برآورد تغذیه و تبادل جریان بین رودخانه و آبخوان بر اساس مدل متصل شده آب سطحی- آب زیرزمینی

نوع مقاله : مقاله پژوهشی

نویسندگان

1 گروه مهندسی آب، دانشگاه رازی، کرمانشاه، ایران

2 دانشیار گروه مهندسی آب دانشگاه رازی، کرمانشاه، ایران

3 استادیار گروه مهندسی آب، دانشگاه رازی، کرمانشاه، ایران

چکیده

بهره­برداری تلفیقی از منابع آب‌سطحی و زیرزمینی یکی از مهم­ترین چالش­های پیش روی محققین منابع آب می باشد. استفاده تلفیقی در واقع، بهره­برداری از منابع آب­سطحی و زیرزمینی به منظور افزایش میزان آب قابل دسترسی و استفاده پایدار از منابع آب موجود است. بنابراین از اهداف اساسی مطالعه جاری، شبیه‌سازی برهم کنش آب‌سطحی و زیرزمینی با استفاده از ایجاد اتصال دینامیکی بین مدل آب‌سطحی WEAP و مدل آب‌زیرزمینی MODFLOW در دشت میان­دربند می باشد. در این راستا برای شبیه‌سازی منطقه غیر اشباع خاک از روش هیدرولوژیکی رطوبت خاک استفاده گردید. نتایج حاصل از برهم کنش آب سطحی و زیرزمینی ارائه شده و شرایط موجود بهره­برداری از منابع آب منطقه در صورت ادامه سیاست­های موجود مورد بررسی قرار گرفت. یکی از مهم‌ترین دستاوردهای این تحقیق ایجاد شبیه‌سازی ناحیه اشباع و غیراشباع خاک با استفاده از مولفه‌های بیلان کامل هیدروکلیماتولوژی به صورت یک مدل متصل شده آب‌سطحی و زیرزمینی است. نتایج نشان داد در یک دوره 6 ساله بیشترین مقدار تغذیه آبخوان در سطح دشت میان‌دربند کرمانشاه در ماه­های آبان تا فروردین در حدود 10 تا 19 میلیون متر مکعب است. در برخی از این ماه­ها علاوه بر بارندگی مقدار‌ی از تغذیه ناشی از نفوذ آب آبیاری می­باشد. بیشترین میزان افت تراز سطح آب‌زیرزمینی به مقدار 5/7 متر مربوط به ناحیه شمالی دشت و میزان متوسط افت در کل دشت در انتهای دوره بهره‌برداری 6 ساله (مهر 86تا شهریور 92) حدود 4 متر خواهد بود.

کلیدواژه‌ها

عنوان مقاله [English]

Estimation of Recharge and Flow Exchange between River and Aquifer Based on Coupled Surface Water-Groundwater Model

نویسندگان [English]

  • Vida Kamkar 1
  • Arash Azari 2
  • Seyed Ehsan Fatemi 3
1 Department of Water Engineering, Razi University, Kermanshah, Iran
2 Associate Professor, Department of Water Engineering, Razi University, Kermanshah, Iran
3 Assistant Professor, Department of Water Engineering, Razi University, Kermanshah, Iran
چکیده [English]

Integrated operation of surface water and groundwater resources is one of the most important challenges facing water resources researchers. Integrated use is, in fact, the exploitation of surface and groundwater resources in order to increase the amount of available water and the sustainable use of available water resources. Therefore, one of the main goals of the present study is to simulate the interaction of surface water and groundwater by creating a dynamic couple between the WEAP surface water model and the MODFLOW groundwater model in the Miandarband plain. In this regard, the Soil Moisture Hydrological method was used to simulate the unsaturated zone of the soil. The results of simulation of surface and groundwater interaction were presented and the conditions for the use of water resources in the area was investigated for the continuous current policy. One of the most important achievements of this research is the simulation of saturated and unsaturated zones of the soil using complete hydroclimatology balance components as a coupled model of surface and groundwater. In the period of 6 years, the highest amount of aquifer recharge in the Miandarband plain, is about 10 to 19 million cubic meters in November to March. In some of these months, in addition to rainfall, the aquifer recharge is due to the infiltration of irrigation water. The highest rate of groundwater drowdown (7.5 meters) is related to the northern part of the plain and the average drowdown in the whole plain at the end of the 6-year operation period (October 2007 to September 2013) will be about 4 meters.

کلیدواژه‌ها [English]

  • River and aquifer interaction
  • Soil unsaturation zone
  • Recharge rate
  • WEAP-MODFLOW

