118 research outputs found

    An integrated model for the assessment of global water resources ? Part 1: Input meteorological forcing and natural hydrological cycle modules

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    International audienceAn integrated global water resources model was developed consisting of six modules: land surface hydrology, river routing, crop growth, reservoir operation, environmental flow requirement estimation, and anthropogenic water withdrawal. It simulates both natural and anthropogenic water flow globally (excluding Antarctica) on a daily basis at a spatial resolution of 1°×1° (longitude and latitude). The simulation period is 10 years, from 1986 to 1995. This first part of the two-feature report describes the input meteorological forcing and natural hydrological cycle modules of the integrated model, namely the land surface hydrology module and the river routing module. The input meteorological forcing was provided by the second Global Soil Wetness Project (GSWP2), an international land surface modeling project. Several reported shortcomings of the forcing component were improved. The land surface hydrology module was developed based on a bucket type model that simulates energy and water balance on land surfaces. Simulated runoff was compared and validated with observation-based global runoff data sets and observed streamflow records at 32 major river gauging stations around the world. Mean annual runoff agreed well with earlier studies at global, continental, and continental zonal mean scales, indicating the validity of the input meteorological data and land surface hydrology module. In individual basins, the mean bias was less than ±20% in 14 of the 32 river basins and less than ±50% in 24 of the basins. The performance was similar to the best available precedent studies with closure of energy and water. The timing of the peak in streamflow and the shape of monthly hydrographs were well simulated in most of the river basins when large lakes or reservoirs did not affect them. The results indicate that the input meteorological forcing component and the land surface hydrology module provide a framework with which to assess global water resources, with the potential application to investigate the subannual variability in water resources. GSWP2 participants are encouraged to re-run their model using this newly developed meteorological forcing input, which is in identical format to the original GSWP2 forcing input

    Unconventional ferromagnetic and spin-glass states of the reentrant spin glass Fe0.7Al0.3

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    Spin excitations of single crystal Fe0.7Al0.3 were investigated over a wide range in energy and reciprocal space with inelastic neutron scattering. In the ferromagnetic phase, propagating spin wave modes become paramagnon-like diffusive modes beyond a critical wave vector q0, indicating substantial disorder in the long-range ordered state. In the spin glass phase, spin dynamics is strongly q-dependent, suggesting remnant short-range spin correlations. Quantitative model for S(energy,q) in the ``ferromagnetic'' phase is determined.Comment: 4 pages, 5 figure

    Absence of Edge Localized Moments in the Doped Spin-Peierls System CuGe1−x_{1-x}Six_{x}O3_3

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    We report the observation of nuclear quadrupole resonance (NQR) of Cu from the sites near the doping center in the spin-Peierls system CuGe1−x_{1-x}Six_{x}O3_3. The signal appears as the satellites in the Cu NQR spectrum, and has a suppressed nuclear spin-lattice relaxation rate indicative of a singlet correlation rather than an enhanced magnetic correlation near the doping center. Signal loss of Cu nuclei with no neighboring Si is also observed. We conclude from these observations that the doping-induced moments are not in the vicinity of the doping center but rather away from it.Comment: 4 pages, 4 figures, accepted for publication in Phys. Rev. Let

    Bulk screening in core level photoemission from Mott-Hubbard and Charge-Transfer systems

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    We report bulk-sensitive hard X-ray (hνh\nu = 5.95 KeV) core level photoemission spectroscopy (PES) of single crystal V1.98_{1.98}Cr0.02_{0.02}O3_{3} and the high-TcT_c cuprate Bi2_2Sr2_{2}CaCu2_{2}O8+δ_{8+\delta} (Bi2212). V1.98_{1.98}Cr0.02_{0.02}O3_{3} exhibits low binding energy "satellites" to the V 2p2p "main lines" in the metallic phase, which are suppressed in the antiferromagnetic insulator phase. In contrast, the Cu 2p2p spectra of Bi2212 do not show temperature dependent features, but a comparison with soft X-ray PES indicates a large increase in the 2p53d92p^5 3d^9 "satellites" or 3d93d^9 weight in the bulk. Cluster model calculations, including full multiplet structure and a screening channel derived from the coherent band at the Fermi energy, give very satisfactory agreement with experiments

    Neutron scattering experiments and simulations near the magnetic percolation threshold of Fe_x Zn_{1-x} F_2

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    The low temperature excitations in the anisotropic antiferromagnetic Fe_{1-x} Zn_x F_2 for x=0.25 and 0.31, at and just above the magnetic percolation threshold concentration x_p=0.25, were measured using inelastic neutron scattering. The excitations were simulated for x=0.31 using a localized, classical excitation model, which accounts well for the energies and relative intensities of the excitations observed in the scattering experiments.Comment: 6 pages, 6 figure

    NMR characterization of spin-1/2 alternating antiferromagnetic chains in the high-pressure phase of (VO)2P2O7

