Modeling absorption and segregation of magnesium and cadmium ions to calcite surfaces:: Introducing MgCO3 and CdCO3 potential models

被引:53
作者
de Leeuw, NH [1 ]
Parker, SC [1 ]
机构
[1] Univ Bath, Sch Chem, Bath BA2 7AY, Avon, England
关键词
D O I
10.1063/1.480979
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We introduce a potential model for MgCO3 and CdCO3 which reproduces experimental structural parameters and solution energies. We employed atomistic simulation techniques to model the absorption and segregation of magnesium and cadmium ions to the low-index surfaces of calcite. Both magnesium and cadmium ions absorb at the surfaces from solution. The absorption energies are surface dependent, due to distinct relaxations of the different surfaces, and ion dependent with the smaller sized magnesium ion showing larger relaxations. The absorption energies are larger for magnesium than for cadmium, mainly due to the closer coordination of the water molecules to the magnesium substituted surfaces. The cadmium ions segregate to the bulk crystal more easily than the magnesium ions which prefer to remain at the surface. However, segregation energies for both cations in second and further layers of some surfaces are positive, indicating that once a calcium carbonate layer has overgrown the substituted surface layer, segregation to the bulk is energetically possible. (C) 2000 American Institute of Physics. [S0021-9606(00)70608-8].
引用
收藏
页码:4326 / 4333
页数:8
相关论文
共 48 条
[1]   CALCITE AND ARAGONITE FORMATION FROM AQUEOUS CALCIUM HYDROGENCARBONATE SOLUTIONS - EFFECT OF INDUCED ELECTROMAGNETIC-FIELD ON THE ACTIVITY OF CACO3 NUCLEI PRECURSORS [J].
BERUTO, D ;
GIORDANI, M .
JOURNAL OF THE CHEMICAL SOCIETY-FARADAY TRANSACTIONS, 1993, 89 (14) :2457-2461
[2]  
Born M., 1954, DYNAMICAL THEORY CRY
[3]   Surface complexation clues to dolomite growth [J].
Brady, PV ;
Krumhansl, JL ;
Papenguth, HW .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1996, 60 (04) :727-731
[4]   Effect of divalent cations on the formation and structure of calcium carbonate polymorphs [J].
Brecevic, L ;
NothigLaslo, V ;
Kralj, D ;
Popovic, S .
JOURNAL OF THE CHEMICAL SOCIETY-FARADAY TRANSACTIONS, 1996, 92 (06) :1017-1022
[5]   Formation and aggregation of polymorphs in continuous precipitation .2. Kinetics of CaCO3 precipitation [J].
Chakraborty, D ;
Bhatia, SK .
INDUSTRIAL & ENGINEERING CHEMISTRY RESEARCH, 1996, 35 (06) :1995-2006
[6]   STEADY-STATE TRANSITIONS AND POLYMORPH TRANSFORMATIONS IN CONTINUOUS PRECIPITATION OF CALCIUM-CARBONATE [J].
CHAKRABORTY, D ;
AGARWAL, VK ;
BHATIA, SK ;
BELLARE, J .
INDUSTRIAL & ENGINEERING CHEMISTRY RESEARCH, 1994, 33 (09) :2187-2197
[7]   Otavite-calcite solid-solution formation at the calcite-water interface studied in situ by synchrotron X-ray scattering [J].
Chiarello, RP ;
Sturchio, NC ;
Grace, JD ;
Geissbuhler, P ;
Sorensen, LB ;
Cheng, LW ;
Xu, ST .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1997, 61 (07) :1467-1474
[8]   COMPARATIVE-STUDY OF THE KINETICS AND MECHANISMS OF DISSOLUTION OF CARBONATE MINERALS [J].
CHOU, L ;
GARRELS, RM ;
WOLLAST, R .
CHEMICAL GEOLOGY, 1989, 78 (3-4) :269-282
[9]   THE INHIBITION OF CALCITE DISSOLUTION PRECIPITATION - MG2+ CATIONS [J].
COMPTON, RG ;
BROWN, CA .
JOURNAL OF COLLOID AND INTERFACE SCIENCE, 1994, 165 (02) :445-449
[10]   Molecular dynamics simulation of crystal dissolution from calcite steps [J].
de Leeuw, NH ;
Parker, SC ;
Harding, JH .
PHYSICAL REVIEW B, 1999, 60 (19) :13792-13799