Isotopes of titanium

(Redirected from Titanium-46)

Naturally occurring titanium (22Ti) is composed of five stable isotopes; 46Ti, 47Ti, 48Ti, 49Ti and 50Ti with 48Ti being the most abundant (73.8% natural abundance). Twenty-one radioisotopes have been characterized, with the most stable being 44Ti with a half-life of 60 years, 45Ti with a half-life of 184.8 minutes, 51Ti with a half-life of 5.76 minutes, and 52Ti with a half-life of 1.7 minutes. All of the remaining radioactive isotopes have half-lives that are less than 33 seconds, and the majority of these have half-lives that are less than half a second.[4]

Isotopes of titanium (22Ti)
Main isotopes[1]Decay
abun­dancehalf-life (t1/2)modepro­duct
44Tisynth59.1 yε44Sc
46Ti8.25%stable
47Ti7.44%stable
48Ti73.7%stable
49Ti5.41%stable
50Ti5.18%stable
Standard atomic weight Ar°(Ti)

The isotopes of titanium range in atomic mass from 39.00 u (39Ti) to 64.00 u (64Ti). The primary decay mode for isotopes lighter than the stable isotopes (lighter than 46Ti) is β+ and the primary mode for the heavier ones (heavier than 50Ti) is β; their respective decay products are scandium isotopes and the primary products after are vanadium isotopes.[4]

List of isotopes

Nuclide
[n 1]
ZNIsotopic mass (Da)
[n 2][n 3]
Half-life
[n 4]
Decay
mode

[n 5]
Daughter
isotope

[n 6]
Spin and
parity
[n 7][n 4]
Natural abundance (mole fraction)
Excitation energyNormal proportionRange of variation
39Ti221739.00161(22)#31(4) ms
[31(+6-4) ms]
β+, p (85%)38Ca3/2+#
β+ (15%)39Sc
β+, 2p (<.1%)37K
40Ti221839.99050(17)53.3(15) msβ+ (56.99%)40Sc0+
β+, p (43.01%)39Ca
41Ti221940.98315(11)#80.4(9) msβ+, p (>99.9%)40Ca3/2+
β+ (<.1%)41Sc
42Ti222041.973031(6)199(6) msβ+42Sc0+
43Ti222142.968522(7)509(5) msβ+43Sc7/2−
43m1Ti313.0(10) keV12.6(6) μs(3/2+)
43m2Ti3066.4(10) keV560(6) ns(19/2−)
44Ti222243.9596901(8)60.0(11) yEC44Sc0+
45Ti222344.9581256(11)184.8(5) minβ+45Sc7/2−
46Ti222445.9526316(9)Stable0+0.0825(3)
47Ti222546.9517631(9)Stable5/2−0.0744(2)
48Ti222647.9479463(9)Stable0+0.7372(3)
49Ti222748.9478700(9)Stable7/2−0.0541(2)
50Ti222849.9447912(9)Stable0+0.0518(2)
51Ti222950.946615(1)5.76(1) minβ51V3/2−
52Ti223051.946897(8)1.7(1) minβ52V0+
53Ti223152.94973(11)32.7(9) sβ53V(3/2)−
54Ti223253.95105(13)1.5(4) sβ54V0+
55Ti223354.95527(16)490(90) msβ55V3/2−#
56Ti223455.95820(21)164(24) msβ (>99.9%)56V0+
β, n (<.1%)55V
57Ti223556.96399(49)60(16) msβ (>99.9%)57V5/2−#
β, n (<.1%)56V
58Ti223657.96697(75)#54(7) msβ58V0+
59Ti223758.97293(75)#30(3) msβ59V(5/2−)#
60Ti223859.97676(86)#22(2) msβ60V0+
61Ti223960.98320(97)#10# ms
[>300 ns]
β61V1/2−#
β, n60V
62Ti224061.98749(97)#10# ms0+
63Ti224162.99442(107)#3# ms1/2−#
64Ti[5]224263.998410(640)#5# ms
[>620 ns]
0+
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Titanium-44

Titanium-44 (44Ti) is a radioactive isotope of titanium that undergoes electron capture to an excited state of scandium-44 with a half-life of 60 years, before the ground state of 44Sc and ultimately 44Ca are populated.[6] Because titanium-44 can only undergo electron capture, its half-life increases with ionization and it becomes stable in its fully ionized state (that is, having a charge of +22).[7]

Titanium-44 is produced in relative abundance in the alpha process in stellar nucleosynthesis and the early stages of supernova explosions.[8] It is produced when calcium-40 fuses with an alpha particle (helium-4 nucleus) in a star's high-temperature environment; the resulting 44Ti nucleus can then fuse with another alpha particle to form chromium-48. The age of supernovae may be determined through measurements of gamma-ray emissions from titanium-44 and its abundance.[7] It was observed in the Cassiopeia A supernova remnant and SN 1987A at a relatively high concentration, a consequence of delayed decay resulting from ionizing conditions.[6][7]

References