Field evaluation of deformation characteristics of a lacustrine clay deposit using seismic piezocone tests

2010 ◽  
Vol 116 (3-4) ◽  
pp. 251-260 ◽  
Author(s):  
Guojun Cai ◽  
Songyu Liu ◽  
Liyuan Tong
1960 ◽  
Vol 11 (1) ◽  
pp. 20-23
Author(s):  
Hans Pichler

Abstract. The discussion deals with the opinion of Ganss (1953) according to which the altitude of a lacustrine-clay deposit found by him, 870 metres above sea-level, is proof for an enormous interglacial filling-up (350 metres in thickness) of the Berchtesgaden basin (Berchtesgaden Alps, Upper Bavaria). This view of Ganss necessarily includes — in accordance with interglacial morphology — similar immense accumulations in the neighbouring Salzach valley and in the Reichenhall basin. The fact, however, that there are no remainders of such enormous gravel beds, is contrary to the Ganss interpretation. The local lacustrine-clay occurrence is to be considered as a deposit of a small cirque lake within the former cirque expanse of the "Resten".


Author(s):  
J. E. O’Neal ◽  
K. K. Sankaran ◽  
S. M. L. Sastry

Rapid solidification of a molten, multicomponent alloy against a metallic substrate promotes greater microstructural homogeneity and greater solid solubility of alloying elements than can be achieved by slower-cooling casting methods. The supersaturated solid solutions produced by rapid solidification can be subsequently annealed to precipitate, by controlled phase decomposition, uniform 10-100 nm precipitates or dispersoids. TEM studies were made of the precipitation of metastable Al3Li(δ’) and equilibrium AL3H phases and the deformation characteristics of a rapidly solidified Al-3Li-0.2Ti alloy.


1992 ◽  
Vol 11 (1) ◽  
pp. 27-37 ◽  
Author(s):  
Peter E. Loeb ◽  
Steven C. Mirabello ◽  
James R. Andrews
Keyword(s):  

1992 ◽  
Vol 11 (1) ◽  
pp. 1-25 ◽  
Author(s):  
Steven C. Mirabello ◽  
Peter E. Loeb ◽  
James R. Andrews
Keyword(s):  

1976 ◽  
Vol 73 ◽  
pp. 1051-1057
Author(s):  
Sadao Isotani ◽  
Alain J.-P. Alix

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