Open Access Open Access  Restricted Access Subscription Access

Calibration of Two-Dimensional Variably Saturated Numerical Model for Groundwater Flow in Arid Inland Basin, China


Affiliations
1 School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China
2 Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Science, Shijiazhuang 050061, China
 

Alluvial fan is an important recharge area for arid and semi-arid inland basins. In order to study groundwater circulation and quantify recharge amount of the groundwater system in arid inland basins, it is necessary to use numerical models. In this study, a 2D variably saturated numerical model of a typical profile has been developed using EOS 9 module of TOUGH2. The mesh for the fine soil plain area was refined compared with previous studies and the minimum cell size was 0.1 m in thickness. An improved approach in TOUGH2 was applied to calculate the groundwater evapotranspiration more efficiently and characterize water transport more accurately. Multiple calibration approaches were combined to calibrate the model. The results show that, the typical profile can be divided into three groundwater flow systems. The circulation depth for the local groundwater flow system is about 200 m and the shallow discharge accounts for 74.4% of the total amount with groundwater age less than 500 a (year). The circulation depth for the middle flow system can reach 800 m and the amount of discharge accounts for 18.5% of the total amount with groundwater age less than 10 ka (kiloyear). The circulation depth for the regional flow system is from 1000 to 1500 m, and the discharge accounts for 7.1% of the total amount with groundwater age ranging from 10 to 50 ka. The improved TOUGH2 numerical model, combined with multiple calibration approaches, can better reflect regional circulation characteristics and quantify the recharge amount of different groundwater sub-systems in arid and semi-arid inland basins with limited datasets.

Keywords

Arid Inland Basin, Groundwater Flow, Numerical Models, Multiple Calibration Approaches.
User
Notifications
Font Size

  • Choi, B. Y., Yun, S. T., Mayer, B., Chae, G. T., Kim, K. H., Kim, K. and Koh, Y. K., Identification of groundwater recharge sources and processes in a heterogeneous alluvial aquifer: results from multi-level monitoring of hydrochemistry and environmental isotopes in a riverside agricultural area in Korea. Hydrol. Process., 2010, 24(3), 317–330.
  • Liu, F., Cui, Y.-l., Zhang, G., Geng, F. and Liu, J., Using the 3H and 14C dating methods to calculate the groundwater age in Nomhon, Qaidam Basin. Geoscience, 2014, 28(6), 1322–1328.
  • Liu, Y., Yamanaka, T., Zhou, X., Tian, F. and Ma, W., Combined use of tracer approach and numerical simulation to estimate groundwater recharge in an alluvial aquifer system: a case study of Nasunogahara area, central Japan. J. Hydrol., 2014, 519(Part A), 833–847.
  • Scanlon, B. R., Healy, R. W. and Cook, P. G., Choosing appropriate techniques for quantifying groundwater recharge. Hydrogeol. J., 2002, 10(1), 18–39.
  • Zhu, Y., Shi, L., Yang, J., Wu, J. and Mao, D., Coupling methodology and application of a fully integrated model for contaminant transport in the subsurface system. J. Hydrol., 2013, 501, 56–72.
  • Xu, T., Sonnenthal, E., Spycher, N. and Pruess, K., TOUGHREACT: A simulation program for non-isothermal multiphase reactive geochemical transport in variably saturated geologic media. Comput. Geosci., 2006, 32(2), 145–165.
  • Audigane, P., Chiaberge, C., Mathurin, F., Lions, J. and PicotColbeaux, G., A workflow for handling heterogeneous 3D models with the TOUGH2 family of codes: applications to numerical modeling of CO2 geological storage. Comput. Geosci., 2011, 37(4), 610–620.
  • Kuang, X., Jiao, J. J., Li, W., Wang, X. and Mao, D., Air and water flows in a vertical sand column. Water Resour. Res., 2011, 47(4), 289–306.
  • Hubschwerlen, N., Zhang, K., Mayer, G., Roger, J. and Vialay, B., Using Tough2-MP on a cluster-optimization methodology and study of scalability. Comput. Geosci., 2012, 45, 26–35.
  • Hamed, Y. et al., Use of geochemical, isotopic, and age tracer data to develop models of groundwater flow: a case study of Gafsa mining basin-Southern Tunisia. J. Afr. Earth Sci., 2014, 100, 418–436.
  • Candela, L., Elorza, F. J., Tamoh, K., Jimenez-Martinez, J. and Aureli, A., Groundwater modelling with limited data sets: the Chari–Logone area (Lake Chad Basin, Chad). Hydrol. Process., 2014, 28(11), 3714–3727.
  • Dahan, O., McGraw, D., Adar, E., Pohll, G., Bohm, B. and Thomas, J., Multi-variable mixing cell model as a calibration and validation tool for hydrogeologic groundwater modeling. J. Hydrol., 2004, 293(1–4), 115–136.
  • Sanford, W. E., Plummer, L. N., Mcada, D. P., Bexfield, L. M. and Anderholm, S. K., Hydrochemical tracers in the middle Rio Grande Basin, USA: 2. Calibration of a groundwater-flow model. Hydrogeol. J., 2004, 12(4), 389–407.
  • Mohammadi, Z., Salimi, M. and Faghih, A., Assessment of groundwater recharge in a semi-arid groundwater system using water balance equation, southern Iran. J. Afr. Earth Sci., 2014, 95, 1–8.
  • Hao, Q., Shao, J., Cui, Y. and Zhang, Q., Development of a new method for efficiently calculating of evaporation from the phreatic aquifer in variably saturated flow modeling. J. Groundwater Sci. Eng., 2016, 4(1), 26–34.
  • Richards, L. A., Capillary conduction of liquids through porous mediums. J. Appl. Phys., 1931, 1(5), 318–333.
  • Cui, Y., Su, C., Shao, J., Wang, Y. and Cao, X., Development and application of a regional land subsidence model for the plain of Tianjin. J. Earth Sci., 2014, 25(3), 550–562.
  • Rui, X.-F., Principles of Hydrology, China Water Power Press, Beijing, 2004, pp. 114–118.
  • Zhang, H. and Hiscock, K. M., Modelling the effect of forest cover in mitigating nitrate contamination of groundwater: a case study of the Sherwood Sandstone aquifer in the East Midlands, UK. J. Hydrol., 2011, 399(3–4), 212–225.
  • Surinaidu, L., Bacon, C. G. D. and Pavelic, P., Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenarios. Hydrol. Earth System Sci., 2013, 17(1), 507–517.
  • Pollock, D. W., User’s Guide for MODPATH/MODPATH-PLOT, Version 3: A Particle Tracking Post-processing Package for MODFLOW, the US: Geological Survey Finite, 1994.
  • Wu, Y., Wang, W., Toll, M., Alkhoury, W., Sauter, M. and Kolditz, O., Development of a 3D groundwater model based on scarce data: the Wadi Kafrein catchment, Jordan. Environ. Earth Sci., 2011, 64(3), 771–785.
  • Gonçalves, T. D., Fischer, T., Gräbe, A., Kolditz, O. and Weiss, H., Groundwater flow model of the Pipiripau watershed, Federal District of Brazil. Environ. Earth Sci., 2013, 69(2), 617–631.
  • Massoudieh, A., Visser, A., Sharifi, S. and Broers, H. P., A Bayesian modeling approach for estimation of a shape-free groundwater age distribution using multiple tracers. Appl. Geochem., 2014, 50, 252–264.
  • Toth, J., A theoretical analysis of groundwater flow in small drainage basins. J. Geophys. Res., 1963, 68(16), 4795–4812.
  • Jiang, X. W., Wan, L., Wang, X. S., Ge, S. and Liu, J., Effect of exponential decay in hydraulic conductivity with depth on regional groundwater flow. Geophys. Res. Lett., 2009, 36(24), 88–113.

