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Secondary carbide precipitation in a directionally solidified cobalt-base superalloy

机译:定向凝固钴基高温合金中的二次碳化物沉淀

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A directionally solidified cobalt-basealloy, DZ40M, was solidified with a columnargrained austenitic matrix with a <001>preferential orientation and primary carbides ofchromium-rich M7C3 and MC at grain boundaries andinterdendritically. Secondary carbides in DZ40Malloy are chromium-rich M23C6 and tungsten-richM6C. The M23C6 carbide has a cube-cube orientationrelationship with the austenitic matrix. Initialprecipitation of secondary carbide, M23C6,occurred on dislocations in the austenitic matrixof the as-cast DZ40M alloy during cooling. Agingtreatment (100 to 1000 hours at 850℃) produced aprofusive precipitation of the M26C6 carbidemainly around the primary carbides. In theinterior of grains, M23C6 precipitatedpreferentially on dislocations and stacking faults.Subsequently, M23C6 grew into laths near theprimary carbides and coalesced into chains. Theprecipitation behavior of M23C6 can be explainedby the following reaction: 23M+6C→M23C6. Theprimary carbides are a carbon reservoir for theprecipitation of M23C6. The M6C carbide was foundonly on the surface of the primary M7C3 carbideadjacent to tungsten-rich MC in the aged condition.The precipitation of the tungsten-rich M6C isattributed to the tungsten segregation, whichresulted from decomposition of the tungsten-richMC and good lattice match between M6C and M7C3.The inhomogeneity of secondary precipitation isdue to the uneven distribution of the alloying elements.
机译:定向凝固的钴基合金DZ40M用优先取向为<001>的柱状奥氏体奥氏体基体以及晶界处和晶界处的富铬M7C3和MC的初生碳化物进行了固化。 DZ40合金中的次生碳化物为富铬M23C6和富钨M6C。 M23C6碳化物与奥氏体基体具有立方立方取向关系。在冷却过程中,铸态DZ40M合金的奥氏体基体中的位错发生了二次碳化物M23C6的初始析出。时效处理(在850℃下100至1000小时)产生了主要在一次碳化物周围的M26C6碳化物的隆突析出。在晶粒内部,M23C6主要在位错和堆积断层上析出。随后,M23C6成长为靠近原始碳化物的板条并聚集成链。 M23C6的沉淀行为可以通过以下反应来解释:23M + 6C→M23C6。初级碳化物是用于M23C6沉淀的碳库。在时效条件下,仅在与富钨MC相邻的原生M7C3碳化物的表面上发现了M6C碳化物。富钨M6C的析出归因于钨的偏析,这是由于富钨MC的分解和良好的晶格匹配导致的。 M6C和M7C3。二次沉淀的不均匀性是由于合金元素的不均匀分布所致。

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