1,382 research outputs found
Graphing and communicating compositional data in high dimensions
Visualization of data becomes more challenging as the dimensionality of the data increases,
impacting not only the display of the data itself but also the modeling results.
This paper discusses common visualization techniques for compositional data. None of them
seem to be well suited for changes in compositions that depend on either a metric covariate or a
factor. The clr-deviation chart as a chart with a factor or covariate as abscissa and all centered log
ratio-transformed component values superimposed on the ordinate axis is then introduced jointly
with the clr-component chart. The clr-deviation chart takes advantage of the sum-equals-zero
property of clr-transformed compositional data. It has some theoretical and practical advantages
over alternatives and one major disadvantage – an arbitrarily scaled ordinate axis; its properties
are discussed.
The usefulness of the methods are illustrated using an example analyzing the changes of proportions of the different diseases treated by hospitalization over a period of 13 years in Germany
Mapping Itinerant Electrons around Kondo Impurities
We investigate single Fe and Co atoms buried below a Cu(100) surface using
low temperature scanning tunneling spectroscopy. By mapping the local density
of states of the itinerant electrons at the surface, the Kondo resonance near
the Fermi energy is analyzed. Probing bulk impurities in this well-defined
scattering geometry allows separating the physics of the Kondo system and the
measuring process. The line shape of the Kondo signature shows an oscillatory
behavior as a function of depth of the impurity as well as a function of
lateral distance. The oscillation period along the different directions reveals
that the spectral function of the itinerant electrons is anisotropic.Comment: 5 pages, 4 figures, accepted by Physical Review Letter
UHF and VHF radar observations of thunderstorms
A study of thunderstorms was made in the Summer of 1985 with the 430-MHz and 50-MHz radars at the Arecibo Observatory in Puerto Rico. Both radars use the 300-meter dish, which gives a beam width of less than 2 degrees even at these long wavelengths. Though the radars are steerable, only vertical beams were used in this experiment. The height resolution was 300 and 150 meters for the UHF and VHF, respectively. Lightning echoes, as well as returns from precipitation and clear-air turbulence were detected with both wavelengths. Large increases in the returned power were found to be coincident with increasing downward vertical velocities at UHF, whereas at VHF the total power returned was relatively constant during the life of a storm. This was attributed to the fact that the VHF is more sensitive to scattering from the turbulence-induced inhomogeneities in the refractive index and less sensitive to scatter from precipitation particles. On occasion, the shape of the Doppler spectra was observed to change with the occurrence of a lightning discharge in the pulse volume. Though the total power and mean reflectivity weighted Doppler velocity changed little during these events, the power is Doppler frequency bins near that corresponding to the updraft did increase substantially within a fraction of a second after a discharge was detected in the beam. This suggests some interaction between precipitation and lightning
Evidence for charge orbital and spin stripe order in an overdoped manganite
We present diffraction data on a single-layered manganite
La(0.42)Sr(1.58)MnO4 with hole doping (x>0.5). Overdoped La(0.42)Sr(1.58)MnO4
exhibits a complex ordering of charges, orbitals and spins. Single crystal
neutron diffraction experiments reveal three incommensurate and one
commensurate order parameters to be tightly coupled. The position and the shape
of the distinct superstructure scattering points to a stripe arrangement in
which ferromagnetic zigzag chains are disrupted by additional Mn4+ stripes
The Voltage-Gated Proton Channel Hv1 Has Two Pores, Each Controlled by One Voltage Sensor
SummaryIn voltage-gated channels, ions flow through a single pore located at the interface between membrane-spanning pore domains from each of four subunits, and the gates of the pore are controlled by four peripheral voltage-sensing domains. In a striking exception, the newly discovered voltage-gated Hv1 proton channels lack a homologous pore domain, leaving the location of the pore unknown. Also unknown are the number of subunits and the mechanism of gating. We find that Hv1 is a dimer and that each subunit contains its own pore and gate, which is controlled by its own voltage sensor. Our experiments show that the cytosolic domain of the channel is necessary and sufficient for dimerization and that the transmembrane part of the channel is functional also when monomerized. The results suggest a mechanism of gating whereby the voltage sensor and gate are one and the same
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