1,217 research outputs found

    Controlling Condensate Collapse and Expansion with an Optical Feshbach Resonance

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    We demonstrate control of the collapse and expansion of an 88Sr Bose-Einstein condensate using an optical Feshbach resonance (OFR) near the 1S0-3P1 intercombination transition at 689 nm. Significant changes in dynamics are caused by modifications of scattering length by up to +- ?10a_bg, where the background scattering length of 88Sr is a_bg = -2a0 (1a0 = 0.053 nm). Changes in scattering length are monitored through changes in the size of the condensate after a time-of-flight measurement. Because the background scattering length is close to zero, blue detuning of the OFR laser with respect to a photoassociative resonance leads to increased interaction energy and a faster condensate expansion, whereas red detuning triggers a collapse of the condensate. The results are modeled with the time-dependent nonlinear Gross-Pitaevskii equation.Comment: 5 pages, 3 figure

    Ultralong-Range Rydberg Molecules in a Divalent-Atomic System

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    We report the creation of ultralong-range Sr2_2 molecules comprising one ground-state 5s25s^2 1S0^1S_0 atom and one atom in a 5sns5sns 3S1^3S_1 Rydberg state for nn ranging from 29 to 36. Molecules are created in a trapped ultracold atomic gas using two-photon excitation near resonant with the 5s5p5s5p 3P1^3P_1 intermediate state, and their formation is detected through ground-state atom loss from the trap. The observed molecular binding energies are fit with the aid of first-order perturbation theory that utilizes a Fermi pseudopotential with effective ss-wave and pp-wave scattering lengths to describe the interaction between an excited Rydberg electron and a ground-state Sr atom.Comment: 5 pages, 2 figure

    Bose-Einstein Condensation of 88^{88}Sr Through Sympathetic Cooling with 87^{87}Sr

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    We report Bose-Einstein condensation of 88^{88}Sr, which has a small, negative s-wave scattering length (a88=−2a_{88}=-2\,a0a_0). We overcome the poor evaporative cooling characteristics of this isotope by sympathetic cooling with 87^{87}Sr atoms. 87^{87}Sr is effective in this role in spite of the fact that it is a fermion because of the large ground state degeneracy arising from a nuclear spin of I=9/2I=9/2, which reduces the impact of Pauli blocking of collisions. We observe a limited number of atoms in the condensate (Nmax≈104N_{max}\approx 10^4) that is consistent with the value of a88a_{88} and the optical dipole trap parameters.Comment: 4 pages, 4 figure

    Degenerate Fermi Gas of 87^{87}Sr

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    We report quantum degeneracy in a gas of ultra-cold fermionic 87^{87}Sr atoms. By evaporatively cooling a mixture of spin states in an optical dipole trap for 10.5\,s, we obtain samples well into the degenerate regime with T/TF=0.26−.06+.05T/T_F=0.26^{+.05}_{-.06}. The main signature of degeneracy is a change in the momentum distribution as measured by time-of-flight imaging, and we also observe a decrease in evaporation efficiency below T/TF∼0.5T/T_F \sim 0.5.Comment: 4 pages, 3 figure

    Rydberg dressed spin-1/2 Fermi gases in one dimension

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    The emergent phases of strongly correlated spin-1/2 Fermi gases of Rydberg dressed atoms in a one dimensional optical lattice are theoretically investigated. At weak coupling a bosonization description is used to demonstrate the ability to drive alternating quantum phase transitions between distinct Luttinger liquids. At strong coupling the ground state develops non-trivial phase separation exhibiting Luttinger liquid ''puddles'' separated by magnetic domain walls due to the interplay of the incommensurate filling and the Rydberg core length scale. These phases can be detected in ultracold gases of Rydberg atoms made from 6^6Li.Comment: 10 pages, 8 figure

    Simulation of underground gravity gradients from stochastic seismic fields

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    We present results obtained from a finite-element simulation of seismic displacement fields and of gravity gradients generated by those fields. The displacement field is constructed by a plane wave model with a 3D isotropic stochastic field and a 2D fundamental Rayleigh field. The plane wave model provides an accurate representation of stationary fields from distant sources. Underground gravity gradients are calculated as acceleration of a free test mass inside a cavity. The results are discussed in the context of gravity-gradient noise subtraction in third generation gravitational-wave detectors. Error analysis with respect to the density of the simulated grid leads to a derivation of an improved seismometer placement inside a 3D array which would be used in practice to monitor the seismic field.Comment: 24 pages, 12 figure
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