Using a surface complexation model to predict the mature and stability of nanoparticles

被引:36
作者
Fukushi, K
Sato, T [1 ]
机构
[1] Kanazawa Univ, Inst Nat & Environm Technol, Kanazawa, Ishikawa 9201192, Japan
[2] Natl Inst Adv Ind Sci & Technol, Res Ctr Deep Geol Environm, Tsukuba, Ibaraki 3058567, Japan
关键词
D O I
10.1021/es0491984
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Nanoparticles are discrete nanometer-scale assemblies of atoms and have dimensions between those characteristic of ions and those of macroscopic materials. These minerals commonly possess extremely large specific surface areas and surface adsorption capacities for foreign ions. Due to the large specific surface area and large fraction of surface atoms, the natures of nanoparticles are expected to be modified by the adsorption (surface complexation) process. In this paper, we discuss theoretically the stability of nanoparticles that make the surface complex with foreign ions. The principal theoretical assumption is that the surface complexation occurs at the bulk of the nanoparticles, as in a solid solution. The surface complexation affects two aspects of the intrinsic stability of the nanoparticles simultaneously: one is the composition of the nanoparticles; the other is the free energy of formation of nanoparticles, The solubility of hydrous ferric oxide WO) was estimated by using surface complexation modeling coupled with published data of the free energy of formation of the relevant components. The solubility modeling of surface-charged (H+ or OH- sorbed) HFO mechanistically and quantitatively explained the observed nonintegral behavior of the solubility of HFO. solubility modeling of anion (SO42-, PO43- and As (V)) sorption by HFO showed that the sorption process strongly influences the stability of the nanoparticles. This result implies that geochemical modeling leads to the erroneous prediction of a natural system if the effect of the sorption process is not taken into account.
引用
收藏
页码:1250 / 1256
页数:7
相关论文
共 18 条
[1]   Nanoparticles in the environment [J].
Banfield, JF ;
Zhang, HZ .
NANOPARTICLES AND THE ENVIRONMENT, 2001, 44 :1-58
[2]   STUDIES ON HYDROLYSIS OF METAL IONS .57. HYDROLYSIS OF IRON(3) ION AND SOLUBILITY PRODUCT OF FE(OH)2.70C10.30 IN 0.5 M (NA+)CL-MEDIUM [J].
BIEDERMANN, G ;
CHOW, JT .
ACTA CHEMICA SCANDINAVICA, 1966, 20 (05) :1376-+
[3]   Direct observations of nonintegral hydrous ferric oxide solubility products:: KSO*=[Fe3+][H+]-2.86 [J].
Byrne, RH ;
Luo, YR .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2000, 64 (11) :1873-1877
[4]  
Cornell R.M., 1996, The Iron Oxide: Structure, Properties, Reactions, Occurance and Uses
[5]  
CORNELL RM, 1989, J CHEM TECHNOL BIOT, V46, P115
[6]   The role of electrolyte anions (ClO4-, NO3-, and Cl-) in divalent metal (M2+) adsorption on oxide and hydroxide surfaces in salt solutions [J].
Criscenti, LJ ;
Sverjensky, DA .
AMERICAN JOURNAL OF SCIENCE, 1999, 299 (10) :828-899
[7]  
DAVIS JA, 1990, REV MINERAL, V23, P177
[8]  
Dzombak D.A., 1990, SURFACE COMPLEXATION
[9]  
ETHKE CM, 1998, GEOCHEMISTS WORKBENC