Industrial experiences have shown that powders can unexpectedly change from normal powder flow properties to exhibit liquid-like flow characteristics. This change in flow properties, known as flooding, can result in a major loss of a powder's containment. The prime objective of the research presented in this thesis is to develop a method which quantifies a powder's likelihood to flood, and to identify the conditions where the tendency to flood becomes important. A powder is known to exhibit liquid flow properties at high shear rates or when aerated at or above the minimum fluidisation velocity. The interaction of these two factors, however, is not fully understood. A new type of shear cell is developed which enables the measurement of the shear characteristics of an aerated powder. This shear cell is based on Couette geometry, where a powder sample is sheared between two concentric cylinders, while under controlled aeration conditions. Evaluation of the equipment with a variety of powders identifies that the transition to liquid-like flow properties can occur at low shear velocities and at an aeration substantially below fluidisation. The characterisation of a sample of flooded material shows that additional fine particles significantly increases the tendency for that material to flow like a liquid. The effect of additional fine particles on a selection of powders is studied in detail and powders with a narrow particle size distribution are shown to be most vulnerable to flooding. The quantities of fines required before a powder is likely to show liquid-like flow properties can be small, highlighting that the flooding problem can be significantly effected by segregation. The ability to characterise the effect of small quantities of additional fines on the likelihood to undergo liquid-like flow is an important step forward in understanding the apparent random nature of flooding.

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Ectotherms are living creatures whose body temperature varies with the environment in which they live. Their physiology and metabolism have to rapidly respond to environmental changes in order to stay viable at across their tolerable thermal range (Lithgow et al. 1994). In nematodes such as Caenorhabditis elegans, temperature is an important factor that defines the fertility of the worm. A feature that delimits an ectotherm’s thermal range is the maximum temperature at which its germ line can produce gametes. How germ cells withstand high environmental stressors such as limiting temperatures is not well understood, especially when considering the thermodynamical principles that dominate the biochemical processes of the cytoplasm (Hyman and Brangwynne 2011). Previous studies in C. elegans have shown that the thermodynamic effects of temperature on the cell cycle rate in nematodes follows an Arrhenius relationship and defines the thermal range where worms can be fertile. At the limits of this relationship a breakdown of the Arrhenius trend is observed (Begasse et al. 2015a). It was hypothesized that some type of discontinuous phase transition occurred in the embryonic cells of C. elegans (Begasse et al 2015). However, it remains unknown if there is the physiological link between a drop off in fertility and the embryonic breakdown of the Arrhenius trend. This work finds the link between a temperature driven phase separation of P granules and fertility. P granules are important for germ line development and the fertility of C. elegans (Kawasaki et al. 1998b). Here it is shown that P granules mix with the cytoplasm upon a temperature quench of 27ºC to T=18ºC and de-mix from the cytoplasm forming droplets upon a temperature downshift of temperature from 18ºC to 27ºC. P granules also show a reversible behavior mixing and de-mixing with changes in temperature in vivo, having a strong dependence of these liquid-like compartments with entropy. These results were further confirmed using a minimally reconstituted, in vitro P granule system and showed that PGL-3, a constitutive component of P granules, can phase separate and form liquid compartments in a similar way as happens in vivo. Additionally, here it is shown that P granule phase separation does not require the chemical activity of other cytoplasmic factors to drive the phase separation of compartments in vivo and in vitro, instead their formation is strongly driven to mix and de-mix with changes in temperature. Furthermore, a binary phase diagram was constructed in order to compare the response of P granules in vivo and in vitro, showing that P granules form and function as a temperature driven liquid phaseseparation. Altogether, this indicates that P granules in vivo and PGL-3 liquid-like compartments in vitro, share the same temperature of mixing and de-mixing which coincides with the fertile temperature range over which Caenorhabditis elegans can reproduce. This suggests that P granule phase separation could define the thermal range of the worm.

