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Estimation of total dissolved solids in Zayandehrood River using intelligent models and PCA

  • A. Taheri Tizro
  • , Alan E. Fryar
  • , A. Vanaei
  • , N. Kazakis
  • , K. Voudouris
  • , P. Mohammadi

Producción científica: Articlerevisión exhaustiva

5 Citas (Scopus)

Resumen

Artificial neural networks (ANN), adaptive neuro-fuzzy inference system (ANFIS) with subtractive clustering (ANFIS-SC) and support vector machine models were used to determine total dissolved solids (TDS) of the Zayandehrood River in Iran. In total, nine hydrochemical parameters [Ca2+, SO42−, Na+, Cl, EC, pH, HCO3, Mg2+ and sodium adsorption ratio (SAR)] were utilized to estimate the TDS of the river at a monthly time scale. Statistical data were categorized into low-flow and wet periods based on river discharge. Principal component analysis (PCA) was used to determine the input of the models. The results indicate that the PCA method, in both wet and low-flow periods, performed suitably based on the evaluation criteria for all models. The parameters of the first component included Ca2+, SO42−, Cl, EC, Mg2+ and SAR in both periods. In contrast, the parameters pH and HCO3 of the second component provided unacceptable precision. The ANFIS-SC model was more precise than the other two models, with an RMSE value of 12.33 meq/l for the first component in the low-flow period. However, the ANN model was most precise in the wet period, with a calculated RMSE value of 13.87 meq/l.

Idioma originalEnglish
Número de artículo22
PublicaciónSustainable Water Resources Management
Volumen7
N.º2
DOI
EstadoPublished - abr 2021

Nota bibliográfica

Publisher Copyright:
© 2021, The Author(s), under exclusive licence to Springer Nature Switzerland AG part of Springer Nature.

ODS de las Naciones Unidas

Este resultado contribuye a los siguientes Objetivos de Desarrollo Sostenible

  1. Affordable and clean energy
    Affordable and clean energy

ASJC Scopus subject areas

  • Renewable Energy, Sustainability and the Environment
  • Water Science and Technology

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