Groundwater: Difference between revisions
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In the shallow aquifers where generally groundwater is located, typically, there is soil, sand, plant roots, hardpan and low permeability bedrock. | In the shallow aquifers where generally groundwater is located, typically, there is soil, sand, plant roots, hardpan and low permeability bedrock. | ||
===Temperature=== | |||
The temperature of groundwater is quite steady because the specific heat capacity of water is high and also because the soil, rock and up layer water protect groundwater from heat changing with the climate. | The temperature of groundwater is quite steady because the specific heat capacity of water is high and also because the soil, rock and up layer water protect groundwater from heat changing with the climate. | ||
===Hydrogeology=== | |||
Groundwater is relatively stable compared to surface water. In the aquifer and other porous media, groundwater not only follows gravity, but also follows pressure gradients. The movement of groundwater also depends on the porosity, water content and hydraulic conductivity of aquifer. | Groundwater is relatively stable compared to surface water. In the aquifer and other porous media, groundwater not only follows gravity, but also follows pressure gradients. The movement of groundwater also depends on the porosity, water content and hydraulic conductivity of aquifer. | ||
[[Image:plume1.jpg|thumb|300px|right|groundwater contaminatioin plume, from earth science australia.]] | [[Image:plume1.jpg|thumb|300px|right|groundwater contaminatioin plume, from earth science australia.]] | ||
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===Bacteria=== | ===Bacteria=== | ||
Gram-negative bacteria are found extensively in groundwater system. Balkwill (1989) studied the aerobic, chemoheterotrophic bacteria in deep aquifers and other subsurface sediments at a site in South Carolina. They found that 95% of the platable colonies contained nonstreptomycete bacteria, more than 80% of which were gram-negative rods. Gram-positive bacteria are not many in groundwater system; however, the gram-positive bacteria include many important human pathogens such as micrococcus, staphylococcus, and streptococcus. | Gram-negative bacteria are found extensively in groundwater system. Balkwill (1989) studied the aerobic, chemoheterotrophic bacteria in deep aquifers and other subsurface sediments at a site in South Carolina. They found that 95% of the platable colonies contained nonstreptomycete bacteria, more than 80% of which were gram-negative rods. Gram-positive bacteria are not many in groundwater system; however, the gram-positive bacteria include many important human pathogens such as micrococcus, staphylococcus, and streptococcus. | ||
===Virus=== | |||
It is estimated that 65% of the water borne disease are caused by enteric viruses. For example, norovirus (also known as Norwalk agent) causes approximately 90% of epidemic non-bacterial outbreaks of gastroenteritis around the world. Infectious hepatitis is the most intensively studied disease that is caused by water borne virus. Virus adsorption to soils and other solids could prolong survival of viruses in the groundwater. Research showed that Viruses originating from wastewater infiltration units are able to migrate horizontal in groundwater for hundreds of meters and vertically as great as 67 meters. | It is estimated that 65% of the water borne disease are caused by enteric viruses. For example, norovirus (also known as Norwalk agent) causes approximately 90% of epidemic non-bacterial outbreaks of gastroenteritis around the world. Infectious hepatitis is the most intensively studied disease that is caused by water borne virus. Virus adsorption to soils and other solids could prolong survival of viruses in the groundwater. Research showed that Viruses originating from wastewater infiltration units are able to migrate horizontal in groundwater for hundreds of meters and vertically as great as 67 meters. | ||
===Eucarya === | |||
Groundwater eukaryotes are comprised of many species, range from single-celled heterotrophic nanoflagellates and fungi to amphipod crustaceans. The location of groundwater eukaryotes might be close to the vadose (unsaturated) zone, the soil or the bottom sediments of surface waters. | Groundwater eukaryotes are comprised of many species, range from single-celled heterotrophic nanoflagellates and fungi to amphipod crustaceans. The location of groundwater eukaryotes might be close to the vadose (unsaturated) zone, the soil or the bottom sediments of surface waters. | ||
===Archaea=== | ===Archaea=== | ||
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Both bacteria and archaea are able to carry out ammonia oxidation in the groundwater. The ammonia oxidation rate is limited by the available oxygen. | Both bacteria and archaea are able to carry out ammonia oxidation in the groundwater. The ammonia oxidation rate is limited by the available oxygen. | ||
===Denitrification=== | |||
Denitrification reduce nitrate in the groundwater. Denitrifying bacteria Burkholderia, Bacillus, and Pseudomonas play an important role in groundwater. | Denitrification reduce nitrate in the groundwater. Denitrifying bacteria Burkholderia, Bacillus, and Pseudomonas play an important role in groundwater. | ||
===Manganese, Iron and sulfate Reduction=== | |||
Anaerobic condition is dominant in groundwater. In anaerobic zone, microbial communities could carry out decomposition through Manganese, Iron and sulfate reduction. | Anaerobic condition is dominant in groundwater. In anaerobic zone, microbial communities could carry out decomposition through Manganese, Iron and sulfate reduction. | ||
Revision as of 04:31, 5 April 2011
Introduction
Surface water moves downward through unsaturated zones –typically tiny pores and cracks in the soil, sand, or rock, and then reaches a stable and completed water saturated layer named water table. Groundwater is beneath the water table. Groundwater provide about 0.6 percent of the world’s total water and 20 percent of the available fresh water resources. Microbial organisms play important role in groundwater ecosystem and affect drinking water quality significantly. Microbial contamination of groundwater is a big concern.
