Dugwells vs. Shallow
Tube well
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
Home
.