General Information
Introduction to BARTs | BART Application Guide | BART User Manual | Technical Information (QC) |
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BART Worksheet | BART Software | Quickbreak Training Guides |
Introduction to BARTs | BART Application Guide | BART User Manual | Technical Information (QC) |
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BART Worksheet | BART Software | Quickbreak Training Guides |
Iron Related Bacteria, IRB-BART Quality Control
Iron is well known to be a critical substance for all life. In animals, it is a common part of the mechanisms for moving oxygen throughout the living body. Because iron plays such an important function in the energy metabolism, there is considerable biological competition for iron. Microorganisms also compete for iron and the use of various types of proteins called siderophores (e.g., hydroxamates and catechols). Additionally, many bacteria can also bind ferric (Fe+++) ions into chelating structures know as ligands. This means that many bacteria are able to bind and hold iron in many forms to make large iron-rich structures that are sometimes seen as encrustations, tubercles and bog iron ore deposits. Little is known of the possible use of this iron to generate electro-motive forces (EMF) as a part of the growth of these iron-related bacteria. There is one group of bacteria, called the magnetotactic bacteria, which actually posses small magnet-like structures ( magnetosomes) and are able to sense magnetic fields. So complex are these various biochemical systems for holding onto iron, the precise nature of these events remain only partially understood. However, there are many bacteria which can continue to accumulate iron to the point that the growth becomes almost saturated with oxidized iron and forms a hardening clog or encrustation. Such mineralizing growths may also incorporate carbonates and sulfides with a high iron content (going from 1% up to as high as 40% dry weight) and reducing organic content (declining to as low as <1% organic carbon). The formation of hardening clogs/encrustations can seriously impair the designed hydraulic characteristics of the infested region, causing degenerated water quality and production capacities. In using the IRB-BART to examine waters for the presence of iron-related bacteria, it has to be remembered that iron bacteria grow predominantly on surfaces and not directly in the water. When testing water, the BART user has to assume that the IRB have detached, are suspended, and possibly are active in the water. As a consequence of this problem, there is a potential for an IRB-BART to give a "false" negative since the IRB are absent from the water but are present on the surfaces over which the water is flowing towards the sampling site. To get IRB to release and enter the flowing waters, it is necessary to cause a shift in the local environment that will make the conditions more hostile to the IRB. This is easily done by changing the pumping conditions (e.g., turn the pump off for a day if it is an active well) or applying a mild chemical shock using something like a low-dosage hypochlorite. IRB infestations usually occur in the presence of oxygen and so may be more readily seen as slimes, clogs or encrustations. Over the century, these growths have had two common features: the presence of high concentration of ferric (Fe+++) and of high populations of IRB (either as stalked Gallionella, the sheathed IRB or the heterotrophic IRB). The seriousness of these growths in engineered structures has led to the use of the term "Iron Bacteria." Recent research has shown that these bacteria are able to shunt the iron through oxidative and reductive states through ferric (Fe+++) and ferrous (Fe++) forms respectively. The BART biodetector is designed for the detection of these bacteria and is able to perform both the oxidative and reductive based reactions involving iron. This comprehensive group is known as the "Iron-related Bacteria" (IRB). The medium selected for the culture of the IRB is based on an original formulation developed by Sergei Winogradsky in which the major form of iron is presented as ferric ammonium citrate. The IRB-BART thus provides the major carbon (citrate), nitrogen (ammonium) and iron (ferric) from the same complex chemical form. When the crystallized pellet in the base of the test vial begins to dissolve after the sample has been added, a complex series of reactions occur. These reactions are influenced by both the chemical and biological composition of the sample and the redox and nutrient gradients created in the BART test. Under sterile conditions, a sample may be expected to cause a gradual dissolving of the nutrients from the pellet with the formation of a colored transparent diffusion front which gradually ascends through the fluid column until all of the liquid medium has a similar color. Where there has not been any major chemical reaction and the sample contains some oxygen (oxidative), the resultant color can