Abstract Views: 252

PDF Views: 75




  • Calibration of Two-Dimensional Variably Saturated Numerical Model for Groundwater Flow in Arid Inland Basin, China

Abstract Views: 252  |  PDF Views: 75

Authors

Xiaomin Gu
School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China
Jingli Shao
School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China
Yali Cui
School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China
Qichen Hao
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Science, Shijiazhuang 050061, China

Abstract


Alluvial fan is an important recharge area for arid and semi-arid inland basins. In order to study groundwater circulation and quantify recharge amount of the groundwater system in arid inland basins, it is necessary to use numerical models. In this study, a 2D variably saturated numerical model of a typical profile has been developed using EOS 9 module of TOUGH2. The mesh for the fine soil plain area was refined compared with previous studies and the minimum cell size was 0.1 m in thickness. An improved approach in TOUGH2 was applied to calculate the groundwater evapotranspiration more efficiently and characterize water transport more accurately. Multiple calibration approaches were combined to calibrate the model. The results show that, the typical profile can be divided into three groundwater flow systems. The circulation depth for the local groundwater flow system is about 200 m and the shallow discharge accounts for 74.4% of the total amount with groundwater age less than 500 a (year). The circulation depth for the middle flow system can reach 800 m and the amount of discharge accounts for 18.5% of the total amount with groundwater age less than 10 ka (kiloyear). The circulation depth for the regional flow system is from 1000 to 1500 m, and the discharge accounts for 7.1% of the total amount with groundwater age ranging from 10 to 50 ka. The improved TOUGH2 numerical model, combined with multiple calibration approaches, can better reflect regional circulation characteristics and quantify the recharge amount of different groundwater sub-systems in arid and semi-arid inland basins with limited datasets.

Keywords


Arid Inland Basin, Groundwater Flow, Numerical Models, Multiple Calibration Approaches.

References





DOI: https://doi.org/10.18520/cs%2Fv113%2Fi03%2F403-412