نتایج جستجو برای: ball clay

تعداد نتایج: 47085  

1999
Elsa C. Y. Yan Kenneth B. Eisenthal

Second harmonic generation (SHG) is applied for the first time to study the surfaces of clay particles. An SHG signal was detected from an aqueous suspension of disk-shaped montmorillonite clay particles of 0.5 μm diameter and 0.01 μm thickness. The origin of the SHG signal is the polarization of water molecules by surface charges located in the edge region of the clay particles. On addition of...

Journal: :Eastern-European Journal of Enterprise Technologies 2023

Multilayered Armor System (MAS) is being extensively studied around the world for its ability to retain ceramic fragmentation after a collision occurs. MAS consist of layer placed at front and supported by composite ramie-fiber-reinforced epoxy resin. Present study utilizes natural fibers 50 % ramie with resin as matrix Silicon Carbide (SiC) panel. The ballistic testing in this used 7.62×51 mm ...

2017
Francine Bertella Sibele B. C. Pergher

Pillared clays (PILCs) are interesting materials mostly due to their high basal spacing and surface area, which make them suitable for adsorption and catalysis applications, for example. However, the production of these materials on industrial scale is dependent on research about what parameters influence the process. Thus, the objective of this work was to evaluate what parameters influence th...

2005
Philip Korman Junping Shi PHILIP KORMAN JUNPING SHI

We consider a class of singular systems of Lane-Emden type      ∆u + λu p 1 v q 1 = 0, x ∈ D, a smooth domain in R n. In case the system is sublinear we prove existence of a positive solution. If D is a ball in R n , we prove both existence and uniqueness of positive radially symmetric solution.

2015
C. R. Jayanarayanan Tanmoy Paul

We investigate a variation of the transitivity problem for proximinality properties of subspaces and intersection properties of balls in Banach spaces. For instance, we prove that if Z ⊆ Y ⊆ X, where Z is a finite co-dimensional subspace of X which is strongly proximinal in Y and Y is an M -ideal in X, then Z is strongly proximinal in X. Towards this, we prove that a finite co-dimensional proxi...

Journal: :Formalized Mathematics 2011
Marco Riccardi

Let x, y be sets. Observe that {〈x, y〉} is one-to-one. In the sequel n denotes a natural number. One can prove the following two propositions: (1) For every non empty topological space T holds T and T ΩT are homeomorphic. (2) Let X be a non empty subspace of En T and f be a function from X into R1. Suppose f is continuous. Then there exists a function g from X into En T such that (i) for every ...

Journal: :Microelectronics Reliability 2001
P. L. Tu Y. C. Chan K. C. Hung J. K. L. Lai

A new re¯ow parameter, heating factor (Q g), which is de®ned as the integral of the measured temperature over the dwell time above liquidus, has been proposed in this report. It can suitably represent the combined e€ect of both temperature and time in usual re¯ow process. Relationship between reliability of the micro-ball grid array (micro-BGA) package and heating factor has been discussed. The...

Arabameri, Elahe , Khanjari, Yaser ,

Objective: Bilateral coordination skills are one of the key factors in performing simple to skillful sports task, so far the differences between ball and non-ball fields have not been determined. Therefore, this study aimed to investigate the differences in asymmetric bilateral coordination between male and female athletes in ballplayers and non-ballplayers. Methods: The samples of this study ...

2006
F. V. CHUKHROV

Clay mineral studies in the U.S.S.R., mainly since 1960, are summarized. Electron diffraction techniques especially have been developed and used extensively. Methods have been developed for simultaneous recording of DTA curves and other properties. Polytypism of phyllosilicates has been studied intensively by Zvyagin and others. Mucfi new information on the structure and morphology of halloysit...

2007
F. Kenn

Isolated patches of white clay occurring in the terminal moraine of Long Island, Staten fsland, and southern New Jersey have been mentioned in a number of geologic descriptions. Such an occurrence was recently encountered during excavation for a building site and samples were submitted to the mineralogical laboratory of Columbia University for identification by Messrs. Schoonmaker and Kirkman. ...

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