Coagulation of Na-Montmorillonite by Inorganic Cations at Neutral pH. A Combined Transmission X-ray Microscopy, Small Angle and Wide Angle X-ray Scattering Study

被引:60
作者
Michot, Laurent J. [1 ]
Bihannic, Isabelle [1 ]
Thomas, Fabien [1 ]
Lartiges, Bruno S. [1 ]
Waldvogel, Yves [1 ]
Caillet, Celine [1 ]
Thieme, Juergen [2 ]
Funari, Sergio S. [3 ]
Levitz, Pierre [4 ]
机构
[1] Univ Lorraine, CNRS, UMR 7360, Lab Interdisciplinaire Environm Cotinentaux, F-54501 Vandoeuvre Les Nancy, France
[2] Univ Gottingen, Inst Rontgenphys, D-37073 Gottingen, Germany
[3] HASYLAB, D-22603 Hamburg, Germany
[4] UPMC, ESPCI, CNRS, Physicochim Electrolytes Colloides & Sci Analyt U, F-75252 Paris 5, France
关键词
AQUEOUS SUSPENSIONS; ISOTROPIC/NEMATIC TRANSITIONS; IONIC EXCHANGE; CLAY; STABILITY; FLOCCULATION; PARTICLES; NANOPARTICLES; AGGREGATION;
D O I
10.1021/la400245n
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The coagulation of sodium montmorillonite by inorganic salts (NaNO3, Ca(NO3)(2) and La(NO3)(3)) was studied by combining classical turbidity measurements with wide-angle-X-ray scattering (WAXS), small-angle-X-ray scattering (SAXS), and transmission X-ray microscopy (TXM). Using size-selected samples, such a combination, associated with an original quantitative treatment of TXM images, provides a true multiscale investigation of the formed structures in a spatial range extending from a few angstroms to a few micrometers. We then show that, at neutral pH and starting with fully Na-exchanged samples, coagulation proceeds via the formation of stacks of particles with a slight mismatch between layers. These stacks arrange themselves into larger porous anisotropic particles, the porosity of which depends on the valence of the cation used for coagulation experiments. Face-face coagulation is clearly dominant under those conditions, and no evidence for significant face-edge coagulation was found. These structures appear to arrange as larger clusters, the organization of which should control the mechanical properties of the flocs.
引用
收藏
页码:3500 / 3510
页数:11
相关论文
共 42 条
[1]   Rheological determination of interaction potential energy for aqueous clay suspensions [J].
Baravian, C ;
Vantelon, D ;
Thomas, F .
LANGMUIR, 2003, 19 (19) :8109-8114
[2]  
Bihannic I, 2009, NEUTRON SCATT APPL T, P521, DOI 10.1007/978-0-387-09416-8_18
[3]   Simple inversion formula for the small-angle X-ray scattering intensity from polydisperse systems of spheres [J].
Botet, Robert ;
Cabane, Bernard .
JOURNAL OF APPLIED CRYSTALLOGRAPHY, 2012, 45 :406-416
[4]   Morphological quantification of hierarchical geomaterials by X-ray nano-CT bridges the gap from nano to micro length scales [J].
Brisard, Sebastien ;
Chae, Rosie S. ;
Bihannic, Isabelle ;
Michot, Laurent ;
Guttmann, Peter ;
Thieme, Juergen ;
Schneider, Gerd ;
Monteiro, Paulo J. M. ;
Levitz, Pierre .
AMERICAN MINERALOGIST, 2012, 97 (2-3) :480-483
[5]   Correlations between the stability of charged interfaces and ionic exchange capacity: A Monte Carlo study [J].
Delville, A ;
Gasmi, N ;
Pellenq, RJM ;
Caillol, JM ;
Van Damme, H .
LANGMUIR, 1998, 14 (18) :5077-5082
[6]   Sensitivity of the acid-base properties of clays to the methods of preparation and measurement - 2. Evidence from continuous potentiometric titrations [J].
Duc, M ;
Gaboriaud, F ;
Thomas, F .
JOURNAL OF COLLOID AND INTERFACE SCIENCE, 2005, 289 (01) :148-156
[7]   COAGULATION IN ESTUARIES [J].
EDZWALD, JK ;
UPCHURCH, JB ;
OMELIA, CR .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1974, 8 (01) :58-63
[8]   CLAY DISTRIBUTIONS IN RECENT ESTUARINE SEDIMENTS [J].
EDZWALD, JK ;
OMELIA, CR .
CLAYS AND CLAY MINERALS, 1975, 23 (01) :39-44
[9]  
FITZSIMM.RF, 1970, ISRAEL J CHEM, V8, P301
[10]  
Harvey CC, 2006, DEV CLAY SCI, V1, P501, DOI 10.1016/S1572-4352(05)01016-0