Physical environment
Substrate and sediment
In the shallow aquifers where generally groundwater is located, typically, there is soil, sand, plant roots, hardpan and low permeability bedrock.
Temperature
The temperature of groundwater is quite steady because the specific heat capacity of water is high and also because the soil, rock and up layer water protect groundwater from heat changing with the climate.
Hydrogeology
Groundwater is relatively stable compared to surface water. In the aquifer and other porous media, groundwater not only follows gravity, but also follows pressure gradients. The movement of groundwater also depends on the porosity, water content and hydraulic conductivity of aquifer.
Groundwater contamination
Pollutants, such as gasoline, oil, road salts and chemicals seep into groundwater can hurt animals, plants, or humans. Two major contaminate sources are Hazardous waste site leaking and landfills. Since groundwater is part of hydrologic cycle, contaminates released to the groundwater could create a contaminant plume within an aquifer and also can be transferred to the other parts of the cycle.
Microorganisms
Bacteria
Gram-negative bacteria are found extensively in groundwater system. Balkwill (1989) studied the aerobic, chemoheterotrophic bacteria in deep aquifers and other subsurface sediments at a site in South Carolina. They found that 95% of the platable colonies contained nonstreptomycete bacteria, more than 80% of which were gram-negative rods. Gram-positive bacteria are not many in groundwater system; however, the gram-positive bacteria include many important human pathogens such as micrococcus, staphylococcus, and streptococcus.
Virus
It is estimated that 65% of the water borne disease are caused by enteric viruses. For example, norovirus (also known as Norwalk agent) causes approximately 90% of epidemic non-bacterial outbreaks of gastroenteritis around the world. Infectious hepatitis is the most intensively studied disease that is caused by water borne virus. Virus adsorption to soils and other solids could prolong survival of viruses in the groundwater. Research showed that Viruses originating from wastewater infiltration units are able to migrate horizontal in groundwater for hundreds of meters and vertically as great as 67 meters.
Eucarya
Groundwater eukaryotes are comprised of many species, range from single-celled heterotrophic nanoflagellates and fungi to amphipod crustaceans. The location of groundwater eukaryotes might be close to the vadose (unsaturated) zone, the soil or the bottom sediments of surface waters.
Archaea
Groundwater Archaea have been found throughout depths of several thousand meters. Ammonia-Oxidizing Archaea and methanogenic Archaea are two major groups in the groundwater.
Microbial processes
Ammonia oxidation
Both bacteria and archaea are able to carry out ammonia oxidation in the groundwater. The ammonia oxidation rate is limited by the available oxygen.
Denitrification
Denitrification reduce nitrate in the groundwater. Denitrifying bacteria Burkholderia, Bacillus, and Pseudomonas play an important role in groundwater.
Manganese, Iron and sulfate Reduction
Anaerobic condition is dominant in groundwater. In anaerobic zone, microbial communities could carry out decomposition through Manganese, Iron and sulfate reduction.
Dehalogenation
Synthetic halogenated organic compounds in the groundwater could persist for very long time and are recognized as a serious health concern. Dehalogenation removes halogens from organic compounds. Anaerobic dehalogenation reactions can effectively degrade a wide variety of halogenated contaminants in ground water.
Current Research
Groundwater treatment
1. W.W.J.M de Vet et al characterized the microbial populations in groundwater sources and sand filters for drinking water production. They found that both bacteria and archaea, especially Nitrospira, are important in ammonia nitrification. No nitrifying organisms were detected in subsurface aerated groundwater; therefore, the nitrifying capacity is low. Iron-oxidizing bacteria Gallionella ferruginea was detected in subsurface aerated groundwater. It indicted the iron oxidation could be existed and thereby could improve nitrification in groundwater.
2. Sven Jechalke et al developed a novel aerated treatment pond for enhanced biodegradation of groundwater contaminants. They use coconut fibre and polypropylene textiles to grow contaminant-degrading biofilms. The results showed that the efficiencies for benzene, MTBE and COD were 99.9%, 38% and 61% respectively. Ammonium degradation rates were low.
Groundwater contamination
3. Amitabha Mukhopadhay et al drilled 29 monitoring well across urban Kuwait City and analyzed inorganic and organic constituents including isotopic composition. They found that one well is highly contaminated in terms of total coliform bacteria, fecal coliform bacteria and boron concentration. Another well is significantly contaminated. Three wells might be contaminated, and seven well were not contaminated.
Detection of groundwater contamination using microbial community profiles
4. Paula J. Mouser proposed a novel groundwater contamination detection method. They characterized bacteria, archaea and family Geobacteraceae in the contaminated groundwater by using T-RFLP. By knowing the information of microbial communities in the groundwater, they stated that this method is able to detect groundwater contamination.
References
Edited by <your name>, a student of Angela Kent at the University of Illinois at Urbana-Champaign.