Leveraging machine learning for sustainable cultivation of Zn-enriched crops in Cd-contaminated karst regions.

Journal: The Science of the total environment
PMID:

Abstract

Karst soils often exhibit elevated zinc (Zn) levels, providing an opportunity to cultivate Zn-enriched crops. (meanwhile) However, these soils also frequently contain high background levels of toxic metals, particularly cadmium (Cd), posing potential health risks. Understanding the bioaccumulation of Cd and Zn and the related drivers in a high geochemical background area can provide important insights for the safe development of Zn-enriched crops. Traditional models often struggle to accurately predict metal levels in crop systems grown on soils with high geochemical background. This study employed machine learning models, including Random Forest (RF), Support Vector Machine (SVM), and Extreme Gradient Boosting (XGBoost), to explore effective strategies for sustainable cultivation of Zn-enriched crops in karst regions, focusing on bioaccumulation factors (BAF). A total of 10,986 topsoil samples and 181 paired rhizosphere soil-crop samples, including early rice, late rice, and maize, were collected from a karst region in Guangxi. The SVM and XGBoost models demonstrated superior performance, achieving R values of 0.84 and 0.60 for estimating the BAFs of Zn and Cd, respectively. Key determinants of the BAFs were identified, including soil iron and manganese contents, pH level, and the interaction between Zn and Cd. By integrating these soil properties with machine learning, a framework for the safe cultivation of Zn-enriched crops was developed. This research contributes to the development of strategies for mitigating Zn deficiency in crops grown on Cd-contaminated soils.

Authors

  • Cheng Li
    College of Food and Bioengineering, Henan University of Science and Technology, Luoyang, China.
  • Tao Yu
    Department of Smart Experience Design Kookmin University, Seoul 02707, Republic of Korea.
  • Zhongcheng Jiang
    Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics, MNR & GZAR/International Research Center on Karst Under the Auspices of UNESCO, Guilin, 541004, Guangxi, People's Republic of China.
  • Wenli Li
    Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics, MNR & GZAR/International Research Center on Karst Under the Auspices of UNESCO, Guilin, 541004, Guangxi, People's Republic of China.
  • Dong-Xing Guan
    Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Key Laboratory of Environmental Remediation and Ecosystem Health, Ministry of Education, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China.
  • Yeyu Yang
    Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics, MNR & GZAR/International Research Center on Karst Under the Auspices of UNESCO, Guilin, 541004, Guangxi, People's Republic of China.
  • Jie Zeng
    Department of Experimental Research, Guangxi Medical University Cancer Hospital, Nanning, 530021, China.
  • Haofan Xu
    School of Environmental and Chemical Engineering, Foshan University, Foshan, 528000, Guangdong, People's Republic of China.
  • Shaohua Liu
    School of Electronic Engineering, Beijing University of Posts and Telecommunications, Beijing 100876, China.
  • Xiangke Wu
    Mineral Resource Reservoir Evaluation Center of Guangxi, Nanning, 530023, People's Republic of China.
  • Guodong Zheng
    Guangxi Institute of Geological Survey, Nanning 530023, China.
  • Zhongfang Yang
    School of Earth Sciences and Resources, China University of Geosciences, Beijing, 100083, People's Republic of China. yangzf@cugb.edu.cn.