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Factors Affecting Dissolution: Polymorphism, Amorphism and Pseudopolymorphism01:21

Factors Affecting Dissolution: Polymorphism, Amorphism and Pseudopolymorphism

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Polymorphism refers to the existence of a drug substance in multiple crystalline forms, known as polymorphs. Recently, this term has been expanded to include solvates (forms containing a solvent), amorphous forms (non-crystalline forms), and desolvated solvates (forms from which the solvent has been removed).
Some polymorphic crystals possess lower aqueous solubility than their amorphous counterparts, leading to incomplete absorption. For instance, the oral suspension of Chloramphenicol, which...
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Polymer Classification: Crystallinity01:21

Polymer Classification: Crystallinity

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Unlike ionic or small covalent molecules, polymers do not form crystalline solids due to the diffusion limitations of their long-chain structures. However, polymers contain microscopic crystalline domains separated by amorphous domains.
Crystalline domains are the regions where polymer chains are aligned in an orderly manner and held together in proximity by intermolecular forces. For example, chains in the crystalline domains of polyethylene and nylon are bound together by van der Waals...
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Molecular and Ionic Solids02:54

Molecular and Ionic Solids

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Crystalline solids are divided into four types: molecular, ionic, metallic, and covalent network based on the type of constituent units and their interparticle interactions.
Molecular Solids
Molecular crystalline solids, such as ice, sucrose (table sugar), and iodine, are solids that are composed of neutral molecules as their constituent units. These molecules are held together by weak intermolecular forces such as London dispersion forces, dipole-dipole interactions, or hydrogen bonds, which...
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Crystal Growth: Principles of Crystallization01:25

Crystal Growth: Principles of Crystallization

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Crystallization is a phase transformation process in which crystals are precipitated from a supersaturated solution or formed from other sources. During crystallization, atoms or molecules arrange themselves into a well-defined, rigid crystal lattice to minimize energy.
Initiating crystallization involves manipulating the concentration of the solute and the temperature of the solution. Since crystal growth occurs when the ratio of concentration and solubility of the solute in the solvent...
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Recrystallization: Solid–Solution Equilibria01:10

Recrystallization: Solid–Solution Equilibria

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Recrystallization is a purification technique used to separate impurities from solid compounds. In this technique, no chemical reactions occur. Instead, it exploits physical properties only, specifically, the solubility differences between the desired compound and impurities, either at a single temperature or at different temperatures, and under other selected conditions. The solid-solution equilibrium (solubility equilibrium) of each component in the solution represents a binary phase...
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Ionic Crystal Structures02:42

Ionic Crystal Structures

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Ionic crystals consist of two or more different kinds of ions that usually have different sizes. The packing of these ions into a crystal structure is more complex than the packing of metal atoms that are the same size.
Most monatomic ions behave as charged spheres, and their attraction for ions of opposite charge is the same in every direction. Consequently, stable structures for ionic compounds result (1) when ions of one charge are surrounded by as many ions as possible of the opposite...
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Updated: Mar 18, 2026

Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity
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¿Qué determina la polimorfidad del hielo en las nubes?

Arpa Hudait1, Valeria Molinero1

  • 1Department of Chemistry, The University of Utah , 315 South 1400 East, Salt Lake City, Utah 84112-0850, United States.

Journal of the American Chemical Society
|June 30, 2016
PubMed
Resumen
Este resumen es generado por máquina.

Los cristales de hielo atmosféricos forman principalmente hielo hexagonal a partir del vapor, no hielo desordenado, excepto bajo sobresaturación extrema. Este hallazgo aclara la formación de polimorfos de hielo en las nubes y tiene implicaciones para las interacciones atmosféricas de aerosoles.

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Área de la Ciencia:

  • Química y física atmosférica
  • Ciencias de los materiales
  • Química computacional

Sus antecedentes:

  • La formación de cristales de hielo afecta el clima al influir en la dispersión de la luz y el contenido de vapor de agua.
  • Investigaciones anteriores sugirieron formas de hielo desordenadas de apilamiento metastable a partir de agua súper enfriada, pero el hielo crecido a partir del vapor permaneció indeterminado.
  • La estructura del hielo crecido a partir del vapor es crucial para comprender los procesos atmosféricos.

Objetivo del estudio:

  • Determinar la estructura de hielo formada por la absorción de vapor de agua en los rangos de temperatura atmosférica pertinentes.
  • Para aclarar los mecanismos moleculares de la formación de hielo en la interfaz de vapor.
  • Para calcular las diferencias de energía libre entre las interfaces de hielo cúbico y hexagonal con vapor.

Principales métodos:

  • Se emplearon simulaciones moleculares a gran escala.
  • Las simulaciones analizaron el crecimiento del hielo a partir de la deposición de vapor de agua.
  • Se realizaron cálculos de energía libre para las interfaces hielo-vapor.

Principales resultados:

  • La deposición de vapor produce el apilamiento de hielo desordenado solo bajo sobresaturación extrema, formando una capa líquida de no equilibrio.
  • En supersaturaciones moderadas (200260 K), el hielo hexagonal crece exclusivamente a partir del vapor.
  • El hielo cúbico es desfavorable debido al volumen y las penalizaciones de energía libre interfaciales significativas, especialmente en la interfaz hexagonal hielo-vapor.

Conclusiones:

  • El hielo hexagonal es el polimorfo dominante crecido a partir de vapor en cirros y nubes de fase mixta.
  • El desorden de apilamiento en el hielo crecido a partir del vapor puede ocurrir a temperaturas muy bajas (tropopausa tropical, nubes estratosféricas polares).
  • El crecimiento selectivo de hielo cúbico es factible en las interfaces hielo-líquido, pero no en las interfaces hielo-vapor.