Evaluation of shallow groundwater contribution by two lentil cultivars water use

Document Type : Original Articles

Authors

1 Department of Water Resources Engineering, Campus of Agriculture & Natural Resources, Razi University, Kermanshah, Iran

2 Agriculture and Plants breeding group, Campus of Agriculture & Natural Resources, Razi university, Kermanshah, Iran

Abstract

Introduction
Shallow groundwater is a resource which can provides and meets high values of plant’s water requirement. Shallow groundwater use by plant depends on different factors as: soil hydraulic conductivity, plant root features and characteristics, salinity tolerance level, a proper drainage system, irrigation system and management. In case of shallow groundwater use by plant, total irrigation number and water requirement will be reduced. Therefore, shallow groundwater, is a potential, efficient and free water resource in agriculture which sometimes defined as subsurface irrigation. The present study was conducted with the aim to examine the effects of shallow water table of 60, 80 and 110 cm depth on the water requirement, water use efficiency and different yield components of two lentil varieties namely that was conducted into two-factor factorial and based on completely randomized design with three replications. This research was carried out at Kermanshah with semi-arid climate by using lysimeters during two growing season 2013 and 2014.
 
Materials & Methods
The research was performed at the Irrigation and Water Resources Engineering Research Lysimetric Station, located at 47°9′ E and 34°21′ N, with an elevation of 1319 m (asl), as a part of the Campus of Agriculture and Natural Resources of Razi University in Kermanshah, Iran. In this study 18 Polyetelen lysimeters with diameter of 280 mm were used. The bottom of lysimeters were blocked to prevent of any leaching. Groundwater levels in the lysimeters were determined and fixed by Marriott siphon that was installed beside of each lysimeter in different groundwater depths of 60, 80 and 110 cm. The soil texture in the lysimeters was Silty clay. The cultivation in the first and second year of the research was conducted in 13 and 16 March, years 2013 and 2014 respectively. To obtain the amount of water requirement of plants, evaporation data of pan class A was received daily from the meteorology station which was located at distance of one hundred meters from research station. In this research, water requirement was determined by considering three stages as: reference evapotranspiration (ETo), the crop coefficient (KC) and finally crop evapotranspiration. Analysis of variance and comparison of means were done for different treatment by MSTATC software
 
Results & Discussion
According to the results in both years of study, maximum and minimum consumption of groundwater belong to depths of 60 and 110 cm, respectively. The ground water contribution for depths of 60, 80 and 110 cm was obtained as 53.76%، 36.50%، 15.23%, respectively. The results showed that maximum groundwater use efficiency, based on seed yield, for ILL6037 and Kimia cultivars was obtained in depths of 110, and the minimum groundwater use efficiency, for ILL6037 cultivar was obtained in depths 60 and 80 cm during both years of study, respectively. Also the maximum and minimum seed yield in both years of study was obtained for Kimia cultivar, in water table depths 60 and 110 cm respectively. Moreover, the maximum and minimum protein values was obtained, for Kimia cultivar in depth of 110 cm and ILL6037 cultivar in depth of 60 cm respectively.
 
Conclusion
It can be concluded that by increasing the depth of water table the values of groundwater contribution to crop water requirement was reduced. It may reason of increasing the distance between plant roots and water table. As a result of this phenomenon, plant root access to water by the use of capillary rise to meet the water requirement reduced and therefore, the groundwater contribution for providing plant water requirement was reduced. The results of this research showed that legume crops such as Lentil can use groundwater properly.

Keywords


  1. Agriculture Statistics. 2011. Ministry of Agriculture, Deputy for Planning and Economic, Technology Center of Information & The First Volume of Crops, 123 pp. (In Persian).
  2. Allen, R.G., Pereira, L.S., Raes, D., and Smith, M. 1998. Crop Evapotranspiration-Guidelines for Computing Crop Water R FAO Irrigation and Drainage Paper 56. FAO, Rome 300(9): p. D05109.
  3. Ayars, J.E., Shouse, P., and Lesch, S.M. 2009. In situ use of groundwater by alfalfa. Agricultural Water Management 96(11): 1579-1586.
  4. Bagheri, A., Nezami, A., and Soltani, M. 2000. Cool SeasonBeansModifiedforToleranceto Stress. Organization ofResearch, Educationand Promoting (In Persian with English Summary).
  5. Benz, L. C., Doering, E.J., and Reichman, G.A. 1985. Water-table and irrigation effects on corn and sugarbeet. Transactions of the ASAE 28(6): 1951-1956.
  6. Ghamarnia, H., Farmani Fard, M., and Sasani, SH. 2012. Effects of shallow water table on water requirement supply, water use efficiency and yield of three cultivars of wheat. Journal of Water Research in Agriculture 26(3): 339-353. (In Persian with English Summary).
  7. Ghamarnia, H., and Jalily, Z. 2014. Shallow saline groundwater use by Black cumin (Nigella sativa) in the presence of surface water in a semi-arid region. Agricultural Water Management 132: 89-100.
  8. Ghamarnia, H., and Khodaei, E. 2016. Evidence on shallow groundwater use by edible green vegetables such as Solanum pseudoca psicum, Ocimum basilicum and Lepidium sativum in a semi-arid climate condition. Agricultural Water Management 165: 198-210.
  9. Goins, T., Lunin, J., and Worley, H.L. 1996. Water table effects on growth of tomatoes, snap beans and sweet corn. Transactions of the ASAE 9(4): 530-0533.
  10. Kahlown, M.A., Iqbal, M., Skogerboe, G.V., and Rehman, S. 1998. Waterlogging, Salinity and Crop Yield R IWMI.
  11. Kheirabi, J., Tavakoli, A., Entesari, M., and Salamat, A. 1996. Guidelines of Low Publications of the National Committee on Irrigation and Drainage. (In Persian).
  12. Prathapar, S.A., and Qureshi, A.S. 1999. Modelling the effects of deficit irrigation on soil salinity, depth to water table and transpiration in semi-arid zones with monsoonal rains. International Journal of Water Resources Development 15(1-2): 141-159.
  13. Ragab, R.A., Amer, F., and El‐Ghamry, W.M. 1988. The conjunctive use of rainfall and shallow water table in meeting water requirements of Faba bean. Journal of Agronomy & Crop Science 160(1): 47-53.
  14. Shih, S.F., and Rahi, G.S. 1985. Evapotranspiration, yield, and water-table studies of celery. Transactions of the ASAE 28(4): 1212-1218.
  15. Singh, K.B., and Saxena, M.C. 1993. The Challenge of Developing Biotic and Abiotic Stress Resistance in Cool-season Food Legumes. In Breeding for Stress Tolerance in Cool Season Food Legume Wiley-Sayce Publication.
  16. Talebnejad, R., and Sepaskhah, A.R. 2015. Effect of different saline groundwater depths and irrigation water salinities on yield and water use of quinoa in lysimeter. Agricultural Water Management 148: 177-188.
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