Dugwells vs. Shallow Tube well

Professor Feroze Ahmed (BUET, Dhaka)
Professor Charles Harvey 
Professor Timir Hore
Dr Meera Smith
Professor J.M. McArthur  London
Columbia University
Richard Wilson, Harvard

Professor Feroze Ahmed:
"some of the deep tubewells installed in acute arsenic problem areas have been found to produce water with increasing arsenic content. Post-construction analysis shows that arsenic contaminated water could rapidly percolate through shrouded materials to produce elevated levels of arsenic in deep tubewell water. Experimentation by sealing the borehole at the level of impermeable layer is yet to be conducted to draw conclusions."  and: "in general, permeability, specific storage capacity and specific yield usually increase with depth because of the increase in the size of aquifer materials. Experience in the design and installation of tubewells shows that reddish sand produces best quality water in respect of dissolved iron and arsenic. The reddish colour of sand is produced by oxidation of iron on sand grains to ferric form. Which will not release arsenic or iron in groundwater, rather ferric iron coated sand will adsorb arsenic from ground water. Dhaka water supply, in spite of arsenic contamination around is probably protected by its red coloured soil. Hence, installation of tubewell in reddish sand, if available, should be safe from arsenic contamination."

Professor Charles Harvey MIT (immediately following)

I don't have any direct experience with dug wells. Two thoughts come to mind --

(1) If the water in the dug well is mixed, then I like your idea about oxidation, although the oxidation of iron is likely most important for lowering arsenic concentrations. The relative amounts of iron, arsenic, phosphate and silicate have to be such that arsenic is taken out with iron precipitation.   Stephan Hug's work with photooxidation in PET bottles has shown that the concentrations in well water are often such that arsenic is naturally removed,   however in some areas iron is too low relative to phosphate and silicate. (Of course a dug well does not have the benefit of photoxidation.) So, where there is enough iron relative to the competing anions, the safety may be basically a matter of timing, i.e. competing rates -- the rate that pumping mixes oxygen in, the rate that new groundwater enters the well, and the kinetic rates of the chemistry. It also helps that the shallowest groundwater often has less arsenic than deeper.

(2) I don't see why arsenic would generally increase in shallow tube wells.   Does pumping from the well itself always increase concentrations? Do shallow wells draw more contaminated water up? Is dissolved arsenic currently increasing regionally at shallow depths? Of course, solutes in an individual well may have different behavior depending on the nearby groundwater concentrations -- but I'd be a little surprised if all shallow wells, or even most shallow wells, have an increase in arsenic concentration after installation.

Dr Timir B. Hore

First let me introduce myself. My name is Timir B Hore. I received my Post Graduate Degee in Applied Geology and Ph.D. in Hyderogeology. My Ph.D work on Bengal Basin.Hydrogeolog, Environmental Impact and Impact due to Unplanned & Unscientific utilisation of groundwater in and around Calcutta was my main area of  studies.Besides, I have studied groundwater and hydrogeology of Deltaic Sediments in three field seasons( each season' duration 5to6 months) while working as Senior Geologist with Geological Survey of India.With two other collegues we prepared Landform Map Of Greater Calcutta and part of Bengal Basin, detailed hydrogeological studies including groundwater quality, occurrences,exploitation of groundwater etc. During this period we have studied 3000 deep tubewells.Earlier I have worked with World Bank, Swedish International Organisation as a Groundwater Consultant, as a Regional Hydrogelogist with Govt. of Tanzania and a Senior Hydrogeologist o! f a Yugoslovian International Organisation. Last 40 years I have been working on Groundwater problem in different parts of the world. Since 1985 I have been working with an Environmental Company in New Jersey , U.S.A. I am very much attached with Prject Well programme. Thanks to Dr. Meera Smith. Due to her sincere interest this shallow well Project has become a focul point or one of the main sources to provide potable water to the poor villagers of Bengal. whole project has been carried on with experienced Geologits.Statement without any field data is totally unceptable. Arsenic is a very popular and Hot Topics. So people in different areas without proper understanding got involved to solve this chronic problem.This is not the place to discuss the whole Geology, Hydrogeology,Utilisation, Development of Groundwater is very  complicated in Detaic Geologic Formation. There are two ways to use the groundwater from Bengal Basin with Permissible arseni! c level (<50ppb) in drinking water.Limited local water supply through Open Shallow Dugwells( Depth of each well preferably between 25 to 30 ft. below ground surface).Please refer Project Well's modified Open Dugwell design. This is totally wrong idea to make a statement that  arsenic concentration will increase in future in the grounwater of shallow dugwell. I would like to request everybody  please try to understand the Geology, Hydrogeology and Geochemistry of any water bearing horizon before making any statement. One should understand why arsenic level within drinking water limit in the groundwater of open shallow dugwells? Secondly I would like to mention here that people should not comment regarding the construction of deep tubewells without any knowledge of general practice of installation of deep tubewells in Bangladesh and West Bengal. I had circulate a design how to install a tubewell in any groundwater impacted aquifers. Swelling of clay can not prevent migration of cross contamination, because the annular space between the clay layer and the casing of the tubewell always filled with well rounded gravels. This gravel layer is the main avenue for vertical migration of contaminated water from upper aquifers to lower aquifers. There is a method how to install a proper deep tubewells in impacted areas. I will happy to help for any deep tubewell construction project. It is sofisticated procedure and can not be installed based on common sence. Please try to develop proper way to provide safe drinking water to people.
 
