43SC    43TI EC DECAY (509 MS)        1987HO14                  15NDS    201506
 43SC  H TYP=FUL$AUT=BALRAJ SINGH AND JUN CHEN{+#}$CIT=NDS 126, 1 (2015)$
 43SC2 H CUT=31-Mar-2015$
 43SC c  1987Ho14: {+43}Ti nuclides were produced by the {+40}Ca(|a,n) reaction
 43SC2c  with an 18 MeV alpha beam from the MC-20 cyclotron of the University of
 43SC3c  Jyvaskyla. |b-rays were detected by a 500 |mm, 300 mm{+2} Si(Au)
 43SC4c  surface-barrier detector and |g-rays by a 15.5% Ge detector. Measured
 43SC5c  E|g, I|g, E(|b). Deduced levels,  |b- and |g-branchings, T{-1/2}.
 43SC6c  Comparison with shell-model calculations
 43SC c  Others:
 43SC c  T{-1/2} and isotopic identification: 1967Al08, 1963Va37, 1961Ja22
 43SC2c  (also 1960Ja12), 1954Ty33, 1948Sc20
 43SC c  |b{++}: 1969Va41 (also 1963Va37), 1961Ja22
 43SC c  |g: 1971BlZH
 43SC cE $There is an apparent |b{++} feeding of 0.11% {I6} to the 3/2-
 43SC2cE at 472.7 giving an unrealistic log| {Ift}=6.3 for 7/2- to 3/2-.
 43SC3cE This imbalance is due either to missing |g transitions to
 43SC4cE the 472.7 level or to intensity problems in the |g-rays involved.
 43SC5cE Due to the large difference between the Q-value and the energy of
 43SC6cE highest populated level, this decay scheme seems incomplete.
 43SC cG M,MR$Multipolarities and mixing ratios from Adopted Gammas
 43SC cG RI(A)$Estimated (evaluators) from log| {If{+1u}t}>8.5 and I|g(2137|g)
 43SC cL E$From least-squares fit to E|g data
 43SC cL J$From Adopted Levels
 43SC cL E(A)$Intensity balance gives apparent |b{++} feeding of 0.11% {I6}
 43TI  P  0           7/2-             509 MS    5              6867       7
 43TI cP J,T$From Adopted Levels of {+43}Ti
 43TI cP QP$From 2012Wa38
 43SC  N  0.044     6          1.0       1.0
 43SC cN NR$I|g(845|g)(per 100 decays)=2.8 {I4}, from comparison of |g-ray
 43SC2cN yield to the yield of 0.5-s component of |g{+|+} radiation (1987Ho14)
 43SC PN                                                                     3
 43SC  L 0            7/2-
 43SC  E               90.2  14 0.0826 16  3.554  9              90.3     14
 43SC cE TI$100-summed feeding to higher levels
 43SCS E EAV=2726.7 35$CK=0.000819 3$CL=8.22E-5 3$CM+=1.400E-5 5
 43SC  L     151.2514 3/2+
 43SC  E               0.07  LT 0.0001 LT   8.5  GT               0.07    LT 1U?
 43SCS E EAV=2663.5 34$CK=0.001872 8$CL=0.0001883 8$CM+=3.207E-5 13
 43SC  G      151.9    2.9   12                                             A  S
 43SC  L      472.7 3 3/2-                                                  A
 43SC  G      472.7 4 4.8    10
 43SC  L     845.17 9 5/2-
 43SC  E                2.6  4  0.0038 6   4.78   7              2.6       4
 43SCS E EAV=2312.8 35$CK=0.001300 6$CL=0.0001306 6$CM+=2.225E-5 10
 43SC  G      845.2 1 62.9   19 M1+E2    +0.15   4
 43SC  L    1408.03 9 7/2-
 43SC  E               0.67  10 0.0014 2   5.13   7              0.67     10
 43SCS E EAV=2038.5 34$CK=0.001853 9$CL=0.0001862 9$CM+=3.171E-5 15
 43SC  G      562.9 2 2.8     5
 43SC  G      936.0 8 1.0     2
 43SC  G     1408.0 1 12.6    4 M1+E2    +0.15   5
 43SC  L     1882.5 3 (5/2,9/2)-
 43SC  E               0.26  5  0.0007515  5.32   9              0.26      5
 43SCS E EAV=1808.4 34$CK=0.002592 14$CL=0.0002605 1$CM+=4.436E-5 24
 43SC  G     1882.5 3 5.9     8
 43SC  L     1963.0 4  (3/2,5/2)-
 43SC CL J$LOGFT=6.35 20 from 7/2- parent state disfavors 3/2, but
 43SC2CL the level is weakly populated and this argument is not strong enough
 43SC3CL to reject 3/2 which is supported by L-transfers in other experiments
 43SC  E               0.022 10  7.E-5 3   6.35  20              0.022    10
 43SCS E EAV=1769.5 34$CK=0.002755 15$CL=0.0002768 1$CM+=4.71E-5 3
 43SC  G     1490.2 2 0.5     2 M1+E2    +0.21   6
 43SC  L    2288.4010 5/2-
 43SC  E                4.6  7   0.018 3   3.85   7              4.6       7
 43SCS E EAV=1612.7 34$CK=0.003574 21$CL=0.0003592 2$CM+=6.12E-5 4
 43SC  G      880.7 5 1.1     2
 43SC  G     1443.5 3 1.3     3
 43SC  G     1815.4 4 0.9     5
 43SC  G     2137.1 1 2.1     4
 43SC  G     2288.3 1 100     4 M1+E2    +0.08   5
 43SC  L    2335.4710 5/2-
 43SC  E               0.38  6  0.0016 3   4.91   7              0.38      6
 43SCS E EAV=1590.1 34$CK=0.003718 23$CL=0.0003737 2$CM+=6.36E-5 4
 43SC  G     2335.4 1 8.7     7
 43SC  L    2458.6810 (5/2:9/2)-
 43SC  E               0.91  13 0.0042 6   4.46   7              0.91     13
 43SCS E EAV=1530.9 34$CK=0.00414 3$CL=0.000416 3$CM+=7.08E-5 5
 43SC  G     2458.6 1 20.7    8
 43SC  L 2760.10   10 (5/2:9/2)-
 43SC  E               0.20  3  0.0012 2   4.94   7              0.20      3
 43SCS E EAV=1386.5 34$CK=0.00546 4$CL=0.000549 4$CM+=9.34E-5 7
 43SC  G     2760.0 1 4.5     3
 43SC  L 3259.7    10 (7/2,9/2)-
 43SC  E               0.011 2  0.000112   5.86   8              0.011     2
 43SCS E EAV=1149.0 34$CK=0.00924 8$CL=0.000929 8$CM+=0.0001583 1
 43SC  G  3259.6   10  0.24   4
 43SC  L     3631.710 (5/2-,7/2-,9/2-)                                         ?
 43SC  E               0.016 4  0.000267   5.40  11              0.016     4   ?
 43SCS E EAV=974.0 33$CK=0.01470 15$CL=0.001478 15$CM+=0.0002518 2
 43SC  G  3631.5   10 0.36    6                                                ?