Infilterability Reduction of Artificial Recharge of Groundwater System in a Desert in the Absence of Sowbugs

Document Type: Research and Full Length Article


1 Research Scientist, Gorgan Research Center for Agriculture and Natural Resources

2 Associate Prof. in Sari University of Agriculture and Natural Resources, Department of Watershed Management.

3 Prof., Sari University of Agriculture and natural Resources

4 Senior Research Scientist of Fars Research Center for Agriculture and Natural Resources

5 Associate Professor, Sari University of Agriculture and Natural Resources


Floodwater spreading for the artificial recharge of groundwater (ARG) is a logical alternative to build large dams for water resources management in dry environments so that it not only enhances water security, but also reclaims the degraded land due to the settlement of suspended load on the spreaders. However, translocation of very fine clay minerals existing in floodwater decreases the infiltration capacity of sedimentation basins (SB) and recharge ponds which eventually terminate their useful life.  Although root channels facilitate infiltration and particularly percolation, crust formation substantially decreases the infiltration rate. As the role of a sowbug (Hemilepistus shirazi Schuttz) in enhancing the infiltrability has been previously reported, its absence had to be assessed too. Thus, the main objective of this research was to monitor the infiltration rate (IR) changes in the research plots devoid of the sowbug burrows in 3 SBs out of 6 ones in the Bisheh Zard1 ARG system in Gareh Bygone Plain (GBP) located in the southeast of Fars province applying the double ring method at constant hydraulic head during a 15 year operation. Each of those SBs was divided into three equal sections. One raised part in each section which had not been covered by floodwater was selected as the control. Results indicated that infiltrability after 15 years had decreased from 10.33 cm/h to 2.16, 2.49 and 7.47 cm/h in the first, second and third SBs, respectively. The largest decrease in infiltrability occurred in the upstream SB and the lowest one in the downstream SB. The volume of floodwater received by each SB and therefore, the volume of the settled suspended load depend on its location, the flow rate and duration of flooding. The ARG systems in the GBP are still functioning satisfactorily since 1983.


Main Subjects

Anon. 1990. A manual for measuring infiltration rate using double– ring. Power Ministry. Fars Regional Water Organization. P. 19. (in Persian).

Arriaga, F. J., Korenki, T. S., Balkcom, K. S., and Raper, R.L., 2010. A Method for automating data collection method from a double ring infiltrometer under falling head condition. Soil Use and Management. 26: 61-67.

Boroomand Nasab, S., Charkhabi, A. H., and Pirani, A., 2004. Floodwater effect on infiltration rate of a floodwater spreading system in Moosian. ICID-FAO International workshop on water harvesting and sustainable agriculture. Moscow, Russia.

Charkhabi, A. H., and Amiri M., 2003. Use of rate earth element in survey of the origin of clay and silt sediments in a flood spreading system in Kabodar Ahang, Hamadan. Seven international conference of dry land development. Tehran, Iran.

Bouwen, H., 1986. Intake rate: Cylinder infiltrometer. Pages 825-843: Methods of Soil Analysis. A. Klute, ed. ASA Monograph 9. ASA. Madison, WI.

Daneshvar, A., Danaeyan, M., 2005. The effects of floodwater spreading on some physico-chemical properties of soil and infiltration in Yazd. Proceeding of 2nd conference on watershed management, Tehran. Iran.

Esfandiari, M., and Rahbar, Gh., 2004. Monitoring of inflow and outflow rate from Kaftari artificial recharge of groundwater system in Dorz-sayeban region in southeastern Iran. Proceeding on management of aquifer recharge and water harvesting in arid and semi arid region Asia. 27, Nov. 2004.

Funseca, R. M., 2003. Dam Reservoir sediment as fertilizer and artificial soil, Case study from Portugal and Brazil. Proceedings of International Symposium Kanazava University.

Hirst, S. M., and Ibrahim A. M., 1996. Effects of flood protection and soil fertility in a flood plain area in Bangladesh. Soil, Science, Plant, Animal. 27:119-156.

