19,879 research outputs found

    Model independent analysis of semileptonic BB decays to DD^{**} for arbitrary new physics

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    We explore semileptonic BB decays to the four lightest excited charm mesons, D={D0,D1,D^{**} = \{D_0^*,\, D_1^*, D1,D2}D_1,\, D_2^*\}, for nonzero charged lepton mass and for all bcνˉb\to c \ell\bar\nu four-Fermi interactions, including calculation of the O(ΛQCD/mc,b){\cal O}(\Lambda_\text{QCD}/m_{c,b}) and O(αs){\cal O}(\alpha_s) corrections to the heavy quark limit for all form factors. In the heavy quark limit some form factors are suppressed at zero recoil, therefore, the O(ΛQCD/mc,b){\cal O}(\Lambda_\text{QCD}/m_{c,b}) corrections can be very important. The DD^{**} rates exhibit sensitivities to new physics in bcτνˉb\to c\tau\bar\nu mediated decays complementary to the DD and DD^* modes. Since they are also important backgrounds to BD()τνˉB\to D^{(*)}\tau\bar\nu, the correct interpretation of future semitauonic BD()B\to D^{(*)} rate measurements requires consistent treatment of both the DD^{**} backgrounds and the signals. Our results allow more precise and more reliable calculations of these BDνˉB\to D^{**}\ell\bar\nu decays, and are systematically improvable by better data on the ee and μ\mu modes. As an example, we show that the DD^{**} rates are more sensitive to a new cˉσμνb\bar c\, \sigma_{\mu\nu} b tensor interaction than the D()D^{(*)} rates.Comment: 17 pages, 4 figures, 5 tables; published versio

    Tensions and correlations in Vcb|V_{cb}| determinations

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    Recently several papers extracted Vcb|V_{cb}| using the Belle measurement of the exclusive BˉDνˉ\bar B \to D^* \ell\bar\nu unfolded differential decay rates, available for the first time. Depending on the theoretical inputs, some of the fits yield higher Vcb|V_{cb}| values, compatible with those from inclusive semileptonic BB decays. Since these four fits use mostly the same data, if their correlations were close to 100\%, the tension between them would be over 5σ5\sigma. We determine the correlations, find that the tension between the results is less than 3σ3\sigma, and explore what might lead to improving the consistency of the fits. We find that fits that yield the higher values of Vcb|V_{cb}|, also suggest large violations of heavy quark symmetry. These fits are also in tension with preliminary lattice QCD data on the form factors. Without additional experimental data or lattice QCD input, there are no set of assumptions under which the tension between exclusive and inclusive determinations of Vcb|V_{cb}| can be considered resolved.Comment: 5 pages, 3 figure

    New predictions for ΛbΛc\Lambda_b\to\Lambda_c semileptonic decays and tests of heavy quark symmetry

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    The heavy quark effective theory makes model independent predictions for semileptonic ΛbΛc\Lambda_b \to \Lambda_c decays in terms of a small set of parameters. No subleading Isgur-Wise function occurs at order ΛQCD/mc,b\Lambda_{\rm QCD}/m_{c,b}, and only two sub-subleading functions enter at order ΛQCD2/mc2\Lambda_{\rm QCD}^2/m_c^2. These features allow us to fit the form factors and decay rates calculated up to order ΛQCD2/mc2\Lambda_{\rm QCD}^2/m_c^2 to LHCb data and lattice QCD calculations. We derive a significantly more precise standard model prediction for the ratio B(ΛbΛcτνˉ)/B(ΛbΛcμνˉ){\cal B}(\Lambda_b\to \Lambda_c \tau\bar\nu) / {\cal B}(\Lambda_b\to \Lambda_c \mu\bar\nu) than prior results, and find the expansion in ΛQCD/mc\Lambda_{\rm QCD}/m_c well-behaved, addressing a long-standing question. Our results allow more precise and reliable calculations of ΛbΛcνˉ\Lambda_b\to \Lambda_c\ell\bar\nu rates, and are systematically improvable with better data on the μ\mu (or ee) modes.Comment: 5 pages, 7 figure

    Effects of experimental floods on periphyton and stream metabolism below a high dam in the Swiss Alps (River Spöl)

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    We investigated the effects of an experimental flood regime on periphyton and stream metabolism downstream of a large reservoir. Three floods took place in summer of 2000 and 2001 and two floods in summer of 2002. Residual flow in the River Spöl was <2.5 m3s-1. The experimental floods lasted 9 to 11 hours with peak flows ranging from 12 to 55 m3s-1. Periphyton was collected in the River Spöl (impact site) and in a reference stream in 1999 (pre-flood) and before and after each flood from 2000 to 2002. We measured ecosystem metabolism with the single station diel oxygen method a few days before and after floods in the River Spöl. Floods temporarily reduced periphyton biomass, but the disturbance impact and recovery patterns were not uniform among floods, thus resulting in high inter-annual variation in seasonal biomass patterns. The average periphyton biomass in the River Spöl even increased after a transient reduction in 2000. A principal component analysis indicated a persistent shift in the structure of the diatom community at the impact site. The floods reduced gross primary production and to minor extent ecosystem respiration, resulting in a transient decline in the P/R ratio. However, ecosystem metabolism recovered relatively fast. The new flow regime increased ecosystem dynamics, but it may take several years until the autotrophic energy base becomes adapted to the new and more dynamic flow regim

