Department of Civil and Environmental Engineering, 3-133 Markin/CNRL Natural Resources Engineering Facility, University of Alberta, Edmonton, AB, T6G 2W2, Canada.
J Phys Chem A. 2010 Nov 18;114(45):12067-74. doi: 10.1021/jp105727s. Epub 2010 Oct 25.
The mechanism of hydroxyl radical initiated degradation of a typical oil sands process water (OSPW) alicyclic carboxylic acid was studied using cyclohexanoic acid (CHA) as a model compound. By use of vacuum ultraviolet irradiation (VUV, 172 nm) and ultraviolet irradiation in the presence of hydrogen peroxide UV(254 nm)/H(2)O(2), it was established that CHA undergoes degradation through a peroxyl radical. In both processes the decay of the peroxyl radical leads predominantly to the formation of 4-oxo-CHA, and minor amounts of hydroxy-CHA (detected only in UV/H(2)O(2)). In UV/H(2)O(2), additional 4-oxo-CHA may also have been formed by direct reaction of the oxyl radical with H(2)O(2). The oxyl radical can be formed during decay of the peroxyl-CHA radical or reaction of hydroxy-CHA with hydroxyl radical. Oxo- and hydroxy-CHA further degraded to various dihydroxy-CHAs. Scission of the cyclohexane ring was also observed, on the basis of the observation of acyclic byproducts including heptadioic acid and various short-chain carboxylic acids. Overall, the hydroxyl radical induced degradation of CHA proceeded through several steps, involving more than one hydroxyl radical reaction, thus efficiency of the UV/H(2)O(2) reaction will depend on the rate of generation of hydroxyl radical throughout the process. In real applications to OSPW, concentrations of H(2)O(2) will need to be carefully optimized and the environmental fate and effects of the various degradation products of naphthenic acids considered.
采用环己烷羧酸(CHA)作为模型化合物,研究了羟基自由基引发的典型油砂开采废水(OSPW)中环烷酸降解的机理。通过真空紫外辐射(VUV,172nm)和过氧化氢存在下的紫外辐射(UV(254nm)/H(2)O(2)),确定 CHA 通过过氧自由基发生降解。在这两种过程中,过氧自由基的衰减主要导致 4-氧代-CHA 的形成,以及少量的羟基-CHA(仅在 UV/H(2)O(2)中检测到)。在 UV/H(2)O(2)中,另外的 4-氧代-CHA 也可能通过氧自由基与 H(2)O(2)的直接反应形成。氧自由基可以在过氧-CHA 自由基的衰减过程中形成,或者在羟基-CHA 与羟基自由基的反应中形成。氧代和羟基-CHA 进一步降解为各种二羟基-CHA。基于无环副产物的观察,包括庚二酸和各种短链羧酸,也观察到环己烷环的断裂。总的来说,羟基自由基诱导的 CHA 降解经过几个步骤,涉及不止一个羟基自由基反应,因此 UV/H(2)O(2)反应的效率将取决于整个过程中羟基自由基的生成速率。在实际应用于 OSPW 时,需要仔细优化 H(2)O(2)的浓度,并考虑环烷酸各种降解产物的环境归宿和影响。