Norm of Operators on the Generalized Ces\`{a}ro Matrix Domain

2020 ◽  
pp. 155-161
Author(s):  
Maryam SİNAEİ
Keyword(s):  
Matrix Domain

scholarly journals The HIV-1 Matrix Domain of Gag Is Required for Vpu Responsiveness during Particle Release

Virology ◽  
1997 ◽  
Vol 237 (1) ◽  
pp. 46-55 ◽  
Author(s):  
Yung-Hui Lee ◽  
Michael D. Schwartz ◽  
Antonito T. Panganiban
Keyword(s):  
Particle Release ◽  
Matrix Domain ◽  
Hiv 1

Some Double Sequence Spaces Generated by Four-Dimensional Pascal Matrix

2021 ◽  
Vol 09 (08) ◽  
Author(s):  
Ahmadu Kiltho ◽  
Keyword(s):  
Double Sequence ◽  
Sequence Spaces ◽  
Schauder Basis ◽  
Topological Properties ◽  
Matrix Domain ◽  
Double Sequence Spaces ◽  
Pascal Matrix

The purpose of this paper is to discover and examine a four-dimensional Pascal matrix domain on Pascal sequence spaces. We show that they are spaces and also establish their Schauder basis, topological properties, isomorphism and some inclusions.

Rb-Sr and Sm-Nd isotopic and REE studies of igneous components in the bulk matrix domain of Martian breccia Northwest Africa 7034

2016 ◽  
Vol 51 (3) ◽  
pp. 483-498 ◽  
Author(s):  
Laurence E. Nyquist ◽  
Chi-Yu Shih ◽  
Francis M. McCubbin ◽  
Alison R. Santos ◽  
Charles K. Shearer ◽  
...  
Keyword(s):  
Matrix Domain ◽  
Northwest Africa ◽  
Bulk Matrix

scholarly journals Quantification of the influence of preferential flow on slope stability using a numerical modelling approach

2015 ◽  
Vol 19 (5) ◽  
pp. 2197-2212 ◽  
Author(s):  
W. Shao ◽  
T. A. Bogaard ◽  
M. Bakker ◽  
R. Greco
Keyword(s):  
Slope Stability ◽  
High Intensity ◽  
Preferential Flow ◽  
Water Pressure ◽  
Subsurface Flow ◽  
Permeability Model ◽  
Rainfall Events ◽  
Matrix Domain ◽  
Low Intensity ◽  
Flow Domain

Abstract. The effect of preferential flow on the stability of landslides is studied through numerical simulation of two types of rainfall events on a hypothetical hillslope. A model is developed that consists of two parts. The first part is a model for combined saturated/unsaturated subsurface flow and is used to compute the spatial and temporal water pressure response to rainfall. Preferential flow is simulated with a dual-permeability continuum model consisting of a matrix domain coupled to a preferential flow domain. The second part is a soil mechanics model and is used to compute the spatial and temporal distribution of the local factor of safety based on the water pressure distribution computed with the subsurface flow model. Two types of rainfall events were considered: long-duration, low-intensity rainfall, and short-duration, high-intensity rainfall. The effect of preferential flow on slope stability is assessed through comparison of the failure area when subsurface flow is simulated with the dual-permeability model as compared to a single-permeability model (no preferential flow). For the low-intensity rainfall case, preferential flow has a positive effect on drainage of the hillslope resulting in a smaller failure area. For the high-intensity rainfall case, preferential flow has a negative effect on the slope stability as the majority of rainfall infiltrates into the preferential flow domain when rainfall intensity exceeds the infiltration capacity of the matrix domain, resulting in larger water pressure and a larger failure area.

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