    Precise predictions for ΛbΛc\Lambda_b \to \Lambda_c semileptonic decays

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    We calculate the ΛbΛcν\Lambda_b \to \Lambda_c \ell \nu form factors and decay rates for all possible bcνˉb\to c \ell\bar\nu four-Fermi interactions beyond the Standard Model, including nonzero charged lepton masses and terms up to order αsΛQCD/mc,b\alpha_s\, \Lambda_\text{QCD}/m_{c,b} and ΛQCD2/mc2\Lambda_\text{QCD}^2/m_c^2 in the heavy quark effective theory. At this order, we obtain model independent predictions for semileptonic ΛbΛc\Lambda_b \to \Lambda_c decays in terms of only two unknown sub-subleading Isgur-Wise functions, which can be determined from fitting LHCb and lattice QCD data. We thus obtain model independent results for ΛbΛcνˉ\Lambda_b\to \Lambda_c\ell\bar\nu decays, including predictions for the ratio R(Λc)=B(ΛbΛcτνˉ)/B(ΛbΛcμνˉ)R(\Lambda_c) = {\cal B}(\Lambda_b\to \Lambda_c \tau\bar\nu) / {\cal B}(\Lambda_b\to \Lambda_c \mu\bar\nu) in the presence of new physics, that are more precise than prior results in the literature, and systematically improvable with better data on the decays with μ\mu (or ee) in the final state. We also explore tests of factorization in ΛbΛcπ\Lambda_b \to \Lambda_c\pi decays, and emphasize the importance of measuring at LHCb the double differential rate d2Γ(ΛbΛcνˉ)/(dq2dcosθ)d^2\Gamma(\Lambda_b\to\Lambda_c\ell\bar\nu) / (d q^2\, d\cos\theta), in addition to the q2q^2 spectrum.Comment: 30 pages, 7 figures, 1 tabl

    Laboratory evaluation of a rapid IgG4 antibody test (BLF Rapid™) for bancroftian filariasis

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    At the end phase of the Global Programme to Eliminate Lymphatic Filariasis, antibody testing may have a role in decision-making for bancroftian filariasis–endemic areas. This study evaluated the diagnostic performance of BLF Rapid ™ , a prototype immunochromatographic IgG4-based test using BmSXP recombinant protein, for detection of bancroftian filariasis. The test was evaluated using 258 serum samples, comprising 96 samples tested at Universiti Sains Malaysia (in-house) and 162 samples tested independently at three international laboratories in the USA and India, and two laboratories in Malaysia. The independent testing involved 99 samples from Wuchereria bancrofti microfilaria or antigen positive individuals and 63 samples from people who were healthy or had other infections. The in-house evaluation showed 100% diagnostic sensitivity and specificity. The independent evaluations showed a diagnostic sensitivity of 84–100% and 100% specificity (excluding non-lymphatic filarial infections). BLF Rapid has potential as a surveillance diagnostic tool to make “Transmission Assessment Survey”–stopping decisions and conduct post-elimination surveillance

    Crystal truncation rods in kinematical and dynamical x-ray diffraction theories

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    Crystal truncation rods calculated in the kinematical approximation are shown to quantitatively agree with the sum of the diffracted waves obtained in the two-beam dynamical calculations for different reflections along the rod. The choice and the number of these reflections are specified. The agreement extends down to at least 107\sim 10^{-7} of the peak intensity. For lower intensities, the accuracy of dynamical calculations is limited by truncation of the electron density at a mathematically planar surface, arising from the Fourier series expansion of the crystal polarizability

    The physico-chemical habitat template for periphyton in alpine glacial streams under a changing climate

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    The physico-chemical habitat template of glacial streams in the Alps is characterized by distinct and predictable changes between harsh and relatively benign periods. Spring and autumn were thought to be windows of favorable environmental conditions conducive for periphyton development. Periphyton biomass (measured as chlorophyll a and ash-free dry mass) was quantified in five glacial and three non-glacial streams over an annual cycle. One glacial stream was an outlet stream of a proglacial lake. In all glacial streams, seasonal patterns in periphyton were characterized by low biomass during summer high flow when high turbidity and transport of coarse sediment prevailed. With the end of icemelt in autumn, environmental conditions became more favorable and periphyton biomass increased. Biomass peaked between late September and January. In spring, low flow, low turbidity, and a lack of coarse sediment transport were not paralleled by an increase in periphyton biomass. In the non-glacial streams, seasonal periphyton patterns were similar to those of glacial streams, but biomass was significantly higher. Glacier recession from climate change may shift water sources in glacier streams and attenuate the glacial flow pulse. These changes could alter predicted periods of optimal periphyton development. The window of opportunity for periphyton accrual will shift earlier and extend into autumn in channels that retain surface flow
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