187 research outputs found
Quantum phases of atomic boson-fermion mixtures in optical lattices
The zero-temperature phase diagram of a binary mixture of bosonic and
fermionic atoms in an one-dimensional optical lattice is studied in the
framework of the Bose-Fermi-Hubbard model. By exact numerical solution of the
associated eigenvalue problems, ground state observables and the response to an
external phase twist are evaluated. The stiffnesses under phase variations
provide measures for the boson superfluid fraction and the fermionic Drude
weight. Several distinct quantum phases are identified as function of the
strength of the repulsive boson-boson and the boson-fermion interaction.
Besides the bosonic Mott-insulator phase, two other insulating phases are
found, where both the bosonic superfluid fraction and the fermionic Drude
weight vanish simultaneously. One of these double-insulator phases exhibits a
crystalline diagonal long-range order, while the other is characterized by
spatial separation of the two species.Comment: 4 pages, 3 figures, using REVTEX
Geochemical and physical sources of radon variation in a subterranean estuary — implications for groundwater radon activities in submarine groundwater discharge studies
Author Posting. © Elsevier B.V., 2007. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Marine Chemistry 110 (2008): 120-127, doi:10.1016/j.marchem.2008.02.011.Submarine groundwater discharge (SGD), in form of springs and diffuse seepage,
has long been recognized as a source of chemical constituents to the coastal ocean.
Because groundwater is two to four orders of magnitude richer in radon than surface
water, it has been used as both a qualitative and a quantitative tracer of groundwater
discharge. Besides this large activity gradient, the other perceived advantage of radon
stems from its classification as noble gas; that is, its chemical behavior is expected not to
be influenced by salinity, redox, and diagenetic conditions present in aquatic
environments.
During our three-year monthly sampling of the subterranean estuary (STE) in
Waquoit Bay, MA, we found highly variable radon activities (50-1600 dpm L-1) across
the fresh-saline interface of the aquifer. We monitored pore water chemistry and radon
activity at 8 fixed depths spanning from 2 to 5.6 m across the STE, and found seasonal
fluctuations in activity at depths where elevated radon was observed. We postulate that
most of pore water 222Rn is produced from particle-surface bound 226Ra, and that the
accumulation of this radium is likely regulated by the presence of manganese
(hydr)oxides. Layers of manganese (hydr)oxides form at the salinity transition zone
(STZ), where water with high salinity, high manganese, and low redox potential mixes
with fresh water. Responding to the seasonality of aquifer recharge, the location of the
STZ and the layers with radium enriched manganese (hydr)oxide follows the seasonal
land- or bay-ward movement of the freshwater lens. This results in seasonal changes in
the depth where elevated radon activities are observed.
The conclusion of our study is that the freshwater part of the STE has a radon
signature that is completely different from the STZ or recirculated sea water. Therefore,
the radon activity in SGD will depend on the ratio of fresh and recirculated seawater in
the discharging groundwater.This work is a
result of research sponsored by NSF (OCE- 0425061 to M.A.C.) and the WHOI
Postdoctoral Scholar program (to H.D.)
Isotopic, geophysical and biogeochemical investigation of submarine groundwater discharge : IAEA-UNESCO intercomparison exercise at Mauritius Island
Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of Environmental Radioactivity 104 (2012): 24-45, doi:10.1016/j.jenvrad.2011.09.009.Submarine groundwater discharge (SGD) into a shallow lagoon on the west coast of Mauritius Island (Flic-en-Flac) was
investigated using radioactive (3H, 222Rn, 223Ra, 224Ra, 226Ra, 228Ra) and stable (2H, 18O) isotopes and nutrients. SGD
intercomparison exercises were carried out to validate the various approaches used to measure SGD including radium and radon
measurements, seepage-rate measurements using manual and automated meters, sediment bulk conductivity and salinity surveys.
