1 / 8

SEDIMENTATION

SEDIMENTATION. Objective: To become familiar with the different types of marine sediments, the processes that make them, and understand how turbidity currents are created. Biogenous Sediments – Exercise 1. Flocculation. How does sediment behave differently in SW vs. FW? Demonstration.

ronny
Download Presentation

SEDIMENTATION

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. SEDIMENTATION Objective: To become familiar with the different types of marine sediments, the processes that make them, and understand how turbidity currents are created

  2. Biogenous Sediments – Exercise 1

  3. Flocculation How does sediment behave differently in SW vs. FW? Demonstration

  4. Exercise 2 – Turbidity Currents (~55mph)

  5. Exercise 2 – Turbidity tubes • Set up tube – • Set angle • Fill with water • Assign tasks (one timer, one recorder, one pourer, one ruler) • LEAVE BLACK CLAMP ON TUBE!!!

  6. Exercise 2 – Turbidity tubes • Run 6 trials • 2 at 40ppt Green (different angles) • 2 at 80ppt Red (different angles) • 2 Silica (Yellow is High density and Orange is Low density plus one small scoop of silica)

  7. Measured vs. Theoretical • U = 0.7 [(d1 - d2)(gh)/d2] -2 Densitiesd2 – Water =1 g/ml d1 – 40ppt = 1.026 g/ml - 80ppt =1.055 g/ml - High Silica = 1.19 g/ml - Low Silica = 1.095g/ml

More Related