Ground state potentials for alkaline-earth–helium diatoms calculated by the surface integral method

2000 ◽  
Vol 324 (5-6) ◽  
pp. 403-410 ◽  
Author(s):  
Ulrich Kleinekathöfer
1997 ◽  
Vol 66 (4) ◽  
pp. 1074-1078 ◽  
Author(s):  
Takashi Ikeda ◽  
Hideyuki Kobayashi ◽  
Yoshihiro Ohmura ◽  
Hirohide Nakamatsu ◽  
Takeshi Mukoyama

1983 ◽  
Vol 4 ◽  
pp. 124-128 ◽  
Author(s):  
Jerome B. Johnson

Two methods are presented for calculating ice loads on structures using measurements from sensors imbedded in a floating ice sheet and from instruments attached to a structure. The first method uses a mathematical model describing ice/structure interaction for a cylindrical structure to interpret stress measurements. This technique requires only a few sensors to develop an estimate of ice loads, However, analytical and experimental results indicate that using a mathematical model to interpret stress measurements can result in inaccurate load estimates due to uncertainty in the accuracy of the model and and the uncertainty of using local ice stresses to calculate total ice forces. The second method of calculating ice loads on structures utilizes Euler and Cauchy’s stress principle. In this, the surface integral method, the force acting on a structure is determined by summing the stress vectors acting on a surface which encompasses the structure. Application of this technique requires that the shear and normal components of stress be known along the surface. Sensors must be spaced close enough together so that local stress variations due to the process of ice failure around a structure can be detected. The surface integral method is a useful technique for interpreting load and stress measurements since a knowledge of the mechanism of ice/structure interactions is not needed. The accuracy of the method is determined by the density of sensors along the surface. A disadvantage of the technique is that a relatively large number of sensors are needed to determine the stress tensor along the surface of interest.The surface integral method can be used to examine the effects of grounded ice rubble on structural ice loads. Two instrumented surfaces, one enclosing a structure and the other enclosing the structure and rubble field can be used to estimate the load acting only on the structure and also on the structure/ rubble-field system.


Author(s):  
T.C. Scott ◽  
M. Aubert-Fr�con ◽  
D. Andrae ◽  
J. Grotendorst ◽  
J.D. Morgan III ◽  
...  

2016 ◽  
Vol 15 (05) ◽  
pp. 1650040 ◽  
Author(s):  
Kaushik Hatua ◽  
Prasanta K. Nandi

In the present work, electronic structure and second hyperpolarizability of a number of alkaline earth metals (M [Formula: see text] Be, Mg and Ca) complexes with carbon nanotube (CNT) has been studied by using different DFT functional. The complexes have sufficient thermal stability. Significant amount of charge transfer from metal to CNT results in stronger ground state polarization. The second hyperpolarizability obtained at different DFT functional (BHHLYP, CAM-B3LYP, B2PLYP, [Formula: see text]B97XD) showed a consistent trend. The magnitude of second hyperpolarizability of M@CNT[3,0] complexes enhances rather appreciably when a second metal atom is introduced into other mouth position. The longitudinal component of second hyperpolarizability of M@CNT[3,0]@M complexes increases with increasing size of metal atom. The magnitude of second hyperpolarizability of Ca@CNT[3,0]@Ca complex is comparable with Fe([Formula: see text]-C[Formula: see text]B[Formula: see text]. However, widening/lengthening of CNT markedly reduces the cubic responses. The two state model can qualitatively explain the variation of second hyperpolarizability.


1997 ◽  
Vol 105 (2-3) ◽  
pp. 108-126 ◽  
Author(s):  
J.M. Rejcek ◽  
S. Datta ◽  
N.G. Fazleev ◽  
J.L. Fry ◽  
A. Korzeniowski

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