SGD measurements using benthic chambers placed on the floor of the Flic-en-Flac Lagoon showed discharge rates up to 500
cm/day. Large variability in SGD was observed over distances of a few meters, which were attributed to different
geomorphological features. Deployments of automated seepage meters captured the spatial and temporal variability of SGD with
a mean seepage rate of 10 cm/day. The stable isotopic composition of submarine waters was characterized by significant
variability and heavy isotope enrichment and was used to predict the contribution of fresh terrestrially derived groundwater to
SGD (range from a few % to almost 100 %). The integrated SGD flux, estimated from seepage meters placed parallel to the
shoreline, was 35 m3/m day, which was in a reasonable agreement with results obtained from hydrologic water balance
calculation (26 m3/m day). SGD calculated from the radon inventory method using in situ radon measurements were between 5
and 56 m3/m per day. Low concentrations of radium isotopes observed in the lagoon water reflected the low abundance of U and
Th in the basalt that makes up the island. High SGD rates contribute to high nutrients loading to the lagoon, potentially leading to
eutrophication. Each of the applied methods yielded unique information about the character and magnitude of SGD. The results
of the intercomparison studies have resulted a better understanding of groundwater-seawater interactions in coastal regions. Such
information is an important pre-requisite for the protection management of coastal freshwater resources.The
financial support provided by the IOC and IHP of UNESCO for travel arrangements, and by the IAEA’s Marine
Environment Laboratories for logistics is highly acknowledged. MAC and MEG were supported in part by the US
National Science Foundation (OCE-0425061 and OCE-0751525). PPP acknowledges a support provided by the EU
Research & Development Operational Program funded by the ERDF (project No. 26240220004), and the Slovak
Scientific Agency VEGA (grant No. 1/108/08). The International Atomic Energy Agency is grateful to the
Government of the Principality of Monaco for support provided to its Marine Environment Laboratories
Phase Diagram of Bosonic Atoms in Two-Color Superlattices
We investigate the zero temperature phase diagram of a gas of bosonic atoms
in one- and two-color standing-wave lattices in the framework of the
Bose-Hubbard model. We first introduce some relevant physical quantities;
superfluid fraction, condensate fraction, quasimomentum distribution, and
matter-wave interference pattern. We then discuss the relationships between
them on the formal level and show that the superfluid fraction, which is the
relevant order parameter for the superfluid to Mott-insulator transition,
cannot be probed directly via the matter wave interference patterns. The formal
considerations are supported by exact numerical solutions of the Bose-Hubbard
model for uniform one-dimensional systems. We then map out the phase diagram of
bosons in non-uniform lattices. The emphasis is on optical two-color
superlattices which exhibit a sinusoidal modulation of the well depth and can
be easily realized experimentally. From the study of the superfluid fraction,
the energy gap, and other quantities we identify new zero-temperature phases,
including a localized and a quasi Bose-glass phase, and discuss prospects for
their experimental observation.Comment: 18 pages, 17 figures, using REVTEX
Abundances of the elements in the solar system
A review of the abundances and condensation temperatures of the elements and
their nuclides in the solar nebula and in chondritic meteorites. Abundances of
the elements in some neighboring stars are also discussed.Comment: 42 pages, 11 tables, 8 figures, chapter, In Landolt- B\"ornstein, New
Series, Vol. VI/4B, Chap. 4.4, J.E. Tr\"umper (ed.), Berlin, Heidelberg, New
York: Springer-Verlag, p. 560-63
Measurement of the Charged Multiplicities in b, c and Light Quark Events from Z0 Decays
Average charged multiplicities have been measured separately in , and
light quark () events from decays measured in the SLD experiment.
Impact parameters of charged tracks were used to select enriched samples of
and light quark events, and reconstructed charmed mesons were used to select
quark events. We measured the charged multiplicities:
,
, from
which we derived the differences between the total average charged
multiplicities of or quark events and light quark events: and . We compared
these measurements with those at lower center-of-mass energies and with
perturbative QCD predictions. These combined results are in agreement with the
QCD expectations and disfavor the hypothesis of flavor-independent
fragmentation.Comment: 19 pages LaTex, 4 EPS figures, to appear in Physics Letters
Evidence for an Excess of Soft Photons in Hadronic Decays of Z^0
Soft photons inside hadronic jets converted in front of the DELPHI main
tracker (TPC) in events of qqbar disintegrations of the Z^0 were studied in the
kinematic range 0.2 < E_gamma < 1 GeV and transverse momentum with respect to
the closest jet direction p_T < 80 MeV/c. A clear excess of photons in the
experimental data as compared to the Monte Carlo predictions is observed. This
excess (uncorrected for the photon detection efficiency) is (1.17 +/- 0.06 +/-
0.27) x 10^{-3} gamma/jet in the specified kinematic region, while the expected
level of the inner hadronic bremsstrahlung (which is not included in the Monte
Carlo) is (0.340 +/- 0.001 +/- 0.038) x 10^{-3} gamma/jet. The ratio of the
excess to the predicted bremsstrahlung rate is then (3.4 +/- 0.2 +/- 0.8),
which is similar in strength to the anomalous soft photon signal observed in
fixed target experiments with hadronic beams.Comment: 37 pages, 9 figures, Accepted by Eur. Phys. J.
Search for the standard model Higgs boson decaying to a pair in events with no charged leptons and large missing transverse energy using the full CDF data set
We report on a search for the standard model Higgs boson produced in
association with a vector boson in the full data set of proton-antiproton
collisions at TeV recorded by the CDF II detector at the
Tevatron, corresponding to an integrated luminosity of 9.45 fb. We
consider events having no identified charged lepton, a transverse energy
imbalance, and two or three jets, of which at least one is consistent with
originating from the decay of a quark. We place 95% credibility level upper
limits on the production cross section times standard model branching fraction
for several mass hypotheses between 90 and . For a Higgs
boson mass of , the observed (expected) limit is 6.7
(3.6) times the standard model prediction.Comment: Accepted by Phys. Rev. Let
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