DELICTIMPost extinguendis, Martensite et retenta austenite est inconstans, habent spontanea organizationem transmutatio trend ad stabilitatem, ut supersaturated carbon in martensite ad subcinctus, ut tempering tempering in ut promoveatur, ut tempering temperatio est in non-aequilibrium organization temperatio est non-aequilibrium organization temperans non est in non-aequilibrium organizationem Ad statera organization in processus hoc processum dependet a nuclei migratio et diffusio huius auctoritatis cum perficitur ignis temperatus est altius, citius diffusa velocitas, in contrario et in caliditas, in structuram subeunt seriem mutationes. Secundum statum microstructure mutatio, temperatio est plerumque dividitur in quattuor gradus: Martensite Decomposition, RELICTUM Austenite corrumpitur, carbide cumulus incrementum et ferrite recrymingtallization.
Primum scaena (CC)
(I) fusilistemperatio animi martensite corrumpitur sub LXXX temperatus tempering, extinguendas ferro sine Ming s organization transmutatione, in occursus carbonis in Martensite tantum, et non incipit et dissolvi in ​​80-200, et non incipit, reducere in Missam fraction of Martensite in carbonis Dimittings in hoc scaena, ex humilis temperatio temperatus, martensitic praecipitatio tantum pars supersaturated carbonis atoms, ita etiam carbonis in - FE carbide uniformiter distribuit in matricem De Martense. Missi structuram humilis saturationum martensite et ipsum ipsum carbide dicitur temperari martensite.

(II)fusilistempering in the second stage (200-300), the residual austenite decomposition when the temperature rose to 200-300, the decomposition of martensite continued, but the dominant change is residual austenite decomposition of the residual austenite decomposition was through the expansion of carbon atoms formare partialis area et resolutum in alpha tempus et mixtisque carbide organization, nimirum formationem Baini ferro duritiam non manifesto diminutio ad hoc scaena
(III)In tertia scaena (250-400) carbide transformationem fabminis temperatio est in hoc temperatus range. Ob altum temperatus, carbon atom diffusio facultatem est fortior, diffusio facultatem ad recuperare ferrum atoms etiam, Martensite decomposita transitus et vertitur in relative stabilis cementite cum separatione et convertit in relative stabilis cementite cum separatione et transformatio in carbidum et decrementum De Martensite in ipsum Missam fraction, Martensite cancellos Distonorted evanescet, Martensitic transmutatio ad Ferrite, ut Ferric matrix distribution intra parva granuloso et lamellae cementite est organization, in organization vocavit ingenio, quod est in organization astenite aurei, duritia, plasticity lenta est melior

(IV)Et quartus scaena de fabrica temperatio (& GT; CD) crevit carbide congregentur et recrystallization of Ferrite ex tempering temperatus est valde altum, carbonis et ferrum atomatibus cementite fickes erit usque ad formationem cementorum fickes et usque ad formationem cementorum fickes erit usque ad tremendum est fortis cementite fickes et usque ad formationem cementorum et in fastis et adest et crevimus Sursum in plus quam 500-600, alpha recrystallization occurs paulatim, amittere Ferrite EXERFICIUM de originali laminam habena et sheet, et forma polygoni granulatum distribution distribution in organization ut a mechanica temperratus, in coetus vocatur tempering Mechanica Proprietatibus Phase et cœnaculum distortionem eliminate internus accentus.

(Ex CLXVIII Forging rete)