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Morphological and physicochemical characteristics of iron corrosion scales formed under different water source histories in a drinking water distribution system

机译:饮用水分配系统中不同水源历史形成的铁腐蚀鳞片的形态和理化特性

摘要

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 (WG) was significantly different depending on the corrosion scale structure and water source conditions. Thick corrosion scales and hard shell of tubercles had much higher WG ratio (>1.0), while the thin corrosion scales had no magnetite detected or with much lower WG ratio. The WG 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 gamma-FeOOH, beta-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. (C) 2012 Elsevier Ltd. All rights reserved.
机译:铁管上的腐蚀垢可能会对饮用水分配系统(DWDS)中的水质产生重大影响。当进入分配系统的水的质量发生显着变化时,不稳定且保护性较小的腐蚀垢是导致“变色水”问题的主要原因之一。在这项工作中,系统地研究了在大约二十年的不同水源水历史下形成的腐蚀垢的形态和理化特性。在输送地表水的管道中通常发现较厚的腐蚀鳞片或密集分布的腐蚀结核,但在输送地下水的管道中主要发现有较薄的腐蚀鳞片和空心结核。磁铁矿和针铁矿是铁腐蚀产物的主要成分,但磁铁矿/针铁矿的质量比(WG)随腐蚀规模结构和水源条件的不同而显着不同。厚的结垢和结节的硬壳具有更高的WG比(> 1.0),而薄的结垢没有检测到磁铁矿或具有低得多的WG比。 WG比可用于识别特性并评估在不同水条件下形成的腐蚀垢的性能。与输送地下水的管道相比,输送地表水的管道受到的腐蚀更严重,并且始终处于相对活跃的腐蚀状态,这与腐蚀等级中相对较高的菱铁矿,生铁锈和总铁含量有关。接受地下水的管道的腐蚀垢中存在较高含量的不稳定铁成分,如γ-FeOOH,β-FeOOH和无定形氧化铁,且腐蚀程度较小。磁铁矿含量低的地下水管上的腐蚀垢具有较高的表面积,因此可能具有较高的吸附能力。腐蚀产物中的主要微量无机元素是溴和重金属。从输送地下水的管道中获得的腐蚀产物中的溴,钛,钡,铜,锶,钒,铬,镧,铅和砷的含量较高。 (C)2012 Elsevier Ltd.保留所有权利。

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