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Handbook of Size Exclusion Chromatography and Related ...

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thespecificporevolume(mL/gadsorbent)<strong>and</strong>VSS isthevolume<strong>of</strong>puresolidper<br />

gram. Equation (11) presents the relationship between particle porosity <strong>and</strong><br />

internal porosity:<br />

eP ¼eSP(1 ei) (11)<br />

Therange for theinterparticleporosity ei listed inTable3islargelybased ondata<br />

fromRef.33.ItwasfoundthatGFCcolumnspackedwithsphericalparticleshave<br />

interparticle porosities ranging from 0.35 to 0.39, but columns packed with<br />

irregularparticlesshowedVi valuesashighas0.47.Thesevaluesareinreasonable<br />

agreement with earlier findings from Giddings (53), who reported ei values in the<br />

range 0.37–0.43. Experiments by the authors with spherical 5-mm, 100 A ˚ pore<br />

sizesilicashaverepeatedlyfound avalue<strong>of</strong>0.40for theinterparticleporosity<strong>and</strong><br />

0.75–0.80 for the mobile-phase porosity. Values as low as 0.34 for ei were<br />

measuredwhenthesesilicasweremorefragile<strong>and</strong>hadmobile-phaseporositieseT<br />

<strong>of</strong> 0.80–0.84. Examples <strong>of</strong> these two types <strong>of</strong> silicas are shown later. Engelhardt<br />

reported0.42fortheinterstitialporosity<strong>of</strong>solidglassbeads<strong>and</strong>0.80–0.88forthe<br />

mobile-phase porosity <strong>of</strong> totally porous supports (56).<br />

For particles with very large pores, porevolume is sometimes sacrificed for<br />

mechanical stability.For example, when particles varying in pore size from 10 to<br />

385 nm,butwithnearlyidenticalporosities,weresubjectedtopressuretests,those<br />

with the largest pore sizes collapsed at lower pressure drops (see Ref. 23, p. 174).<br />

Thus, the mechanical stability<strong>of</strong> larger pore size particles can only be maintained<br />

by reducing the pore volume. Alternatively,larger pore size particles must be<br />

slurry packed at lower pressures, thereby decreasing the stability <strong>and</strong> lifetime <strong>of</strong><br />

the packed bed.<br />

Chemical modification <strong>of</strong> the silica surface results in aloss <strong>of</strong> porevolume.<br />

Thus, the bonded phase layer must be optimized to reduce effectively interactions<br />

with silanol groups while minimizing the thickness <strong>of</strong> the bonded layer to avoid<br />

reducing the pore volume <strong>and</strong> preventing slow transport kinetics in the stationary<br />

phase. For example, the thickness <strong>of</strong> the stationary phase layer was estimated as<br />

0.56 nmforaC3-alkylfunctionalgroup<strong>and</strong>2.45 nmforC18-alkyl,assumingthat<br />

the lig<strong>and</strong>s st<strong>and</strong> upright on the surface (57). This assumption is thought to be<br />

correct under conditions that fully solvate the stationary phase layer, which is the<br />

case in GFC as well as GPC, in which the stationary <strong>and</strong> mobile phases have<br />

similar polar or nonpolar characteristics, respectively. Under such conditions,<br />

however, the bonded phase layer can be partially penetrated by the solutes <strong>and</strong>,<br />

thus, the loss <strong>of</strong> porevolume is smaller than expected based on thevolume <strong>of</strong> the<br />

bonded-phase layer. Henry recently showed the shift in the pore diameter<br />

distribution for apolyethyleneimine phasewith alayer thickness <strong>of</strong> 0.85 nm (26).<br />

The averagepore size <strong>of</strong> modern analytical HPLC packings is 100 A ˚ ,range<br />

60–120 A ˚ .Figure 5shows the internal surface area vs. pore diameter for four<br />

© 2004 by Marcel Dekker, Inc.

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