Academic Journal

Turbulence Processes within Turbidity Currents

التفاصيل البيبلوغرافية
العنوان: Turbulence Processes within Turbidity Currents
المؤلفون: Wells, Mathew G., Dorrell, Robert M.
بيانات النشر: Annual Reviews
سنة النشر: 2020
المجموعة: University of Hull: Repository@Hull
مصطلحات موضوعية: Turbidity current, Basal drag coefficient, Entrainment ratio, Sinuouschannel, Convective sedimentation, Coriolis force
الوصف: Sediment-laden gravity currents, or turbidity currents, are density-driven flows that transport vast quantities of particulate material across the floor of lakes and oceans. Turbidity currents are generated by slope failure or initiated when a sediment-laden flow enters into a lake or ocean; here, lofting or convective sedimentation processes may control flow dynamics. Depending upon the internal turbulent mixing, which keeps particles in suspension, turbidity currents can travel for thousands of kilometers across the seafloor. However, despite several competing theories, the process for the ultralong runout of these flows remains enigmatic. Turbidity currents often generate large sinuous channel-levee systems, and the dynamics of how turbidity currents flow around channel bends are strongly influenced by internal density and velocity structure, with large-scale flows being modified by the Coriolis force. Therefore, understanding some of the largest sedimentary structures on the Earth's surface depends on understanding the turbulence processes within turbidity currents.
نوع الوثيقة: article in journal/newspaper
اللغة: English
تدمد: 0066-4189
Relation: https://hull-repository.worktribe.com/output/3646212; Annual Review of Fluid Mechanics; Volume 53; Issue 1; Pagination 59-83
DOI: 10.1146/annurev-fluid-010719-060309
الاتاحة: https://hull-repository.worktribe.com/output/3646212
https://doi.org/10.1146/annurev-fluid-010719-060309
رقم الانضمام: edsbas.74374059
قاعدة البيانات: BASE
الوصف
تدمد:00664189
DOI:10.1146/annurev-fluid-010719-060309