SwePub
Sök i SwePub databas

  Utökad sökning

Träfflista för sökning "WFRF:(Kiese P.) srt2:(2014)"

Sökning: WFRF:(Kiese P.) > (2014)

  • Resultat 1-5 av 5
Sortera/gruppera träfflistan
   
NumreringReferensOmslagsbildHitta
1.
  • Ablikim, M., et al. (författare)
  • Measurement of the $D\to K^-\pi^+$ strong phase difference in $\psi(3770)\to D^0\overline{D}{}^0$
  • 2014
  • Ingår i: PHYSICS LETTERS B. - : Elsevier BV. - 0370-2693. ; 734
  • Tidskriftsartikel (refereegranskat)abstract
    • We study $D^0\overline{D}{}^0$ pairs produced in $e^+e^-$ collisions at $\sqrt{s}=3.773$ GeV using a data sample of 2.92 fb$^{-1}$ collected with the BESIII detector. We measure the asymmetry $\mathcal{A}^{CP}_{K\pi}$ of the branching fractions of $D \to K^-\pi^+$ in $CP$-odd and $CP$-even eigenstates to be $(12.7\pm1.3\pm0.7)\times10^{-2}$. $\mathcal{A}^{CP}_{K\pi}$ can be used to extract the strong phase difference $\delta_{K\pi}$ between the doubly Cabibbo-suppressed process $\overline{D}{}^{0}\to K^-\pi^+$ and the Cabibbo-favored process $D^0\to K^- \pi^+$. Using world-average values of external parameters, we obtain $\cos\delta_{K\pi} = 1.02\pm0.11\pm0.06\pm0.01$. Here, the first and second uncertainties are statistical and systematic, respectively, while the third uncertainty arises from the external parameters. This is the most precise measurement of $\delta_{K\pi}$ to date.
  •  
2.
  • Ablikim, M., et al. (författare)
  • Observation of $e^+e^− → γX$(3872) at BESIII
  • 2014
  • Ingår i: PHYSICAL REVIEW LETTERS. - 1079-7114. ; 112:9
  • Tidskriftsartikel (refereegranskat)abstract
    • With data samples collected with the BESIII detector operating at the BEPCII storage ring at center-of-mass energies from 4.009 to 4.420 GeV, the process $e^{+} e^{-} \to \gamma X(3872)$ is observed for the first time with a statistical significance of $6.3\sigma$. The measured mass of the $X(3872)$ is ($3871.9\pm 0.7_{\rm stat.}\pm 0.2_{\rm sys.}$) MeV/$c^2$, in agreement with previous measurements. Measurements of the product of the cross section $\sigma[e^{+} e^{-} \to \gamma X(3872)]$ and the branching fraction $\mathcal{B}[X(3872) \to \pi^{+} \pi^{-} J/\psi]$ at center-of-mass energies 4.009, 4.229, 4.260, and 4.360 GeV are reported. Our measurements are consistent with expectations for the radiative transition process $Y(4260) \to \gamma X(3872)$.
  •  
3.
  • Ablikim, M., et al. (författare)
  • Observation of electromagnetic Dalitz decays J/\psi \to P e^+e^-
  • 2014
  • Ingår i: PHYSICAL REVIEW D. - 2470-0010 .- 1550-7998 .- 1550-2368. ; 89:9
  • Tidskriftsartikel (refereegranskat)abstract
    • Based on a sample of (225.3\pm2.8)\times 10^{6} J/\psi events collected with the BESIII detector, the electromagnetic Dalitz decays of J/\psi \to P e^+e^-(P=\eta'/\eta/\pi^0) are studied. By reconstructing the pseudoscalar mesons in various decay modes, the decays J/\psi \to \eta' e^+e^-, J/\psi \to \eta e^+e^- and J/\psi \to \pi^0 e^+e^- are observed for the first time. The branching fractions are determined to be \mathcal{B}(J/\psi\to \eta' e^+e^-) = (5.81\pm0.16\pm0.31)\times10^{-5}, \mathcal{B}(J/\psi\to \eta e^+e^-) = (1.16\pm0.07\pm0.06)\times10^{-5}, and \mathcal{B}(J/\psi\to \pi^0 e^+e^-)=(7.56\pm1.32\pm0.50)\times10^{-7}, where the first errors are statistical and the second ones systematic.
  •  
4.
  • Ablikim, M., et al. (författare)
  • Precision measurements of $B(D^+ \rightarrow \mu^+ \nu_{\mu})$, the pseudoscalar decay constant $f_{D^+}$, and the quark mixing matrix element $|V_{\rm cd}|$
  • 2014
  • Ingår i: PHYSICAL REVIEW D. - 2470-0010 .- 1550-7998 .- 1550-2368. ; 89:5
  • Tidskriftsartikel (refereegranskat)abstract
