Category Archives: Geoscience Blog

Borewell Deepening

Recently, my office decided to go deeper in search of groundwater. This is in Coimbatore and the existing borewell had been yielding water at 200 feet. Now the water table has fallen and they had to go down to 436 feet. Excessive drawdown, lack of rains, and overall poor water management has contributed to this.

Here are a few images of the drilling work:

 

Another abandoned borewell devours yet another child

Another sad story of a child who fell into a borewell and died.

Oh dear how many such gory deaths?

Okay most of the cases of children falling into borewells seem to occur in rural India. This says something about the borewell diameters. In the cities, borewells are dug for domestic purposes. These are lesser in diameter. So looks like the bigger borewells are the problem. Some manufacturing companies too dig large-diameter borewells. These might be typically located in the villages or suburbs.

However, this is not the primary reason – in the villages, people constantly seek groundwater. The moment a farm or company needs water, they try to dig a well. However, open wells are not always the solution (open wells are dug when you have groundwater available easily at shallow depths. Open wells are convenient. But then groundwater is not easily available – thus borewells are dug to a greater depth. Also companies need more water and wells won’t suffice).

People need water and where does that come from? River or lake water supplies is not always available to all areas. Thus, groundwater is the source. And people dig to great depths to get groundwater. Groundwater for various reasons – summer, over exploitation, less recharge etc at times goes down deeper (water table).

However, many of the borewells do not yield water and are “abandoned”. The driller might have used casing and partially sealed the hole. Mostly, though the moment there is no water, the drillers pack up and leave. Vegetation takes over and these borewells are forgotten.

Some day a child wanders over and falls. in. The diameter is enough for the child to fall in. However, it takes time to realize that the lost child could have fallen into the borewell.

The inside of the now defunct or not used borewell might have collapsed. Some bores are 300 feet deep (or more). The child might not always fall to the bottom but get stuck in the mud in between. This is not easy to find out as the hole is dark and deep. It is not a case of just pulling out the child through a vertical shaft.

So rescue operations begin and if the child is closer to the surface, a rescuer gets in and pulls them out. However, if the child has fallen to greater depths, a camera is sent into the hole and then a parallel bore is dug. From there another horizontal bore is dug. Quiet often the rescue succeeds but not always. A lot of Geology is involved and rescue plans must be fast and precise. But even with the best geophysical instruments, it is not easy to estimate the type and size of rock that blocks access to the point where the child is stuck. Moreover, drilling through rock can make the entire borewell collapse.

The simplest solution should be to seal all the holes the moment they are not used. Sadly, this negligence and ineptitude devours a child.

 

Chaotic erosion along a culvert

The northeast monsoon brings rainfall to Chennai in October-November. However, 2015 witnessed excess rainfall and the city was “surprised”. Rains have not been good enough in Tamil Nadu in the past. However, now and then it rains in excess and many parts of the state suffers due to unplanned development. Buildings have come up in dry lake beds (also when streams were dry). Obviously, this leads to inundation.

Several small rivers (large streams) in Chennai started to carry water. This in turn wreaked havoc along its path. Here is a waterway – probably a small stream that has been cemented to just carry water. However, parts of the embankment have not been strong enough. Possibly, water from the Chembarambakkam Lake has been released. Or this could be water from another state…

The runoff was not much – just about 2-3 feet but because the entire culvert is paved, water gains speed. Notice the small local streams serving the main stream. The culvert is reddish with sediments.

Notice the left bank – that has given away to the force of water and rain.

 

DSC_0229DSC_0228DSC_0186DSC_0185DSC_0227

Geology apps on the iPad landscape

Wallpapers of oil rigs or volcanoes or rock formations. This is probably how a geology lovers iPad screen might look like.  Add these days geology-related apps make up the tablet screen morphology. There are quiet a few Android and iPad apps for Geology and what better way to start blogging about them than with Screen shots of them all?

The screens here are from my iPad. Ironically, I used a Samsung Note (a tablet) to scribble down this blog! Yes, I used the stylus to write this post. Technology is really useful!

I will review a few of the geology apps in later posts.

14112259314011411225930124

Flying Over Auckland

Wow!

Elaine R. Smid

Late last year, I had the good fortune to meet a trained pilot who volunteered to take me and my flatmate up in his plane over Auckland. I’ve always wanted to do this–and in fact had investigated flight prices ($199 for 15 minutes?! Ouch!)–so leapt at the opportunity. We were up there for a few hours on a beautiful early summer day, flying from south Auckland around to Rangitoto and Whangaparaoa, then to Devonport and over the Harbour Bridge and behind the Sky Tower. It was exhilarating. Flying is one of my absolute favourite things to do–if I had the time and money, I’d definitely take pilot lessons.