Ectotherms are living creatures whose body temperature varies with the environment in which they live. Their physiology and metabolism have to rapidly respond to environmental changes in order to stay viable at across their tolerable thermal range (Lithgow et al. 1994). In nematodes such as Caenorhabditis elegans, temperature is an important factor that defines the fertility of the worm. A feature that delimits an ectotherm’s thermal range is the maximum temperature at which its germ line can produce gametes. How germ cells withstand high environmental stressors such as limiting temperatures is not well understood, especially when considering the thermodynamical principles that dominate the biochemical processes of the cytoplasm (Hyman and Brangwynne 2011). Previous studies in C. elegans have shown that the thermodynamic effects of temperature on the cell cycle rate in nematodes follows an Arrhenius relationship and defines the thermal range where worms can be fertile. At the limits of this relationship a breakdown of the Arrhenius trend is observed (Begasse et al. 2015a). It was hypothesized that some type of discontinuous phase transition occurred in the embryonic cells of C. elegans (Begasse et al 2015). However, it remains unknown if there is the physiological link between a drop off in fertility and the embryonic breakdown of the Arrhenius trend. This work finds the link between a temperature driven phase separation of P granules and fertility. P granules are important for germ line development and the fertility of C. elegans (Kawasaki et al. 1998b). Here it is shown that P granules mix with the cytoplasm upon a temperature quench of 27ºC to T=18ºC and de-mix from the cytoplasm forming droplets upon a temperature downshift of temperature from 18ºC to 27ºC. P granules also show a reversible behavior mixing and de-mixing with changes in temperature in vivo, having a strong dependence of these liquid-like compartments with entropy. These results were further confirmed using a minimally reconstituted, in vitro P granule system and showed that PGL-3, a constitutive component of P granules, can phase separate and form liquid compartments in a similar way as happens in vivo. Additionally, here it is shown that P granule phase separation does not require the chemical activity of other cytoplasmic factors to drive the phase separation of compartments in vivo and in vitro, instead their formation is strongly driven to mix and de-mix with changes in temperature. Furthermore, a binary phase diagram was constructed in order to compare the response of P granules in vivo and in vitro, showing that P granules form and function as a temperature driven liquid phaseseparation. Altogether, this indicates that P granules in vivo and PGL-3 liquid-like compartments in vitro, share the same temperature of mixing and de-mixing which coincides with the fertile temperature range over which Caenorhabditis elegans can reproduce. This suggests that P granule phase separation could define the thermal range of the worm.:Table of Contents 1. Abstract 2. Introduction 2 . 1 . CYTOPLASMIC ORGANIZAT ION 2 . 2 . CYTOPLASMIC PHASE SEPARATIONS 2 . 3 . P GRANULES RESEMBLE L IQUID- L IKE PROPERTI ES 2 . 4 . PHASE CHANGES AND THE CELL CYCLE 3. Aim 4. Methods 4 . 1 . STRAINS 4 . 2 . TEMPERATURE CONTROL 4.2.1. HEATING/COOLING SETUP DEVELOPMENT AND MICROSCOPE STAGE 4.2.2. CONFOCAL SAMPLE HOLDER AND HEATING/COOLING DEVICE 4.2.3. SAMPLE PREPARATION 4.2.4. TEMPERATURE OF THE MICROSCOPE OBJECTIVE 4 . 3 . IN VI VO ASSAYS 4 . 4 . IN VI TRO ASSAY 5. Results 5 . 1 . TEMPERATURE AND P GRANULE PHASE SEPARATION 5 . 2 . P GRANULES ARE TEMPERATURE SENSITIVE COMPARTMENTS 5 . 3 . P GRANULES MIX WITH THE CYTOPLASM AT 27ºC 5 . 4 . P GRANULES DO NOT NEED THE INFLUENCE OF PPTR- 1 TO FORM DROPLETS 5 . 5 . P GRANULES REVERSIBLY MIX AND DE-MIX IN VIVO 5 . 6 . PGL- 3 GRANULES PHASE SEPARATE IN V ITRO AT PHYSIOLOGICAL CONDITIONS 5 . 7 . P GRANULE PHASE SEPARATION IS REVERSIBLE IN VI VO AND IN VI TRO 5 . 8 . AN IN V ITRO PHASE DIAGRAM TO COMPARE THE THERMAL L IMITS OF P GRANULES IN V IVO 6. Discussion 6 . 1 . P GRANULES MIX AND DE-MIX IN A REVERSIBLE MANNER 6 . 2 . CONCENTRATION AND THE SPATIAL CONTROL OF P GRANULES 6 . 3 . THE ROLE OF OTHER CHEMICAL REGULATORS 6 . 4 . ECOLOGICAL RELEVANCE OF P GRANULE PHASE SEPARATION 7. Concluding Remarks 8. Bibliography

