The traditional water deducting techniques are not always reliable as it depends very much on the experience/skills of the individual. In these circumstanceswest
- I have tried this personally but I did not check the availability of water. But the person who informed me the technique claims that the water is found !
Take a full coconut after removing the bulky fibre. Leave little fibre almost in a triangular look at the top.There will be two or three black spots on the coconut at this place.
Now keep lower arm up in L shape & palm unfolded
Keep your palm almost flat. No curving of fingures.
Now place the coconout on your palm ( O> like this ) .
Now slowly move by walking, keeping your hand in " L " Shape. You will find that the coconut will lift on its own when you come across the water current. That is, the bowl shaped coconut bottom on your palm and the pointer will be towards the sky. ^
Where there is more water current it will lift up fully. If you move slowly backwards, the coconut will come to the resting point. The same effect will be there if you try in third floor of your apatrtment.( Not tried in wooden Floors )
One has to be little patient while doing this experiment. Repeat it and do not give up.
It is noticed that few people do not get response from the coconut. I do not know why.
Pl try and report your feed back and if possible the finding of water. But this way also some farmers have succeeded in finding water.
E9 - Methods for finding underground water and water tables
This method is mainly used in developing countries or other regions where water is rare and where irrigation is essential for crops. It is also used in developed countries but mainly for uses other than direct consumption (gardening, geothermal energy).
Groundwater is usually good-quality water. As it is often buried at significant depths, it is highly advisable to locate it as precisely as possible and assess its quantity and quality before undertaking costly drilling work and thus avoid costly failures.
This water can be detected with more or less precision depending on the methods used, through the electromagnetic waves it emits.
It particularly concerns regions prone to severe droughts. Indeed, aquifers are natural underground reservoirs capable of supplying large quantities of drinking water during the dry season, when rivers are likely to dry up.
The purpose of this document is not to give detailed explanations of the mode of operation and use of the various techniques, as most of them are fairly costly and can only be used by specialists. Instead, it aims to explain the principle and main advantages and drawbacks of the techniques, so that the communities and people concerned can find out about their main characteristics and be able to contact specialised companies, having gained better knowledge of the facts.
The search for groundwater sources must take account of technical (hydrogeological) criteria as well as socio-economic criteria (closeness to a village, cost of investigation). In actual fact, closeness to the beneficiaries often remains the prime criterion.
There are various methods for investigating phreatic layers. Traditionally, dowsing was the only way of searching for groundwater. Subsequently, more modern and scientific techniques were developed, significantly improving the success rate of water collection facilities.
a) Preliminary surveyIt is highly advisable for phreatic layer investigators, especially if they are not from the region concerned, to carry out preliminary surveys in order to collect information which can give them precious data on the places where there is a likelihood of finding water.
Depending on the size of the expected source, this can consist of either :
- after a first look at the site and a meeting with the chiefs or heads of the villages, a survey with their population to find out where wells would have been dug or where springs would have been used, where the vegetation is greenest and remains green during the dry season, where trees and plants naturally grow best, where the existing water sources have the highest outflow in all seasons, where the termite mounds are located, if any, etc.
- or, at the same time, research into the region’s geological map, climatic data and all appropriate information which may be obtained from the local or regional authorities or other organisations or operators working in the region.
b) DowsingIn numerous countries (including France), certain people have the ability to investigate and determine the presence of water on a site and detect water channels (veins, faults and aquifers).
These "dowsers" are often people who have special abilities passed down by their predecessors or a village wise man or woman.
The principle consists in :
- Choosing a forked or Y-shaped twig from a tree such as a mango tree or using metal rods
Use of a forked twig by a dowser in
Burkina Faso - Photo Sogreah
- Positioning the twig or rods between the fingers so as to amplify the sensations felt and seeing if they twitch and go down (or cross) at the expected place.
- Criss-crossing the area in order to determine the most promising areas.
There are different types of divining rods :
- The Y-shaped or V-shaped twig
- Metal rods
- Parallel rods
- The Hartmann lobe
- The Lecher antenna
When the dowser uses metal rods, he holds them parallel between his fingers. When he comes close to a place under which there is water, the rods get closer together and end up crossing over one another where a groundwater source is significant. This can be tested and proves successful with many people, but the findings are imprecise and do not indicate the size of the aquifer.
