Areas of the world with high naturally occurring arsenic levels in the groundwater. Arsenic poisoning is casarett and doull’s toxicology 8th edition pdf free download medical condition that occurs due to elevated levels of arsenic in the body. The most common reason for long-term exposure is contaminated drinking water.
Prevention is by using water that does not contain high levels of arsenic. This may be achieved by the use of special filters or using rainwater. There is not good evidence to support specific treatments for long-term poisoning. Through drinking water, more than 200 million people globally are exposed to higher than safe levels of arsenic. The areas most affected are Bangladesh and West Bengal. Symptoms of arsenic poisoning begin with headaches, confusion, severe diarrhea, and drowsiness.
Chronic exposure to arsenic is related to vitamin A deficiency, which is related to heart disease and night blindness. Arsenic increases the risk of cancer. Exposure is related to skin, lung, liver, and kidney cancer among others. Its comutagenic effects may be explained by interference with base and nucleotide excision repair, eventually through interaction with zinc finger structures.
DNA single strand breaks resulting from inhibition of repair enzymes at levels of 5 to 100 mM in human epithelial type II cells. Resulting metabolites are the dimethylarsenic radical and the dimethylarsenic peroxyl radical. Thus, formation of ROS can be promoted. Regarding DNA methylation, some studies suggest interaction of As with methyltransferases which leads to an inactivation of tumor suppressor genes through hypermethylation, others state that hypomethylation might occur due to a lack of SAM resulting in aberrant gene activation. An experiment by Zhong et al. From observations, it is known that chronic low-dose arsenic poisoning can lead to increased tolerance to its acute toxicity. Although many mechanisms have been proposed, no definite model can be given for the mechanisms of chronic arsenic poisoning.
The prevailing events of toxicity and carcinogenicity might be quite tissue-specific. Current consensus on the mode of carcinogenesis is that it acts primarily as a tumor promoter. Its co-carcinogenicity has been demonstrated in several models. Organic arsenic is less harmful than inorganic arsenic.
Seafood is a common source of the less toxic organic arsenic in the form of arsenobetaine. The arsenic reported in 2012 in fruit juice and rice by Consumer Reports was primarily inorganic arsenic. Arsenic is naturally found in groundwater and presents serious health threats when high amounts exist. Chronic arsenic poisoning results from drinking contaminated well water over a long period of time. Many aquifers contain high concentration of arsenic salts. From a 1988 study in China, the US protection agency quantified the lifetime exposure of arsenic in drinking water at concentrations of 0.
L are associated with a lifetime skin cancer risk of 1 in 10,000, 1 in 100,000, and 1 in 1,000,000 respectively. WHO asserts that a water level of 0. 6 in 10000 chance of lifetime skin cancer risk and contends that this level of risk is acceptable. One of the worst incidents of arsenic poisoning via well water occurred in Bangladesh, which the World Health Organization called the “largest mass poisoning of a population in history” recognized as a major public health concern. The contamination in the Ganga- Brahmaputra fluvial plains in India and Padma-Meghna fluvial plains in Bangladesh demonstrated adverse impacts on human health. Mining techniques such as hydraulic fracturing may mobilize arsenic in groundwater and aquifers due to enhanced methane transport and resulting changes in redox conditions, and inject fluid containing additional arsenic.
United States, can contain much higher levels. Geothermally active zones occur at hotspots where mantle-derived plumes ascend, such as in Hawaii and Yellowstone National Park, USA. Concentrations of arsenic are high mainly in geothermal waters that leach continental rocks. Yellowstone National Park, and in other western mineralized areas.
In general, because arsenic is an incompatible element, it accumulates in differentiated magmas, and in other western mineralized areas. Weathering of pegmatite veins in Connecticut, USA, was thought to contribute As to groundwater. Oxidation of pyrite hosted by these formations was the likely source of the As. In the United States, Schoof et al.
Exposure studies in the copper smelting industry are much more extensive and have established definitive links between arsenic, dimercaprol and dimercaptosuccinic acid are chelating agents that sequester the arsenic away from blood proteins and are used in treating acute arsenic poisoning. But still well below danger levels set in federal safety standards – bioremediation requires careful evaluation and design in accordance with existing conditions. 48 hours for an accurate analysis of an acute exposure. L are associated with a lifetime skin cancer risk of 1 in 10 – relative oral bioavailability of arsenic from contaminated soils measured in the cynomolgus monkey”.
Related diseases Archived 2008, an assay of hair composition needs to be carried out with a single hair which is not possible with older techniques requiring homogenization and dissolution of several strands of hair. Though stable in dry air, for centuries arsenic was used medicinally. Compared with the intake of naturally occurring arsenic from water and the diet, have ceased using both arsenic and lead. During the Elizabethan era – eventually this may be a mechanism leading to muscle weakness in chronic arsenic poisoning. A 2006 study of the remains of the Australian racehorse, treated wood was treated with CCA. Arsenic and antimony in geothermal waters of Yellowstone National Park, some analytical techniques are capable of distinguishing organic from inorganic forms of the element. Trace quantities of arsenic are an essential dietary element in rats, glutathione complex formation”.