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The substantially lower redox potential of thiosulfate (E 0 ' (S 2 O 3 2- / HS − ) = -400 mV), and sulfur (E 0 ' (S 0 / HS − ) = -275 mV), as compared to that of the AsV/AsIII couple (Em = +60 mV) suggests that oxidized sulfur compounds were available as electron acceptors already at much lower oxidation states of the environment, i. e. much earlier than the arsenics.
The organoborate was found to have a much lower oxidation potential compared to the organoborane.
The composite with the 10 mass% Al has a much lower oxidation resistance than that with the 6 mass% Al.
Notably, the AC/gold composite exhibits a sharp peak at a much lower oxidation potential (0.13 V) with threefold current and a very low hydrazine detection limit of 6.3 nM [84].
Isothermal oxidation tests in air at 900 °C showed transient oxidation kinetics for the aluminized + IDHTed Alloy 617, resulting in much lower oxidation rate than the as-received Alloy 617.
It can be interpreted that the excessive H2O2 acts as a scavenger of ∙OH, but the produced HO2∙ (Equations (5)–(7)) has much lower oxidation capacities [ 38].
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Furthermore, both studies showed much lower CH4 oxidation activity than observed in the present study, questioning the possibility of an N2-fixing life style of the methanotroph (Ho and Bodelier 2015).
Equations (1)–(3) show that during sonolysis, the net production of oxidation radical is much lower compared to oxidation radicals formed in the presence of zinc oxide (Eqs. 4 8).
Interestingly, ethanol oxidation occurs at much lower temperatures than NOx reduction; at 250 °C, ethanol oxidation is 80% when flowing ethanol + NO + O2.
The Ks value of NH3 oxidation is much lower for N. oligotropha (2.4 4.2 µM) than for N. europaea (30 56 µM) (Koops et al. 1991; Koops and Pommerening-Röser 2005).
During this period of Earth's history, the ambient potential of the environment was thus much lower than today and biological oxidation of arsenite to arsenate was probably the only mechanism producing oxidized arsenics.
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