88BR 88BR IT DECAY (5.3 US) 1999GE01 14NDS 201401
88BR H TYP=FUL$AUT=E.A. McCutchan and A.A. Sonzogni$CIT=NDS 115, 135 (2014)$
88BR2 H CUT=1-Nov-2013$
88BR c {+88}Br activity produced with {+241}Pu(n,F), En=thermal and
88BR2c separated using LOHENGRIN spectrometer with |DE-E for fission
88BR3c fragment identification. Measured E|g, I|g, |g|g, ce, and T{-1/2}
88BR4c using two large volume Ge and two Si(Li) detectors.
88BR c Others: 2010Re01, 2009Fo05, 1976SeZN, 1972GrYM, 1970Gr38
88BR cL E,J,T(A)$From the Adopted Levels.
88BR D CC$FROM BrIcc v2.3a (30-Jun-2013) 2008Ki07, "Frozen Orbitals" appr.
88BR P 270.1 5 (3-,4-,5-) 5.3 US 4
88BR N 1.0 1.0
88BR L 0.0 (2-) 16.34 S 8 A
88BR2 L %B-=100$%B-N=6.58 18
88BR L 159.20 23 (1-,2-,3-)
88BR G 159.1 5 M1+E2 0.24 2 0.039713 100
88BRX G K/T=0.0337 11$L/T=0.00380 14$M/T=0.000603 22$N/T=5.53E-5 19
88BRS G KC=0.0350 12$LC=0.00395 14$MC=0.000627 23$NC=5.75E-5 20
88BR cG $|a(K)exp=0.047 {I10}
88BR cG M,MR$1999Ge01 reported a M1 multipolarity, however, the |a(K)exp
88BR2cG value and the ratio of intensities suggest an E2 admixture. Using
88BR3cG I|g(110.9)/I|g(159.1)=0.65 (and an estimated uncertainty of 5% based
88BR4cG on Fig. 4), one obtains |d=0.24 {I2}. Alternatively, using
88BR5cG |a(K)exp=0.047 {I10}, |d=0.44 {I15}. In either case, the sign of the
88BR6cG mixing ratio cannot be determined.
88BR L 270.1 5 (3-,4-,5-) 5.3 US 4 M1
88BR2 L %IT=100
88BR cL T$weighted average of 5.1 |ms {I4} (1999Ge01), 4.9 |ms {I4}
88BR2cL (1976SeZN) and 6.3 |ms {I5} (1970Gr38,1972GrYM). Other 4 |ms {I1}
88BR3cL (extracted from Fig. 2 of 2009Fo05 by evaluator).
88BR cL $Configuration of (|nd{-5/2}|pp{-3/2}){-4-} is favored by 1999Ge01
88BR2cL based on comparison with {+88}Rb.
88BR G 110.9 5 E2 0.599 14 100
88BRX G K/T=0.322 5$L/T=0.0445 11$M/T=0.00704 18$N/T=0.000595 15
88BRS G KC=0.516 12$LC=0.0712 17$MC=0.0113 3$NC=0.000951 22
88BR cG $|a(K)exp=0.48 {I10}
88BR cG M$from |a(K)exp.