Selenium Contamination in Water. Группа авторов

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Selenium Contamination in Water - Группа авторов


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hoof disease and hair loss in horses due to toxically high levels of Se accumulated from plant consumption. In addition, Se is the most important constituent of the body's antioxidant defense mechanism through selenoproteins such as GPx (Hefnawy and Tórtora‐Pérez 2010; Pascual and Aranda 2013). Despite all these useful qualities of Se, it causes several disorders in domestic animals after consuming high doses. The main sources of Se for livestock animals are soil, water, forages, and feed supplements. Coal‐mining regions mainly contain a higher level of Se due to the presence of pyrite oxidation (Dreher and Finkelman 1992). The level of Se varies from state to state and from country to country (Dhillon and Dhillon 2003; Lenz and Lens 2009).

      Higher levels of Se exposure triggered alkali disease and the effect of selenium toxicity was blind staggers (National Research Council [NRC] 1983). The higher Se level triggered three forms of toxicity primarily: acute, sub‐acute, and chronic toxicity. Animal poisoning is described as being acute, sub‐chronic, or chronic (National Research Council [NRC] 1983). A lot of factors control the selenosis in an animal’s body, such as the properties of Se and animal health properties. It was also found that selenosis varies from species to species of livestock animals (horses > cattle) (Ehlig et al. 1968; Rosenfeld and Beath 2013). Sub‐chronic and chronic Se toxicity causes pathological changes mainly in skeletal muscle, heart, liver, spleen, and kidney as Se is mostly accumulated at a higher level in these organs (Rosenfeld and Beath 2013). Therefore, some preventive measurement like agricultural field management, the feeding of high protein‐rich feed, dietary sulfate, methionine supplement, linseed meal, spraying sulfur‐containing materials on fodders grown in selenium‐rich soil, clean water, phyto‐remediation etc. are being implemented to maintain the health and higher productivity of domestic animals (Dhillon and Dhillon 1991). Therefore, this book chapter discusses in detail the sources and mechanism of Se toxicity in the bodies of livestock animal, as well as the probable preventive measures to attenuate Se toxicity leading to better health and higher production of the livestock animals and reduction of selenium in the human food chain through milk and meat intake.

      

Food
Country Cereals (mg/kg) Meat (mg/kg) Dairy food (mg/kg) Vegetables (mg/kg)
India 0.23–1.64a 0.01–0.09b 0.92–1.34a
Australiac 0.01−/0.31 0.06–0.34 </0.001–0.11 </0.001–0.022
U.K.d 0.11 0.12–0.6 0.01–0.085 0.005–0.01
U.S.d 0.3–0.56 0.06–1.33 0.006–0.3 0.004–0.07
Canadad 0.01 0.06–1.22 0.005–0.01 0.005–0.01
Finlandd 0.02 0.05–0.48 0.002–0.025 0.002
New Zealandd 0.035 0.03–0.38 0.004–0.025 0.003

      a Dhillon and Dhillon (1991).

      b Giri (2019).

      c Australia (Tinggi et al. 1992; Tinggi 1999; Tinggi and Conor Reilly 2001).

      d Combs (1988).

      4.2.1 Soil

      Weathering is the primary natural process to release Se in the soil. In different forms, Se present in the soil like elemental selenium, calcium selenate, basic ferric selenite, and organic selenium compounds after the decomposing of animal and plant materials. The coal‐mining region mainly contains a higher level of Se due to the presence of pyrite oxidation (Dreher and Finkelman 1992). The level of Se varies from states to states, country to country (Dhillon and Dhillon 2003; Lenz and Lens 2009). Usually, the soil contains 0.1–2 mg Se/kg (Fishbein 1983). It was found that soil in the US, India, and Ireland has a higher level of Se (100 mg Se/kg), while soil in Brazil and Argentina has a relatively lower level of Se (< 0.1 mg/kg) (Dhillon and Dhillon 2003; Lenz and Lens 2009). Depending on the higher and lower levels, one region may recognize each as a region that is seleniferous and nonseleniferous. Soil which contains 5 mg/kg Se is very toxic (Rogers et al. 1990).

      4.2.2 Water

      Se's presence in groundwater and surface water depends largely on soil characteristics, and anthropogenic factors relating to that area (Giri 2019). Underground water of a seleniferous region showed 2.54–69.53 μg/l of Se, whereas a nonseleniferous region was characterized by 0.25–8.63 μg/l (Dhillon and Dhillon 1991). Freshwater showed


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