Ground Water: What an Aquifer Is
Chapter Twenty-Seven
Syllabus topic 1, "Water"
Pages 110 to 113 of 885
In one line
Ground water is not an underground lake, it is water held in the pores of rock, and the law went wrong because the lawyers of the nineteenth century thought it was untraceable.
In the wording a student can write in an exam: an aquifer is a body of permeable rock or sediment saturated with water and able to yield it in usable quantity; recharge is the water that enters it, mostly from rainfall and from surface bodies; draft is the water taken out; and the stage of ground water extraction is the draft expressed as a percentage of the annual recharge, on which the Central Ground Water Board classifies an assessment unit as safe, semi-critical, critical or over-exploited.
The physical vocabulary
Aquifer. A saturated permeable formation. In India the main types are the alluvial aquifers of the Indo-Gangetic plain and the coastal deltas, which are thick, productive and easily drilled; and the hard rock aquifers of the Deccan trap and the crystalline shield, which hold water only in weathered zones and fractures and are quickly emptied. Peninsular India, including most of Maharashtra, is hard rock, and that fact decides most of the State's groundwater law.
Water table. The upper surface of the saturated zone in an unconfined aquifer. It rises after the monsoon and falls through the dry season.
Unconfined and confined. An unconfined aquifer is open to the surface and recharges directly. A confined aquifer lies between impermeable layers and recharges only where it outcrops, sometimes hundreds of kilometres away, so what is drawn from it may be very old water that will not be replaced.
Recharge and draft. Recharge is what enters. Draft is what is taken. The whole of groundwater law is an attempt to keep draft below recharge.
Stage of extraction. Draft as a percentage of annual extractable recharge. The Central Ground Water Board's categories are, broadly, safe below seventy per cent, semi-critical between seventy and ninety, critical between ninety and one hundred, and over-exploited above one hundred.
Cone of depression. A pumping well lowers the water table around itself in a cone. If two wells are close enough their cones overlap, and each reduces the other's yield. This is the physical fact the absolute dominion rule ignores, and it is why a neighbour's tube well can empty an open well.
Saline ingress. In a coastal aquifer fresh water floats on denser sea water. Over-pumping thins the fresh lens and draws the interface upward and inland. The chapter on salinity works this out.
Why the resource is legally difficult
It is invisible. Nobody can see whether a neighbour is taking too much, and nobody can see the boundary of the resource.
It is a classic common pool resource. Nobody can be kept out cheaply, and what one person pumps is not there for the next. The tragedy of the commons argument in module III is about exactly this.
Ground Water: What an Aquifer Is
Ownership of the surface does not correspond to the resource. An aquifer under four hundred fields is one physical body, and the law gave each of the four hundred owners a right to it.
And extraction is subsidised. Free or heavily subsidised electricity for agricultural pumping removes the price signal that would otherwise limit draft. A student who leaves the electricity tariff out of an answer about groundwater has left out the main cause.
The Indian position, in numbers a student can use
India is the largest user of ground water in the world; ground water supplies the greater part of irrigated area and the great majority of rural drinking water. The Central Ground Water Board assesses the country in units and reports that a substantial proportion of units in Punjab, Haryana, Rajasthan, Delhi and Tamil Nadu are over-exploited, while the eastern States are largely safe. The resource is therefore in surplus and in crisis at the same time in different places, which is why a national rule would be wrong and why the subject is with the States.
Worked example
A village in a hard rock district of Maharashtra had forty open wells in 1975 and has three hundred bore wells today. The open wells are dry by January.
Step one, what has happened physically? The bore wells reach the fractured zone below the weathered mantle that fed the open wells. Draft has risen far above recharge, the water table has fallen below the bottom of the open wells, and the cones of depression overlap.
Step two, has anybody done anything unlawful? At common law, no. Each owner has drawn percolating water from under his own land, which illustration (g) to section 7 of the Easements Act permits.