Moreover, this method doesn’t make it possible to detect small, relatively deep groundwater flows.
c) Modern methodsThese methods make it possible to locate aquifers with more precision, and they are much more efficient in assessing their size, volume, quality and sustainability.
Analysing maps and local vegetation gives a first indication of the presence of water. In the case of large-scale investigations, a global geological analysis can even be carried out through the interpretation of satellite images or aerial photos. These can highlight the presence of the major geological outlines liable to give rise to fractures with an identifiable direction or outcrops.
Geophysical methods are now the main methods of investigation and detection of underground aquifers. The method chosen mainly depends on the geological context.
Traditional geophysical methods
A material’s electrical resistivity is its capacity to oppose the flow of electric current.
These methods are thus based on the capacity of the soil or rock to conduct electricity and the measurement of their conductivity or resistivity (the opposite of conductivity).
From these measurements, the type, size and quality of the aquifer is deduced and specified, or perhaps only presumed, but with a high probability.
There are two main types of methods, which are sometimes used successively :
a) The measurement of electrical resistivity using direct current.
It consists in sending direct current into a geological structure on a given site (50 to 400 volts depending on its resistivity - conductivity) using two electrodes (A and B).
There are several possible electrode arrays (Wenner, Schlumberger, 4 terminals, etc.).
The area investigated must not be too large and must be relatively flat and free of buildings which may cause interference and would make it impossible to have AB lines of the required length (over 300m).
b) Methods for measuring this reactivity by magnetic means
Easier to implement, such as the Slingram and VLF methods, these methods measure electromagnetic signals due to magnetic induction phenomena. They don’t need any contact with the ground and thus no electrodes. They make it possible to measure the soil’s reactivity to electromagnetic excitation. However, they cannot be used on all types of grounds or for aquifers over 20 metres deep, or even less. Their use seems to have dwindled.
Proton Magnetic Resonance (PMR)
Search for water using the magnetic
resonance method in Tchad
Photo Iris Instrument
This is a direct water detection method. It consists in sending electric currents into the ground, then measuring the signals emitted by the nuclei of hydrogen atoms in water molecules. It requires sophisticated equipment including proton magnetometers which can measure electromagnetic fields ; their recordings can be interpreted on site and, most importantly, the quantity of groundwater present in the rock can be deduced in a few seconds.
The isotope method
This method is mainly useful for tracing the water flow and to estimate the age of the groundwater. We know that the phreatic layer is renewed by the infiltration of water through the inflow area, where the aquifer’s geological structure is exposed to the surface. Investigations using the isotope method can often give useful indications.
If there are infiltrations, they can be detected and assessed by analysing the variations in the isotope content of the damp soil above the phreatic layer. The most used isotopes are tritium, deuterium, oxygen 18 and carbon 14. The results have shown that this method is reliable and promising, in particular if it is used with the physical models describing the water flow.
- To avoid considerable risks, it is indispensable to call on the services of hydrogeophysics experts for major drilling work.
Indeed, it is essential to have highly sophisticated equipment and to know how to maintain it, and to have solid knowledge and experience.
a) AdvantagesThese methods sometimes avoid serious or costly errors in groundwater investigation and save both time and money.
Preliminary on-site surveys and dowsing provide interesting indications at a very low cost when little means are available.
The methods based on electrical resistivity and conductivity are much more precise and offer great spatial measurement density, which will allow relatively detailed exploration. They make it possible to detect indirect signs of the presence of water.
Search for an aquifer via a geophysical study in Namou
Kounlogue, Togo - Photo Cartas Togo
The PMR method is an innovative, rapid method for the direct detection of the presence of water. Its use is expanding.
b) DrawbacksMost of the time, operations based solely on a dowser’s findings do not bear fruit or the findings are too imprecise.
What’s more, the effectiveness of a type of operation is difficult to assess since situations are rarely comparable.
Moreover, the use of this equipment presents drawbacks : it only allows detection down to a certain depth and the indications may be distorted by the presence of electromagnetic signals or electric lines.
Modern hydrogeophysics techniques are costly. They can only be used for the set-up of large or numerous water extraction facilities for which large budgets are available.
While the cost of a dowser is low (a few tens of euros), the cost of using modern methods is much higher and depends on the situations encountered and the methods used. It always amounts to several tens of thousands of euros.
