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The arsenate is an with the . Bonding in arsenate consists of a central atom, with +5, to one oxygen atom and to a further three atoms. The four oxygen atoms orient around the arsenic atom in a tetrahedral geometry. Resonance disperses the ion's −3 charge across all four oxygen atoms.

Arsenate readily reacts with metals to form arsenate metal compounds. Arsenate is a moderate and an electron acceptor, with an electrode potential of +0.56 for its reduction to . Due to arsenic having the same valency and similar atomic radius to , arsenate shares similar geometry and reactivity with . Arsenate can replace phosphate in and is to most .


Natural occurrence
Arsenates occur naturally, in and form, in a variety of . Examples of arsenate-containing minerals include , , , and . When two arsenate ions balance the in a formula, it is called diarsenate for example zinc diarsenate, .


Uses
Arsenate-based such as lead hydrogen arsenate were commonly used until their replacement by newer pesticides such as and subsequent ban by multiple regulatory bodies due to health concerns.

arsenate compounds are often brightly coloured and have been used to make . Copper arsenate was a minor compound used in the pigment used by the ancient Egyptians and . Cobalt violet pigment was made from cobalt arsenate before its toxicity led to its replacement by cobalt phosphate.

Chromated copper arsenate (CCA) has been a widely used wood preservative since the 1930s. Safety concerns have led to the phasing out of CCA-treated wood for projects in many countries. CCA remains a common and economical treatment choice for non-residential uses such as .


Speciation
Depending on the pH, arsenate can be found as trihydrogen arsenate (that is ), dihydrogen arsenate (), hydrogen arsenate (), or arsenate (). Trihydrogen arsenate is also known as . At a given pH, the distribution of these arsenate can be determined from their respective acid dissociation constants.
(p Ka1 = 2.19)
(p Ka2 = 6.94)
(p Ka3 = 11.5)

These values are similar to those of . Hydrogen arsenate and dihydrogen arsenate predominate in aqueous solution near neutral pH.

The reduction potential (pe) of a solution also affects arsenate speciation. In natural waters, the is the main factor influencing reduction potential. Arsenates occur in oxygenated waters, which have a high pe, while arsenites are the main arsenic species in with a low pe.

A shows the combined influence of pH and pe on arsenate speciation.


Contamination
Arsenates, along with arsenites, are a significant source of contamination in some natural and can lead to arsenic poisoning with repeated exposure. Countries with high levels of arsenic minerals in and rock, such as , are especially at risk of arsenate contamination.


Arsenate poisoning
Arsenate is harmful to and as it interferes with the normal functioning of and the Krebs cycle. Arsenate replaces inorganic in the step of that produces 1,3-bisphosphoglycerate from glyceraldehyde 3-phosphate. This yields 1-arseno-3-phosphoglycerate instead, which is unstable and quickly , forming the next intermediate in the pathway, 3-phosphoglycerate. Therefore, glycolysis proceeds, but the ATP molecule that would be generated from 1,3-bisphosphoglycerate is lost – arsenate is an of glycolysis, explaining its toxicity.

As with other arsenic compounds, arsenate binds to , inhibiting the conversion of into , blocking the and therefore resulting in further loss of ATP.


See also

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