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Online since: July 2021
Authors: Supachart Muangyai, Parames Chutima
Al-Ghonamy1, M.
El-Wakil., 2010.
El-Wakil., 2010.
Online since: December 2019
Authors: Antonio Caggiano, Diego Said Schicchi, Stefan Harenberg, Sha Yang, Viktoria Malarics-Pfaff, Matthias Pahn, Frank Dehn, Eddie Koenders
El-Tawil and A.E.
Al-Gadhib, M.
Al-Gadhib, M.
Online since: June 2008
Authors: Marianna Halász, Péter Tamás, József Gräff, Lajos Szabó
Four pictures of a cross section curves and the reconstructed cross section
pe of
i,j
Patches a el.
al p p *+ *+ *+]_ *+]_ 2 n2 n2 1i S i M i 1i S i M i S 0 M 0 pbbpaapa 2 1 a 2 1 pD Â Â ??
al p p *+ *+ *+]_ *+]_ 2 n2 n2 1i S i M i 1i S i M i S 0 M 0 pbbpaapa 2 1 a 2 1 pD Â Â ??
Online since: April 2020
Authors: Allwar Allwar, Gusti D. Apriliani, Fairus M. Wokas, Eka Y. Saputri
Saragi, et al.
El-Geundi, Comparative cost of color removal from textile ef- fluents using natural adsorbents, J.
El-Geundi, Comparative cost of color removal from textile ef- fluents using natural adsorbents, J.
Online since: July 2005
Authors: Julian Martínez-Fernández, António Ramirez de Arellano-López, J.J. Quispe Cancapa, José M. López-Cepero
Martínez Fernández:
Avances en el estudio fractográfico de fibras cerámicas de circona-erbia mediante microscopía
óptica confocal, Bol.
Peña et al: Bol.
Peña et al: Bol.
Online since: July 2005
Authors: Ke Lu, Jian Lu, Delphine Retraint, T. Roland
This has for effect to relax the stress inside the material and
mi cr o
comput er
CCD
camer a
l ens
spat i al
f i l t er
M1
l aser
speci men
gr at i ng
dr i l l i ng machi ne
t r ansl at i on
st age
M8
M7
M3
M2
M9
M10
M6
M11
M5
M4
M1- M11: mi r r or s
(a)
Nanostructured layers
(b) Sample thickness (µm) by this way to give it back some more possibility of deformation.
Erb, A.M El-Sherik, G.
Erb, A.M El-Sherik, G.
Online since: May 2011
Authors: Hui Zhou, Fei Kang, Jun Jie Li
ZHANG et al [10] studied the seismic coefficient of earth- rockfill dams with the height more than 150 m.
Four seismic waves with different frequency spectra were adopted, including Taft wave (the first wave), El Centro wave (the second wave), Banshen wave (the third wave) and Shenhu wave (the fourth wave).
Four seismic waves with different frequency spectra were adopted, including Taft wave (the first wave), El Centro wave (the second wave), Banshen wave (the third wave) and Shenhu wave (the fourth wave).
Online since: October 2011
Authors: You Liang Ji, Rui Zhang
References
[1] Cross T A, Baker M R, Chapin M A, et al.
[2] Vail P R,Audemard F,Bowman S A,el a1.The stratigraphic signatures of tectonics,eustasy and sedimentology an overview [A].In:Einsele G,Ricken W,Seilacher A eds.Cycles and Events in Stratigraphy[c].Berlin Heidberg:Springer Verlag,1 991:617-659
[2] Vail P R,Audemard F,Bowman S A,el a1.The stratigraphic signatures of tectonics,eustasy and sedimentology an overview [A].In:Einsele G,Ricken W,Seilacher A eds.Cycles and Events in Stratigraphy[c].Berlin Heidberg:Springer Verlag,1 991:617-659
Online since: October 2014
Authors: Xiao Bing Liu, Fei Yan Gong
Lenhardt, A.L.
Canamero, J.L. de la Fuente, E.L.
Canamero, J.L. de la Fuente, E.L.
Online since: April 2013
Authors: Bao Jun Pang, Yong Chen, Wei Zheng
McCARTHY et al.[12] used CDM model to simulate bird-strike impact, but the input parameters of the model were mostly characterized on the estimated stress-strain curves as no extensive experimental tests on corresponding S2-glass/epoxy were conducted.
Ladeveze, E.L.
Ladeveze, E.L.