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| SUNYSB-AMS-08-01: |
  |
Understanding the Rate of Clean Up for Oil Zones after a Gel Treatment
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| SUNYSB-AMS-08-02: |
  |
Dominance Hierarchies as a Model of Network Formation in Small Groups
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| SUNYSB-AMS-08-03: |
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Tomographic Analysis of Reactive Fluid Induced Pore Structure Changes in
Flow Column Experiments
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| SUNYSB-AMS-08-04: |
  |
Supporting Online Material for Tomographic Analysis of Reactive Fluid Induced
Pore Structure Changes in Flow Column Experiments
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| SUNYSB-AMS-08-05: |
  |
Continuous Shifts in the Active Set of Spinal Interneurons During Changes in
Locomotor Speed
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| SUNYSB-AMS-08-06: |
  |
Direct Observations of Three Dimensional Growth of Hydrates Hosted in Porous
Media
|
| SUNYSB-AMS-08-07: |
  |
Subgrid Models for Mass and Thermal Diffusion in Turbulent Mixing
|
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www@ams.sunysb.edu.
In our previous work, X-ray computed microtomography (XMT) was used to establish
why pore-filling Cr(III)-acetate-HPAM gels reduced permeability to water much
more than to oil. Our results suggest that permeability to water was reduced to
low values because water must flow through gel itself, whereas oil pressing on
the gel in Berea sandstone or porous polyethylene forced pathways by dehydration
- leading to relatively high permeability to oil. Those studies involved
obtaining 3D pore-level X-ray images at the saturation endpoints - for example,
after forcing 20 pore volumes of oil or water through the core after gel
placement.
The dependence of oil permeability on oil throughput determines how long it
takes for a production well to "clean up" or restore productivity after a gel
treatment. Consequently, we were interested in how the gel dehydration process
progresses as a function of oil throughput. This paper describes a new study
where pore-scale XMT images were obtained at a variety of oil (hexadecane)
throughput values after gel placement (involving a pore-filling Cr(III)-acetate-
HPAM gel). For each pore in our image volume, we followed oil and water
saturations as a function of oil throughput. These studies were performed both
in water-wet Berea sandstone and in hydrophobic porous polyethylene. In
hydrophobic porous polyethylene, oil saturations increased and gel was destroyed
(presumably dehydrated) quite quickly in the smallest pores (10-6 mm3). Also,
oil saturations increased and gel was destroyed quickly in the largest pores
(<0.005 mm3). In contrast, oil saturations rose much more gradually for the most
common or intermediate-sized pores (around 5x10-5 mm3, the peak in the pore size
distribution). The minimum in oil saturation versus pore size may result from a
balance between gel dehydration by oil film growth versus gel extrusion.
Presumably, during oil injection after gel placement, an oil film forms with a
thickness that is about the same on all polyethylene surfaces. However, because
the ratio of film thickness to pore or throat size increases with decreased pore
size, gel dehydration occurs faster and more effectively in the smallest
polyethylene pores, causing oil saturation to increase with decreased pore size.
This effect may lose its signicance for pore sizes above 10-4 mm3.
As pore size increases above 10-4 mm3, gel extrusion from the pore becomes more
lIKELY - explaining why oil saturation increased with increased pore size for
the largest pores.
In contrast in water-wet Berea sandstone, increases in oil saturation occurred
evenly over all pore sizes (10-6 to 0.02 mm3) for all oil throughput values.
Consistent with imbibition and drainage studies performed before gel placement,
oil apparently had equal access to Berea pores of all sizes, and thus uniformly
dehydrated gel in pores of all sizes. Gel extrusion did not appear to be
significant in the Berea pores.
To be presented at the 2008 SPE Improved Oil Recovery Symposium, Tulsa, OK, Apr. 19-23, 2008.
Available in:
PDF
Virtually all human societies show elements of hierarchical organization
- top to bottom arrangements in which some individuals have greater access to
material goods, participate more in group activities, receive more attention,
or exert more power and influence than do other individuals. The near
universality of hierarchies indicates that they are of fundamental significance
for the social organization of groups and societies. Some of the core questions
concerning the development of these social structures are: What mechanisms
generate hierarchies? Do these mechanisms reflect differences among individuals
or their actions during hierarchy formation? What theoretical models exist to
explain the structural forms of hierarchies, and what are the levels of support
for the different models? Can understanding the development of hierarchies
provide more general insight into the evolution of other kinds of networks?
We explore these questions in an unusual way for sociology: we first look at
theoretical models for the explanation of dominance hierarchies ("pecking
orders") in small groups of animals before considering hierarchies in small
groups of humans. We describe dominance relationships and dominance hierarchies
in animal groups, evaluate the various theoretical models that biologists have
proposed to explain the structural forms of these hierarchies, outline a new
type of model for animal hierarchies that avoids some of the problems inherent
in the earlier models, and then compare current models for human small group
hierarchies with those of animal hierarchies. We conclude that both our new
model and current experimental work on animals indicate, ironically, that
animals generate their hierarchies through richer and more sociologically
sophisticated dynamics than those proposed in the current models for humans.
