111 research outputs found

    Structure des isotopes de bore et de carbone riches en neutrons aux limites de la stabilité

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    The unbound nuclei 18B and 21C have been studied in an experiment undertaken at the RIBF-RIKEN using the recently commissioned SAMURAI spectrometer and NEBULA neutron array. The two systems were probed using single-neutron and single and two-proton knockout from secondary beams of 22C, 22N, et 23O respectively in the case of 21C and 19B, 19C and 20N for 18B. The invariant mass spectra were reconstructed from the momentum of the fragment (17B, 20C) and neutron. In order to interpret the results a complete simulation of the experimental setup was utilised. The analysis procedures as well as the calibrations were verified through a measurement of the well-known ground state of 16B. In the case of 18B three states were observed: an s-wave virtual state (as < -50 fm), an l=2 resonance at Er =0.77 +- 0.09 MeV and an l=0 resonance at Er = 1.6 +- 0.6 MeV. These results suggest that the low-lying level structure of 18B is governed by a competition between the neutron 2s1/2 and 1d5/2 configurations. In the case of 21C resonances were observed at Er = 0.8 +- 0.15 MeV (l = 0) and Er = 1.5 +-0.1 MeV (l=2), a result which confirms predictions of an inversion of the 5/2+ and 1/2+ levels. Finally an analysis of the momentum distributions for 18B and 21C produced in single-neutron knockout was carried out. The results indicate that the valence neutrons 19B and 22C are in mixed (2s1/2)2 and (1d5/2)2 configurations. Les noyaux non liĂ©s 18B et 21C sont Ă©tudiĂ©s suite Ă  une expĂ©rience rĂ©alisĂ©e au RIBF-RIKEN en utilisant le nouveau spectromĂštre SAMURAI couplĂ© au dĂ©tecteur neutron NEBULA. Ces systĂšmes furent sondĂ©s grĂące Ă  des rĂ©actions de knock-out d'un neutron , d'un proton et de deux protons, Ă  partir de faisceaux secondaires de 22C, 22N, et 23O pour le 21C et de 19B , 19C, et 20N pour le 18B. La masse invariante fut reconstruite Ă  partir des moments du fragment chargĂ© (17B, 20C) et du neutron. Afin de pouvoir interprĂ©ter les rĂ©sultats, une simulation complĂšte du dispositif expĂ©rimental fut utilisĂ©e. L'Ă©talonnage des dĂ©tecteurs et les techniques d’analyse furent testĂ©s en sondant l'Ă©tat fondamental connu du 16B. Dans le cas du 18B trois Ă©tats furent observĂ©s : un Ă©tat s virtuel (as < -50 fm), rĂ©sonance l=2 Ă  Er =0.77 +- 0.09 MeV et une rĂ©sonance l=0 Ă  Er = 1.6 +- 0.6 MeV. Ces rĂ©sultats plaident en faveur d'un mĂ©lange de configuration des niveaux neutron 2s1/2 et 1d5/2. En ce qui concerne le 21C, deux Ă©tats rĂ©sonnant respectivement situĂ©s Ă  Er = 0.8 +- 0.15 MeV (l = 0) et Er = 1.5 +-0.1 MeV (l=2) furent observĂ©s. L'ordre confirme les rĂ©sultats thĂ©oriques prĂ©disant l'inversion des niveaux 5/2+ et 1/2+. Une analyse en impulsion reconstruite des systĂšmes 18B et 21C, produits par la rĂ©action de knock-out d’un neutron a Ă©tĂ© rĂ©alisĂ©e. Les rĂ©sultats soutiennent un mĂ©lange de configurations neutrons de valence (2s1/2)2 et (1d5/2)2 pour ces deux noyaux Ă  halo.  

    Silent and equivalent magnetic distributions on thin plates

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    International audienceIn geosciences and paleomagnetism, estimating the remanent magnetization in old rocks is an important issue to study past evolution of the Earth and other planets or bodies. However, the magnetization cannot be directly measured and only the magnetic field that it produces can be recorded.In this paper we consider the case of thin samples, to be modeled as a planar set S of R^2&nbsp;x&nbsp;{0}, carrying a magnetization m (a 3-dimensional vector field supported on S). This setup is typical of scanning microscopy that was developed recently to measure a single component of a weak magnetic field, close to the sample. Specifically, one is given a record of b_3[m] (tiny: a few nano Teslas), the vertical component of the magnetic field produced by m, on a planar region Q of R^2&nbsp;x&nbsp;{h} located at some fixed height h &gt; 0 above the sample plane. We assume that both S and Q are Lipschitz-smooth bounded connected open sets in their respective planes, and that the magnetization m belongs to [L^2(S)]^3, whence b_3[m] belongs to L^2(Q). Such magnetizations possess net moments &lt;m&gt; (belonging to R^3) defined as their integral on S.Recovering the magnetization m or its net moment &lt;m&gt; from available measurements of b_3[m] are inverse problems for the Poisson-Laplace equation in the upper half-space R^3_+ with right hand side in divergence form. Indeed, Maxwell's equations in the quasi-static approximation identify the divergence of m with the Laplacian of a scalar magnetic potential in R^3_+ whose normal derivative on Q coincides with b_3[m]. Hence Neumann data b_3[m] are available on Q (subset of R^3_+), and we aim at recovering m or &lt;m&gt; on S. We thus face recovery issues on the boundary of the harmonicity domain from (partial) data available inside.Such inverse problems are typically ill-posed and call for regularization. Indeed, magnetization recovery is not even unique, due to the existence of silent sources m != 0 such that b_3[m] = 0. And though such sources have vanishing moment so that net moment recovery is unique, estimation of the latter turns out to be unstable with respect to measurements errors.The present work investigates silent sources, equivalent magnetization of minimal L^2(S)-norm to some given m in [L^2(S)]^3 (two magnetizations are called equivalent if their difference is silent), as well as density / instability results

    Dipole localization in Moon rocks from sparse magnetic data

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    International audienceWe consider dipole recovery issues from sparse magnetic data, with the use of best quadratic rational approximation techniques, together with geometrical and algebraic properties of the poles of the approximants

    Dipole recovery from sparse measurements of its field on a cylindrical geometry

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    International audienceWe consider the inverse problem of recovering the position and moment of a magnetic dipolefrom sparse measurements of the field it generates, known on sections of three orthogonal cylindersenclosing it. This problem is motivated by recent measurements performed on Moon rocks, in viewof determining their magnetic properties. The key ingredient of the presented method is the useof rational approximation techniques, together with properties of the poles of the approximants, inorder to estimate the position of the dipole

    Asymptotic method for estimating magnetic moments from field measurements on a planar grid

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    Scanning magnetic microscopes typically measure the vertical component B_3 of the magnetic field on a horizontal rectangular grid at close proximity to the sample. This feature makes them valuable instruments for analyzing magnetized materials at fine spatial scales, e.g., in geosciences to access ancient magnetic records that might be preserved in rocks by mapping the external magnetic field generated by the magnetization within a rock sample. Recovering basic characteristics of the magnetization (such as its net moment, i.e., the integral of the magnetization over the sample's volume) is an important problem, specifically when the field is too weak or the magnetization too complex to be reliably measured by standard bulk moment magnetometers.In this paper, we establish formulas, asymptotically exact when R goes large, linking the integral of x_1 B_3, x_2 B_3, and B_3 over a square region of size R to the first, second, and third component of the net moment (and higher moments), respectively, of the magnetization generating B_3. The considered square regions are centered at the origin and have sides either parallel to the axes or making a 45-degree angle with them. Differences between the exact integrals and their approximations by these asymptotic formulas are explicitly estimated, allowing one to establish rigorous bounds on the errors.We show how the formulas can be used for numerically estimating the net moment, so as to effectively use scanning magnetic microscopes as moment magnetometers. Illustrations of the method are provided using synthetic examples

    Wavelength-scale stationary-wave integrated Fourier-transform spectrometry

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    Spectrometry is a general physical-analysis approach for investigating light-matter interactions. However, the complex designs of existing spectrometers render them resistant to simplification and miniaturization, both of which are vital for applications in micro- and nanotechnology and which are now undergoing intensive research. Stationary-wave integrated Fourier-transform spectrometry (SWIFTS)-an approach based on direct intensity detection of a standing wave resulting from either reflection (as in the principle of colour photography by Gabriel Lippmann) or counterpropagative interference phenomenon-is expected to be able to overcome this drawback. Here, we present a SWIFTS-based spectrometer relying on an original optical near-field detection method in which optical nanoprobes are used to sample directly the evanescent standing wave in the waveguide. Combined with integrated optics, we report a way of reducing the volume of the spectrometer to a few hundreds of cubic wavelengths. This is the first attempt, using SWIFTS, to produce a very small integrated one-dimensional spectrometer suitable for applications where microspectrometers are essential

    Response to rituximab induction is a predictive marker in B-cell post-transplant lymphoproliferative disorder and allows successful stratification into rituximab or r-chop consolidation in an international, prospective, multicenter Phase II trial

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    Purpose The Sequential Treatment of CD20-Positive Posttransplant Lymphoproliferative Disorder (PTLD-1) trial ( ClinicalTrials.gov identifier, NCT01458548) established sequential treatment with four cycles of rituximab followed by four cycles of cyclophosphamide, doxorubicin, vincristine, and prednisone (CHOP) chemotherapy as a standard in the management of post-transplant lymphoproliferative disorder (PTLD) and identified response to rituximab induction as a prognostic factor for overall survival. We hypothesized that rituximab consolidation might be sufficient treatment for patients with a complete response after rituximab induction. Patients and Methods In this prospective, international, multicenter phase II trial, 152 treatment-naive adult solid organ transplant recipients, with CD20+ PTLD unresponsive to immunosuppression reduction, were treated with four weekly doses of rituximab induction. After restaging, complete responders continued with four courses of rituximab consolidation every 21 days; all others received four courses of rituximab plus CHOP chemotherapy every 21 days. The primary end point was treatment efficacy measured as the response rate in patients who completed therapy and the response duration in those who completed therapy and responded. Secondary end points were frequency of infections, treatment-related mortality, and overall survival in the intention-to-treat population. Results One hundred eleven of 126 patients had a complete or partial response (88%; 95% CI, 81% to 93%), of whom 88 had a complete response (70%; 95% CI, 61% to 77%). Median response duration was not reached. The 3-year estimate was 82% (95% CI, 74% to 90%). Median overall survival was 6.6 years (95% CI, 5.5 to 7.6 years). The frequency of grade 3 or 4 infections and of treatment-related mortality was 34% (95% CI, 27% to 42%) and 8% (95% CI, 5% to 14%), respectively. Response to rituximab induction remained a prognostic factor for overall survival despite treatment stratification. Conclusion In B-cell PTLD, treatment stratification into rituximab or rituximab plus CHOP consolidation on the basis of response to rituximab induction is feasible, safe, and effective
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