-------- Forwarded Message --------
Subject: [powders-and-grains] Granular Matter Webinar Series Announcement
Date: Fri, 6 May 2022 16:14:48 +0000
From: Jack Manzi <[log in para visualizar]>
Reply-To: Jack Manzi <[log in para visualizar]>
To: [log in para visualizar] <[log in para visualizar]>

Dear Powders and Grains Community,


Hello all, I hope you are well.


On behalf of the Editors-in-Chief Hans Herrmann, Stefan Luding, and Heinrich Jaeger, I would like to announce a webinar presented by the journal Granular Matter, on Friday, 27 May 2022. Our speaker is Prof. Glenn McDowell (University of Nottingham), the topic and abstract are:


“What is the Normal Compression of Soil?”

It has long been widely accepted that the normal (plastic) compression of sand and clay are very similar: a linear relationship exists beyond some sort of yield point when voids ratio is plotted against the logarithm of applied stress – at least over one log cycle of stress.  However the reason for this similarity in behaviour has not been exposed.  We present some early thoughts for sand on the evolution of a fractal distribution of particle sizes as stress increases and particles break.  Only recently have we been able to explain the normal compression line more clearly and to propose a new linear relationship in log voids ratio – log stress space.  The approach recognises the role of the smallest grains, getting smaller and statistically stronger as a grading with a fractal number of 2.5 emerges.  However many questions have remained unanswered: why should the fractal number be 2.5, what are the smallest particles (how small is small?) and what about the rest of critical state soil mechanics (peak strength, dilatancy, state boundary surface and so on)?  And the important question as to why clay should behave macroscopically in the same way has remained unanswered.  In this talk, using DEM we explain the micro mechanics of normal compression of sand, and propose a space-filling argument for why the fractal number should be 2.5.  In addition we explain what we mean by the "smallest" particles (because newly formed dust doesn’t contribute to mechanical behaviour). We then introduce a simple attraction/repulsion model for clay platelets and show that a fractal distribution of macro particles evolves as stress increases in order to fill the void space.   We believe this is the first time a unifying picture of soil appears to be emerging.



For more information, this is the landing page: https://www.springer.com/journal/10035/updates/18300828

And this is the link to the registration page: https://attendee.gotowebinar.com/register/8640125521658905869


Registration is free, anyone can register, and there is no limit on how many people can attend.


Feel free to distribute these links among your networks to help advertise a colleague’s presentation. Thank you, and I hope to see you at the webinar!






Jack Manzi


Assistant Editor, Physics, Astronomy, and Materials Science

Springer, a part of Springer Nature


1 New York Plaza, 47th Floor | New York, NY 10004 | USA

tel +1 212-815-0249

[log in para visualizar]



Vicente Garzó,
Departamento de Fisica  
and Instituto de Computación Científica Avanzada (ICCAEx), Universidad de Extremadura
E-06071 Badajoz
Fax:34-924289651	Phone: 34-924289527
Email: [log in para visualizar]
URL: http://www.unex.es/eweb/fisteor/vicente/