Sediments and Sedentate - Clay 

Page / - last modified by Roelof Zwaan on 2022/01/12 13:43 

Clay 
last modified by Roelof Zwaan
on 2022/01/12 13:43

Table of Contents

Clay is a clastic sedimentary rock consisting of consolidated grains. The grains need to have a diameter smaller than 2 micrometer according to european norms, or more than 25% lutum content. The grains of this rock are less coarse than those of silt. In the field this soil type is hard to distinguish from silt. By adding water and rubbing the found soil in your hand one can distinguish silt from clay. With silt still some loose particles can be felt and with clay these particles are not present.
What is clay?
Clay is a very fine grained sedimentary material. It has a very abundant occurence, coming mostly from Shale, the most abundant sedimentary rock. Aside from grain size, clay tends to be defined by it's changing plastic properties based on the moisture level. This is one of the ways that silt and clay can be told apart in the field without the aid of analytical techniques.
Silt or clay?
There are several tests you can do to determine if the soil you're dealing with is Silt or Clay.
Dry strength test
Roll the soil up to a ball and let it dry completely. Then, once the soil is dry, try crushing the soil with your fingers. If it crushes easily, it's more likely to be silt. If it takes effort to crush, it's more likely to be clay.
Dilatency test
Because the permeability of clay and silt are different, we can use this factor as an identification test. This is done my mixing a small ammount of soil with water in the palm of your hand. Once this is done, tap the back of your hand or shake the soil inside your hand. If it is Silty soil, a quick reaction will occur where water will rise to the surface and gives the soil a glistening appearance. In the case of clay, the water will be quickly absorbed into the clay again and leave the soil with a dull look. There can be several reaction speeds / testresults.
Plasticity test
This test makes use of the molding characteristic of clay. This is done by taking a bit of moist soil, rolling it into a ball and then try to roll it into a thin 3mm long thread. If the soil holds clay this should pose no problems, whereas with silt the soil will crack / it should be almost impossible to roll the soil into a thin thread and still support its own weight.
Dispersion test
For the dispersion test, you can add some soil to a flask or jar with water and shake it up, so that the soil particles will be suspended in the water. Then, you can determine rough percentages of sand, silt and clay by seeing how long it takes for particles to settle. Sand particles will settle at around 15 seconds, silt particles will settle at around 30 seconds and clay particles can remain suspended for hours.
References
•	NEN-EN-ISO 14688-1:2019
Clay

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Contents
•	What is clay?
•	Silt or clay?
•	References
•	Clay