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Evidence of Dual Scale Porous Mechanisms During fluid migration in Hardwood Species (Ⅱ) A Dual Scale Computational Model to Describe the Experimental Results

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Chinese Journal of Chemical Engineering 2004年第6期12卷 783-791页

作者： Patrick PERR LERMAB-UMR INRA/ENGREF/UHP 1093 ENGREF-INRA-14 rue Girardet 54042 Nancy Cedex France

The second part of this paper is devoted to the computational modelling of transient water migration in hardwood. During re-saturation, the moisture content, measured during the process by using X-ray attenuation (see part 1 of this paper), increases quickly very close to the cavity, but requires a very long time for the remaining part of the sample to absorb the moisture in wetting. For this configuration and this material, the macroscopic approach fails. Consequently, a dual-porosity approach is proposed. The computational domain uses a 2-D axisymmetric configuration for which the axial coordinate represents the macroscopic longitudinal direction of the sample whereas the radial coordinate allows the slow migration from each active vessel towards the fibre zone to be considered. The latter is a microscopic space variable. The moisture content field evolution depicts clearly the dual scale mechanisms:a very fast longitudinal migration in the vessel followed by a slow migration from the vessel towards the fibre *** macroscopic moisture content field resulting from this dual scale mechanism is in quite good agreement with the experimental data.

关键词： fluid migration dual-porosity computational model hardwood vessel fibre

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Dynamics of thinning and destruction of the continental cratonic lithosphere: Numerical modeling

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Science China Earth Sciences 2018年第7期61卷 823-852页

作者： Mingqi LIU Zhonghai LI Key Laboratory of Computational Geodynamics College of Earth and Planetary Sciences University of Chinese Academy of Sciences Institute of Geology Chinese Academy of Geological Sciences

Thinning of the cratonic lithosphere is common in nature, but its destruction is not. In either case, the mechanisms for both thinning and destruction are still widely under debate. In this study, we have made a review on the processes and mechanisms of thinning and destruction of cratonic lithosphere according to previous studies of geological/geophysical observations and numerical simulations, with specific application to the North China Craton(NCC). Two main models are suggested for the thinning and destruction of the NCC, both of which are related to subduction of the oceanic lithosphere. One is the "bottom-up" model, in which the deeply subducting slab perturbs and induces upwelling from the hydrous mantle transition zone(MTZ). The upwelling produces mantle convection and erodes the bottom of the overriding lithosphere by the fluid-meltperidotite reaction. Mineral compositions and rheological properties of the overriding lithospheric mantle are changed, allowing downward dripping of lithospheric components into the asthenosphere. Consequently, lithospheric thinning or even destruction occurs. The other is the "top-down" model, characterized by the flat subduction of oceanic slab beneath the overriding cratonic lithosphere. Dehydration reactions from the subducting slab would significantly hydrate the lithospheric mantle and decrease its rheological strength. Then the subduction angle may be changed from shallow to steep, inducing lateral upwelling of the asthenosphere. This upwelling would heat and weaken the overriding lithospheric mantle, which led to the weakened lithospheric mantle dripping into the asthenosphere. These two models have some similarities, in that both take the subducting oceanic slab and relevant fluid migration as the major driving mechanism for thinning or destruction of the overriding cratonic lithosphere. The key difference between the two models is the effective depth of the subducting oceanic slab. One is stagnation and flattening in t

关键词： Lithospheric thinning Cratonic destruction Big mantle wedge Plate subduction fluid migration Numericalmodeling

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Perspectives on the Potential migration of fluids Associated with Hydraulic Fracturing in Southwest Florida

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Journal of Environmental Science and Engineering(A) 2018年第3期7卷 108-124页

作者： William C. Hutchings Richard G. Lewis Environmental Department GHD Services Inc. Fort Myers 33901 USA Lewis Solutions Fort Myers 33907 USA

The variable-density flow model-SEAWAT Version 4, was used to evaluate the hydrogeological conditions associatedwith hydraulic fracturing （fracking） the limestone oil reservoir in the Lower Cretaceous Sunniland Formation of Southwest *** research contributes to the understanding of the controls on fluid and potential contaminant migration, following high pressurehydraulic fracturing. A hydraulic fracturing treatment used recently in this formation at the Collier-Hogan 20-3H well represents thebase case simulation. Multiple stage fracturing using typical stress periods, a modelled fracture zone radius, and various injectionrates were tested to evaluate the potential for horizontal and vertical fluid migration in and from the reservoir under dynamicconditions, with TDS used as a tracer. Hypothetical scenarios including preferential vertical pathways between the SunnilandFormation and the Lower Floridan aquifer Boulder Zone were also simulated. Results indicate that injected fluids do not migratesignificantly in the lateral and vertical directions beyond the design fractured zone, unless a preferential pathway exists within closeproximity to the fractured zone. In a worst-case scenario under the simulated conditions, vertical heads are approximately 580 metersgreater than static conditions and fluids associated with hydraulic fracturing vertically migrate approximately 500 meters; therefore,the quality of the deepest sources of drinking water is not compromised. Analytical results from a monitoring well installed in theimmediate vicinity of the Collier-Hogan 20-3H well and at the base of the deepest source of drinking water support the conclusionthat impacts from hydraulic fracturing fluids have not migrated into the deepest sources of drinking water.

关键词： Hydraulic fracturing Sunniland Formation fluid migration

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