    • We report a measurement of the branching fraction $B(D^+ \rightarrow \mu^+ \nu_{\mu}) = [3.71 \pm 0.19 (\rm stat) \pm 0.06 (\rm sys)]\times 10^{-4}$ based on 2.92 ${\rm fb^{-1}}$ of data accumulated at $\sqrt{s}=3.773$ GeV with the BESIII detector at the BEPCII collider. This measurement, in conjunction with the Cabibbo-Kobayashi-Maskawa matrix element $|V_{\rm cd}|$ determined from a global Standard Model fit, implies a value for the weak decay constant $f_{D^+}=(203.2 \pm 5.3 \pm 1.8)$ MeV. Additionally, using this branching fraction measurement together with a Lattice QCD prediction for $f_{D^+}$, we find $|V_{\rm cd}|=0.2210\pm 0.0058 \pm 0.0047$. In either case, these are the most precise results for these quantities to date.
  •  
5.
  • Gharahi Ghehi, N., et al. (författare)
  • N2O and NO emission from the Nyungwe tropical highland rainforest in Rwanda
  • 2014
  • Ingår i: Geoderma Regional. - 2352-0094. ; 2-3, s. 41-49
  • Tidskriftsartikel (refereegranskat)abstract
    • Tropical forest soils are a significant source for N2O and NO. Current estimates of N2O and NO emissions are uncertain due to the limited number of fieldmeasurements and model input data. Furthermore, considerable spatial and temporal variability exists due to variation of soil properties, vegetation characteristics and meteorology.We used a process-based model (ForestDNDC-tropica) to estimate N2O and NO emissions from the entire (970 km2) tropical highland forest (Nyungwe) in southwestern Rwanda. Scaling these results to that regional level using legacy soil, meteorological and simulated vegetation data we found in most cases agreement between N2O and NO measurements and model predictions. Limited agreement was found for acid soils with high clay content and reduced metals, indicating that abiotic N2O and NO forming processes in acidic soils might be under-represented in the current ForestDNDC-tropica model. The Nyungwe forest was estimated to emit 439 t N2O-N year−1 (2.8– 5.5 kg N2O-N ha−1 year−1) and 244 t NO-N year−1 (0.8–5.1 kg N ha−1 year−1), corroborating previous studies in tropical forests and highlighting that also tropical highland rainforest soils are a major source of atmospheric N2O and NO. The uncertainty for the N2O and NO emission estimates was 153 and 50 t N2O-N year−1 and 36 and 16 t NO-N year−1 considering uncertainty in model input data and annual variability, respectively. The results showed that soil bulk density and pH were the most influential factors driving spatial variation and model uncertainty. To improve global model-based estimates of N2O and NO emission from tropical forest focus should therefore also be oriented in delivering more detailed soil and vegetation data.
  •  
Skapa referenser, mejla, bekava och länka
  • Resultat 1-5 av 5
Typ av publikation
tidskriftsartikel (5)
Typ av innehåll
refereegranskat (5)
Författare/redaktör
Liu, X (4)
Cakir, O. (4)
Cetin, S. A. (4)
Chen, X. (4)
Fang, Y. (4)
Huang, Y. (4)
visa fler...
Jin, S. (4)
Liu, D. (4)
Liu, J. B. (4)
Liu, K. (4)
Ouyang, Q. (4)
Peters, K. (4)
Wang, K. (4)
Xu, L. (4)
Yang, Y. (4)
Zhang, L. (4)
Zhemchugov, A. (4)
Zhou, L. (4)
Gao, Y. (4)
Liu, J. (4)
Ma, L. L. (4)
Guo, Y (4)
Huang, G. S. (4)
Qi, M. (4)
Zhang, Q. (4)
Kupsc, Andrzej (4)
Zhang, Y. (4)
Chen, G. (4)
Liu, Q. (4)
Wu, Z. (4)
Zeng, Y. (4)
Hu, Y. (4)
Cai, X. (4)
Wang, D. (4)
Ferroli, R. Baldini (4)
Wang, M. (4)
Li, G. (4)
Zhu, Y. C. (4)
Pan, Y. (4)
Wang, Z. (4)
Chen, H. -Y (4)
Varner, G. S. (4)
Yang, L. (4)
Zhu, S. (4)
Boyko, I. (4)
Dedovich, D. (4)
Lu, Y (4)
Wang, P. (4)
Han, S. (4)
Zhao, Q (4)
visa färre...
Lärosäte
Uppsala universitet (4)
Göteborgs universitet (1)
Språk
Engelska (5)
Forskningsämne (UKÄ/SCB)
Naturvetenskap (5)
År

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy