193AU    193AU IT DECAY (3.9 S)        1970FO08                  17NDS    201709
193AU  H TYP=FUL$AUT=M. Shamsuzzoha Basunia$CIT=NDS 143, 1 (2017)$
193AU2 H CUT=31-Mar-2017$
193AU C  1970Fo08: activity from 193HG EC (3.80 H) + 193HG (11.8 H) decay
193AU2C  (produced by spallation of PB by 600-MEV protons, MS).
193AU2C  Measured EG, IG (GELI), ECE, ICE (mag spect), G(CE), (CE)(CE)t
193AU C  Others: 1974ViZS, 1958Br88, 1955Br12, 1955Br41, 1955Fi30, 1954Gi04,
193AUxC  1952Fi06
193AU CG           All data are from 1970Fo08, unless otherwise noted.
193AU CG E         Deduced from E(CE); calibrated with E(CEK) of the
193AU2CG 117.99 2 G in 193PT.
193AU CG RI        Calculated from intensity balances in the level scheme, the
193AU2CG conversion coefficients, and the ratio I(219.75G)/I(257.97G)=0.0572 30
193AU3CG (1970Fo08).
193AU CL           The decay scheme is that proposed by 1970Fo08.
193AU CL E,J,T     From Adopted Levels, unless otherwise noted.
193AU DG CC$FROM BrIcc v2.3a (30-Jun-2013) 2008Ki07, "Frozen Orbitals" appr.
193AU CG MR$IF NO VALUE GIVEN IT WAS ASSUMED MR=1.00 FOR E2/M1,
193AU2CG MR=1.00 FOR E3/M2 AND MR=0.10 FOR THE OTHER MULTIPOLARITIES
193AU  P 290.20    3  11/2-            3.9 S     3
193AU  N    1.001     1.000    0.9997
193AU PN              1                                                      3
193AU CN NR        From TI(219.75G)+TI(257.97G)-TI(289.8G)=99.47
193AU CN BR        99.97% from TI(258.0G (M1) in 193AU): TI(135.5G (M4) in
193AU2CN 193PT)=1000:0.3 (1955Br41). Ratio deduced from CE-intensities and
193AU2CN theoretical conversion coefficients (not given).
193AU  L 0.0          3/2+             17.65 H   15
193AU  L 38.23     2 (1/2)+            3.81 NS   18
193AU  G 38.22     2           M1+E2     0.42    +5-4  89     14   4.81   26
193AUS G  L/T=0.75 9$M/T=0.19 4
193AUS G  N/T=0.046 10$O/T=0.0076 17$P/T=0.000119 19
193AUS G  LC=67 11$MC=17 3
193AUS G  NC=4.2 7$OC=0.68 11$PC=0.0107 4
193AU CG TI        from TI(38.22)=TI(219.75) in level scheme
193AU CG M         from L1:L2:L3=42 4:98 9:100
193AU CG MR        from L1/L3=0.50 10, weighted average from 1970Fo08 and
193AU2CG 1974ViZS (193HG (3.80 H) decay)
193AU  L 257.98    2  5/2+             45 PS     20
193AU CL T         from (CEL(32.21G))(CEK(257.95G)t) (1970Fo08)
193AU  G 219.75    5  3.85   20E2                      0.273
193AUS G  KC=0.1344 19$LC=0.1039 15$MC=0.0266 4
193AUS G  NC=0.00655 10$OC=0.001076 16$PC=1.385E-5 20
193AU CG M         from K:L1:L2:L3=14.0 15:2.35 30:6.7 7:5.1 6
193AU  G 257.97    3   67.1    M1+E2     0.52    15    0.43   4
193AUS G  KC=0.34 4$LC=0.0654 17$MC=0.0154 3
193AUS G  NC=0.00383 8$OC=0.000692 19$PC=4.1E-5 4
193AU CG M         from L1:L2:L3=100:22 4:4.7 +47-30
193AU CG MR        from weighted average of CEL ratios from 1970Fo08 and
193AU2CG 1974ViZS (193HG (11.8 H) decay)
193AU  L 290.20    3  11/2-            3.9 S     3                           M
193AU2 L %IT=99.97
193AU CL T         from 1955Fi30. Other: 3.8 S 3 (1955Br41).
193AU  G 32.21     3           E3                      9.29E4    99.47
193AUS G  L/T=0.699 9$M/T=0.232 5
193AUS G  N/T=0.0592 13$O/T=0.00907 20$P/T=7.33E-6 16
193AUS G  LC=6.50E4 10$MC=2.16E4 4
193AUS G  NC=5.50E3 9$OC=843 13$PC=0.681 10
193AU CG E         from 1974ViZS.
193AU CG M         from (M1+M2+M3)/(M4+M5)=11.3 (1958Br88); other subshell
193AU2CG ratios allow E2 or E3, but (M1+M2+M3)/(M4+M5)=71.2 (E2
193AU3CG theory), =9.13 (E3 theory) is consistent only with E3.
193AU4CG L2/L3=0.65 (1954Gi04)
193AU CG TI        from 99.97 - TI(289.8G)
193AU  G 289.8                 [M4]                    18.1        0.5
193AUS G  K/T=0.472 7$L/T=0.349 6$M/T=0.0972 18
193AUS G  N/T=0.0247 5$O/T=0.00423 9$P/T=0.000162 4
193AUS G  KC=9.01 13$LC=6.67 10$MC=1.86 3
193AUS G  NC=0.472 7$OC=0.0807 12$PC=0.00310 5
193AU CG E,TI      from 1955Br41
193AU CG TI        deduced from I(CE) relative to I(CE 257.97G) and theoretical
193AU2CG conversion coefficients (values not given by 1955Br41).
193AU CG TI        upper limit AP 3% from comparison of the CE-lines of the
193AU2CG 290 and 256 transitions (1954Gi04)