Intrinsic instability of electromigration induced mass transport in a two-dimensional conductor

1999 ◽  
Vol 47 (13) ◽  
pp. 3571-3578 ◽  
Author(s):  
C.Q Ru
2019 ◽  
Vol 10 (23) ◽  
pp. 5875-5883 ◽  
Author(s):  
Fujian Liu ◽  
Xianfeng Yi ◽  
Wei Chen ◽  
Zhiqiang Liu ◽  
Wei Chen ◽  
...  

2D hybrid solid superacids with extremely high acid strength and outstanding mass transfer properties were prepared and exhibit superior activities for biomass conversion.


2016 ◽  
Vol 212 ◽  
pp. 201-211 ◽  
Author(s):  
Sen Yao ◽  
Ya-Ling He ◽  
Bing-Ye Song ◽  
Xiao-Yue Li

1977 ◽  
Vol 83 (3) ◽  
pp. 415-431 ◽  
Author(s):  
Jacques Lamoure ◽  
Chiang C. Mei

Mass transport close to the sea bottom is investigated for simple harmonic waves around a body with a small horizontal dimension. For gravity waves it is shown that the mass transport very near the bottom points towards a convex corner, but near the top of the boundary layer its direction reverses. Possible implications for silting near a pile and a harbour entrance are discussed and some experimental evidence given. For tides, the Coriolis force introduces a spiralling variation within the boundary layer, and possible inferences for coastline modification are drawn.


2000 ◽  
Vol 147 (8) ◽  
pp. 3021 ◽  
Author(s):  
Maria Georgiadou ◽  
Rebecca Mohr ◽  
Richard C. Alkire

1991 ◽  
Vol 231 ◽  
pp. 395-415 ◽  
Author(s):  
Mohamed Iskandarani ◽  
Philip L.-F. Liu

Mass transport in various kind of two-dimensional water waves is studied. The characteristics of the governing equations for the mass transport depend on the ratio of viscous lengthscale to the amplitude of the free-surface displacement. When this ratio is small, the nonlinearity is important and the mass transport flow acquires a boundary-layer character. Numerical schemes are developed to investigate mass transport in a partially reflected wave and above a hump in the seabed. When the mass transport is periodic in the horizontal direction, a spectral scheme based on a Fourier–Chebyshev expansion, is presented for the solution of the equations. For the ease of a hump on the seabed, the flow domain is divided into three regions. Using the spectral scheme, the mass transport in the uniform-depth regions is calculated first. and the results are used to compute the steady flow in the inhomogeneous flow region which encloses the hump on the seabed.


2018 ◽  
Vol 10 (30) ◽  
pp. 25409-25414 ◽  
Author(s):  
Ge Wang ◽  
Jingying Tao ◽  
Yijie Zhang ◽  
Shengping Wang ◽  
Xiaojun Yan ◽  
...  

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