State Key Laboratory of Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, 18 Shuangqing Road, P.O. Box 2871, Beijing 100085, China.
Water Res. 2012 Oct 15;46(16):5423-33. doi: 10.1016/j.watres.2012.07.031. Epub 2012 Jul 25.
The corrosion scales on iron pipes could have great impact on the water quality in drinking water distribution systems (DWDS). Unstable and less protective corrosion scale is one of the main factors causing "discolored water" issues when quality of water entering into distribution system changed significantly. The morphological and physicochemical characteristics of corrosion scales formed under different source water histories in duration of about two decades were systematically investigated in this work. Thick corrosion scales or densely distributed corrosion tubercles were mostly found in pipes transporting surface water, but thin corrosion scales and hollow tubercles were mostly discovered in pipes transporting groundwater. Magnetite and goethite were main constituents of iron corrosion products, but the mass ratio of magnetite/goethite (M/G) was significantly different depending on the corrosion scale structure and water source conditions. Thick corrosion scales and hard shell of tubercles had much higher M/G ratio (>1.0), while the thin corrosion scales had no magnetite detected or with much lower M/G ratio. The M/G ratio could be used to identify the characteristics and evaluate the performances of corrosion scales formed under different water conditions. Compared with the pipes transporting ground water, the pipes transporting surface water were more seriously corroded and could be in a relatively more active corrosion status all the time, which was implicated by relatively higher siderite, green rust and total iron contents in their corrosion scales. Higher content of unstable ferric components such as γ-FeOOH, β-FeOOH and amorphous iron oxide existed in corrosion scales of pipes receiving groundwater which was less corroded. Corrosion scales on groundwater pipes with low magnetite content had higher surface area and thus possibly higher sorption capacity. The primary trace inorganic elements in corrosion products were Br and heavy metals. Corrosion products obtained from pipes transporting groundwater had higher levels of Br, Ti, Ba, Cu, Sr, V, Cr, La, Pb and As.
铁管上的腐蚀层会对饮用水分配系统(DWDS)的水质产生重大影响。不稳定和保护作用较小的腐蚀层是导致“变色水”问题的主要因素之一,尤其是当进入分配系统的水质发生显著变化时。本工作系统地研究了在大约二十年的不同水源历史条件下形成的腐蚀层的形态和物理化学特性。在输送地表水的管道中,大多发现了厚的腐蚀层或密集分布的腐蚀瘤,但在输送地下水的管道中,大多发现了薄的腐蚀层和空心瘤。磁铁矿和针铁矿是铁腐蚀产物的主要成分,但由于腐蚀层结构和水源条件的不同,磁铁矿/针铁矿的质量比(M/G)差异显著。厚的腐蚀层和瘤的硬壳具有更高的 M/G 比(>1.0),而薄的腐蚀层则未检测到磁铁矿或具有更低的 M/G 比。M/G 比可用于识别不同水质条件下形成的腐蚀层的特征和评估其性能。与输送地下水的管道相比,输送地表水的管道腐蚀更为严重,且可能一直处于相对更活跃的腐蚀状态,这表明其腐蚀层中的菱铁矿、绿锈和总铁含量相对较高。腐蚀层中不稳定的三价铁成分,如γ-FeOOH、β-FeOOH 和无定形氧化铁的含量较高,这表明输送地下水的管道腐蚀程度较低。磁铁矿含量较低的地下水管道的腐蚀层具有更高的表面积,因此可能具有更高的吸附能力。腐蚀产物中的主要痕量无机元素是 Br 和重金属。输送地下水的管道中获得的腐蚀产物具有更高的 Br、Ti、Ba、Cu、Sr、V、Cr、La、Pb 和 As 水平。