کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4546391 1627022 2016 15 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Characterization of physical mass transport through oil sands fluid fine tailings in an end pit lake: a multi-tracer study
ترجمه فارسی عنوان
خصوصیات انتقال جرم فیزیکی از طریق ماسه های نفتی مایع بتونی خوب در یک دریاچه گودال: یک مطالعه چند تکراری است
کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


• Mass transport through fluid fine tailings is primarily advection due to dewatering.
• Isotope and temperature profiles do not match simple advection-diffusion models.
• Models with mixing in the top portion of the fluid fine tailings provided better fit.
• Mixing of the tailings is possible due to low values for viscosity and yield stress.
• Notable consideration for groundwater regime at lake bottoms with soft sediments.

Soft tailings pose substantial challenges for mine reclamation due to their high void ratios and low shear strengths, particularly for conventional terrestrial reclamation practices. Oil sands mine operators have proposed the development of end pit lakes to contain the soft tailings, called fluid fine tailings (FFT), generated when bitumen is removed from oil sands ore. End pit lakes would be constructed within mined-out pits with FFT placed below the lake water. However, the feasibility of isolating the underlying FFT has yet to be fully evaluated. Chemical constituents of interest may move from the FFT into the lake water via two key processes: (1) advective-diffusive mass transport with upward pore water flow caused by settling of the FFT; and (2) mixing created by wind events or unstable density profiles through the lake water and upper portion of the FFT. In 2013 and 2014, temperature and stable isotopes of water profiles were measured through the FFT and lake water in the first end pit lake developed by Syncrude Canada Ltd. Numerical modelling was undertaken to simulate these profiles to identify the key mechanisms controlling conservative mass transport in the FFT. Shallow mixing of the upper 1.1 m of FFT with lake water was required to explain the observed temperature and isotopic profiles. Following mixing, the re-establishment of both the temperature and isotope profiles required an upward advective flux of approximately 1.5 m/year, consistent with average FFT settling rates measured at the study site. These findings provide important insight on the ability to sequester soft tailings in an end pit lake, and offer a foundation for future research on the development of end pit lakes as an oil sands reclamation strategy.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Contaminant Hydrology - Volume 189, June 2016, Pages 12–26
نویسندگان
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