369 research outputs found
Comment on ``Confirmation of the Sigma Meson''
We comment on the recent paper by N.A. Tornqvist and M. Roos published in
Phys. Rev. Lett. 76, 1575 (1996).Comment: 3 pages (LaTeX), 1 PostScript Figur
Estimating sigma-meson couplings from D \to 3\pi decays
Using recent experimental evidence from E791 on the sigma meson in D \to 3\pi
decays, we study the relevant couplings in D \to \sigma \pi and \sigma \to \pi\
pi within the accepted theoretical framework for non leptonic D decays. We also
review the linear sigma model, finding that it gives a description which is
consistent with the experimental data.Comment: 6 pages, no figures. Final version accepted for publication as a
Brief Report in Physical Review
Measuring rates of present-day relative sea-level rise in low-elevation coastal zones: a critical evaluation
Although tide gauges are the primary source of data used to
calculate multi-decadal- to century-scale rates of relative sea-level change,
we question the usefulness of tide-gauge data in rapidly subsiding
low-elevation coastal zones (LECZs). Tide gauges measure relative sea-level
rise (RSLR) with respect to the base of associated benchmarks. Focusing on
coastal Louisiana, the largest LECZ in the United States, we find that these
benchmarks (n=35) are anchored an average of 21.5 m below the land
surface. Because at least 60 % of subsidence occurs in the top 5 m of
the sediment column in this area, tide gauges in coastal Louisiana do not
capture the primary contributor to RSLR. Similarly, global navigation
satellite system (GNSS) stations (n=10) are anchored an average of
> 14.3 m below the land surface and therefore also do not
capture shallow subsidence. As a result, tide gauges and GNSS stations in
coastal Louisiana, and likely in LECZs worldwide, systematically
underestimate rates of RSLR as experienced at the land surface. We present an
alternative approach that explicitly measures RSLR in LECZs with respect to
the land surface and eliminates the need for tide-gauge data in this context.
Shallow subsidence is measured by rod surface-elevation table–marker horizons
(RSET-MHs) and added to measurements of deep subsidence from GNSS data, plus
sea-level rise from satellite altimetry. We show that for an LECZ the size of
coastal Louisiana (25 000–30 000 km2), about 40 RSET-MH instruments
suffice to collect useful data. Rates of RSLR obtained from this approach are
substantially higher than rates as inferred from tide-gauge data. We
therefore conclude that LECZs may be at higher risk of flooding within a
shorter time horizon than previously assumed.</p
On Deusons or Deuteronlike Meson-Meson Bound States
The systematics of deuteronlike two-meson bound states, {\it deusons}, is
discussed. Previous arguments that many of the present non- states are
such states are elaborated including, in particular, the tensor potential. For
pseudoscalar states the important observation is made that the centrifugal
barrier from the P-wave can be overcome by the and terms of the
tensor potential. In the heavy meson sector one-pion exchange alone is strong
enough to form at least deuteron-like and composites
bound by approximately 50 MeV, while and states are
expected near the threshold.Comment: Invited talk at the Hadron93 International Conf. on Hadron
Spectroscopy, Como, Italy 22.-25.6. 1993. 5 pages in LATEX HU-SEFT R 1993-13
Baryons with Two Heavy Quarks as Solitons
Using the chiral soliton model and heavy quark symmetry we study baryons
containing two heavy quarks. If there exists a stable (under strong
interactions) meson consisting of two heavy quarks and two light ones, then we
find that there always exists a state of this meson bound to a chiral soliton
and to a chiral anti-soliton, corresponding to a two heavy quark baryon and a
baryon containing two heavy anti-quarks and five light quarks, or a
``heptaquark".Comment: 7 pages and 2 postscript figures appended, LaTex, UCI-TR 94-3
Mechanism for a next-to-lowest lying scalar meson nonet
Recent work suggests the existence of a non-conventional lowest-lying scalar
nonet containing the a0(980). Then the a0(1450) and also the K0*(1430) are
likely candidates to belong to a conventional p-wave nonet. However
a comparison of their properties with those expected on this basis reveals a
number of puzzling features. It is pointed out that these puzzles can be
resolved in a natural and robust way by assuming a ``bare'' conventional p-wave
scalar nonet to mix with a lighter four quark
scalar nonet to form new ``physical'' states. The essential mechanism is driven
by the fact that the isospinor is lighter than the isovector in the unmixed multiplet.Comment: 22 pages, 6 figure
Tracking the sea-level signature of the 8.2 ka cooling event: New constraints from the Mississippi Delta
The ever increasing need for accurate predictions of global environmental change under greenhouse conditions has sparked immense interest in an abrupt, century‐scale cooling around 8200 years ago, with a focal point in the North Atlantic and with hemispheric teleconnections. Despite considerable progress in the unraveling of this striking feature, including a conceivable driving mechanism (rapid drainage of proglacial Lake Agassiz/Ojibway and a resulting reduced strength of North Atlantic thermohaline circulation), several key questions remain unanswered. One salient aspect concerns the total amount of freshwater released during this catastrophic event, likely echoed by a near‐instantaneous eustatic sea‐level rise. So far, no attempts have been made to perform high‐resolution sea‐level studies that explicitly focus on this critical time interval. Here, we present new data from the Mississippi Delta suggestive of abrupt sea‐level rise associated with the 8.2 ka event. However, the amount of sea‐level rise was likely less than ∼1.2 m, corresponding to a meltwater volume of less than ∼4.3 1014 m3; values lower than estimates used by several recent studies
Another look at scattering in the scalar channel
We set up a general framework to describe scattering below 1 GeV
based on chiral low-energy expansion with possible spin-0 and 1 resonances.
Partial wave amplitudes are obtained with the method, which satisfy
unitarity, analyticity and approximate crossing symmetry. Comparison with the
phase shift data in the J=0 channel favors a scalar resonance near the
mass.Comment: 17 pages, 5 figures, REVTe
Comment on Intrinsic and dynamically generated scalar meson states
The scalar-meson assignments of Shakin and Wang in a generalized
Nambu--Jona-Lasinio model are contradicted by recent experimental information.
Also the strict distinction made by these authors between ``intrinsic'' and
``dynamically generated'' states is contested, as well as a number of other
statements.Comment: 7 pages, (v2 cosmetics, v3 corrections in one reference), to be
published in Phys.Rev.
Structure of scalar mesons and the Higgs sector of strong interaction
The scalar mesons , , and
together with the pseudo Goldstone bosons , , and may be
considered as the Higgs sector of strong interaction. After a long time of
uncertainty about the internal structure of the scalar mesons there now seems
to be consistency which is in line with the major parts of experimental
observations. Great progress has been made by introducing the unified model of
Close and T\"ornqvist. This model states that mesons below 1 GeV may be
understood as in S-wave with some in P-wave in the
center, further out they rearrange as and finally as meson-meson
states. The P-wave component inherent in the structure of the neutral scalar
mesons can be understood as a doorway state for the formation of the scalar
meson via two-photon fusion, whereas in nucleon Compton scattering these P-wave
components serve as intermediate states. The masses of the scalar mesons are
predicted in terms of spontaneous and explicit symmetry breaking.Comment: 5 figure
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