Search Results - (Author, Cooperation:P. J. Ross)
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1J. Wu ; D. Okamura ; M. Li ; K. Suzuki ; C. Luo ; L. Ma ; Y. He ; Z. Li ; C. Benner ; I. Tamura ; M. N. Krause ; J. R. Nery ; T. Du ; Z. Zhang ; T. Hishida ; Y. Takahashi ; E. Aizawa ; N. Y. Kim ; J. Lajara ; P. Guillen ; J. M. Campistol ; C. R. Esteban ; P. J. Ross ; A. Saghatelian ; B. Ren ; J. R. Ecker ; J. C. Izpisua Belmonte
Nature Publishing Group (NPG)
Published 2015Staff ViewPublication Date: 2015-05-07Publisher: Nature Publishing Group (NPG)Print ISSN: 0028-0836Electronic ISSN: 1476-4687Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsKeywords: Animals ; Cell Culture Techniques/methods ; Cell Line ; *Chimera ; Embryonic Stem Cells/cytology ; Female ; Germ Layers/cytology ; Humans ; Induced Pluripotent Stem Cells/cytology ; Male ; Mice ; Pan troglodytes ; Pluripotent Stem Cells/*cytology/metabolism ; Regenerative Medicine ; Species SpecificityPublished by: -
2H. Han ; M. Irimia ; P. J. Ross ; H. K. Sung ; B. Alipanahi ; L. David ; A. Golipour ; M. Gabut ; I. P. Michael ; E. N. Nachman ; E. Wang ; D. Trcka ; T. Thompson ; D. O'Hanlon ; V. Slobodeniuc ; N. L. Barbosa-Morais ; C. B. Burge ; J. Moffat ; B. J. Frey ; A. Nagy ; J. Ellis ; J. L. Wrana ; B. J. Blencowe
Nature Publishing Group (NPG)
Published 2013Staff ViewPublication Date: 2013-06-07Publisher: Nature Publishing Group (NPG)Print ISSN: 0028-0836Electronic ISSN: 1476-4687Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsKeywords: *Alternative Splicing/genetics ; Amino Acid Motifs ; Animals ; Cell Differentiation/genetics ; Cell Line ; *Cellular Reprogramming ; DNA-Binding Proteins/chemistry/deficiency/genetics/*metabolism ; Embryonic Stem Cells/*cytology/*metabolism ; Fibroblasts/cytology/metabolism ; Forkhead Transcription Factors/metabolism ; Gene Knockdown Techniques ; HEK293 Cells ; HeLa Cells ; Humans ; Induced Pluripotent Stem Cells/cytology/metabolism ; Kinetics ; Mice ; RNA-Binding Proteins/chemistry/genetics/*metabolism ; Repressor Proteins/metabolismPublished by: -
3Staff View
ISSN: 1476-4687Source: Nature Archives 1869 - 2009Topics: BiologyChemistry and PharmacologyMedicineNatural Sciences in GeneralPhysicsNotes: [Auszug] LOSSES of nitrogen from the soil: plant system have never been measured directly, and gains have almost always been estimated from conventional nitrogen balance experiments. Quantitative knowledge of changes in nitrogen occurring in an enclosed atmosphere surrounding the system should not only ...Type of Medium: Electronic ResourceURL: -
4Ross, P. J. ; Webb, A. ; Cunningham, D. ; Prendiville, J. ; Norman, A. R. ; Oates, J.
Springer
Published 1997Staff ViewISSN: 1569-8041Keywords: ambulatory chemotherapy ; 5-fluoruouracil ; protracted venous iinfusionSource: Springer Online Journal Archives 1860-2000Topics: MedicineType of Medium: Electronic ResourceURL: -
5Staff View
ISSN: 0037-7996Topics: HistoryURL: -
6Staff View
ISSN: 0037-7996Topics: HistoryURL: -
7Parlange, J.-Y. ; Hogarth, W. L. ; Parlange, M. B. ; Haverkamp, R. ; Barry, D. A. ; Ross, P. J. ; Steenhuis, T. S.
