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[PDF] Top 20 Existence of Positive Solution to a Quasilinear Elliptic Problem in <B>R</B><SUP>N</SUP>

Has 10000 "Existence of Positive Solution to a Quasilinear Elliptic Problem in <B>R</B><SUP>N</SUP>" found on our website. Below are the top 20 most common "Existence of Positive Solution to a Quasilinear Elliptic Problem in <B>R</B><SUP>N</SUP>".

Existence of Positive Solution to a Quasilinear Elliptic Problem in &lt;B&gt;R&lt;/B&gt;&lt;SUP&gt;N&lt;/SUP&gt;

Existence of Positive Solution to a Quasilinear Elliptic Problem in <B>R</B><SUP>N</SUP>

... the problem (1) in the case l = 0. In this article consider the problem when l > ...The problem (1) arises, for example, in non- Newtonian ‡uid theory, the quantity p is a ... See full document

6

Existence of solutions for a class of degenerate quasilinear elliptic equation in R-N with vanishing potentials

Existence of solutions for a class of degenerate quasilinear elliptic equation in R-N with vanishing potentials

... Alves, CO, Carrião, PC, Miyagaki, OH: Nonlinear perturbations of a periodic elliptic problem with critical growth.. Alves, CO, Soares, SHM: Existence and concentration of positive soluti[r] ... See full document

16

Existence and asymptotic behavior of positive solutions of a semilinear elliptic system in a bounded domain

Existence and asymptotic behavior of positive solutions of a semilinear elliptic system in a bounded domain

... studied in [21] system (1.4) for a different range of exponents to those in ...β, r, s < 0 satisfying some appropriate conditions, problem ...classical solution (u, v) ... See full document

22

Meridional transport and deposition of atmospheric &lt;sup&gt;10&lt;/sup&gt;Be

Meridional transport and deposition of atmospheric <sup>10</sup>Be

... differences of the normalised deposi- tion fluxes at these latitudes we see that the fluctuations can be considered as ...fluxes in the polar regions are extremely low, even small fluctuations account for a ... See full document

13

The influence of temperature and seawater carbonate saturation state on &lt;sup&gt;13&lt;/sup&gt;C–&lt;sup&gt;18&lt;/sup&gt;O bond ordering in bivalve mollusks

The influence of temperature and seawater carbonate saturation state on <sup>13</sup>C–<sup>18</sup>O bond ordering in bivalve mollusks

... School of Ocean Sciences, Ban- gor University, ...acclimated to the lab- oratory environment at a temperature of ∼ 13 ◦ C for more than two ...Animals of similar size (< 1 yr) were then ... See full document

16

Hemispheric average Cl atom concentration from &lt;sup&gt;13&lt;/sup&gt;C/&lt;sup&gt;12&lt;/sup&gt;C ratios in atmospheric methane

Hemispheric average Cl atom concentration from <sup>13</sup>C/<sup>12</sup>C ratios in atmospheric methane

... It is possible that stratosphere-troposphere exchange could introduce 13 C-rich methane into the ETSH. Using model results (e.g. Rosenlof and Holton, 1993) on downward mass fluxes into the ETSH from the lower ... See full document

18

Late-glacial to late-Holocene shifts in global precipitation δ&lt;sup&gt;18&lt;/sup&gt;O

Late-glacial to late-Holocene shifts in global precipitation δ<sup>18</sup>O

... number of potential processes could bias the preser- vation of precipitation isotope composition in ice core, speleothem or groundwater archives (Wang et ...record of precipitation that ... See full document

19

Hydrogen dynamics in soil organic matter as determined by &lt;sup&gt;13&lt;/sup&gt;C and &lt;sup&gt;2&lt;/sup&gt;H labeling experiments

Hydrogen dynamics in soil organic matter as determined by <sup>13</sup>C and <sup>2</sup>H labeling experiments

... result of the mineral protec- tion processes (Derrien et ...dynamics in this continuum have been widely studied using the natural 14 C / 12 C and 13 C / 12 C (Rafter and Stout, 1970; Balesdent et ...results ... See full document

12

Maintaining consistent traceability in high-precision isotope measurements of CO&lt;sub&gt;2&lt;/sub&gt;: a way to verify atmospheric trends of δ&lt;sup&gt;13&lt;/sup&gt;C and δ&lt;sup&gt;18&lt;/sup&gt;O

Maintaining consistent traceability in high-precision isotope measurements of CO<sub>2</sub>: a way to verify atmospheric trends of δ<sup>13</sup>C and δ<sup>18</sup>O

... independent of the WRG. It is, however, dependent on cross contaminations (CC) in the ion source due to the mixing of sample and refer- ence gases (Meijer et ...made of), the pump- ing ... See full document

21

A combustion setup to precisely reference &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C and &amp;delta;&lt;sup&gt;2&lt;/sup&gt;H isotope ratios of pure CH&lt;sub&gt;4&lt;/sub&gt; to produce isotope reference gases of &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C-CH&lt;sub&gt;4&lt;/sub&gt; in synthetic air

A combustion setup to precisely reference &delta;<sup>13</sup>C and &delta;<sup>2</sup>H isotope ratios of pure CH<sub>4</sub> to produce isotope reference gases of &delta;<sup>13</sup>C-CH<sub>4</sub> in synthetic air

... values of pure CH 4 gases (top panel) and of NEEM, measured with the produced isotope reference gases (bottom ...calculations of the uncertainties are explained in Sect. 3 and are based on ... See full document