Please wite me for any help.
 
Timir B. Hore  

Dr Meera M. Smith of the University of California and worker in West Bengal writes as follows:

Future of the tube wells: The 15,000 tube wells, depending on their depth, may get contaminated with arsenic within one year followed by installation of filters to remove the arsenic in the water. Within the following year, these filters will be labeled as "out-of-order" due to improper management, and back to square one. What a waste of funds!

It is indeed extremely difficult to say what is the best option because the options need to be suitable for the specific area. 

According to my opinion the best, long-term option is distribution of water by pipelines stored in the overhead tanks. The water from the third aquifer needs to be accessed very cautiously, to avoid cross contamination, and pumped up to overhead tanks.

Until the implementation of such huge projects to cover the whole country the best option, for the interim period, is harvesting of rainwater. Awareness, training and management are the three main components to run these projects successfully in the beginning. The objective of Project Well is to make the dug well project sustainable at the village level. To make it sustainable, a team of three field staff has been involved who would train and supervise the users of 26 dug wells only for one year.

To increase the crop production during the period of green revolution methods like workshops organized by local NGOs, programs broadcasted on the radio mainly for the farmers (chasi bhaid'eyr bolchhi) were/are used to promote the use of high yield variety of seeds and the use of fertilizers and pesticides. These informative methods can be used for training the users of dug wells. As the farmers know today when to apply fertilizers and pesticides to their crops, similarly the dug well users would know how to maintain their dug wells, community or private, in few years. Rome was not built in one day.

Suggestions for the schools:
a) If there is a pond nearby, preserve it and install a bacteria removal filter before supplying water to the school tap. Many families in the villages of the district of South 24 Parganas, West Bengal, use pond water >for cooking that constitutes 25% of their daily water usage.
b)Try excavating a couple of shallow dug wells using the guidelines used by Project Well and test the water for arsenic, quarterly. (Details are available on the web site). The arsenic level in water of 5 concrete, shallow dug wells provided by Project Well were monitored for one year (ending July 2003) and it was found that in all the five wells arsenic level was lower than 50 PPB throughout the year except for one which increased to more than 100 PPB in the driest months of April and May. During this period the consumers were requested to collect water from other sources that are located far. According to the users, it is worth having an arsenic safe water source that would provide water for ten >months rather than having no source at all in their locality. Project Well is trying to assess the cause of the increase in arsenic in this particular well. Suggestions from the experts would be a great help. The bacteria can be removed by filtering the water if the use of Theoline, a disinfectant, is not preferred.
c) During the monsoon period rainwater can be collected for drinking. There are several methods practiced in many parts of the world. If none of the rainwater harvesting methods can be implemented then properly installed deep tube wells (refer to John McArthur's suggestion circulated to arsenic crisis group on 14th July,2003) can be an option. But extra caution need to be taken in detecting the level "deep". It is also important to strictly supervise the drilling, insertion of the pipes, to avoid cross contamination and detecting the safe depth.

Use of arsenic removal filters is the last option if none of the above works. There are problems with all methods suggested so far for the long-term disposal of arsenic waste. The 'green' disposal method recently developed by Naval Materials Research Laboratory ( NMRL), DRDO, Ministry Of Defence, Shil-Badlapur Road, Addl. Ambernath-421506 "A SIMPLE AND ENVIRONMENTALLY SAFE DRINKING WATER FILTER FOR ARSENIC REMEDIATION" sounds very good but who knows that the construction industries that would use the non-leachable cement blocks made >from the arsenic sludge would not face the same fate as the asbestos industries are facing today.

Use of a checklist in prioritizing the methods suitable for the schools based on its location would be a good start.
 
Thanking you.

Dr. Meera M Hira Smith


Comment by John Macarthur, University College London

Does not the answer to the question "how can we provide safe water" depend on the area of the country under consideration and include the following?

Reliance on:

1] The 75% of shallow wells that are not polluted with arsenic,
2] Deep wells,
3] Traditional dug wells, modernised as appropriate, and
4] Rainwater harvesting.