مراجع

Bayesteh, M and Azari, A. (2021). Stochastic Optimization of Reservoir Operation by Applying Hedging Rules. J. Water Resour. Plann. Manage., 147(2), 04020099.
Bear, J. (2010). Modeling Groundwater Flow and Contaminant Transport. Springer Verlag. Vol. 23. 834 P.
Brenot, A., Petelet-Giraud, E. and Gourcy, L. (2015). Insight from surface water-groundwater interactions in an alluvial aquifer: contributions of δ2H and δ18O of water, δ34SSO4 and δ18OSO4 of sulfates, 87Sr/86Sr ratio. Procedia Earth and Planetary Science, 13, 84 – 87.
Eastoe, C. J., Hutchison, W. R., Hibbs, B. J., Hawley, J. and Hogan, J. F. (2010). Interaction of a river with an alluvial basin aquifer: Stable isotopes, salinity and water budgets. Journal of Hydrology, 395, 67–78.
Engeler, I ., Hendricks Franssen H. J., Müller, R. and Stauffe, F.  (2011). The importance of coupled modelling of variably saturated groundwater flow-heat transport for assessing river–aquifer interactions. Journal of Hydrology, 397, 295-305.
Fleckenstein, J. H., Krause, S., Hannah, D. M. and Boano, F. (2010).  Groundwater-surface water interactions-New methods and models to improunderstanding of processes and dynamics. Journal of Advances in Water Resources, 33, 1291-1295.
Gorelick, S. M. (1983). A review of distributed parameter groundwater management modelling methods. Water Resources Research, 19 (2), 305-319.
Graham, P. W., Andersen, M. S., McCabe, M. F., Ajami, H., Baker, A. and Acworth, I. (2015). To what extent do long-duration high-volume dam releases influence river–aquifer interactions? A case study in New South Wales, Australia. Hydrogeology Journal, 23, 319–334.
Guzman, S. M., Paz, J. O., Tagert, M. L. M. and Mercer, A. E. (2019). Evaluation of Seasonally Classified Inputs for the Prediction of Daily Groundwater Levels: NARX Networks Vs Support Vector Machines. Environmental Modeling & Assessment, 24(2), 223-234.
Hu, L., Xu, Z. and Huang, W. (2016). Development of a river-groundwater interaction model and its application to a catchment in Northwestern China. Journal of Hydrology, 543, 483–500.
Ivkovic , K. M. (2009). A top–down approach to characterise aquifer–river interaction processes. Journal of Hydrology, 365, 145–155.
Jonoubi, R., Rezaei, H. and Bahmanesh, J. (2013). Underground water management through combining surface and sub-surface water using Modflow model in urmia plain. Journal of water and irrigation management, 3 (1), 49-68. (In Farsi)
Luo,Y. and Sophocleous, M. (2011). Tow-way coupling of unsaturated-saturated flow by integrating the SWAT and MODFLOW models with application in an irrigation district in arid region of West China. Journal of Arid Land, 3(3), http://doi.org/ 10.3724/SP.J.1227.2011.00164.
Nadiri, A. A., Naderi, K., Khatibi, R., and Gharekhani, M. (2019). Modelling groundwater level variations by learning from multiple models using fuzzy logic. Hydrological sciences journal, 64(2), 210-226.
Nazri, A. A. M., Syafalni., Abustan I., Rahman, M T A., Zawawi M H. and Dor N. (2012). Authentication Relation between Surface-Groundwater in Kerian Irrigation Canal System, Perak using Integrated Geophysical, Water Balance and Isotope Method. Procedia Engineering, 50, 284 – 296.
Pahar, G. and Dhar, A. (2014). A Dry Zone-Wet Zone Based Modeling of Surface Water and Groundwater Interaction for Generalized Ground Profile. Journal of Hydrology, 519(27), 2215-2223.
 Ramírez-Hernández, J., Hinojosa-Huerta, O., Peregrina-Llanes, M., Calvo-Fonseca, A. and Carrera-Villa, E. (2013). Groundwater responses to controlled water releases in the limitrophe region of the Colorado River: Implications for management and restoration. Journal of Ecological Engineering, 59, 93-103.
Rugel, K., Golladay, S. W., Jackson, S. R. and Rasmussen, T. C. (2016). Delineating groundwater/surface water interaction in a karstwatershed: Lower Flint River Basin, southwestern Georgia, USA. Journal of Hydrology: Regional Studies, 5, 1–19.
Sanz, D., Castaño, S., Cassiraga, E., Sahuquillo, A., José Gómez-Alday, J., Peña, S. and Calera, A. (2011). Modeling aquifer–river interactions under the influence of groundwater abstraction in the Mancha Oriental System (SE Spain). Hydrogeology Journal,  19, 475–487.
Sieber, J. and Purkey, D. (2015) User guide for WEAP. Stockholm Environment Institute, U.S. Center.
Sophocleous. M. )2002(. Interaction between Ground Water and Surface Water: The State of the Science, Hydrogeology Journal, 10, 52-67.
Shamsaei., A., and Forghani, A. (2011). Integrated exploitation of surface water and groundwater resources in arid areas. Iranian Water Resources Research, 7(2), 26- 36. (In Farsi)
Weitz, J. and Demlie, M. (2013). Conceptual modelling of groundwater–surface water interactions in the Lake Sibayi Catchment, Eastern South Africa. Journal of African Earth Sciences, 99(2), 613-624.
Zampieri, M.,  Serpetzoglou, E., Anagnostou, E. N.,  Nikolopoulos. E. I. and Papadopoulos, A. (2012). Improving the representation of river–groundwater interactions in land surface modeling at the regional scale: Observational evidence and parameterization applied in the Community Land Model.  Journal of Hydrology, 420(421), 72–86.
Zeinali, M., Azari, A. and Heidari, M. (2020a). Simulating Unsaturated Zone of Soil for Estimating the Recharge Rate and Flow Exchange Between a River and an Aquifer. Water Resources Management, 34, 425–443.
Zeinali, M., Azari, A. and Heidari, M. (2020b). Multiobjective Optimization for Water Resource Management in Low-Flow Areas Based on a Coupled Surface Water–Groundwater  Model. Journal of Water Resource Planning and Management (ASCE), 146(5), 04020020.
Zibaei, M. H., Zibaei, M. and Ardokhani, K. (2013). Evaluation of scenarios of integrated use of surface and groundwater resources in Firoozabad plain of Fars. Journal of Agricultural Economics Research, 5(1), 157-181.
 
تحقیقات آب و خاک ایران
دوره 52، شماره 7
مهر 1400
صفحه 1779-1793

فایل ها

هم رسانی

ارجاع به این مقاله

آمار