Step three, is there a statute? In Maharashtra, yes. If the watershed is notified as over-exploited under the Maharashtra Groundwater (Development and Management) Act, 2009, sinking a well needs permission, and a public drinking water source is protected within a prescribed distance.
Step four, is there a constitutional argument? Yes. Attakoya Thangal v. Union of India, a decision of the Kerala High Court of 1990, held that the right to sweet water is an attribute of the right to life under article 21 and that over-exploitation must be contained. Facts. The Lakshadweep administration proposed to pump ground water from the coral islands to augment supply; the petitioners said the fresh water lens was only 0.6 to 0.75 metres deep and that pumping would let sea water in. Held. The administration cannot function so as to make inroads into article 21; the right to sweet water and the right to free air are attributes of the right to life; a methodology must be evolved for extraction and over-exploitation contained; the matter was referred to the Ministries with a direction to issue appropriate directions and, if necessary, to make statutory regulations and set up a monitoring agency. Why it matters here. It treats an aquifer as something the State itself may not simply pump.
Ground Water: What an Aquifer Is
Step five, and the deeper answer. The physical unit is the aquifer and the legal unit is the plot. Until the two are made to correspond, by notifying an area and regulating within it, nothing else works.
Distinctions
| Surface water | Ground water | |
|---|---|---|
| Visible | Yes | No |
| Legal starting point | Riparian rights, illustration (h) to section 7 | Absolute dominion, illustration (g) to section 7 |
| Who may take it | Only a riparian owner | Any landowner above it |
| Unit of the resource | The stream, and the basin | The aquifer, which crosses every boundary |
| Statutory control | Irrigation Acts, and an award for an inter-State river | State groundwater Acts, and the Central Ground Water Authority under section 3(3) of the Environment (Protection) Act 1986 |
| Recovery after over-use | Next monsoon | Years, or never, and never at all after saline ingress |
What it does NOT mean
It does not mean ground water is separate from surface water. They are one resource: a river in the dry season is largely the aquifer draining into it, and pumping near a river reduces its flow. The Supreme Court acted on that unity in the 2018 Cauvery decree when it accounted for the ground water of the Tamil Nadu delta.
It does not mean an aquifer refills like a tank. Recharge is slow, and in a confined aquifer it may be geological.
And it does not mean the problem is the number of wells. It is the total draft. Ten efficient wells can take more than a hundred inefficient ones.
Quick revision
Aquifer: saturated permeable formation yielding water in usable quantity. Alluvial in the plains and deltas; hard rock in peninsular India.
Recharge, draft, and the stage of extraction as draft over annual extractable recharge; safe, semi-critical, critical, over-exploited.
Cone of depression: why one well affects another. Saline ingress: why a coastal over-draft is irreversible.
Four legal difficulties: invisibility; a common pool resource; the mismatch between the plot and the aquifer; and subsidised power.
Attakoya Thangal v. Union of India, Kerala High Court, 1990: the right to sweet water is an attribute of the right to life; over-exploitation must be contained.
Test yourself
1. What is the stage of ground water extraction, and what are the four categories? Draft expressed as a percentage of the annual extractable recharge. The categories are safe, semi-critical, critical and over-exploited.
Ground Water: What an Aquifer Is
2. Why does a bore well dry a neighbour's open well? Because pumping creates a cone of depression around the well; where the cones of many wells overlap the water table falls below the bottom of the shallower wells.
3. Why is the mismatch between the plot and the aquifer a legal problem? Because the aquifer is one physical resource that lies under many separately owned plots, while the law gave each surface owner a right to take from it, so no individual owner has any reason to restrain.
4. What did the Kerala High Court hold in Attakoya Thangal? That the administrative agency cannot function so as to make inroads into article 21, that the right to sweet water and the right to free air are attributes of the right to life, and that a methodology must be evolved for the extraction of ground water so that over-exploitation is contained.
The rest of this subject
These notes are cut from the University's printed syllabus. Open the syllabus itself, or the past papers, for the same subject.