(a) and (b) shows the administrative boundaries of India and National Capital Region (NCR) of India which includes Delhi, and neighboring urban cities. In this study we focused on Delhi, Faridabad and Gurgaon.
(c) shows the deformation results (in line of sight) obtained during phase 2 (2016–2018) analysis acquired in ascending direction.
The color bar represents the land subsidence velocity in (mm/year).
Red color represents high subsidence region, whereas blue color represents an uplift.
Three displacement features (two of them undergoing subsidence, and one showing uplift) are delineated and are marked with a black square in (c).
The close-up view of the three areas is shown in (d), (e), (f) respectively.
Here (d) refers to Kapashera;
(e) refers to Faridabad, and
(f) refers to Dwarka.
Maps were generated in ArcMap software (Version 10.4; Base Map: World Map; copyright and licensed by ESRI https://desktop.arcgis.com/).
Credit: Scientific Reports (2022). DOI: 10.1038/s41598-021-04193-9
Land subsidence is a severe often overlooked geological hazard and is a widespread global problem. It can be attributed to underground extraction of minerals, oil, gas and water, as well as natural events such as soil compaction, earthquake, and loess deposits. According to U.S. Geological Survey, more than 80% of land subsidence across the world is caused due to excessive groundwater extraction. When water is extracted from aquifers, the clay between pockets of water collapse gradually, leading to land subsidence.
A study titled "Tracking hidden crisis in India's capital from space: implications of unsustainable groundwater use," published in Scientific Reports co-authored by researchers from IIT Bombay, German Research Centre for Geosciences, University of Cambridge and the Southern Methodist University US have found that the rate of land subsidence near Delhi airport is accelerating rapidly.
During the years 2014–2016, the subsidence was found to be approximately 11cm/year which rose significantly by almost 50% over the next two years to around 17cm/year. The trend remained almost the same during 2018–2019, the study found.
"Of all the areas that are under threat, Kapashera near the airport was the most vulnerable because the subsidence rate is extremely high" said Shagun Garg, a doctoral researcher in the EPSRC Centre for Doctoral Training in Future Infrastructure and Built Environment: Resilience in a Changing World (FIBE2) who is part of the project team.
"The airport requires stable ground because of the risk of major disruption if there's significant ground movement," Garg said. "Kuala Lumpur airport is an example to understand the implications of land subsidence where cracks on taxiways, and water-logging emerged due to soil settlement. Continuous monitoring of Delhi International airport and its connecting roads is therefore crucial."
The study found another deformation in Mahipalpur, just 500m away from the airport where deformation of 15mm per year was observed in 2014–16, 30mm a year in 2016–18 and 50mm per year in 2018–19.
The growing population expansion and urbanization require an enormous amount of water to fulfill the demand. There is a huge gap of 750 million liters a day between the demand and the supply. Millions of residents do not have access to a piped water supply and rely on groundwater for their daily needs. In some places, the water depth is as high as 120m below ground level. The groundwater shortage is further complicated by Delhi's unchecked urbanization, which is disrupting the rejuvenation of the city's aquifers. Concrete and other infrastructure have overtaken the city, blocking rainwater from absorbing into the ground.
Rainwater harvesting is one solution to the problem. Delhi receives an average annual rainfall of 611mm, mostly in July, August, and September. Harvesting rainwater will not only bridge the gap between demand and supply but will also replenish the falling groundwater levels. The groundwater recharge can reduce the increasing rate of land subsidence and can mitigate the risk associated with subsidence.
The Indian Central Ground Water Authority in December 2018, introduced "Water Conservation Fees' for groundwater extraction for domestic and industrial purposes. The fee varies depending on the amount of extraction and the exploited zone (highest for overexploited, critical, and semi-critical blocks). However, it exempts individual households and agricultural users (the largest user of groundwater). Moreover, the current policies are solely based on mitigating the water scarcity problem and do not take into account the hazardous effect of land subsidence.
Despite its slow pace, land subsidence is known to cause losses worth billions of dollars all over the world due to damage to infrastructure, roads, pavements, and underground utilities such as drainage systems, aggravated flood risks and more frequent water-logging.
Can subsidence be reversed? Garg said that a detailed hydro-geological study is required to understand aquifer properties as current available data are limited.
"The Central Ground Water Board, the Geological Survey of India, and the Ministry of Urban Affairs need to investigate whether these trends are reversible," he said. "We suggest the government and policymakers should have a detailed understanding of the geophysical properties of the areas undergoing subsidence, and incentivize rainwater harvesting while ensuring strict implementation of laws against illegal mining of groundwater. The building conditions in hazard zones should be evaluated and proper measures should be taken."
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