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    Local-susceptibility measurements via the NMR shifts of 31^{31}P and 51^{51}V nuclei in the high-pressure phase of (VO)2_{2}P2_{2}O7_{7} confirmed the existence of a unique alternating antiferromagnetic chain with a zero-field spin gap of 34 K. The 31^{31}P nuclear spin-lattice relaxation rate scales with the uniform spin susceptibility below about 15 K which shows that the temperature dependence of both the static and dynamical spin susceptibilities becomes identical at temperatures not far below the spin-gap energy.Comment: 6 pages, 5 figures; To be published in J. Phys. Condens. Matte

    Phase Inhomogeneity of the Itinerant Ferromagnet MnSi at High Pressures

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    The pressure induced quantum phase transition of the weakly itinerant ferromagnet MnSi is studied using zero-field 29Si^{29}Si NMR spectroscopy and relaxation. Below P∗≈1.2GPaP^*\approx 1.2GPa, the intensity of the signal and the nuclear spin-lattice relaxation is independent of pressure, even though the amplitude of the magnetization drops by 20% from the ambient pressure amplitude. For P>P∗P>P^*, the decreasing intensity within the experimentally detectable bandwidth signals the onset of an inhomogeneous phase that persists to the highest pressure measured, P≥1.75GPaP\ge 1.75GPa, which is well beyond the known critical pressure Pc=1.46GPaP_c=1.46GPa. Implications for the non-Fermi Liquid behavior observed for P>PcP>P_c are discussed.Comment: 4 pages, 4 figure

    Itinerant-Electron Magnet of the Pyrochlore Lattice: Indium-Doped YMn2Zn20

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    We report on a ternary intermetallic compound, "YMn2Zn20", comprising a pyrochlore lattice made of Mn atoms. A series of In-doped single crystals undergo no magnetic long-range order down to 0.4 K, in spite of the fact that the Mn atom carries a local magnetic moment at high temperatures, showing Curie-Weiss magnetism. However, In-rich crystals exhibit spin-glass transitions at approximately 10 K due to a disorder arising from the substitution, while, with decreasing In content, the spin-glass transition temperature is reduced to 1 K. Then, heat capacity divided by temperature approaches a large value of 280 mJ K-2 mol-1, suggesting a significantly large mass enhancement for conduction electrons. This heavy-fermion-like behavior is not induced by the Kondo effect as in ordinary f-electron compounds, but by an alternative mechanism related to the geometrical frustration on the pyrochlore lattice, as in (Y,Sc)Mn2 and LiV2O4, which may allow spin entropy to survive down to low temperatures and to couple with conduction electrons.Comment: 5 pages, 4 figures, J. Phys. Soc. Jpn., in pres

    Nonlinear magnetic susceptibility and aging phenomena in reentrant ferromagnet: Cu0.2_{0.2}Co0.8_{0.8}Cl2_{2}-FeCl3_{3} graphite bi-intercalation compound

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    Linear and nonlinear dynamic properties of a reentrant ferromagnet Cu0.2_{0.2}Co0.8_{0.8}Cl2_{2}-FeCl3_{3} graphite bi-intercalation compound are studied using AC and DC magnetic susceptibility. This compound undergoes successive phase transitions at the transition temperatures ThT_{h} (= 16 K), TcT_{c} (= 9.7 K), and TRSGT_{RSG} (= 3.5 K). The static and dynamic behaviors of the reentrant spin glass phase below TRSGT_{RSG} are characterized by those of normal spin glass phase with critical exponent β\beta = 0.57 ±\pm 0.10, a dynamic critical exponent xx = 8.5 ±\pm 1.8, and an exponent pp (= 1.55 ±\pm 0.13) for the de Almeida -Thouless line. A prominent nonlinear susceptibility is observed between TRSGT_{RSG} and TcT_{c} and around ThT_{h}, suggesting a chaotic nature of the ferromagnetic phase (TRSG≤T≤TcT_{RSG} \leq T \leq T_{c}) and the helical spin ordered phase (Tc≤T≤ThT_{c} \leq T \leq T_{h}). The aging phenomena are observed both in the RSG and FM phases, with the same qualitative features as in normal spin glasses. The aging of zero-field cooled magnetization indicates a drastic change of relaxation mechanism below and above TRSGT_{RSG}. The time dependence of the absorption χ′′\chi^{\prime \prime} is described by a power law form (≈t−b′′\approx t^{-b^{\prime \prime}}) in the ferromagnetic phase, where b′′≈0.074±0.016b^{\prime \prime} \approx 0.074 \pm 0.016 at ff = 0.05 Hz and TT = 7 K. No ωt\omega t-scaling law for χ′′\chi^{\prime \prime} [≈(ωt)−b′′\approx (\omega t)^{-b^{\prime \prime}}] is observed.Comment: 14 pages, 16 figures, and 2 table
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