Baryon-Baryon Interactions

After a short survey of some topics of interest in the study of baryon-baryon scattering, the recent Nijmegen energy dependent partial wave analysis (PWA) of the nucleon-nucleon data is reviewed. In this PWA the energy range for both pp and np is now 0 < Tlab < 350 MeV and a chi^2_{d.o.f.}=1.08 was reached. The implications for the pion-nucleon coupling constants are discussed. Comments are made with respect to recent discussions around this coupling constant in the literature. In the second part, we briefly sketch the picture of the baryon in several, more or less QCD-based, quark-models that have been rather prominent in the literature. Inspired by these pictures we constructed a new soft-core model for the nucleon-nucleon interaction and present the first results of this model in a chi^2 -fit to the new multi-energy Nijmegen PWA. With this new model we succeeded in narrowing the gap between theory and experiment at low energies. For the energies Tlab = 25-320 MeV we reached a record low chi^2_{p.d.p.} = 1.16. We finish the paper with some conclusions and an outlook describing the extension of the new model to baryon-baryon scattering.Comment: 12 pages LaTeX and one postscript figure included. Invited talk presented at the XIVth European Conference of Few-Body Problems in Physics, Amsterdam, August 23-28, 199

Active Tension Network model suggests an exotic mechanical state realized in epithelial tissues.

Mechanical interactions play a crucial role in epithelial morphogenesis, yet understanding the complex mechanisms through which stress and deformation affect cell behavior remains an open problem. Here we formulate and analyze the Active Tension Network (ATN) model, which assumes that the mechanical balance of cells within a tissue is dominated by cortical tension and introduces tension-dependent active remodeling of the cortex. We find that ATNs exhibit unusual mechanical properties. Specifically, an ATN behaves as a fluid at short times, but at long times supports external tension like a solid. Furthermore, an ATN has an extensively degenerate equilibrium mechanical state associated with a discrete conformal - "isogonal" - deformation of cells. The ATN model predicts a constraint on equilibrium cell geometries, which we demonstrate to approximately hold in certain epithelial tissues. We further show that isogonal modes are observed in the fruit y embryo, accounting for the striking variability of apical areas of ventral cells and helping understand the early phase of gastrulation. Living matter realizes new and exotic mechanical states, the study of which helps to understand biological phenomena

Measurement of Multiply Substituted Isotopologues (\u27Clumped Isotopes\u27) of CO\u3csub\u3e2\u3c/sub\u3e using a 5 kV Compact Isotope Ratio Mass Spectrometer: Performance, Reference Frame, and Carbonate Paleothermometry

RATIONALE: The burgeoning field of \u27clumped isotope\u27 paleothermometry, which has broad applications in geosciences, depends almost entirely on measurements made on two types of mass spectrometer with the same ion source design. Demonstration that these measurements can be carried out on a retrofitted mass spectrometer with a different type of ion source is important to the growing community of geoscientists considering employing this technique. METHODS: We summarize the sample preparation techniques, mass spectrometry, and data processing involved in establishing an absolute reference frame for the measurement of Δ47 in CO2 from carbonate minerals using a prototype 5 kV mass spectrometer. The prototype differs from previously marketed mass spectrometers only in the presence of six extra Faraday cups designed specifically to measure ion beams of masses 44–49. We employ pressure baseline corrections on the small mass 47 signal. RESULTS: The system was fully capable of establishing absolute reference frames for clumped isotope carbonate paleothermometry, despite alternative use of the system for other types of measurements (carbonate δ18O and δ13C values, water δ18O and δ2H values via equilibration, and δ13C and δ15N values of sedimentary organic material) in different reference frames. Repeated measurements of CO2 from carbonate standards yielded external precisions comparable with those from other laboratories and adequate for paleothermometry to a precision of near or below ±5 °C. The accuracy was demonstrated by reasonable temperatures being obtained for different types of repeatedly measured carbonates. Measurements of the pressure baseline with every sample increased analysis times by 20 min, but decreased the stabilization time of the reference frame by days to weeks, while improving precision. CONCLUSIONS: Simple modifications to existing instrumentation will allow more laboratories to perform clumped isotope measurements. The prototype mass spectrometer used herein provides precision comparable with all published data. We show that, where negatively charged species are associated with large ion beams, making pressure baseline corrections with every measurement is increasingly important no matter what instrument is used