To appear in The Oxfold Handbook of Analytic Sociology, P. Hedstrom and P. Bearman (Eds.) Oxford University Press
Available in:
Word
and
PDF
Dissolution followed by precipitation is a major reaction mechanism in forming
secondary precipitates in most porous sediments. Secondary precipitation is of
interest as a structure modifying mechanism tp control contaminant transport
in the subsurface environment. We employed synchrotron X-ray computed
microtomography in combination with flow-column experiments to capture and
quantify dissolution and secondary precipitation changes in the microstructure
of Hanford sediments exposed to simulated caustic waste. Dissolution induced
changes include: an increase in the number of larger pores. Precipitation
induced changes include reduction in the number of small pores and closure of
small throats, with accompanying reduction in pore coordination numbers and
reduction in the number of pore pathways. Pathway tortuosities however, are
not dramatically affected.
Available in:
PDF
| SUNYSB-AMS-08-04 |
Supporting Online Material for Tomographic Analysis of Reactive Fluid Induced
Pore Structure Changes in Flow Column Experiments
|
R. Cai,
W.B. Lindquist,
W. Um,
and
K.W. Jones
|
This is the Materials and Methods section for SUNYSB-AMS-08-03.
Available in:
PDF
| SUNYSB-AMS-08-05 |
Continuous Shifts in the Active Set of Spinal Interneurons During Changes in
Locomotor Speed
|
D.L. McLean, M.A. Masino, I.Y.Y. Koh,
W.B. Lindquist
and
J.R. Fetcho
|
The classic 'size principle' of motor control describes how increasingly
forceful movements arise by the recruitment of motoneurons of progressively
larger size and force output into the active pool. Here, we explore the activity
of pools of spinal interneurons in larval zebrafish and find that increases in
swimming speed are not associated with the simple addition of cells to the
active pool. Instead, the recruitment of interneurons at faster speeds is
accompanied by the silencing of those driving movements at slower speeds. This
silencing occurs both between and within classes of rhythmically-active
premotor excitatory interneurons. Thus, unlike motoneurons, there is a
continuous shift in the set of cells driving the behavior, even though changes
in the speed of the movements and the frequency of the motor pattern appear
smoothly graded. We conclude that fundamentally different principles may
underlie the recruitment of motoneuron and interneuron pools.
To appear in Nature Neuroscience
Available in:
PDF
| SUNYSB-AMS-08-06 |
Direct Observations of Three Dimensional Growth of Hydrates Hosted in Porous
Media
|
P. Kerakr,
K.W. Jones,
R. Kleinberg,
W.B. Lindquist,
S. Tomov, H. Feng,
and
D. Mahajan
|
We present the first visualization of time-resolved 3-D growth of
tetrahydrofuran (THF) hydrates in porous media using X-ray computed
microtomography (CMT). The 1119?m x 1630?m x 1443?m volume rendered from a
stack of images shows patchy hydrates formed from excess THF in aqueous
solution. Hydrate growth is found convex away from the grains, showing that
liquid, not hydrate, is the wetting phase. This is similar to ice growth in
porous media in which mineral grains are coated with unfrozen water films.
Hydrates formed at several locations in the system before the first images
were taken, 28 hours after the system was cooled to hydrate-forming temperature.
The size and shape of hydrate patches varied within a sample of glass spheres
of uniform size, consistent with the random nature of nucleation and growth.
Tracking individual grains in tomoscans taken over a three day period indicated
grain movement during the hydrate growth. No container-wall effect was
observed. The extension of the observed growth behavior to methane hydrate
could have implication in understanding the role of hydrate in seafloor
stability and climate change.
Available in:
Word
| SUNYSB-AMS-08-07 |
Subgrid Models for Mass and Thermal Diffusion in Turbulent Mixing
|
H. Lim, Y. Yu, J. Glimm, X.-L. Li and D. H. Sharp
|
We are concerned with the chaotic flow fields of turbulent mixing.
Chaotic flow is found
in an extreme form in multiply shocked Richtmyer-Meshkov unstable
flows. The goal of a converged simulation for this problem is twofold:
to obtain converged solutions for macro solution features, such as the
trajectories of the principal shock waves, mixing zone edges, and
mean densities and velocities within each phase, and also
for such micro solution features as the joint probability distributions
of the temperature and species
concentration. We
introduce parameterized subgrid models of
mass and thermal diffusion, to define LES
that replicate the micro features observed in the DNS. The
Schmidt numbers and Prandtl numbers are chosen to represent typical
liquid, gas and plasma parameter values.
Our main result is to explore the variation of the Schmidt, Prandtl and
Reynolds numbers by three orders of magnitude, and the mesh
by a factor of 8 per linear
dimension (up to 3200 cells per dimension),
to allow exploration of both DNS and LES regimes
and verification of the simulations for both macro and micro observables.
We find mesh convergence for key properties describing the molecular
level of mixing, including chemical reaction rates between the distinct
fluid species. We find results nearly independent of Reynolds number
for Re ~ 300,~ 6000, ~600K.
Methodologically, the results are also new. In common with the shock capturing
community, we allow and maintain sharp solution gradients, and we
enhance these gradients through use of front tracking. In common with
the turbulence modeling community, we include subgrid scale models with no
adjustable parameters for LES. To the authors' knowledge, these two
methodologies have not been previously combined.
In contrast to both of these methodologies, our use of Front Tracking,
with DNS or LES resolution of the momentum equation at
or near the Kolmogorov scale,
but without resolving the Batchelor scale, allows a feasible approach to
the modeling of high Schmidt number flows.
Submitted to Physics of Fluids
Available in:
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