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The cardiovascular system's chief role is to disseminate gases, nutrients, waste, and other substances to the body's cells. Small molecules like gases, lipids, and lipid-soluble substances directly diffuse through capillary wall endothelial cell membranes. Glucose, amino acids, and ions, including sodium, potassium, calcium, and chloride, use transporters for facilitated diffusion via membrane-specific channels. Glucose, ions, and bigger molecules may also pass through intercellular...
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Ion exchange chromatography separates charged molecules from a solution by reversibly exchanging them with mobile, or 'active', ions associated with the oppositely charged stationary phase. This method can be used to separate ions, soften and deionize water, and purify solutions. The polymers comprising the ion-exchange column are high-molecular-weight and chemically stable polymers, crosslinked to be porous and essentially insoluble. They are also functionalized with either acidic or...
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Ion-exchange chromatography, or IEC, is a technique for separating ions based on their affinity for the stationary phase. The stationary phase is a cross-linked polymer resin with covalently attached ionic functional groups. The functional groups can be either positively charged (cation exchangers) or negatively charged (anion exchangers). A cation exchanger consists of a polymeric anion and active cations, while an anion exchanger is a polymeric cation with active anions. The choice of...
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Lipid Exchange Assay in Living Cells
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Cross-Shelf Exchange.

K H Brink1

  • 1Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543;

Annual Review of Marine Science
|January 10, 2016
PubMed
Summary
This summary is machine-generated.

Cross-shelf exchange is crucial for transporting materials on the continental shelf, despite being limited by Earth

Keywords:
coastal instabilitiescoastal physical oceanographynutrient suppliesturbulent boundary layerswind forcing

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Area of Science:

  • Oceanography
  • Physical Oceanography
  • Continental Shelf Dynamics

Background:

  • Cross-shelf exchange is a primary mechanism for nutrient and material transport on continental shelves.
  • Cross-shelf gradients are typically stronger than alongshore gradients, influencing transport dynamics.
  • Earth's rotation limits cross-shelf flow, making it weaker than alongshore currents and posing observational challenges.

Purpose of the Study:

  • To review the dominant mechanisms driving cross-shelf exchange.
  • To explore the interplay of physical processes influencing material transport.
  • To identify future research directions in observational and theoretical studies.

Main Methods:

  • Review of existing literature on cross-shelf transport.
  • Analysis of physical processes including turbulent mixing and nonlinear dynamics.
  • Discussion of observational and theoretical approaches.

Main Results:

  • Cross-shelf exchange is primarily driven by factors overcoming rotational constraints.
  • Turbulent mixing, nonlinear processes, and time dependence enable critical cross-shelf flows.
  • Transport mechanisms vary significantly across different natural settings.

Conclusions:

  • Understanding cross-shelf exchange is vital for continental shelf dynamics.
  • Multiple physical processes contribute to nutrient and material transport.
  • Further research is needed to fully elucidate these complex transport pathways.