Springer
Published 1998Staff ViewISSN: 1573-1634Keywords: nonlinear diffusion ; analytic solutions ; exact solutions ; approximations ; similaritySource: Springer Online Journal Archives 1860-2000Topics: GeosciencesTechnologyNotes: Abstract A general approximation for the solution of the one-dimensional nonlinear diffusion equation is presented. It applies to arbitrary soil properties and boundary conditions. The approximation becomes more accurate when the soil-water diffusivity approaches a delta function, yet the result is still very accurate for constant diffusivity suggesting that the present formulation is a reliable one. Three examples are given where the method is applied, for a constant water content at the surface, when a saturated zone exists and for a time-dependent surface flux.Type of Medium: Electronic ResourceURL: -
8Staff View
ISSN: 1573-1634Keywords: Porous media ; water movement ; analytical solutions ; numerical solutions ; two-dimensional solutions ; impervious layersSource: Springer Online Journal Archives 1860-2000Topics: GeosciencesTechnologyNotes: Abstract Wetting-front movement can be impaired whenever the flow region includes boundaries such as the soil surface, seepage faces, planes of symmetry, or actual layers that are effectively impermeable, such as heavy clays or coarse materials below the water-entry pressure. An approximate analytical solution for interaction of flow from a line source with a parallel plane, impervious layer is derived. The solution ignores gravity and assumes a particular diffusivity that is related to the constant flow rate. It is exact until interaction begins, and provides an accurate approximation for short times thereafter. It can therefore be used to test the accuracy of numerical solutions of the flow equation, which can then be used with confidence for later times when the analytical approximation breaks down, for instance because gravity is ignored. A finite difference solution was tested in this way for both gradual and steep wetting fronts. Agreement between the two solutions was excellent for the gradual front, with the analytical approximation only slightly in error at later times. Numerical errors at the steep front were much greater; an accurate solution needed a finer spatial grid and a restart from the exact analytical values at the beginning of the interaction. The analytical approximation, though not as accurate as for the gradual front, was still ‘good’.Type of Medium: Electronic ResourceURL: -
9Staff View
ISSN: 1573-1634Keywords: water movement ; infiltration ; water balance ; analytical solutions ; hydraulic propertiesSource: Springer Online Journal Archives 1860-2000Topics: GeosciencesTechnologyNotes: Abstract Simple equations for predicting infiltration of water into soil are valuable both for hydrological application and for investigating soil hydraulic properties. Their value is greatly enhanced if they involve parameters that can be related to more basic soil hydraulic properties. In this paper we extend infiltration equations developed previously for positive surface heads to negative heads. The equations are then used to calculate infiltration into a sand and a clay for a range of initial and surface conditions. Results show errors of less than three percent compared with accurate numerical solutions. Analytical approximations to parameters in the equations are developed for a Brooks and Corey power law hydraulic conductivity-water content relation combined with either a Brooks and Corey or a van Genuchten water retention function. These are compared with accurate numerical values for a range of hydraulic parameters encompassing the majority of soil types and a range of initial and boundary conditions. The approximations are excellent for a wide range of soil parameters. An important attribute of the infiltration equations is their use of dimensionless parameters that can be calculated from normalised water retention and hydraulic conductivity functions. These normalised functions involve only parameters that it may be possible to estimate from surrogate data such as soil particle size distribution. Application of the equations for predicting infiltration, or their use in inferring hydraulic properties, then involves only simple scaling parameters.Type of Medium: Electronic ResourceURL: -
10Staff View
ISSN: 1435-0661Source: Springer Online Journal Archives 1860-2000Topics: GeosciencesAgriculture, Forestry, Horticulture, Fishery, Domestic Science, NutritionType of Medium: Electronic ResourceURL: -
11Staff View
ISSN: 1573-5036Source: Springer Online Journal Archives 1860-2000Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, NutritionNotes: Summary A gas lysimeter study showed negligible losses of gaseous N2 or N2O from rhodes grass plants growing in soil fertilized with either (N15H4)2SO4 or KN15O3; isotope recovered from the soil: plant system averaged respectively 100.5% and 98.9%; neither differed significantly from 100%. Small amounts of ammonia were volatilized into lysimeter atmospheres, averaging 0.6% of that applied as labelled ammonium-N and 0.1% of that as nitrate-N. The importance of these findings is discussed in relation to the conduct of N balance studies.Type of Medium: Electronic ResourceURL: