We report a measurement of the lifetime of the 2 1 + state in 18 Ne using the Doppler shift attenuation method, the 3 He͑ 16 O,n͒ reaction, and large volume germanium ␥-ray detectors of the "clover" design. The present measurement gives a B͑E2;0 g.s. + →2 1 + ͒ value somewhat lower than that obtained in a previous measurement more than 25 years ago made using the same technique but with a smaller volume germanium detector. In addition, we report a semimicroscopic reanalysis of recent 18 Ne+ 197 Au data on the 0 g.s. + →2 1 + transition in 18 Ne and compare the B͑E2;0 g.s. + →2 1 + ͒ results obtained using the two experimental techniques. The comparison between the two methods demonstrates the need for a basis for setting the imaginary part of the optical model potential in the analysis of the scattering experiment before reliable B͑E2;0 g.s. + →2 1 + ͒ values can be extracted by inelastic scattering when nuclear scattering contributions are significant. The optical model potential could be fixed via a detailed elastic scattering measurement.The relationship between the electromagnetic matrix elements B͑E2;0 g.s. + →2 1 + ͒ in the mirror nuclei 18 O and 18 Ne plays an important role in our understanding of core polarization since each of these isotopes has a pair of identical nucleons outside the doubly-magic 16 O core (for example, see Ref.[1]). In addition, these two matrix elements, when taken together with the corresponding matrix element for the analog transition in the N=Z nucleus 18 F, provide a test of isospin purity in the mass 18 system [2,3]. The degree of isospin purity has important implications for our understanding of Coulomb energies [1], -decay matrix elements [4], and nuclear interaction symmetries [5].For the stable isotope 18 O, the B͑E2;0 g.s. + →2 1 + ͒ value is known with considerable precision. It is not surprising that the situation for 18 Ne is much less clear since it is unstable. A measurement of the lifetime of the 2 1 + state in 18 Ne was performed by McDonald et al. [6] using the Doppler shift attenuation method (DSAM) and the 3 He͑ 16 O,n͒ reaction. It is worth noting that this experiment was limited by the detector technology available at that time-Ge detector volumes were much smaller than those available now and Compton suppression was not available. The limitation on detector volume was a particular handicap because the 2 1 + →0 g.s. + ␥ ray has a rather large energy of 1.887 MeV. The result reported in Ref.[6] is B͑E2;0 g.s. + →2 1 + ͒=260±25 e 2 fm 4 . A measurement of the 0 g.s. + →2 1 + transition in 18 Ne using the 18 Ne+ 197 Au reaction with a 65 MeV/nucleon beam of the radioactive isotope 18 Ne cast doubt on the previous B͑E2;0 g.s. + →2 1 + ͒ result. Riley et al.[3] measured an integrated cross section for the excitation of the 2 1 + state in 18 Ne in the forward angle ͑ lab Ͻ4.0°͒ scattering of 18 Ne from 197 Au at 65 MeV/nucleon. The data were analyzed using a macroscopic model that included both Coulomb and nuclear excitation mechanisms. They did not have an opportu...