As always, I had my geologists’ cap on. The trip offered some great vantage points to see Auckland’s volcanoes and geology like I’d never seen them before:

(All photos by Elaine Smid. Feel free to use with proper citation and…

View original post 258 more words

Borewell drilling in cramped urban areas: problems aplenty

IMG_0005 IMG_0006IMG_0009IMG_0014

 

 

 

 

 

 

 

 


In Chennai, during summer, groundwater levels dip. Water supplies through tankers or pipe lines also dwindle in many areas. So people naturally look at borewells to provide water at least for essential purposes such as washing. Drinking water anyhow is purchased.

However, borewell drilling leads to plenty of problems. Some of my observations and thoughts are:

  • Cramped spaces between houses. This essentially is a city planner problem and India cannot afford to provide spacious housing to all its citizens. Only the very wealthy can have some elbow room. The poorer you are, the less space you occupy. Therefore, those who do own a house with enough space to get a borewell, are in some sense lucky. However, many house owners have only a parking lot or a small entrance that is quiet often shared with other houses. Often they do not have pipe lines that supply water. So they have no other go but to go underground in search of water.
  •  Total lack of scientific approach. While the house owners desperately need water, the water well drilling services agencies seem to take up any job they can. Of course they need the money. Yet, in many cases, I have never seen a hydrogeologist or some qualified person make an initial assessment. If there is space – such as in large apartment complexes or shopping malls, then yes a geologist uses geophysical resistivity methods and provides an assessment. It doesn’t make sense to do a study when you just have room enough for a car or motor cycle to be parked.  So if you can spare only 15 feet, then what options do you have?
  • Are basic factors looked into?   Yes hardly enough ground space exists but at least are the basic factors addressed? I hear people say that the groundwater smells of sewage. Now how is that possible? Are there adjacent drains that leak? Or are ponds of sewage mixing with groundwater? Or are the pungent smells due to another factor? Is the salt content due to fluorides or nitrates? Are there any other harmful elements? Is the surface clean or is it capable of polluting the groundwater?
  • A nuisance to all residents nearby. I watch borewell drilling as I am interested in the Geology and hydrogeology. However, for many people this is sheer noise. Often these rotary drilling jobs take up to 4 hours. Plenty of dust flies into homes whenever the drill bit hits rock in between.
  • Scientific monitoring and management not available. Is there an aquifer in that area? If so what type? Would puncturing the aquifer have any impact? How many wells can the aquifer support? What were the geological conditions 30 years ago? Was there a lake bed on which these houses were built? Are standard procedures in place and followed? I don’t see any of this. The wells are not numbered or used for mapping.
  • Safety aspects not considered. The drillers don’t have any protective equipment. Am sure they are not insured. They don’t provide any specific masks or other such equipment to residents. What if there is an infant or an ailing person? What if someone is allergic to dust? Finally, is the hole sealed properly? Okay these are small holes but this negligence is what devours young children across suburbs in India. How horrific can we get? A well cap to seal water wells is mandatory for large diameter wells such as for agricultural or small factories. However, these have become “graveyard holes”. Okay the urban borewells are smaller – yet should they not have some indication? A marker maybe?

A subject so close to heart and fascinating – hydrogeology. What is the use of developments in technology and science if the basic standards are not followed? What use is a new modelling software that can calculate infinite parameters and provide stunning 3D visualization if safety is compromised? No GIS tool will be able to use data if the wells are not licensed and monitored.

The driller in these pictures was okay as this did not compromise safety issues. However, I have seen far worse borewell drilling reports on YouTube  and elsewhere.

Maybe it will take a catastrophe of monumental proportions to stir something and lead to better practices.

In this piece am not discussing the effects of non-pervious surfaces such as roads and concrete that prevent proper rainwater drainage. Am worried about the drilling approach in populous and cramped cities.

Fresh water from a well in the sea at Rameswaram

In Rameswaram, an Island on the South east coast of India, there is a well some distance into the sea that provides water which is not salty and can be drunk. This is  a holy place and according to Hindu mythology Lord Rama shot an arrow into the sea to get water to drink for his wife Sita. This is known as the Villundi Tīrtham well.  How is it possible that you get non-salty water amid the sea water?

The Earth has Oceans which occur in “basins”. Continents, that is land we live on, is higher than the water level in the Oceans. (If you are keen for more, read about Isostasy.)

On land, groundwater occurs beneath the surface in what geologists call as Aquifers. Aquifers are geologic formations that can store and transmit water. Note that geologic formations are rock strata that have similar properties (for example rocks of a certain chemical and mineral nature is one such property). These have been deposited over millions of years (if you are interested read about stratigraphy, erosion, landforms, geologic time, etc).

Under some instances water gets collected from rain, rivers, and other sources and is stored underground in aquifers.

