Gamow shell-model calculations of drip-line oxygen isotopes

We employ the Gamow shell model (GSM) to describe low-lying states of the oxygen isotopes O24 and O25. The many-body Schrödinger equation is solved starting from a two-body Hamiltonian defined by a renormalized low-momentum nucleon-nucleon (NN) interaction and a spherical Berggren basis. The Berggren basis treats bound, resonant, and continuum states on an equal footing and is therefore an appropriate representation of loosely bound and unbound nuclear states near threshold. We show that the inclusion of continuum effects has a significant effect on the low-lying 1+ and 2+ excited states in O24. On the other hand, we find that a correct description of binding energy systematics of the ground states is driven by the proper treatment and inclusion of many-body correlation effects. This is supported by the fact that we get O25 unstable with respect to O24 in both oscillator and Berggren representations starting from a O22 core. Furthermore, we show that the structure of these loosely bound or unbound isotopes is strongly influenced by the 1S0 component of the NN interaction. This has important consequences for our understanding of nuclear stability.