Self-generated diffusioosmotic flows from calcium carbonate micropumps

Calcium carbonate particles, ubiquitous in nature and found extensively in geological formations, behave as micropumps in an unsaturated aqueous solution. The mechanism causing this pumping is diffusioosmosis, which drives flows along charged surfaces. Our calcium carbonate microparticles, roughly ∼...

Ausführliche Beschreibung

Bibliographische Detailangaben
Veröffentlicht in:Langmuir : the ACS journal of surfaces and colloids. - 1992. - 28(2012), 44 vom: 06. Nov., Seite 15491-7
1. Verfasser: McDermott, Joseph J (VerfasserIn)
Weitere Verfasser: Kar, Abhishek, Daher, Majd, Klara, Steve, Wang, Gary, Sen, Ayusman, Velegol, Darrell
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2012
Zugriff auf das übergeordnete Werk:Langmuir : the ACS journal of surfaces and colloids
Schlagworte:Journal Article
LEADER 01000naa a22002652 4500
001 NLM221874305
003 DE-627
005 20231224052923.0
007 cr uuu---uuuuu
008 231224s2012 xx |||||o 00| ||eng c
024 7 |a 10.1021/la303410w  |2 doi 
028 5 2 |a pubmed24n0739.xml 
035 |a (DE-627)NLM221874305 
035 |a (NLM)23072458 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a McDermott, Joseph J  |e verfasserin  |4 aut 
245 1 0 |a Self-generated diffusioosmotic flows from calcium carbonate micropumps 
264 1 |c 2012 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Completed 19.04.2013 
500 |a Date Revised 06.11.2012 
500 |a published: Print-Electronic 
500 |a Citation Status PubMed-not-MEDLINE 
520 |a Calcium carbonate particles, ubiquitous in nature and found extensively in geological formations, behave as micropumps in an unsaturated aqueous solution. The mechanism causing this pumping is diffusioosmosis, which drives flows along charged surfaces. Our calcium carbonate microparticles, roughly ∼10 μm in size, self-generate ionic gradients as they dissolve in water to produce Ca(2+), HCO(3)(-), and OH(-) ions that migrate into the bulk. Because of the different diffusion coefficients of these ions, spontaneous electric fields of roughly 1-10 V/cm arise in order to maintain electroneutrality in the solution. This electric field drives the diffusiophoresis of charged tracers (both positive and negative) as well as diffusioosmotic flows along charged substrates. Here we show experimentally how the directionality and speed of the tracers can be engineered by manipulating the tracer zeta potential, the salt gradients, and the substrate zeta potential. Furthermore, because the salt gradients are self-generated, here by the dissolution of solid calcium carbonate microparticles another manipulated variable is the placement of these particles. Importantly, we find that the zeta potentials on surfaces vary with both time and location because of the adsorption or desorption of Ca(2+) ions; this change affects the flows significantly 
650 4 |a Journal Article 
700 1 |a Kar, Abhishek  |e verfasserin  |4 aut 
700 1 |a Daher, Majd  |e verfasserin  |4 aut 
700 1 |a Klara, Steve  |e verfasserin  |4 aut 
700 1 |a Wang, Gary  |e verfasserin  |4 aut 
700 1 |a Sen, Ayusman  |e verfasserin  |4 aut 
700 1 |a Velegol, Darrell  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Langmuir : the ACS journal of surfaces and colloids  |d 1992  |g 28(2012), 44 vom: 06. Nov., Seite 15491-7  |w (DE-627)NLM098181009  |x 1520-5827  |7 nnns 
773 1 8 |g volume:28  |g year:2012  |g number:44  |g day:06  |g month:11  |g pages:15491-7 
856 4 0 |u http://dx.doi.org/10.1021/la303410w  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_22 
912 |a GBV_ILN_350 
912 |a GBV_ILN_721 
951 |a AR 
952 |d 28  |j 2012  |e 44  |b 06  |c 11  |h 15491-7