Thermodynamics of vivianite-group arsenates M3(AsO4)2.8H2O (M is Ni, Co, Mg, Zn, Cu) and chemical variability in the natural arsenates of this group
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00023272%3A_____%2F24%3A10136227" target="_blank" >RIV/00023272:_____/24:10136227 - isvavai.cz</a>
Result on the web
<a href="https://ejm.copernicus.org/articles/36/31/2024/" target="_blank" >https://ejm.copernicus.org/articles/36/31/2024/</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5194/ejm-36-31-2024" target="_blank" >10.5194/ejm-36-31-2024</a>
Alternative languages
Result language
angličtina
Original language name
Thermodynamics of vivianite-group arsenates M3(AsO4)2.8H2O (M is Ni, Co, Mg, Zn, Cu) and chemical variability in the natural arsenates of this group
Original language description
In this work, we investigated the M3(AsO4)2.8H2O end members annabergite (M = Ni), erythrite (M = Co), hornesite (M = Mg), and their solid solutions. Acid-solution calorimetry and relaxation calorimetry were used to determine the solubility products (logKsp) for annabergite (MINUS SIGN 33.7), erythrite (MINUS SIGN 32.1), and hornesite (MINUS SIGN 22.3). Solubility products for other end members of this group were extracted from literature and critically evaluated. The enthalpies of mixing are complex, related to subsystems M(1)3(AsO4)2.8H2O - M(1)M(2)2(AsO4)2.8H2O and M(1)M(2)2(AsO4)2.8H2O - M(2)3(AsO4)2.8H2O. They are small and positive for the annabergite-erythrite solid solution and small and negative for the annabergite-hornesite solid solution. Autocorrelation analysis of FTIR spectra shows correlation of strain decrease in the structure with the negative enthalpies of mixing in the annabergite-hornesite solid solution. A set of more than 600 electron microprobe analyses of the M3(AsO4)2.8H2O minerals documents the variability and complexity in this group. Most common compositions are those dominated by Ni, Co, or Ni-Co. The analytical results were used to calculate the maximal configurational entropies which could be a factor that compensates for the small enthalpies of mixing in the annabergite-erythrite solid solution. The data presented here can be used to model sites polluted with metals and arsenic and to enhance our understanding of complex solid solutions.
Czech name
—
Czech description
—
Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10504 - Mineralogy
Result continuities
Project
—
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2024
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
European Journal of Mineralogy
ISSN
1617-4011
e-ISSN
—
Volume of the periodical
36
Issue of the periodical within the volume
1
Country of publishing house
DE - GERMANY
Number of pages
24
Pages from-to
31-54
UT code for WoS article
001173378300001
EID of the result in the Scopus database
—