2009
DOI: 10.1016/j.epsl.2009.03.044
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Oxidation of water to hydrogen peroxide at the rock–water interface due to stress-activated electric currents in rocks

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Cited by 57 publications
(58 citation statements)
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“…In line with the presented model, the generation of a superoxide anion radical, a substrate for SOD, might be induced by the radioactive decay of uranium present in the natural environment of this organism (Chivian et al, 2008). The production of H 2 O 2 at the rock-water interface has also been reported, which suggests that ROS must have been generated long before the rise of free O 2 in the atmosphere (Balk et al, 2009). The occurrence of ROS removal systems in so many strict anaerobes (Fig.…”
Section: Reactions Involving H 2 Omentioning
confidence: 66%
“…In line with the presented model, the generation of a superoxide anion radical, a substrate for SOD, might be induced by the radioactive decay of uranium present in the natural environment of this organism (Chivian et al, 2008). The production of H 2 O 2 at the rock-water interface has also been reported, which suggests that ROS must have been generated long before the rise of free O 2 in the atmosphere (Balk et al, 2009). The occurrence of ROS removal systems in so many strict anaerobes (Fig.…”
Section: Reactions Involving H 2 Omentioning
confidence: 66%
“…However, in general, as to the possible causes of geochemical anomalies in water, two immediate mechanisms emerge: 1) a simple increase in fluid flow in the surrounding of the future epicenter and selective dissolution of some K-Mg-Ca-rich rocks (e.g., Federico et al, 2008); or 2) "electro-corrosion" whereby the dissolution of rocks is accelerated by the flow of stress-activated positive hole currents (Balk et al, 2009;Freund, 2011). Following the second mechanism, the increased amount of cations in water could be related to oxidation of water to hydrogen peroxide at the rock-water interface (Balk et al, 2009).…”
Section: Resultsmentioning
confidence: 99%
“…Following the second mechanism, the increased amount of cations in water could be related to oxidation of water to hydrogen peroxide at the rock-water interface (Balk et al, 2009). Balk et al (2009) chemical equation predicts that every positive hole (i.e., O -state) arriving at the rockwater interface reacts by oxidizing the water which turns into an OH -within the rock surface. This implies that the rock surface becomes solvated and turns into a gel.…”
Section: Resultsmentioning
confidence: 99%
“…The strange phenomena observed in water coming from springs located in caves could be analyzed just in this context. A very interesting article from Balk et al [75] reported that at the rock-water interface very interesting oxidative phenomena and also oxidative stresses appear analogously to what occurs in living organisms. Actually, rocks and living organisms have in common the presence of an interfacial layer of coherent water, which appears as a reasonable candidate to be the actor of the reported effects.…”
Section: The Dialog Between Liquid Coherent Water and The Environmentmentioning
confidence: 99%