A chemistry-informed hybrid machine learning approach to predict metal adsorption onto mineral surfaces

被引:3
|
作者
Chang, Elliot [1 ]
Zavarin, Mavrik [1 ]
Beverly, Linda [2 ]
Wainwright, Haruko [2 ,3 ]
机构
[1] Lawrence Livermore Natl Lab, Seaborg Inst, 7000 East Ave, Livermore, CA 94550 USA
[2] Lawrence Berkeley Natl Lab, Earth & Environm Sci Area, 1 Cyclotron Rd, Berkeley, CA 94720 USA
[3] Univ Calif Berkeley, Dept Nucl Engn, 4153 Etcheverry Hall, Berkeley, CA 94720 USA
关键词
Adsorption; Metal; Mineral; Surface complexation modeling; Random forest; Hybrid machine learning; URANIUM(VI) ADSORPTION; SORPTION BEHAVIOR; U(VI) SORPTION; CENTRAL VALLEY; COMPLEXATION; MONTMORILLONITE; GROUNDWATER; CARBONATE; TRANSPORT; BINDING;
D O I
10.1016/j.apgeochem.2023.105731
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Historically, surface complexation model (SCM) constants and distribution coefficients (Kd) have been employed to quantify mineral-based retardation effects controlling the fate of metals in subsurface geologic systems. Our recent SCM development workflow, based on the Lawrence Livermore National Laboratory Surface Complexation/Ion Exchange (L-SCIE) database, illustrated a community FAIR data approach to SCM development by predicting uranium(VI)-quartz adsorption for a large number of literature-mined data. Here, we present an alternative hybrid machine learning (ML) approach that shows promise in achieving equivalent high-quality predictions compared to traditional surface complexation models. At its core, the hybrid random forest (RF) ML approach is motivated by the proliferation of incongruent SCMs in the literature that limit their applicability in reactive transport models. Our hybrid ML approach implements PHREEQC-based aqueous speciation calculations; values from these simulations are automatically used as input features for a random forest (RF) algorithm to quantify adsorption and avoid SCM modeling constraints entirely. Named the LLNL Speciation Updated Random Forest (L-SURF) model, this hybrid approach is shown to have applicability to U(VI) sorption cases driven by both ion-exchange and surface complexation, as is shown for quartz and montmorillonite cases. The approach can be applied to reactive transport modeling and may provide an alternative to the costly development of self-consistent SCM reaction databases.
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页数:10
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