Dowsers’ rates vary according to countries, the dowser’s experience and travel expenses. For instance, the dowsers of Dapaong in Togo charge between €80 and €160 for their services.
The cost of machines which take hydrogeophysical measurements depends on the size of the machine, maintenance costs and training costs. These costs are difficult to assess with precision as their is little information on the remuneration of aquifer investigation specialists, on the method(s) they use and on the type of area studied.
Other costs include the transportation of equipment to the sites and accommodation and meals for the team of technicians.
It is generally accepted that the search for a drilling site should not exceed 20% of the cost of the drilling operation itself.
In Chad, over 300,000 refugees from neighbouring countries have settled in the east of the country, where water was already in very short supply.
PMR instrument - Photo IRIS Instruments
In order to find new water resources, several NGOs including OXFAM and UNHCR (UN Refugee Agency) have been working in partnership with Iris Instruments, a French company which manufactures equipment and provides training.
The main method used has been that of magnetic resonance imaging : by sending electric currents into the ground, it makes it possible to detect hydrogen atoms and determine the quantity of water present in the rock, provided the water is less than 150 m deep, which was the case in Chad.
Several aquifers were thus found around Iriba.
A complete magnetic resonance kit weighs around 350 Kg and costs about €140,000.
a) Websites- IRIS : 3-page article, "TCHAD_ Faire une radiographie du désert pour trouver de l’eau",
explaining the magnetic resonance method for finding water and how it was used in Chad (mentioned in item 9 as a good practice) :
Available online at : http://www.irinnews.org/fr/ReportFr...
- International Office for Water : brings together the work documents (title/author/country) focusing on water or sanitation research :
Available online at : http://www.oieau.fr/ciedd/contribut...
- RWSN (Rural Water and Sanitation Network). This Swiss NGO published a noteworthy document in collaboration with with UNICEF : "Cartographier les zones favorables au forage manuel". Available online at :
- PS Eau-AFD : "Réalisation et gestion des forages équipés d’une pompe à motricité humaine en Afrique subsaharienne" 6 pages (22 to 27) of this illustrated 86-page brochure on drilling techniques and installations deal with the problem of the search for water and positioning of water points. Available online at :
- International Atomic Energy Agency website : The article presents the isotope method through the investigation of water resources in the desert :
Available at : http://www.iaea.org/Publications/Ma...
- Thesis presented by Ghislain Toé “Apport de nouvelles techniques géophysiques à la connaissance des aquifers de socle”, on the use of new geophysical techniques in Burkina Faso, a preparatory document for a Doctorate from Université Paris 6, June 2004, 274 pages :
Available online at : http://horizon.documentation.ird.fr...
- Teaching site of the University of Strasbourg : presentation on hydrogeophysics :
Available at : http://phineas.u-strasbg.fr/marquis...
- JCRC, Japanese site : "Guide technique du développement des ressources en eau", 50 pages in French comprising several chapters, including one on groundwater investigations methods ; the other chapters focus on the problems to be examined before seeking to develop water resources, the ways of taking stock of existing resources and
how to build surface dams.
b) VideoDaily motion : Short video (2 min) on how to find a water source, showing how a dowser can find groundwater using simple rods.
Available online at : http://www.dailymotion.com/video/x4...
c) Bibliography- Action Contre la Faim : "Eau - Assainissement – Hygiène pour les populations à risques"
Comprehensive 745-page book published by Hermann 6 rue de la Sorbonne 75 006 Paris (€50) explaining and illustrating the various methods used by ACF to provide access to water and sanitation ; pages 131 to 173 focus on the search for aquifers, a topic which is well covered with detailed explanations and numerous examples and illustrations of the various existing methods.
- MARGAT, J. : “Les resources en eau. Conception, évaluation, cartographie, comptabilité.”
146-page book published by FAO/BRGM, in the collection Manuels et Méthodes, n°28, Orléans, France. It explains the need to adopt a prospective approach in order to avoid water crises.
- CINAM (Cie d’études industrielles et d’aménagement-Montpellier) : training booklet for trainers "Le point d’eau au village" containing numerous factsheets on wells, pumps, hygiene, latrines as well as 4 factsheets (2.1 to 2.4) on the search for aquifers. Available online at :