isotope Techniques. Proceedings of an Advisory Group Meeting on Application of Isotope Techniques in Arid Zones Hydrology, Vienna, 6-9 Nov 1978, International Atomic Energy Agency, Vienna, 47 -68. [38] Edmunds, W. M., Bath, A. H. & Miles, D. L. 1982. Hydrogeochemical evolution of the east midlands Triassic sandstone aquifer. Geochimica et Cosmochi-mica Acta, 46, 2069. [39] Edmunds, W. M., Darling, W. G. & Kinniburgh, D. G. 1988. Solute profile techniques for recharge estimation in semi-arid and arid terrain. In: Estimation of Natural Groundwater Recharge. NATO ASI Series. Reidel, Dordrecht, 139-158. [40] Edmunds, M. W., Gaye, C. B. & Fontes, J. C. 1992. A record of climatic and environmental change contained in the interstitial waters from the unsaturated zone of northern Senegal. In: Proceedings of an International Symposium on Isotope Techniques in Water Resource Development, IAEA/UNESCO, Vienna, 11-15 March 1991,533-549. [41] Essex, C. & McKitrick, R. 2003. Taken By Storm: The Troubled Science, Policy and Politics of Global Warming. Key Porter Books. [42] Fagan, B. M. 2001. The Little Ice Age: How Climate Made History, 1300-1850. Basic Books.
Copyright © 2023 Shruti Yerpude, Tushar Kodwate, Vijaya Banafar, Radha Deshkar, Rushikesh Chavan, Prof. Abhilasha Deshmukh. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Paper Id : IJRASET53673
Publish Date : 2023-06-03
ISSN : 2321-9653
Publisher Name : IJRASET
DOI Link : Click Here