10

Application of &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C and &amp;delta;&lt;sup&gt;15&lt;/sup&gt;N isotopic signatures of organic matter fractions sequentially separated from adjacent arable and forest soils to identify carbon stabilization mechanisms

Application of &delta;<sup>13</sup>C and &delta;<sup>15</sup>N isotopic signatures of organic matter fractions sequentially separated from adjacent arable and forest soils to identify carbon stabilization mechanisms

... changes in C3/C4 vegetation, have in- terpreted the stable isotopic signature (δ 13 C and δ 15 N) of OM fractions to determine mean residence times (Balesdent and Mariotti, 1996; Liao ... See full document

12

A combustion setup to precisely reference &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C and &amp;delta;&lt;sup&gt;2&lt;/sup&gt;H isotope ratios of pure CH&lt;sub&gt;4&lt;/sub&gt; to produce isotope reference gases of &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C-CH&lt;sub&gt;4&lt;/sub&gt; in synthetic air

A combustion setup to precisely reference &delta;<sup>13</sup>C and &delta;<sup>2</sup>H isotope ratios of pure CH<sub>4</sub> to produce isotope reference gases of &delta;<sup>13</sup>C-CH<sub>4</sub> in synthetic air

... Assessment of the completeness of the combustion of pure CH 4 ...scans of mass abundances, resulting from fossil CH 4 (green line), CO 2 -40 339 (blue filled line) and CH 4 derived CO 2 (black ... See full document

20

&lt;sup&gt;90&lt;/sup&gt;Sr and &lt;sup&gt;89&lt;/sup&gt;Sr in seawater off Japan as a consequence of the Fukushima Dai-ichi nuclear accident

<sup>90</sup>Sr and <sup>89</sup>Sr in seawater off Japan as a consequence of the Fukushima Dai-ichi nuclear accident

... leakage of contam- inated waters that occurred in December ...that of the global at- mospheric fallout produced by nuclear weapon tests, which was ...used in future studies to track wa- ... See full document

11

Consulta de enfermagem às pessoas com Diabetes Mellitus: experiência com metodologia ativa Consulta de enfermería a las personas con diabetes mellitus: experiencia con metodología activa

Consulta de enfermagem às pessoas com Diabetes Mellitus: experiência com metodologia ativa Consulta de enfermería a las personas con diabetes mellitus: experiencia con metodología activa

... evaluation of the suggested and implemented interventions has been carried out by the unit’s nurse and by other academics (who took part in the USF dur- ing subsequent ...longitudinality in the care ... See full document

6

The Caenorhabditis elegans iodotyrosine deiodinase ortholog SUP-18 functions through a conserved channel SC-box to regulate the muscle two-pore domain potassium channel SUP-9.

The Caenorhabditis elegans iodotyrosine deiodinase ortholog SUP-18 functions through a conserved channel SC-box to regulate the muscle two-pore domain potassium channel SUP-9.

... 1. sup-18 encodes the C. elegans ortholog of mammalian iodotyrosine ...map of the sup-18 region of linkage group III (LG ...below sup-18 represent the cosmids tested for rescue ... See full document

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Controls on the spatial distribution of oceanic &amp;delta;&lt;sup&gt;13&lt;/sup&gt;C&lt;sub&gt;DIC&lt;/sup&gt;

Controls on the spatial distribution of oceanic &delta;<sup>13</sup>C<sub>DIC</sup>

... low to mid latitudes, which may have important consequences for biological production via impacts on stratification- dependent mixing and the redistribution of nutrients back to the photic ...zone. ... See full document

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&lt;i&gt;HESS Opinions&lt;/i&gt; &quot;The art of hydrology&quot;&lt;sup&gt;*&lt;/sup&gt;

<i>HESS Opinions</i> "The art of hydrology"<sup>*</sup>

... precipitate in their root zones, lifting the trees into the air, at time scales beyond our visibility, of ...concentrations of solutes in the river water, even though more than 90% of ... See full document

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An estimation of the &lt;sup&gt;18&lt;/sup&gt;O / &lt;sup&gt;16&lt;/sup&gt;O ratio of UT/LMS ozone based on artefact CO in air sampled during CARIBIC flights

An estimation of the <sup>18</sup>O / <sup>16</sup>O ratio of UT/LMS ozone based on artefact CO in air sampled during CARIBIC flights

... analysis in a laboratory. A famous example is the filling of pairs of glass flasks at South Pole Station for the much later analysis at NOAA in Boulder, Colorado, USA (Nov- elli et ... See full document

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Comparing the efficacy of Truvada&lt;sup&gt;® &lt;/sup&gt;and Kivexa&lt;sup&gt;® &lt;/sup&gt;combination therapy in HAART-naive individuals with different viral loads

Comparing the efficacy of Truvada<sup>® </sup>and Kivexa<sup>® </sup>combination therapy in HAART-naive individuals with different viral loads

... HIV positive people ...background of increasing criminalisation of HIV transmission, difficulty of disclosure, and the psychological burden of living with a stigmatised and chronic ... See full document

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An estimation of the &lt;sup&gt;18&lt;/sup&gt;O / &lt;sup&gt;16&lt;/sup&gt;O ratio of UT/LMS ozone based on artefact CO in air sampled during CARIBIC flights

An estimation of the <sup>18</sup>O / <sup>16</sup>O ratio of UT/LMS ozone based on artefact CO in air sampled during CARIBIC flights

... Distribution of CO mixing ratios as a function of concomitant O 3 mixing ratios measured by CARIBIC in the LMS ([O 3 ] > 300 nmol mol −1 ...histogram of the C2 measurements (all C2 data ... See full document

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