The document discusses arsenic and fluoride contamination of drinking water. It provides background on sources of arsenic and fluoride in the environment and their health effects. It also describes various technologies for removing arsenic and fluoride from drinking water, such as iron nails in biosand filters and ion exchange resins. Guidelines for safe levels of arsenic and fluoride in drinking water from different organizations are presented.
Fluoride and Arsenic in Ground water.
Causes for groundwater pollution.
Fluoride in groundwater , sources for fluoride , Health implications.
Arsenic in groundwater , sources for arsenic , Health implications.
Structural and Geological Study of a part of the Chitradurga Schist BeltSai Bhaskar Reddy Nakka
Indian plate consists of several microplates, in the plate tectonic process they merged and disintegrated. The stable part of India i.e., Southern India, consists of several microplates, including the Eastern Dharwad and Western Dharwad in between lies the Chitradurga Schist belt. It has even the primordial rocks and rich in minerals. It was a pleasure to see the oldest rocks and understand all the structural changes happened in the history. This structural and geological study gives a glimpse into one of the oldest parts on earth. I am thankful to Prof. K. V. Subba Rao, a very well known Geologist of India for introducing me to this field area.
Key words: geology books, tectonic geomorphology, physical geology of India, minerals of India, plate tectonics and crustal evolution, Karnataka Geography, structural geology
Fluoride and Arsenic in Ground water.
Causes for groundwater pollution.
Fluoride in groundwater , sources for fluoride , Health implications.
Arsenic in groundwater , sources for arsenic , Health implications.
Structural and Geological Study of a part of the Chitradurga Schist BeltSai Bhaskar Reddy Nakka
Indian plate consists of several microplates, in the plate tectonic process they merged and disintegrated. The stable part of India i.e., Southern India, consists of several microplates, including the Eastern Dharwad and Western Dharwad in between lies the Chitradurga Schist belt. It has even the primordial rocks and rich in minerals. It was a pleasure to see the oldest rocks and understand all the structural changes happened in the history. This structural and geological study gives a glimpse into one of the oldest parts on earth. I am thankful to Prof. K. V. Subba Rao, a very well known Geologist of India for introducing me to this field area.
Key words: geology books, tectonic geomorphology, physical geology of India, minerals of India, plate tectonics and crustal evolution, Karnataka Geography, structural geology
GEOLOGICAL THERMOMETERS
DEFINITION AND CLASSIFICATION
Proper understanding of origin of mineral deposits and their classification requires the knowledge of formation-temperatures of these deposits. Certain minerals, present over there, give information’s with regard to temperatures of their formations and of the enclosing deposits and they are known as geological thermometers. These geological thermometers may be classed chiefly into the following groups based on their preciseness:
1. The thermometers that record fairly accurately the specific temperature condition of formation of deposits.
2. The thermometers that provide an upper or a lower temperature, above or below which the deposits do not form
3. The thermometers that provide a range of temperature within which the deposits form; and
4. The thermometers that serve as rough indications of temperatures of formation of mineral deposits.
The presence of two or more of less precise geological thermometers in a deposit narrows the range of temperature of formation for the deposits
THE PRESENCE AND VARIETY OF A PARTICULAR PLANTS
SPECIES IN THE AREA OF MINERALISATION HAVE BEEN RECOGNISED AS A GUIDE TO LOCATING ORE, METHOD,UNIVERSAL INDICATORS , UNIVERSAL INDICATOR ,LOCAL INDICATOR
The name ophiolite derived from Greek root which means
Ophio : snake or serpent Litho : Stone
The green colour, structure and texture of sheared ultramafic rocks is similar to some serpents
Economically :
Massive Sulphide
It founded within pillow lava most of massive Sulphide associated in ophiolites have well developed Gossans (bright colored iron oxide, hydroxides, and sulfides) which is very rich in gold.
