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Under-deposit chloride-induced stress corrosion cracking in austenitic stainless steels: Aspects associated with deposit type, size and composition

机译:奥氏体不锈钢中沉积不足的氯化物引起的应力腐蚀开裂:与沉积物类型,尺寸和成分相关的方面

摘要

The occurrence of Atmospheric chloride-Induced Stress Corrosion Cracking (AISCC) in austenitic stainless steels beneath 'wetted' deposits of either artificial sea-salt, organically-enriched artificial sea-salt or MgCl 2.6H2O has been investigated under controlled climatic conditions (40°C and 33% relative humidity). The presence of organic exudate in relatively large artificial sea-salt deposits (~3 mm diameter) appears to markedly decrease the induction time associated with AISCC; cracking occurred within a week in one U-bend specimen, well inside the ~12 week period usually observed under 'wetted' deposits of artificial sea-salt alone. Cracks appear to initiate from crevices formed under NaCl crystals. It is tentatively proposed that the organic species promotes greater coverage by the MgCl2 electrolyte in the vicinity of these crystals. This increases the probability of crevice initiation, and allows more rapid production of localized corrosion sites (pits or crevices) propagating under conditions that allow the transition to AISCC (pit/crevice dissolution rate crack velocity). © 2014 The Electrochemical Society.
机译:在受控气候条件下(40°C),研究了奥氏体不锈钢在湿润的沉积物下的大气氯化物引起的应力腐蚀开裂(AISCC),该沉积物是人造海盐,有机富集的人造海盐或MgCl 2.6H2O的“湿润”沉积物。 C和33%的相对湿度)。在相对较大的人工海盐沉积物中(直径约3毫米),有机渗出物的存在似乎显着减少了与AISCC相关的诱导时间;一个U型弯曲试样在一周之内就发生了开裂,通常在约12周的时间里,通常仅在人造海盐的“湿润”沉积下观察到。裂纹似乎是由NaCl晶体下形成的缝隙引起的。初步提出有机物在这些晶体附近促进MgCl2电解质的覆盖。这增加了缝隙引发的可能性,并允许在允许过渡到AISCC的条件下(凹坑/缝隙溶解速率<裂纹速度)传播的局部腐蚀部位(凹坑或缝隙)的产生更快。 ©2014年电化学学会。

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