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DTSTART:20181212T130000Z
DTEND:20181212T160000Z
SUMMARY:The 2018 DCAMM Annual Seminar Speaker
DESCRIPTION:<p style="text-align: center;"><strong>Ken Kamrin<br />\nMassachusetts Institute of Technology (MIT)<br />\nCambridge, USA&nbsp;<br />\n<br />\n</strong></p>\n<p>will give the lecture </p>\n<p style="text-align: center;"><strong>Continuum modeling of flowing grains<br />\n</strong></p>\n<p><strong>Abstract:</strong> <br />\n<span style="color: black;"></span></p>\n<p style="margin-top: 0pt; margin-bottom: 0pt; margin-left: 0in; text-align: justify;"><span style="color: black;">Granular materials are common in everyday life but are historically difficult to model.&nbsp; This has direct ramifications owing to the prominent role granular media play in multiple industries and terrain dynamics.&nbsp; One can attempt to track every grain with discrete particle methods, but realistic systems are often too large for this approach and a continuum model is desired.&nbsp; However, granular media display unusual behaviors that complicate the continuum treatment: they can behave like solid, flow like liquid, or separate into a "gas", and the rheology of the flowing state displays remarkable subtleties that have been historically difficult to model.&nbsp; To address these challenges, in this talk we develop a family of continuum models and solvers, permitting quantitative modeling capabilities for a variety of applications, ranging from general problems to specific techniques for problems of intrusion, impact, </span><span style="color: black;">driving, and locomotion </span><span style="color: black;">in grains.&nbsp; </span></p>\n<p style="margin-top: 0pt; margin-bottom: 0pt; margin-left: 0in; text-align: justify;">&nbsp;</p>\n<p style="margin-top: 0pt; margin-bottom: 0pt; margin-left: 0in; text-align: justify;"><span style="color: black;">To </span><span style="color: black;">calculate flows in general cases, a rather significant nonlocal effect is evident, which is well-described with our recent nonlocal model accounting for grain cooperativity within the flow rule.&nbsp; On the other hand, to model only intrusion forces on submerged objects, we will show, and explain why, many of the experimentally observed results can be captured from a much simpler tension-free frictional plasticity model.&nbsp; This approach gives way to some surprisingly simple general tools, including the granular Resistive Force Theory, and a broad set of scaling laws inherent to the problem of granular locomotion.&nbsp; These </span><span style="color: black;">scalings</span><span style="color: black;"> are validated experimentally and in discrete particle simulations suggesting a new down-scaled paradigm for granular locomotive design, on earth and beyond, to be used much like scaling laws in fluid mechanics. </span></p>\n&nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp;
X-ALT-DESC;FMTTYPE=text/html:<p style="text-align: center;"><strong>Ken Kamrin<br />\nMassachusetts Institute of Technology (MIT)<br />\nCambridge, USA&nbsp;<br />\n<br />\n</strong></p>\n<p>will give the lecture </p>\n<p style="text-align: center;"><strong>Continuum modeling of flowing grains<br />\n</strong></p>\n<p><strong>Abstract:</strong> <br />\n<span style="color: black;"></span></p>\n<p style="margin-top: 0pt; margin-bottom: 0pt; margin-left: 0in; text-align: justify;"><span style="color: black;">Granular materials are common in everyday life but are historically difficult to model.&nbsp; This has direct ramifications owing to the prominent role granular media play in multiple industries and terrain dynamics.&nbsp; One can attempt to track every grain with discrete particle methods, but realistic systems are often too large for this approach and a continuum model is desired.&nbsp; However, granular media display unusual behaviors that complicate the continuum treatment: they can behave like solid, flow like liquid, or separate into a "gas", and the rheology of the flowing state displays remarkable subtleties that have been historically difficult to model.&nbsp; To address these challenges, in this talk we develop a family of continuum models and solvers, permitting quantitative modeling capabilities for a variety of applications, ranging from general problems to specific techniques for problems of intrusion, impact, </span><span style="color: black;">driving, and locomotion </span><span style="color: black;">in grains.&nbsp; </span></p>\n<p style="margin-top: 0pt; margin-bottom: 0pt; margin-left: 0in; text-align: justify;">&nbsp;</p>\n<p style="margin-top: 0pt; margin-bottom: 0pt; margin-left: 0in; text-align: justify;"><span style="color: black;">To </span><span style="color: black;">calculate flows in general cases, a rather significant nonlocal effect is evident, which is well-described with our recent nonlocal model accounting for grain cooperativity within the flow rule.&nbsp; On the other hand, to model only intrusion forces on submerged objects, we will show, and explain why, many of the experimentally observed results can be captured from a much simpler tension-free frictional plasticity model.&nbsp; This approach gives way to some surprisingly simple general tools, including the granular Resistive Force Theory, and a broad set of scaling laws inherent to the problem of granular locomotion.&nbsp; These </span><span style="color: black;">scalings</span><span style="color: black;"> are validated experimentally and in discrete particle simulations suggesting a new down-scaled paradigm for granular locomotive design, on earth and beyond, to be used much like scaling laws in fluid mechanics. </span></p>\n&nbsp; &nbsp; &nbsp; &nbsp; &nbsp; &nbsp;

URL:http://www.dcamm.dk/da/Kalender/2018/12/Annual_speaker_2018_DTU
DTSTAMP:20260914T063900Z
UID:{CE76EAEB-66CA-42A9-8EB2-07AEEC1321CA}-20181212T130000Z-20181212T130000Z
LOCATION: Meeting Room 1, Building 101, Technical University of Denmark
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