Chromite
Stratiform (be tabular or pencil shape) or podiform (irregular shape) within ultra-mafic rocks
These deposits are developed on serpentinite peridotite
Laterites (nickel and iron)
Asbestos
Talc
Magenesite
ophiolite sequence :
Sediments
Pillow Lavas
Dykes
Gabbros
Layered Gabbro
Layered Peridotite
Upper mantle
Groundwater province is an area or region in which geology and climate combine to produce groundwater conditions consistent enough to permit useful generalisations.
SUPERGENE ENRICHMENT; Definition; Zones; Morphology of Zoning; Oxidized zone ; Supergene zone ; Gossans and Cappings; Chemical Changes Involved; Electrowinning; Formation of Copper Oxides
Dr. Jagannath Dinda
Chief Medical Officer of Health.Bankura
Office of the Chief Medical Officer of Health
Tamlibandh
Post + District : Bankura
Pin-722101
GEOLOGICAL THERMOMETERS
DEFINITION AND CLASSIFICATION
Proper understanding of origin of mineral deposits and their classification requires the knowledge of formation-temperatures of these deposits. Certain minerals, present over there, give information’s with regard to temperatures of their formations and of the enclosing deposits and they are known as geological thermometers. These geological thermometers may be classed chiefly into the following groups based on their preciseness:
1. The thermometers that record fairly accurately the specific temperature condition of formation of deposits.
2. The thermometers that provide an upper or a lower temperature, above or below which the deposits do not form
3. The thermometers that provide a range of temperature within which the deposits form; and
4. The thermometers that serve as rough indications of temperatures of formation of mineral deposits.
The presence of two or more of less precise geological thermometers in a deposit narrows the range of temperature of formation for the deposits
THE PRESENCE AND VARIETY OF A PARTICULAR PLANTS
SPECIES IN THE AREA OF MINERALISATION HAVE BEEN RECOGNISED AS A GUIDE TO LOCATING ORE, METHOD,UNIVERSAL INDICATORS , UNIVERSAL INDICATOR ,LOCAL INDICATOR
The name ophiolite derived from Greek root which means
Ophio : snake or serpent Litho : Stone
The green colour, structure and texture of sheared ultramafic rocks is similar to some serpents
Economically :
Massive Sulphide
It founded within pillow lava most of massive Sulphide associated in ophiolites have well developed Gossans (bright colored iron oxide, hydroxides, and sulfides) which is very rich in gold.
Chromite
Stratiform (be tabular or pencil shape) or podiform (irregular shape) within ultra-mafic rocks
These deposits are developed on serpentinite peridotite
Laterites (nickel and iron)
Asbestos
Talc
Magenesite
ophiolite sequence :
Sediments
Pillow Lavas
Dykes
Gabbros
Layered Gabbro
Layered Peridotite
Upper mantle
Groundwater province is an area or region in which geology and climate combine to produce groundwater conditions consistent enough to permit useful generalisations.
SUPERGENE ENRICHMENT; Definition; Zones; Morphology of Zoning; Oxidized zone ; Supergene zone ; Gossans and Cappings; Chemical Changes Involved; Electrowinning; Formation of Copper Oxides
Dr. Jagannath Dinda
Chief Medical Officer of Health.Bankura
Office of the Chief Medical Officer of Health
Tamlibandh
Post + District : Bankura
Pin-722101
Low Cost Design of Arsenic Removal from Groundwater in BangladeshKevin Banahan
Low-Cost Design of Arsenic Removal from Groundwater
Jeremy Kozub*, Kevin Banahan*, Jesse Amsel*
*Wentworth Institute of Technology, Environmental Engineering Program, Class of 2005 (Jack Duggan, Ph.D., P.E., faculty advisor)
For this project, a student team designed and evaluated treatment alternatives for the removal of arsenic from groundwater used in developing countries. The application of sorption technologies was evaluated using bench-scale testing of a range of sorption materials, support media and differing contact geometries. Sorption capacity of treatment units were designed to accommodate the daily consumption of individual families using a community well in Bangladesh.