The last may be a good option for schools, where the children might incorporate a knowledge of, and maintenance of, the water system as part of  their curriculum.  Certainly, deep wells, properly constructed, have much to offer, and this is an option employed much in West Bengal (my definition of  a "deep" well  is a well completed entirely in sands beneath the Holocene/latest Pleistocene transgressive surface). 

Provided the wells are constructed so as to prevent leakage between the upper and lower aquifers, it is likely that they will be free of arsenic (and other undesirables) for the foreseeable future, particularly if they are screened several tens of metres below the top of the deep aquifer. There are several reasons why this should be so; they range from geochemical considerations to
an observation, based on the DPHE database (DPHE 1999, 2001) and summarised in the accompanying table, that deep wells seem to remain free of arsenic.  Isolated instances of pollution in deep wells have ready explanations in casing failure, contamination, leakage etc.

Area       No.    Age, range  As, range  Depth, range  % Shallow wells
           DTW       (y)       (ug/L)         (m)        > 50 As ug /L
Chandpur    4        2- 3         0-6        221-269         98
Lakshmipur  6        3-10         0-8        183-318         64
Noakhali    6        5-15         2-10       246-292         79


No doubt all of this has been gone over many times.  What is not often  stated is that 75% of wells in the Bengal Basin are doing the job for which they were intended - providing good quality water for public consumption: proof enough that, in the right place and at the right depth, the tubewell has a future in water supply in the area.

Sincerely,

John McArthur

Further comment by John. McArthur in March 2004

I  have answered this first part as much as I can. Dug wells are aerated (maybe), but there is no evidence that this is keeping them arsenic-free: its just a suggestion I made the suggestion in one of my papers and others have followed. Its logical and simple, but not yet proven as a mechanism. If it does operate, then the dug-wells should be lined with FeOOH soon after comissioning, as oxygen gets to the iron and precipitates arsenic. Are they? I have never heard they are.

So, dug wells may be arsenic-free because they are near the surface (about 5m deep) and are tapping water at the water table. That is the youngest water around and so has not had time, nor opportunity, to get deeper, pick up organic matter, and so cause FeOOH reduction and arsenic pollution. Which is what both Charlie and I told you. Its probably the better explanation.

Yes, there is concern about deep wells mixing water in the deep and shallow aquifer. Currently, deep and shallow aquifers are separated most places by a clay that differs in thickness from place-to-place. Where we put in our deep wells last month in West Bengal, that clay was > 240 feet thick. The concern is that punching a hole through the clay to put in the pipe for the deep well may allow water to flow through the hole from one aquifer to the other. Water will flow down a pressure gradient, and it seems generally to be assumed that the pressure in the deep aquifer is always lower than that in the shallow aquifer, but I am not sure that is always the case. The standard way to deal with that is to fill the annual space between hole and pipe with sand up to the base of the clay, then fill the space with clay (especially a swelling clay termed bentonite) to the top of the clay at least. This then seals the hole made around the pipe and prevents flow between aquifers. Of course, it takes a good driller to know just how to get the clay in the right place. A bad driller will put it in the wrong place, or not fill the hole at all with impermeable material. Then water flows between aquifers and can take arsenic with it, if the pressure head in the deep aquifer is less than it is in the shallow aquifer.

As to how the deep aquifer gets recharged - that is not something I can answer authoritatively. Its probably a combination of southward flow from outcrops in the north of the basin and diffuse leakage through the clay. Much of the water seems (very sparse data) very old, so much of the pumping might be from confined storage - mining the water to some extent. Of couse, the diffuse downward leakage might just carry arsenic down with it. Its all a bit complex for me, so don't quote me on this last paragraph.

In Dhaka, deep wells are all in Dupi Tilla formation (Pleistocene or older). The sediments are old, weathered, and have had all organic matter removed by oxidation during several hundred thousand years up to 18000 years ago. So, there is no organic matter left to drive FeOOH reduction, so there is almost no pollution by arsenic. Where is occurs, its organic matter in splled petrol and the like, and organic matter in latrines, that drives the reduction (very local).

Regards,

John

Columbia University

Deep Wells Can Target Low Arsenic Aquifers in Bangladesh, New Study Shows
Columbia researchers advance plan to mitigate arsenic crisis

A solution to arsenic-poisoned drinking water in Bangladesh has come two steps closer with two new research papers by Lex van Geen, Doherty Senior Researcher at the Lamont-Doherty Earth Observatory, part of the Earth Institute at Columbia University, and a team of researchers from Columbia.