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Icing severely affects society, especially in the Nordic countries. Iceaccumulation can result in critical performance problems and safetyconcerns for instance in road, air and sea transportation, transmissionlines, marine and offshore structures, wind turbines and heat exchangers.Present active ice-combating approaches possess environmental,efficiency and cost drawbacks. Thus, fabricating icephobic surfaces orcoatings impeding ice formation (anti-icing), but facilitating ice removal(de-icing) is desired. However, different conditions in the environmentduring ice formation and growth add to the complexity of the problem.An icephobic surface that works for a certain application might not be agood candidate for another. These surfaces and the challenges are infocus in this thesis.Wetting properties are important for ice formation on surfaces fromthe liquid phase (often supercooled water), where the water repellency ofthe surfaces could enhance their anti-icing effect. Considering this,different hydrophobic and superhydrophobic surfaces with differentchemistry, morphology and roughness scale were prepared. Since anyinduced wetting state hysteresis on hydrophobic surfaces could influencetheir performance, the wetting stability was investigated. In particulardynamic wetting studies of the hydrophobic surfaces revealed whatsurface characteristics benefit a stable wetting performance. Further, theeffect of temperature, particularly sub-zero temperatures, on the wettingstate of flat and nanostructured hydrophobic surfaces was investigated.This was complemented with studies of the wetting stability of sessilewater droplets on flat to micro- and multi-scale (micro-nano) roughhydrophobic samples in a freeze-thaw cycle. To be consistent with mostapplications, all temperature-controlled experiments were performed inan environmental condition facilitating frost formation. Further, antiicingproperties of hydrophobic surfaces with different topography butsimilar chemistry were studied by freezing delay measurements.A dynamic wetting study using hydrophobic samples with similarchemistry but different topography revealed that multi-scale roughnesscould benefit the wetting stability. However, when these surfaces areutilized at low temperatures the wetting hysteresis observed during acooling/heating cycle is significant. Such a temperature-inducedhysteresis is also significant on superhydrophobic surfaces. I attributethis to condensation followed by frost formation facilitating spreading of  the supercooled water droplet. The freezing delay measurementsdemonstrate no significant effect of surface topography on anti-icingproperties of hydrophobic surfaces, however the flat surfaces showed thelongest delay. These findings are in agreement with heterogeneous icenucleation theory, suggesting preferential ice nucleation in concave sites,provided they are wetted.In the second part of this thesis, I consider the findings from theprevious part illustrating the limitations of (super)hydrophobic surfaces.The de-icing properties of hydrophilic surfaces with a hydration waterlayer, hypothesized to lubricate the interface with ice, were studied. Heretemperature-controlled shear ice adhesion measurements, down to -25oC, were performed on an adsorbed layer of a polymer, either bottle-brushstructured poly(ethylene oxide) or linear poly(ethylene oxide). The iceadhesion strength was reduced significantly on the bottle-brushstructured polymer layer, specifically at temperatures above -15 oC,whereas less adhesion reduction was observed on the layer formed by thelinear polymer. These findings are consistent with differential scanningcalorimetry (DSC) data, demonstrating that the hydration water, boundto the bottle-brush structured polymer, is in the liquid state at thetemperatures where de-icing benefit is observed. Further, continuingwith the hypothesis of the advantage of surfaces with a natural lubricantlayer for de-icing targets, I studied shear ice adhesion on the molecularlyflat basal plane of hydrophilic mica down to -35 oC. Interestingly, ultralowice adhesion strength was measured on this surface. I relate this to theproposed distinct structure of the first ice-like but fluid water layer onmica, with no free OH groups, followed by more bulk liquid-like layers.This combined with the molecularly smooth nature of mica results in aperfect plane for ice sliding. / Isbildning har en stark inverkan på samhället, speciellt