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Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
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Theories of Dissolution: The Danckwerts' Model and Interfacial Barrier Model01:09

Theories of Dissolution: The Danckwerts' Model and Interfacial Barrier Model

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Various dissolution theories provide insight into the factors that influence the dissolution rate. Danckwerts' Model suggests that turbulence, rather than a stagnant layer, characterizes the dissolution medium at the solid-liquid interface. In this model, the agitated solvent contains macroscopic packets that move to the interface via eddy currents, facilitating the absorption and delivery of the drug to the bulk solution. The regular replenishment of solvent packets maintains the...
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Isothermal Processes01:21

Isothermal Processes

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A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
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Boundary Layer Characteristics01:18

Boundary Layer Characteristics

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When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
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Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

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Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
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Isochoric and Isobaric Processes01:21

Isochoric and Isobaric Processes

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A thermodynamic process that occurs at constant volume is called an isochoric process. According to the first law of thermodynamics, heat supplied or removed from the system is partially utilized to perform work and change the internal energy of the system. However, in an isochoric process, the volume remains constant. Hence, the work done by the system is zero. Therefore, the exchange of heat changes the internal energy of the system only. 
Suppose 1000 g of water is heated from 40...
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Revealing the Antarctic marginal ice zone with a decade-long wave-in-ice climatology.

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Wind waves in sea ice of the western Arctic and a global coupled wave-ice model.

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Modelling wave-ice interactions in three dimensions in the marginal ice zone.

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Theory, modelling and observations of marginal ice zone dynamics: multidisciplinary perspectives and outlooks.

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Related Experiment Video

Updated: Aug 29, 2025

Laser-Induced Fluorescence Emission L.I.F.E. as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
13:38

Laser-Induced Fluorescence Emission L.I.F.E. as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

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Marginal ice zone dynamics: future research perspectives and pathways.

L G Bennetts1, C M Bitz2, D L Feltham3

  • 1School of Mathematical Sciences, University of Adelaide, Adelaide, South Australia 5005, Australia.

Philosophical Transactions. Series A, Mathematical, Physical, and Engineering Sciences
|September 11, 2022
PubMed
Summary
This summary is machine-generated.

Future research in marginal ice zone (MIZ) dynamics should focus on climate system impacts. Understanding MIZ trends is crucial for predicting Arctic and Antarctic sea ice responses to climate change.

Keywords:
climate changemarginal ice zonesea ice

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Area of Science:

  • * Physical Oceanography and Sea Ice Physics
  • * Climate System Science
  • * Arctic and Antarctic Research

Background:

  • * Significant advancements in marginal ice zone (MIZ) dynamics theory, modeling, and observations over the last decade.
  • * Established foundation for exploring broader climate implications of MIZ processes.

Purpose of the Study:

  • * To propose future research directions for MIZ dynamics.
  • * To shift focus towards the role of MIZ in the broader climate system.
  • * To recommend research pathways investigating MIZ trends' impact on polar sea ice.

Main Methods:

  • * Review and synthesis of recent progress in MIZ theory, modeling, and observations.
  • * Identification of key research themes and future directions.
  • * Conceptual framework for linking MIZ dynamics to global climate change.

Main Results:

  • * Identification of critical research gaps and opportunities in MIZ dynamics.
  • * Proposed shift in research focus to climate-relevant MIZ processes.
  • * Recommendations for studies on MIZ-climate interactions and sea ice feedbacks.

Conclusions:

  • * The field of MIZ dynamics is poised for significant contributions to climate science.
  • * Future research must integrate MIZ understanding into global climate models and predictions.
  • * Prioritizing research on MIZ-sea ice-climate interactions is essential for understanding polar climate change.