Aquifers constantly interact with other water sources, atmosphere, and is governed by forces such as pressure and gravity. The geologic formations too determine the aquifer’s nature – porosity, permeability, storage capacity, etc.

Groundwater near the coast interacts with the sea water too. The figure (source: Solinst) shows theoretically how groundwater exists. In reality though it is very complex.

Groundwater is recharged by rain and lakes or rivers. Thus Groundwater is not stagnant and flows. The flow is described by Darcy’s law which in simple terms means “groundwater flows depending on pressure and the length of the aquifer medium”. This pressure is the reason we are able to dig wells. This is often the capillary pressure.

Groundwater can be confined within strata and be under pressure. Or it may not have a confining layer and could be seen close to the surface.

The level to which groundwater can raise is the water table. Of course this is only for groundwater that is not confined by impervious or semi impervious strata. The potentiomentric surface is used to describe the water table level.

On the coasts, groundwater exists in “dynamic and often transient equilibrium” with sea water. Sea water is denser and filtrates into the ground beneath the sea and on to the land.

Groundwater should flow – discharge into the sea – as long as the water table level is at a higher pressure gradient. Sea water in turn will try to flow in and contaminate the fresh groundwater. There is a seawater-freshwater interface (not a sharp line!) that is transient and keeps changing with rainfall, river or lake discharge, tides and evaporation.

If humans pump out water from the coastal areas, sea water intrudes the fresher groundwater. The Gyben-Herzberg equation governs the fresher groundwater aquifer-sea water interface. For every feet of water on the surface, some 40 feet of groundwater exists below sea level.

So what does it have to do with this freshwater well in the sea? If you dig a well in the sea you expect to get saline water. Yet, the well provides drinkable water because of these possible scenarios:- the freshwater-sea water interface extends far into the sea even beneath the waves. Highly unlikely as the water table pressure would need to be immensely high on the land!
– there is submarine discharge of groundwater from a confined aquifer beneath the sea at this place. The strata confining the aquifer prevents water from seeping out on the land side but there is a hidden interface on the sea side.This is possible.
– maybe seawater has “transgressed” only on the surface and below the surface is stopped from infiltering by impervious formations.

So this must be some kind of mix of these situations. The sea water here is pretty static – no waves in sight. Modeling coastal aquifers is a major headache. On Islands, the Fetter analytical solution applies better. I will not describe that here.

Usually, salt water intrusion into coastal aquifers is due to:

– lateral movement of salt water from the sea due to heavy water loss (withdrawals by humans) from the coastal aquifers
– “Saline zones” deep in the interface move up to cause “upconing” near coastal pumping wells

So is it possible? Yes. Fresh water is less denser than salt water and “floats” on salt water. This is important when you bore into the groundwater in islands. Rain water percolates into the ground and pushes the salt water beneath it. So you need to model the interface where freshwater and saltwater mix and take care not to disturb this by puncturing into sea water (when you drill).

Here is a citation that explains why this well gives freshwater:

“This natural movement of fresh water towards the sea prevents salt water from entering freshwater coastal aquifers (Barlow, 2003).”

Similar examples exist at Cuba and the Gulf of Mexico.

There are 22 wells in the Rameswaram temple – on a shallow coastal aquifer (unconfined) and close to the sea. The dissolved solids vary in each.

So even if shooting the arrow part is not an acceptable theory, one must note the intelligence behind these wells. There was no technology and yet, this well was predicted to yield non-salty water.

Lake Ontario fights another cold winter – to prevent being frozen over

Ice formed it. Silurian-age rocks were covered by glacial ice that retreated and advanced over many cycles. Finally, the glaciers melted to leave huge volumes of water in the Great Lakes. Lake Ontario still has its annual rendezvous with ice – in winter. The lake is huge – is almost like a sea. The waves try to keep the ice at bay at Rochester…

Iron Ore and Magnesite Mining in Karnataka and Goa: The losers at the end of the greed chain

As you move north from Bangalore (India), the landscape changes – vast areas of reddish soil dotted with plenty of trees, agricultural lands, and low hillocks now and then and…lots of forest cover. This is the Tumkur district and used to be full of nondescript towns and people leading a simple life.

Tumkur is also home to Iron ore.

Geologically speaking Tumkur is made up of rocks of Archaean Complex (Granitic Gneisses, and Schists) with some Deccan trappean and intertrappean formations.

Haematite is the most prominent iron ore in this area. The iron ore occurs within banded iron ore formations in massive, laminated, friable form.

The Cauvery and  Tungabhadra make the land fertile enough.

Iron ore is a gift of nature that brings in revenue and helps in technological advancement. However, in the name of mining, there has been exploitation. This has two aspects: 1. the country has been denied money from its own resources with some individuals resorting to fraud and 2. the environment has been severely affected as all norms have been flouted.