i de nordiskaländerna. Isuppbyggnad kan resultera i kritiska prestandaproblem ochsäkerhetsrisker inom t.ex. väg-, luft-, och sjötransport, kraftledningar,marina- och offshorestrukturer, vindkraftverk och värmeväxlare.Nuvarande aktiva isbekämpningsmetoder uppvisar brister i avseende påmiljö, effektivitet och kostnad. Det finns därmed ett behov av attframställa ytor eller ytbeläggningar som förhindrar isbildning (antiisning)eller underlättar borttagandet av redan bildad is (avisning). Dockkompliceras problemet av de många olika förhållanden under vilka is kanbildas. En beläggning som fungerar för en viss tillämpning behöver intenödvändigtvis vara en bra kandidat för en annan. Dessa ytor ochutmaningar relaterade till dem är i fokus i denna avhandling.Vätningsegenskaper är viktiga för isbildning på ytor från vätskefas(ofta underkylt vatten), och det har visats att vattenavstötande ytor i vissasammanhang kan motverka isbildning. Med detta i åtanke framställdesolika hydrofoba och superhydrofoba ytor, med varierande kemi,morfologi och ytråhet. Eftersom en förändring i de hydrofoba ytornasvätningsegenskaper kan påverka deras funktion studerades vätningsstabilitetenför dessa ytor. I synnerhet dynamiska vätningsstudier av dehydrofoba ytorna avslöjade vilka ytegenskaper som är fördelaktiga förvätningsstabiliteten. Vidare studerades hur temperaturen, särskilt undernoll grader, påverkar vätningstillståndet på släta och nanostruktureradehydrofoba ytor. Arbetet kompletterades med studier av vätningsstabilitetenför vattendroppar på släta samt mikro- och multistrukturerade(mikro-nano) hydrofoba ytor under flera frysningsupptiningscykler.För att vara i linje med de flesta tillämpningar, utfördesalla temperaturkontrollerade mätningar i en miljö där frost kunde bildaspå ytorna. Anti-isegenskaperna hos de hydrofoba ytorna med varierandetopografi men samma kemi studerades vidare genom att studera hur långtid det dröjde innan en vattendroppe på ytan fryste vid en visstemperatur.De dynamiska vätningsstudierna på hydrofoba ytor med samma kemimen olika topografi avslöjade att en ytråhet på flera längdskalor kan haen positiv inverkan på vätningsstabiliteten. När dessa ytor är exponeradeför låga temperaturer är dock vätningshysteresen under en nedkylnings-/uppvärmnings-cykel significant. Den temperatur-inducerade hysteresenär också betydande för superhydrofoba ytor. Detta tillskriver jag  kondensation på ytan som följs av frostbildning, vilket i sin tur möjliggörspridning av den underkylda vattendroppen på ytan. Mätning avfördröjningen i frysningsförloppet påvisade ingen betydande effekt avyttopografin för hydrofoba ytor, men släta hydrofoba ytor uppvisade denlängsta fördröjningen. Dessa resultat är i överensstämmelse med rådandeheterogen iskärnbildningsteori, som visar på fördelaktig iskärnbildningpå konkava delar av ytan, förutsatt att dessa väts.I den andra delen av avhandlingen utnyttjar jag observationerna frånden första delen vilka illustrerade begränsningarna för superhydrofobaytor, och söker en annan lösning. Avisningsegenskaper för hydrofilastarkt hydratiserade ytor studerades, med hypotesen att hydratiseringkan smörja gränsskiktet med is. Temperatur-kontrolleradeisadhesionsmätningar ned till -25 °C utfördes på adsorberade skikt av enpolymer med många sidokedjor av polyetylenoxid (”bottle-brush”), såvälsom på ett skikt av linjär polyetylenoxid. Isadhesionen blev kraftigtreducerad på ”bottle-brush”-polymeren, speciellt vid temperaturer högreän -15°C. Däremot kunde knappast ingen minskad isadhesion observerasför den linjära polymeren. Dessa observationer överensstämmer meddifferentialskanningskalorimetri (DSC) data, som visar att dethydratiserade vattenskiktet, vilket är bundet till ”bottle-brush”-polymeren, är i vätskeform vid de temperaturer där avisningsfördelar ärobserverade. För att vidare undersöka hypotesen att det vore fördelaktigtmed ett naturligt smörjande skikt på ytan för att uppnå godaavisningsegenskaper, utförde jag isadhesionsmätningar på molekylärtsläta glimmerytor ner till -35 °C. Intressant nog uppmättes extremt lågisadhesion på denna yta. Detta relaterar jag till den föreslagna utprägladehydratiseringsstrukturen, bestående av ett första is-liknande vattenskiktutan fria OH-grupper, följt av ett mer bulkliknande skikt. Detta ikombination med den molekylärt släta naturen hos glimmer resulterar iett perfekt plan för isen att glida på. / <p>QC 20160504</p> / TopNano