A new study by Columbia University researchers shows highly variable arsenic levels in water drawn from wells in the 10-25 m depth range, while wells deeper than 30 m in this particular village are consistently low in arsenic. The upper panel based on an IKONOS satellite image of the village and surrounding rice fields shows the location and arsenic content of individual wells. The lower panel is a depth section of the same wells. The large blue circle indicates the location and depth of a communal well installed and monitored by the program.

Satellite image by: spaceimaging.com

The first paper, titled "Spatial variability of arsenic in 6000 tube wells in a 25km2 area of Bangladesh," was published in a recent issue of the highly-ranked journal Water Resources Research and was selected by the American Geological Union for highlighting in July. The paper describes a study that involved testing all tube wells in a portion of Araihazar upazila, one of 490 sub-districts of Bangladesh. The study confirms that although the arsenic content of aquifers shallower than 30 meters is spatially very variable and difficult to predict, wells that tap into deeper sandy deposits that are over 10,000 years old yield groundwater that is consistently low in arsenic ( Less than 10 micrograms of arsenic per liter, the WHO guideline value).

A complication is that the depth of these safe aquifers varies from less than 10 meters to up to 300 meters, even varying over an unexpectedly wide range from village to village as this new study shows. The challenge, therefore, is to provide the expertise and equipment needed to target these aquifers at the village scale. Click HERE to download the paper in PDF format.

Further research by the team, in a study published in the Bulletin of the World Health Organization, shows that when communal wells producing safe drinking water are provided to a village, they are surprisingly well accepted and widely used by the local population, serving an average of 500 people living within a 200 meter radius. On the basis of geographic information obtained with hand-held Global Positioning System (GPS) receivers, the study documents that most women started to walk hundreds of meters each day to fetch water from these communal wells once they were installed, switching from their private wells that had tested high for arsenic.

Local-level mapping of arsenic content in groundwater, used as a tool to site deep, safe community wells in Bangladesh, could therefore be used extensively to reduce the exposure of the population to arsenic. "On the basis of these two studies and the experiences of many other scientists and engineers," Van Geen explains, "we are beginning to form a new strategy to propose to the government of Bangladesh to mitigate the arsenic crisis."

Columbia University has been central to a five year, $11 million grant from the NIEHS Superfund Basic Research Program aimed at understanding and addressing the health impact and origin of elevated arsenic levels in groundwater in the US and in Bangladesh. The Columbia team, led by Joe Graziano of the Mailman School of Public Health and Lex van Geen, is approaching the problem from a unique, multidisciplinary perspective that spans the health, social, and earth sciences. The Columbia team also collaborates with NGOs active in Bangladesh, universities and research organizations in Bangladesh and the US, as well as with UNICEF.

The Earth Institute at Columbia is the world's leading academic center for the integrated study of Earth, its environment, and society. The Earth Institute stresses cross-disciplinary approaches to complex problems. Through its research, training and global partnerships, it mobilizes science and technology to advance sustainable development, while placing special emphasis on the needs of the world's poor.





http://www.earthinstitute.columbia.edu/news/2003/story07-18-03.html


4.  Richard Wilson of Harvard  University comments:

At first sight it seems obvious that one should use deep wells (into an arsenic free aquifer) for drinking and continue to use shallow wells for irrigation.  However I am nervous about a number of issues and raise them as questions.  
(1)  If one used deep wells for everything  would one soon reduce the ability to get water therefrom?  How is the deep acquifer recharged?  from a long way away as John McArthuir suggests?  I would like to know.
(2)    I am very nervous about any large program to indiscriminantly install new tube wells.  It is likely that 90% of them would be sunk by local people.  If cement were provided for grouting them, the cement might well be used for the more urgent needs such as laying a kitchen floor or otherwise fixing up a house.  Failure to grout even  20% of the proposed wells would lead to disaster as arsenic laden water from the upper aquifer leaked into the lower one    The disaster would be compounded by the fact that measurement of arsenic in the field is still very inaccurate, and very infrequent.  It might be a few years before the realization set in that Bangladesh had once again taken the wrong route on the basis of foreign advice.  The crisis is not merely one of arsenic but of capacity of the villagers to cope with the problem (as outlined in the report by Ms Patel listed in the references).    Professor Feroze Ahmed has commented that if the deep well is truly below a thick clay layer, the clay should (soft) seal around the well.    Is this true?  always?  Sometimes?
(3)     These particular questions are avoided if  sanitary dug wells are used which have been shown to be arsenic free.    Measuring for coliform bacteria, to check on the sanitary conditions, is much more reliable than measuring arsenic concentrations, and cheaper.   Sanitary dugwells cost about twice as much as a deep tube well, but that cost may well be worthwhile.
==============================================================================================================
Professor Charles Harvey 

Professor Timir Hore
Dr Meera Smith
Professor J.M. McArthur  London
Columbia University
Richard Wilson, Harvard

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