<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-09-22T06:01:21Z</responseDate><request verb="GetRecord" identifier="oai:www.repository.cam.ac.uk:1810/274140" metadataPrefix="uketd_dc">https://api.repository.cam.ac.uk/server/oai/request</request><GetRecord><record><header><identifier>oai:www.repository.cam.ac.uk:1810/274140</identifier><datestamp>2021-04-21T17:39:06Z</datestamp><setSpec>com_1810_213729</setSpec><setSpec>com_1810_256065</setSpec><setSpec>col_1810_219485</setSpec></header><metadata><uketd_dc:uketddc xmlns:uketd_dc="http://naca.central.cranfield.ac.uk/ethos-oai/2.0/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:uketdterms="http://naca.central.cranfield.ac.uk/ethos-oai/terms/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://naca.central.cranfield.ac.uk/ethos-oai/2.0/ http://naca.central.cranfield.ac.uk/ethos-oai/2.0/uketd_dc.xsd">
   <dc:title>Splitting solution scheme for material point method</dc:title>
   <dc:identifier xsi:type="dcterms:DOI">10.17863/CAM.21225</dc:identifier>
   <dc:creator>Kularathna, Shyamini</dc:creator>
   <uketdterms:advisor>Soga, Kenichi</uketdterms:advisor>
   <uketdterms:advisor>Liang, Dongfang</uketdterms:advisor>
   <dcterms:abstract>Material point method (MPM) is a numerical tool which was originally used for modelling
large deformations of solid mechanics problems. Due to the particle based spatial discretiza-
tion, MPM is naturally capable of handling large mass movements together with topological
changes. Further, the Lagrangian particles in MPM allow an easy implementation of history
dependent materials.

So far, however, research on MPM has been mostly restricted to explicit dynamic formu-
lations with linear approximation functions. This is because of the simplicity and the low
computational cost of such explicit algorithms. Particularly in MPM analysis of geomechan-
ics problems, a considerable attention is given to the standard explicit formulation to model
dynamic large deformations of geomaterials. Nonetheless, several limitations exist. In the
limit of incompressibility, a significantly small time step is required to ensure the stability of
the explicit formulation. Time step size restriction is also present in low permeability cases
in porous media analysis. Spurious pressure oscillations are another numerical instability
present in nearly incompressible flow behaviours.

This research considers an implicit treatment of the pressure in MPM algorithm to simu-
late material incompressibility. The coupled velocity (v)-pressure (p) governing equations are
solved by applying Chorin’s projection method which exhibits an inherent pressure stability.
Hence, linear finite elements can be used in the MPM solver. The main purpose of this
new MPM formulation is to mitigate artificial pressure oscillations and time step restrictions
present in the explicit MPM approach. First, a single phase MPM solver is applied to free
surface incompressible fluid flow problems. Numerical results show a better approximation
of the pressure field compared to the results obtained from the explicit MPM. The proposed
formulation is then extended to model fully saturated porous materials with incompress-
ible constituents. A solid velocity(v S )-fluid velocity (v F )-pore pressure (p) formulation is
presented within the framework of mixture theory. Comparing the numerical results for
the one-dimensional consolidation problem shows that the proposed incompressible MPM
algorithm provides a stable and accurate pore pressure field even without implementing
damping in the solver. Finally, the coupled MPM is used to solve a two-dimensional wave
propagation problem and a plain strain consolidation problem. One of the important features
of the proposed hydro mechanical coupled MPM formulation is that the time step size is not
dependent on the incompressibility and the permeability of the porous medium.</dcterms:abstract>
   <uketdterms:institution>University of Cambridge</uketdterms:institution>
   <dcterms:issued>2018-04-07</dcterms:issued>
   <dc:type>Thesis</dc:type>
   <uketdterms:qualificationlevel>Doctoral</uketdterms:qualificationlevel>
   <uketdterms:qualificationname>Doctor of Philosophy (PhD)</uketdterms:qualificationname>
   <dc:language>en</dc:language>
   <dcterms:isReferencedBy xsi:type="dcterms:URI">https://www.repository.cam.ac.uk/handle/1810/274140</dcterms:isReferencedBy>
   <uketdterms:embargotype>controlled.access</uketdterms:embargotype>
   <dcterms:license>https://apollo8-f-pro.lib.cam.ac.uk/bitstreams/dc8245de-9ace-44ad-b4a7-943c95b29aa8/download</dcterms:license>
   <uketdterms:checksum xsi:type="uketdterms:MD5">87eda9de84448d1f82354d60eee3eb5f</uketdterms:checksum>
   <dc:identifier xsi:type="dcterms:URI">https://apollo8-f-pro.lib.cam.ac.uk/bitstreams/afe68ddf-1774-419c-8620-d7ce398b5f96/download</dc:identifier>
   <uketdterms:checksum xsi:type="uketdterms:MD5">d89cb748bc15f02c750e0139e04badb9</uketdterms:checksum>
   <dc:rights>https://www.rioxx.net/licenses/all-rights-reserved/</dc:rights>
   <dc:subject>material point method</dc:subject>
   <dc:subject>incompressibility</dc:subject>
   <dc:subject>incompressible material point method</dc:subject>
   <dc:subject>semi-implicit material point method</dc:subject>
   <dc:subject>two phase material point method</dc:subject>
   <dc:subject>hydro-mechanical coupled material point method</dc:subject>
   <dc:subject>projection method</dc:subject>
   <dc:subject>fractional step method in mpm</dc:subject>
   <dc:subject>splitting method in mpm</dc:subject>
   <dc:subject>pressure correction method in mpm</dc:subject>
   <dc:subject>mpm for saturated porous media</dc:subject>
</uketd_dc:uketddc>
</metadata></record></GetRecord></OAI-PMH>