19 research outputs found
Approximate k-state solutions to the Dirac-Yukawa problem based on the spin and pseudospin symmetry
Using an approximation scheme to deal with the centrifugal
(pseudo-centrifugal) term, we solve the Dirac equation with the screened
Coulomb (Yukawa) potential for any arbitrary spin-orbit quantum number
{\kappa}. Based on the spin and pseudospin symmetry, analytic bound state
energy spectrum formulas and their corresponding upper- and lower-spinor
components of two Dirac particles are obtained using a shortcut of the
Nikiforov-Uvarov method. We find a wide range of permissible values for the
spin symmetry constant C_{s} from the valence energy spectrum of particle and
also for pseudospin symmetry constant C_{ps} from the hole energy spectrum of
antiparticle. Further, we show that the present potential interaction becomes
less (more) attractive for a long (short) range screening parameter {\alpha}.
To remove the degeneracies in energy levels we consider the spin and pseudospin
solution of Dirac equation for Yukawa potential plus a centrifugal-like term. A
few special cases such as the exact spin (pseudospin) symmetry Dirac-Yukawa,
the Yukawa plus centrifugal-like potentials, the limit when {\alpha} becomes
zero (Coulomb potential field) and the non-relativistic limit of our solution
are studied. The nonrelativistic solutions are compared with those obtained by
other methods.Comment: 21 pages, 6 figure
Hurricane-induced modification of nitrogen and phosphorus resorption in an aspen clone: an example of diffuse disturbance
Foliar senescence in an aspen (Populus tremuloides) clone: the response of element resorption to interramet variation and timing of abscission
Global pattern of leaf litter nitrogen and phosphorus in woody plants
Forest ecosystems exert an important influence on global biogeochemical cycles.
A global dataset of nitrogen (N) and phosphorus (P) concentrations in leaf-
litter of woody plants was compiled from the literature. Among the 677 data
sets, 482 included P concentrations and the N:P ratio. At a global scale, the
mean leaf-litter N and P and N:P ratio were 10.9 mg g-1, 0.85 mg g-1 and 18.3,
respectively. Leaf-litter N and P were significantly correlated. When the data
was grouped by continents, the highest mean N was found in Africa (19.5 mg g-1),
and the lowest in North America (8.18 mg g-1). P was significantly smaller in
the Asian Islands (Japan and Malaysia, 0.44 mg g-1) than on the Asian mainland.
For the global dataset, leaf-litter N increased linearly with mean annual
temperature and annual precipitation and decreased with latitude. Although leaf-
litter P showed no significant relationship with temperature, it declined
linearly with precipitation and there was a convex quadratic relationship with
latitude. For the global dataset and also for different functional groups (e.g.
shrubs, evergreen broadleaf, deciduous broadleaf, and conifers) the leaf-litter
N:P ratio generally followed a positive linear relationship with temperature and
precipitation, and showed a concave quadratic response with latitude. The
differences in leaf-litter N:P ratio among functional groups and among
continents should be taken into account when modeling biogeochemical cycles in
different regions as well as on a global scale