The mining scam as it has been called by the media has rocked the country. Iron ore mining was run by authorized mines and everything was fine. Suddenly after 2000, China was ready to pay for iron ore to meet its infrastructure needs. In India mining licenses meanwhile had been issued to private companies in keeping with the opening up of the economy. Some mine owners started mining and exporting a lot of Iron ore. They provided false data about the iron ore mines and the money actually they got. They bribed the right people to help their cause. This resulted in loss for the government, honest stakeholders, and people.

However, the people involved in illegal mining ranged from the top brass to the simple farmer. With the boom in mining, people started to sell their agricultural lands to mining companies. The companies would easily get a mining license and convert the agricultural land to a mining one. This dealt a blow the environment too.  Account books were cooked and mine reports had false data.

Many sold everything they had to invest in the so-called mining lands. Many millionaires were made. The money was never accounted for. Some waited too long to sell their lands and are desperate now – the losers at the end of the greed chain.

Elsewhere – to the northwest, the scenery is spectacular. The story is not. As the Arabian sea beckons, the “smell” of magnesite too seems to add to the salty air. This is the border between Goa and Karnataka. The entire karwar-shimoga belt is lovely. Here too there are mines of Iron ore and Magnesite. This area too has suffered a similar fate. I will point you to an article link in The Hindu, one of India’s leading newspapers: http://www.thehindu.com/arts/magazine/article2540038.ece

In photo: agricultural lands in Tumkur that a a farmer wants to sell as “mineable” land. Typically many people bought such lands close to mines and prepared false geochemical sheets and tried to sell their lands. Haematite ore is reddish with some “banded” striations while magnesite is black. Samples too may not be from the agricultural land that farmers sell. Samples are not always indication that ore is available in that land.

Soil testing for constructing a 55 storey building in Chennai

Soil testing (in  geotechnical investigations) is a broad term used to describe the various tasks involved in gathering the required information for planning foundations and “earth works”.  Structures such as buildings or bridges require a strong and stable foundation to stand on. Geotechnical experts gather
information about the physical properties of rocks and soil from a proposed site to assess the suitability of the particular site. For example, bridges are
meant to support heavy loads such as vehicles or trains. Bridges are built on piles and the foundation should support the load. Swampy areas often have
“loose” soil with high water content and are not ideal for construction. However, soil testing studies would confirm the property of the soil and rocks at a site.

To get adequate information about a site, surface and subsurface investigations must be undertaken. Geologic mapping and direct field studies provide information about the surface. For large projects such as bridges on seas, geophysical methods are used to gather subsurface data. For building constructions and designing foundations for bridges, many methods are available. However, the most common method is the use of boring techniques to get soil or rock samples.

Soil samples provide evidence of what lies beneath the surface. Geology of the area might indicate the age and type of rock one can expect in
the formations. Boring brings up the soil or rock and often the lithology can be established. Rocky sub surfaces act as strong bed rocks. However, soil
testing focuses more on finding out whether the site is suitable for construction or whether there could be potentially dangerous sink holes, mud
slides, or faults. This is done through analysis of the sand grains for grain size, water content, ability to withstand stress and shear, etc.

To test soils or rocks of a site:

  • Conduct field or site investigations in situ
  • Study associated geological maps
  • Gather data from nearby sites
  • Use appropriate method to understand subsurface
  • Get samples and analyze physical property of soil in the laboratory
  • Depending on the results, make a decision

Here are some photographs of the equipment used to gather core samples. The usual tools used include samplers such as augers, Shelby tubes
or pistons. At times, undisturbed samples are required to make a decision. The sampler selected depends on the type of sample required and the rock or soil
property. The photographs show sampler tubes with the core.

The Volcanism Blog

volcanoes, volcanism and volcanology

Written In Stone...seen through my lens

A passion for Geology...active after a hiatus

Magma Cum Laude

By Jessica Ball

Arizona Geology

A passion for Geology...active after a hiatus

Blog - Agile

A passion for Geology...active after a hiatus

Highly Allochthonous

A passion for Geology...active after a hiatus

AGU Blogosphere | Site-Wide Activity

A passion for Geology...active after a hiatus

Letters from Gondwana.

Paleontology, books and other stuff.

The Failed Rift

Gist from a triple-junction.

Rock-Head Sciences

A science blog that brings you closer to the world of geology! Featuring the "A Day in the GeoLife" and "GeoProject" guest blog series from geoscientists around the world.

verseherder

Birding in south India and life on planet earth

Elaine R. Smid

Volcanologist. Erupting at you from the City of Volcanoes.

Anisotropic Reflections

interpretations of a geological geophysicist

Ancient Shore

Paleontology, Geology, and Landscape

The Trembling Earth

now at blogs.agu.org/tremblingearth