Upscaling calcite dissolution rates in a tight reservoir sandstone
نویسندگان
چکیده
Abstract Calcite is a highly abundant mineral in the Earth’s crust and occurs as cement phase numerous siliciclastic sediments, where it often represents most reactive component when fluid percolates through rock. Hence, objective of this study to derive calcite dissolution rates on different scales reservoir sandstone using surface experiments combined with vertical scanning interferometry (VSI) two types core plug experiments. The 3D geometry inside rock cores was characterized by X-ray micro-computed tomography (µXCT) used attempt rate upscaling from scale. Initially (without upscaling), our comparison far-from-equilibrium at (µm-mm-scale, low residence time) normalized obtained (cm-scale, high revealed differences 0.5–2 orders magnitude. µXCT geometric area connected open pore space $$\left( {GSA_{{Cc,{\text{open}}}} } \right)$$ G S A C c , open considers accessibility heterogeneously distributed that can largely vary between individual samples, but greatly affects effective rates. Using parameter upscale µm- cm-scale, deviation upscaled total measured less than one order magnitude for all investigated cores. Thus, $$GSA_{{Cc,{\text{open}}}}$$ showed be reasonably suitable
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ژورنال
عنوان ژورنال: Environmental Earth Sciences
سال: 2022
ISSN: ['2199-9163', '2199-9155']
DOI: https://doi.org/10.1007/s12665-022-10399-5