Unit of sedimentology

 

During field campaigns, suspended sediment samples, bottom sediment samples and cores are taken and subjected to non-destructive (only in the case of cores) and destructive analysis.

Sample taken with Shipek Sampler

Guayas GIS Project - Guayaquil, Ecuador

A sample of bottom sediments taken with a Shipek-sampler

A core (1 m length) taken by a diver in the Guayas Estuary

 

Non-destructive analysis comprises radiography and gamma-densitometry

X-Ray Radiograph

Gammadensitometry log

Radiograph from core

Dark regions are fine cohesive sediments, while light layers are coarser, sandy sediments.

Gamma-log

 

Afterwards the core is opened and after a visual inspection destructive analysis are performed.  Suspended sediments and bottom sediments (bulk samples) are always submitted to destructive analysis immediately.

 

Environmental Scanning Electron Microscope (ESEM) Image

Grain Size Spectrum (1/4 Phi interval)

ESEM photo of bottom sediments showing flocs and diatoms

Grain size spectrum of suspended sediments

   
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