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24-Pet-A1 Principles of Stratigraphy and Sedimentation · December 2014

Question 13 of 24: Sediment Transport Modes in Fluvial Systems

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Notes on this paper

EGBC National Exam — Petroleum Engineering, 98-Pet-A1 Principles of Stratigraphy & Sedimentation, 2014-Dec. 3 hours duration; closed book, no calculator permitted. The paper has three parts: Part A1 (Questions 1–7, sedimentary processes, 5 marks each, answer any 4 of 7 for 20 marks), Part A2 (Questions 8–15, brief/multiple-choice, 3 marks each, answer any 5 of 8 for 15 marks), and Part B (Questions 16–24, stratigraphy, 5 marks each, answer any 6 of 9 for 30 marks) – a 65-mark maximum.

Reference texts: Boggs, S. Jr., Principles of Sedimentology and Stratigraphy, 5th ed., Pearson (grain texture, sediment transport, bedforms, carbonate/evaporite systems, sequence stratigraphy, unconformities, stratigraphic principles); Tucker, M.E., Sedimentary Petrology, 3rd ed., Blackwell (carbonate classification, diagenesis, dolomitization); Nichols, G., Sedimentology and Stratigraphy, 2nd ed., Wiley-Blackwell (fluvial systems, sequence stratigraphy, stratigraphic units); Reading, H.G. (ed.), Sedimentary Environments: Processes, Facies and Stratigraphy, 3rd ed., Blackwell (facies models, trace fossils); Selley, R.C. & Sonnenberg, S., Elements of Petroleum Geology, 3rd ed., Academic Press (source rocks, reservoir quality); International Commission on Stratigraphy, International Chronostratigraphic Chart (geological time scale).

Question 13: Sediment Transport Modes in Fluvial Systems (3 marks)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Rivers transport sediment in three principal modes. Dissolved (solute) load – material transported in true chemical solution (e.g. Ca²⁺, HCO₃⁻, dissolved silica), invisible and unrelated to bed material. Suspended load – fine sand, silt and clay held aloft by turbulent upward eddies, moving essentially at the flow's own velocity; it is conventionally split into wash load (very fine material, e.g. clay, kept permanently in suspension and supplied mainly from outside the channel, e.g. hillslope wash) and suspended bed material (coarser silt/fine sand that periodically exchanges with the bed). Bed load – coarser sand and gravel moving along or very near the bed by traction: rolling, sliding, and saltation (short intermittent hops as the current briefly lifts a grain before it is redeposited downstream).