Until the early 1990's, there was little awareness that groundwater in Bangladesh contained high levels of arsenic. The adverse health affects of chronic exposure to arsenic are well documented. Although current technologies to treat arsenic in groundwater exist, there are economic, social and cultural factors that prevent these technologies from being used in Bangladesh. This project focused on developing a low-cost alternative technology that could be readily assembled and implemented by local villagers.
As a capstone project for the environmental engineering program at Wentworth of Technology, this project has been performed by three students under the supervision of a faculty advisor. Students applied previous coursework in the areas of economics, engineering theory and application, design, communication skills and ethical principles to complete this project. The project was performed in collaboration with external non-profit and non-governmental organizations. The goal of this project is to further develop the creation of a low-cost system that will become available to large populations of those in need.
DENTAL FLUOROSIS: A CASE STUDY IN VAUVNIYA DISTRICT, DRY ZONE OF SRI LANKASivanesan Somanathar
Abstract: High fluoride contents in ground water are very big problem in the dry zone of Sri
Lanka. Fluoride and some other parameters determined in the ground water sample. Study has been
made of groundwater of 72 wells at five villages of the Vavuniya district in Northern Province, Sri
Lanka, with special focus on fluorine contamination. Study area 90 people were examined and 23 of
them were identified to be affected by dental fluorosis. The samples were collected on during the
period of February and March. Fluoride concentration was determined using UV visible
spectrophotometer and Field measurements of temperature, pH, and electrical conductivity were
made during sampling. Fluoride concentrations in the study area vary from 0.14 to 1.52 mg/L, water
table range from 3.9m to7.3m respectively. Electrical conductivity range from 120μs/cm to
1952μs/cm. out of the 72 wells only six wells were observed with higher F concentration than the
WHO standard maximum (1.5mg/L) level. However, F concentration of 32wells higher than the
desirable (0.6mg/L) level of WHO. Elevated fluoride concentrations in shallow groundwater in
intensive agricultural areas appear to be related to the leaching of fluoride from soils due to successive
irrigation and flooding time.
Kerala state is having abundant water source and people are really proud of it and lavishly wastes water.But due to the uprising scarcity of good potable drinking water we should think about conserving water before polluting the sources.This presentation is a description about the water scenario in India briefly and describes about the major water pollution and the main regions that are being affected severely.
Ground water Arsenic Contamination in IndiaDr Sayan Das
Extent, related research and remedication meassures
Chemistry of arsenic, Use of arsenic, reference value , Oxidation method, Ion exchange method, Membrane method
Arsenic is a heavy metal occurring naturally in the environment. It's low concentration is important for various life processes on the Earth but the misuse and overexploitation of mineral resources caused the arsenic contamination to natural resources, which in turn get exposed to living beings causing various toxicity problems and severe health issues. Arsenic has not remained an important mineral for sustaining life but it becomes a category pollutant for which heavy precautions should be taken to avoid an exposure.
2. 2007-07 Zheng Gong, MIT department of Civil and Environmental Engineering, August 2005 Over 30 countries in the world is affected by arsenic in drinking water
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5. 2007-07 Baseline Arsenic in the Environment Water Source Typical baseline concentrations Atmospheric precipitation (rain and snow) Usually < 0.03 ug/L River water Usually < 2 ug/L Lake water Usually < 1 ug/L Seawater Usually about 1.5 ug/L Groundwater Usually < 10 ug/L
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7. Chronic Health Effects Source: Harvard University. “Harvard Arsenic Project.” Internet. Accessed Sep 27, 05. http://phys4.harvard.edu/%7Ewilson/arsenic/arsenic_project_introduction.html After melanosis, keratosis and other lesions may occur Keratosis is the hardening skin bulges on palms and feet
8. 2007-07 Guideline Value in Drinking Water WHO 10 ug/L(ppb) = 0.01 mg/L (ppm) Australia 7 ug/L Canada 25 ug/L EU 10 ug/L Japan 10 ug/L USA 10 ug/L Bangladesh 50 ug/L Cambodia 50 ug/L China 50 ug/L India 50 ug/L Lao 50 ug/L Myanmar 50 ug/L Nepal 50 ug/L Pakistan 50 ug/L Vietnam 10 ug/L urban, 50 ug/L rural Source: World Bank. Towards a More Effective Operational Response. Volume 1. 2005
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11. Diffuser Basin Brick Chips / Iron Nails Outlet Pipe Filter Lid Fine Sand Layer Standing Water Layer Separating Gravel Under drain Gravel
12. THE REMOVAL OF ARSENIC By adding 5 kg (11lbs) of small non-galvanized iron nails, covered by a layer of brick chips, the Biosand filter can remove a certain level of arsenic from water. This is accomplished by replacing the diffuser plate with a deep diffuser basin. The iron nails in the diffuser basin, after contact with water and air, will quickly rust. Iron rust (ferric hydroxide) is an excellent adsorbent for arsenic. When arsenic-containing water is poured into the filter, surface reactions with iron occurs, and arsenic is rapidly adsorbed onto the surface of ferric hydroxide particles . The arsenic loaded iron particles are then flushed down and trapped on top of fine sand. The purpose of the brick chips is to disperse the water over the nails to allow for further absorption.
