scholarly journals Fourier analysis of Ramsey fringes observed in a continuous atomic fountain for in situ magnetometry

2011 ◽  
Vol 56 (1) ◽  
pp. 11001 ◽  
Author(s):  
G. Di Domenico ◽  
L. Devenoges ◽  
A. Stefanov ◽  
A. Joyet ◽  
P. Thomann
2019 ◽  
Vol 52 (7) ◽  
pp. 075003
Author(s):  
Ottó Elíasson ◽  
Robert Heck ◽  
Jens S Laustsen ◽  
Mario Napolitano ◽  
Romain Müller ◽  
...  
Keyword(s):  

2018 ◽  
Vol 89 (1) ◽  
pp. 013108 ◽  
Author(s):  
Ludwig Krinner ◽  
Michael Stewart ◽  
Arturo Pazmiño ◽  
Dominik Schneble

2019 ◽  
Vol 52 (21) ◽  
pp. 219601
Author(s):  
Ottó Elíasson ◽  
Robert Heck ◽  
Jens S Laustsen ◽  
Mario Napolitano ◽  
Romain Müller ◽  
...  
Keyword(s):  

Catalysts ◽  
2021 ◽  
Vol 11 (5) ◽  
pp. 636
Author(s):  
Malebelo Maphutha ◽  
Dominic de Oliveira ◽  
Thulani M. Nyathi ◽  
Mohamed I. Fadlalla ◽  
Robert Henkel ◽  
...  

The presented study investigated the effects of temperature (350–650 °C) and gas environment (pure Ar versus a H2O/H2 partial pressure ratio (PH2O/PH2) of 5) on the extent of sintering and oxidation of Al2O3-supported Ni0 nanoparticles (≈4 nm). We note that a PH2O/PH2 of 5 corresponds to a simulated CO conversion of 94% during methanation. Sintering and oxidation were studied using in situ magnetometry, while ex situ TEM analyses confirmed the particle sizes before and after the magnetometry-based experiments. It was found that increasing the temperature from 350 to 650 °C in Ar at atmospheric pressure causes a negligible change to the average size and degree of reduction (DOR) of the starting Ni0 nanoparticles. However, studying the same temperature window under hydrothermal conditions at 10 bar causes significant particle growth (≈9 nm) and the development of a bimodal distribution. Furthermore, the presence of steam decreases the DOR of Ni0 from 86.2% after initial activation to 22.2% due to oxidation. In summary, this study reports on the expected sintering and oxidation of Ni-based catalysts under high CO conversion conditions at elevated temperatures during methanation. Importantly, we were able to demonstrate how magnetometry-based analyses can provide similar size information (and changes thereof) as those observed with TEM but with the added advantage that this information can be obtained in situ.


Author(s):  
Gus Jeans ◽  
Wenting Xiao ◽  
Alfred R. Osborne ◽  
Christopher R. Jackson ◽  
Douglas A. Mitchell

This paper describes the first application of Nonlinear Fourier Analysis to the quantification of internal soliton current speeds in offshore engineering design. Large amplitude solitary internal waves produce strong, rapidly varying currents that may cause hazards to offshore operations in several regions of the world. These phenomena are commonly referred to in Industry as “solitons.” Soliton quantification was undertaken using the latest methodologies and software available from the Nonlinear Fourier Analysis Spectral Tools (NFAST) Joint Industry Project. Solitons require rapidly sampled in-situ data for reliable quantification. Such measurements are typically of very short duration compared to the time scales needed for engineering quantification. Similarly, numerical models capable of representing solitons are computationally expensive, and thus have limited capabilities for efficiently developing the long-term simulations required to supplement in-situ data. NFAST aims to address these issues by enabling new Hyperfast Nonlinear Fourier Analysis computational techniques. Interface displacements, derived from temperature measurements, were the primary input to soliton quantification. Associated current speeds were estimated from relevant theory and validated with available measured current data. In this particular case, the temperature measurements are considered to be more reliable than using the measured current data directly. Application of NFAST codes produced a synthetic dataset of soliton amplitudes and speeds with an effective duration of approximately 100 years, a period that is considerably greater than the duration of available measured data. This provided extreme values consistent with extrapolation of the measured soliton data, but with a considerable reduction in uncertainty.


1955 ◽  
Vol 3 (2) ◽  
pp. 119-126
Author(s):  
H.J. Timmers

The theory of non-stationary flow has, been applied to the movement of water in the upper layers of the Pleistocene terrace on the western side of the river IJssel. A Fourier analysis of the movement of the water levels in the river and in several wells permitted calculation of the ratio of permeability to the storage coefficient of the soil. Assuming that the storage coefficient was o. I0 and the average thickness of the aquifer was I5 m, the average permeability was calculated to be 53 m/day. The discharge of water from the soil (0.8 cu m/day) can be calculated without knowing the thickness of the aquifer. The method can be used to calculate the amount of water needed for irrigation and the amount of water percolating from the hinterland to the river. (Abstract retrieved from CAB Abstracts by CABI’s permission)


2020 ◽  
Vol 20 (1) ◽  
pp. 76-83 ◽  
Author(s):  
Qiang Li ◽  
Hongsen Li ◽  
Qingtao Xia ◽  
Zhengqiang Hu ◽  
Yue Zhu ◽  
...  

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