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  • 1
    Publication Date: 2019
    Description: Abstract Backflow phenomenon, as a consequence of hydraulic fracturing, is of considerable technical and environmental interest. Here, backflow of a non‐Newtonian fluid from a disc‐shaped elastic fracture is studied theoretically and experimentally. The fracture is of constant aperture ℎ and the outlet section at constant pressure pe. We consider a shear‐thinning power‐law fluid with flow behavior index n. Fracture walls are taken to react with a force proportional to hλ with λ a positive elasticity exponent; for λ = 1 linear elasticity holds. Constant overload f0, acting on the fracture, is also embedded in the model. A transient closed‐form solution is derived for the (і) fracture aperture, (іі) pressure field, and (ііі) outflow rate. The particular case of a Newtonian fluid (n = 1) is explicitly provided. For pe = 0 and f0 = 0, the residual aperture and outflow rate scale asymptotically with time t as t‐n/(n+λ+1) and tn/(2n+λ+1)/(n+λ+1) respectively, thus generalizing literature results for n = 1 and/or λ = 1. For non‐zero exit pressure and/or overload, the fracture aperture tends asymptotically to a constant value depending on λ, n, pe, f0, and other geometrical and physical parameters. Results are provided in dimensionless and dimensional form including the time to achieve a given percentage of fluid recovery. In addition, an example application (with values of parameters derived from field scale applications) is included to further characterize the influence of fluid rheology. Experimental tests are conducted with Newtonian and shear‐thinning fluids and different combinations of parameters to validate the model. Experimental results match well the theoretical predictions, mostly with a slight overestimation.
    Print ISSN: 0043-1397
    Electronic ISSN: 1944-7973
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 2020-06-24
    Description: The purpose of this study is to analyze the surface temperature and the distribution of thermal signatures on Tuscany’s geothermal districts using data obtained through three separate surveys via satellite and an unmanned aerial vehicle (UAV). The analysis considers the highest available spatial resolution ranging from hundreds of meters per pixel of the satellite thermal images and the tenths/hundreds of centimeters per pixel of the thermal images acquired by the UAV. The surface temperature maps obtained by satellite data acquired at suitable spatial resolution and the thermal measurements obtained by the thermal camera installed on the UAV were orthorectified and geocoded. This allowed, for example, following the evolution of thermal anomalies, which may represent a modification of the current state of the geothermal field and a possible hazard for both the population and industrial assets. Here, we show the results obtained in three field campaigns during which the simultaneous acquisition of Landsat 8 satellite and UAV (FlyBit octocopter, IDS, Rome, Italy) thermal data were analyzed. By removing the atmosphere contribution from Landsat 8 data, we have produced three surface temperature maps that are compared with the ground field measurements and the surface temperature maps elaborated by FLIR VUE PRO-R on the UAV.
    Electronic ISSN: 2072-4292
    Topics: Architecture, Civil Engineering, Surveying , Geography
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