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14. 2007-07 Diffuser Basin Lid Container Pipe Kanchan TM Arsenic Filter Components Gravel Coarse Sand Water Fine Sand Iron Nails Brick chips
17. 2007-07 Arsenic Symptoms, Diagnosis and Treatment UPdate Summer 2002 Diagnosis of arsenic poisoning, especially from low doses of inorganic arsenic, the type found in CCA lumber, is not easy. There is no one set of symptoms. Different people respond differently, depending on how much exposure they get, and by what means. Arsenic can be inhaled, ingested (swallowed) or absorbed through contact. Arsenic poisoning is difficult to pin down because most of the arsenic leaves the body within three days of exposure. The arsenic which remains is stored in the brain, bones, and tissue and continues to do serious damage. Some people have no immediate symptoms, but the exposure can cause many types of cancer or diabetes later on. T There is new evidence that arsenic may also lead to heart disease or strokes. It may cause long term liver, kidney, and central nervous system damage.
18. Arsenic exposure, even at low levels, can result in a range of symptoms. Swallowing or inhaling low levels of inorganic arsenic can result in stomach ache, nausea, vomiting and diarrhea. It can also result in decreased production of red and white blood cells which may cause fatigue, abnormal heart rhythm, blood-vessel damage resulting in bruising, and impaired nerve function. One of the early warning signs of arsenic poisoning is a "pins and needles" sensation in hands and feet. Long-term oral exposure to inorganic arsenic can result in skin changes including a darkening of the skin and the appearance of small "corns" or "warts" on the palms, soles, and torso.
19. 2007-07 Other signs and symptoms include skin thickening, fluid accumulation (resulting in puffiness) especially around the lower eyelids, face and ankles, diarrhea, garlic breath, perspiration, excessive salivation, generalized itching, oral inflammation, sore throat, runny nose, excessive tearing, numbness, skin inflammation, hair loss, weakness, and loss of appetite. Arsenic can also cause a range of neurological effects, including headaches and vision problems. It can cause noticeable behavioral changes, most commonly aggression or depression.
20. 2007-07 Because most arsenic leaves your body within a few days, analysis of urine cannot detect if a person was exposed to arsenic in the past. Tests of hair or fingernails can determine exposure to high levels of arsenic over the past 6-12 months, but these tests are not very useful in detecting low-level exposures. Early treatment of arsenic poisoning is critical. The longer arsenic remains in the body, the more damage is done. If arsenic poisoning is determined, oxygen therapy, chelation therapy, saunas and other methods used for detoxification of heavy metals is the usual treatment. There is some new information that selenium may help decrease the effects of arsenic. Naturopaths may be able to help with diagnosis and treatment with other methods.
Instructor Notes Introduce This module looks at the incidence of water-related disease, and the types of pathogens that cause it. as the caption under the title indicates, we are going to look at the cause of diseases “bad bugs”!