generate yellow. If the sample is reductive (devoid of oxygen) and contains a relatively high calcium-magnesium concentration, the diffusion front may become a transparent green color. RPS (reaction pattern signatures) revolve around a complex pattern of signals which are generated when the IRB in the water sample begin to utilize the nutrients and manipulate the ferric form of iron present in the base of the inner BART test vial. Common events range from: - gas formation (common where anaerobic conditions exist), Careful QC is employed during manufacturing to ensure that the ferric ammonium citrate yields a consistent reproducible response to the various test cultures. Iron-related bacteria (IRB) are difficult to enumerate since they are subdivided into a number of groupings (e.g., iron oxidizing and iron-reducing bacteria). These bacteria function under different Redox conditions and utilize a variety of substrates for growth. By the routine (e.g., monthly) testing of water or wastewater using this technique, the levels of ggressivity, possible population and community structure (RPS) can all be determined. The status of an iron-related bacterial population within a given sample can be determined and related to any biofouling in the surrounding environment. To conduct the test, it is necessary to add 15ml of the sample to the biological activity reaction test biodetector. The ball floats up and restricts the entry of oxygen into the liquid medium. At the same time, components in the modified Winogradsky selective culture medium for IRB begin to diffuse upwards into the sample from a dried medium pellet in the base of the biodetector. Two gradients form within the fluid column: nutrients diffusing upwards, and oxygen diffusing downwards. These gradients form a variety of different habitats in which IRB can flourish. The color displayed by microbial activity may be a result of the form into which the ferric iron becomes modified in the medium. It should be noted that, in a biologically active BART tester, the ferric form of the iron added with the selective Winogradsky medium will revert to the ferrous form along the reductive (lower) part of the redox gradient. Commonly, where there is a radical reduction of the ferric form to the ferrous during the early phase of an IRB-BART test, the color of the diffusing medium in the bottom of the BART tester may shift from a yellow to a green. This should be considered negative unless this "greening" at the base of the inner test vial is accompanied with clouding. Reaction Patterns BC Brown Cloudy (Reaction 4) BG Brown Gel (Reaction 3) BL Blackened Liquid (Reaction 10) BR Brown Ring (Reaction 4) CL Cloudy Growth (Reaction 2) FO Foam (Reaction 5) GC Green Cloudy (Reaction 8 & 9) RC Red Cloudy (Reaction 7) Each of the reactions has been produced in a unique manner by the various species and consortia of bacteria becoming active in the test. There is, therefore, no specific form of any reaction pattern because these are controlled by the form of bacterial growths. Below is listed the descriptions for each of the IRB-BART test reactions. CL - Clouded Growth BG - Brown Gel BC - Brown Cloudy FO - Foam Do not confuse this reaction with the generation of bubbles (usually randomly) when oxygen supersaturates as the sample temperature comes up from a lower temperature (of the sample's source). These bubbles are recognized as being reflective and not bound in any slime and dispersed within the inner test vial under the ball and on the walls. They usually disappear within two days. This FO reaction is most commonly related to a sample in which many microbes are functioning anaerobically. It can often be "harmonized" with the presence of SRB (reactions BB, BT or BA). In other words, the occurrence of a FO in the IRB-BART can often be followed by a positive detection of SRB in the SRB-BART if that test has been performed on the same sample. RC - Red, Slightly Clouded BR - Brown Ring GC - Green Clouded BL - Blackened Liquid Other reactions not coded are described below. These reactions occur less than 1% of the time in water testing using the IRB-BART. If "fuzzy" growths form around the ball in the IRB-BART, then it is probable that the a water sample had traveled through a semi-saturated zone where there was fungal activity. These create reaction 13 in which a white, grey or speckled "fuzzy" mat forms around and even over the ball. The upper surface of the mat often forms into a tight mass with an irregular surface. The lower surface of the mat can often be seen to be extending into the liquid medium by thread-like processes 2 to 5 mm in length. These growths may bio-lock the ball to the wall of the inner test vial for a period of time. Solution usually remains fairly clear but globular-like deposits may be present. Solution may cloud over time. This reaction is caused by the presence of large populations of fungal spores in the water. RPS (Reaction Pattern Signatures)
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