Jafari, A., and Tavakoli Rad, F., 2014. The study of floodwater spread in systems on soil infiltration changes trend in Bousherhr Province. Range and Watershed Management. 67(4): 515-523. (In Persian).

Khalafi, J., Bayat, Movahed, F., Rezaei, A. and Mojtahedi, Gh., 2007. Effects of flood water spreading on chemical-physical characteristics of soil surface in Zanjan Province. Journal of soil and water science (in Persian).

Kowsar, A., 1991. Floodwater spreading for desertification control: An integrated approach. Des. Con. Bull. (UNEP) 19: 3-18.

Kowsar, A., 1995. An introduction to flood mitigation and optimization of floodwater utilization. Ministry of Agriculture, Research Institute of Forests and rangelands. Technical Publication No. 150.

Kowsar, A. 1998. Aquifer management: A key to food security in the deserts of the Islamic Republic of Iran. Des. Con. Bull., (UNEP), 33: 24-28.

Kowsar, A. 2005. Abkhandari (Aqifer Management): a green path to the sustainable development of marginal drylands. Journal of Mountain Science. 2(3): 233-243.

Kowsar, A. 2011. Desertification control through floodwater harvesting: the current state of know-how. The future of drylands, Chapter Five. P 229- 241. UNESCO.

Mohammadnia, M. and Kowsar, A., 2003. Clay translocation in the artificial recharge of groundwater system in the Southern Zagros Mountains. J. Mountain Res. Dev., 23: 50-55.

Mohammadnia, M., Kowsar, A., and Che, F., 2015. Eucalyptus camaldulensis Dehnh. Offers excellent potential to reduce NO32- concentration in groundwater. Global Advanced Research Journal of Plant Science. 1(1): 17-29.

Mahdian, M. H., Sokouti Oskoee R., and Kamali K., 2011. Appraisal of the trend of soil infiltration rate changes in the floodwater spreading stations of Iran. International Journal of Natural Resources and Marine Science. 1(1): 33-43.

Nejabat, M., 2009. Decision support system for desertification control through floodwater spreading in Islamic Republic of Iran. PhD thesis, University Putra Malaysia.

Newman, J.C., 1963. Water spreading on marginal arable area. Journal of soil conservation. New South Wales (NSW), 19: 49-58.

Phillips, J. R. H., 1957. Level- sill bank outlet. Jour. soil conservation. New South Wales (NSW), 13(2): 15p.

Quilty, J.A., 1972. Soil conservation structures for marginal arable areas- Gap absorption and gap spreader banks Journal of soil conservation. New South Wales (NSW), 28: 116-130.

Rahbar, Gh., 2008. The effects of floodwater spreading on soil physic-chemical changes in Fasa follodwater spreader. Final report of research plan. S/N 85.573. (in Persian).

Rajaie, H., Esmaili, K., Abbasi, A. A., and Ziaei, A. N. 2013. Study of permeability changes in floodwater spreading project (case study: Jajarm Project). Iranian Journal of Irrigation and Drainage. 7: 114-121. (In Persian).

Shariati, M. H., 2001. Investigation the floodwater spreading on soil infiltration in Damghan. M.Sc. Imam Khomeini education center. (In Persian).

Sokouti, R., and Mahdian M. H., 2005. The effects of floodwater spreading on soil properties in Iran. A case study of Poldasht flood spreading station. Journal of Pejuhesh and Sazandagi. 7: 42-50. (In Persian).

Tavassoli, A., and Mahdian, M. H., 2005. The study of floodwater spreading on Soil infiltration in Kaboudar Ahang aquifer management station. Proceeding of 2nd conference on watershed management, Tehran. Iran. (In Persian).

Teh, C.B.S., And Talib, J., 2006. Soil Physics Analysis. Vol. 1. University Putra Malaysia Press. 42 p.

Tricker, A. S., 1978. The infiltration cylinder: Some comments on its use. J. Hydrology. (Amsterdam) 36:383-391.

Zaremehrjardi, M., Mahdian, M. H. and Barkhordari, J. 2013. The study of soil infiltration rate changes in Sarchahan Aquifer of Hormozegan Province. Journal of Watershed Management Science and Engineering. 20(7):1-8. (in Persian).