Abstract The radiation of steady surface gravity waves by a uniform stream$$U_{0}$$ over locally confined (width$$L$$ ) smooth topography is analyzed based on potential flow theory. The linear solution to this classical problem is readily found by Fourier transforms, and the nonlinear response has been studied extensively by numerical methods. Here, an asymptotic analysis is made for subcritical flow$$D/\lambda > 1$$ in the low-Froude-number ($$F^{2} \equiv \lambda /L \ll 1$$ ) limit, where$$\lambda = U_{0}^{2} /g$$ is the lengthscale of radiating gravity waves and$$D$$ is the uniform water depth. In this regime, the downstream wave amplitude, although formally exponentially small with respect to$$F$$ , is determined by a fully nonlinear mechanism even for small topography amplitude. It is argued that this mechanism controls the wave response for a broad range of flow conditions, in contrast to linear theory which has very limited validity.
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The northeastern Algeria hydrothermal system: gravimetric data and structural implication
Abstract The Tell Atlas of Algeria has a huge potential for hydrothermal energy from over 240 thermal springs with temperatures up to$$98^\circ$$ C in the Guelma area. The most exciting region is situated in the northeastern part which is known to have the hottest hydrothermal systems. In this work, we use a high-resolution gravity study to identify the location and origin of the hot water, and how it reaches the surface. Gravimetric data analysis shows the shapes of the anomalies arising due to structures at different subsurface depths. The calculation of the energy spectrum for the data also showcases the depths of the bodies causing anomalies. 3D-Euler deconvolution is applied to estimate the depths of preexisting tectonic structures (faults). These preprocessing steps assist with assessing signal attenuation that impacts the Bouguer anomaly map. The residual anomaly is used in a three-dimensional inversion to provide a subsurface density distribution model that illustrates the locations of the origin of the dominant subsurface thermal systems. Overall, the combination of these standard processing steps applied to the measurements of gravity data at the surface provides new insights about the sources of the hydrothermal systems in the Hammam Debagh and Hammam Ouled Ali regions. Faults that are key to the water infiltrating from depth to the surface are also identified. These represent the pathway of the hot water in the study area.
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- PAR ID:
- 10415384
- Publisher / Repository:
- Springer Science + Business Media
- Date Published:
- Journal Name:
- Geothermal Energy
- Volume:
- 11
- Issue:
- 1
- ISSN:
- 2195-9706
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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