TECHNICAL PAPERS
Apr 1, 2007

Effect of Periodic and Continuous Irrigation on Water Transport through Porous Media

Publication: Journal of Irrigation and Drainage Engineering
Volume 133, Issue 2

Abstract

In this paper, we compare the effect of two modes of irrigation on water transport through an unsaturated porous medium. The two modes studied are (1) periodic and (2) continuous irrigation. The former process consists of two stages, i.e., imbibition and drainage. The entire volume of water is assumed to be added during the imbibition stage at a constant rate. The time during which imbibition occurs is taken as a fraction of the total time period. In the drainage stage, no fresh water is added and the water inside the soil redistributes itself and drains from the soil. In the continuous mode, water is added at a constant rate during the whole time period. To ensure a fair comparison, the rate of water addition in the continuous mode is kept the same as the average rate of water addition over a time period in the periodic mode that includes the drainage and imbibition steps. The recharge is calculated as the volume of water drained from the bottom of the soil during a time period. The transport of water in the unsaturated zone is studied in the presence of water uptake by plant roots. The two modes of operation were simulated using a mass conservative algorithm based on a modification of Picard’s iterative scheme. Predictions in the periodic mode were performed using direct simulation and the results obtained were compared with an algorithm based on a shooting method. The performances of these two modes have been evaluated by calculating the recharge amount. When the sink term due to the plant roots was included, it was found that the recharge is significantly higher for the case of periodic operation. A physical explanation for the results obtained is proposed. The effect of hysteresis in the water retention curves was simulated using an empirical method. We have found that the total recharge amount in the periodic operation calculated using a mean nonhysteretic curve is very close to that obtained when we include the effect of hysteresis.

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References

Abdu, H. M., and Flury, M. (2004). “Simulation of water flow and solute transport in free drainage lysimeters and field soils with heterogeneous structures.” Eur. J. Soil. Sci., 55, 229–241.
Bruckler, L., Lafolie, F., Ruy, S., Gamier, J., and Baudequin, D. (2000). “Modeling the agricultural and environmental consequences of non-uniform irrigation on a maize crop: I. Water balance and yield.” Agronomie, 20, 609–624.
Celia, M. A., Boulotas, E. T., and Zarba, R. L. (1990). “A general mass conservative numerical solution for the unsaturated flow equation.” Water Resour. Res., 26, 1483–1496.
Cote, C. M., Bristow, K. L., Charlesworth, P. B., Cook, F. J., and Thorburn, P. J. (2003). “Analysis of soil wetting and solute transport in subsurface trickle irrigation.” Irrig. Sci., 22, 143–156.
Dane, J. H., and Wierenga, P. J. (1975). “Effect of hysteresis on the prediction of infiltration, redistribution and drainage of water in a layered soil.” J. Hydrol., 25, 229–242.
Dehadrai, P. V. (2003). “Irrigation in India.” Fisheries in irrigation systems of arid Asia, FAO Fisheries Technical Paper No. 430, T. Petr, ed., 59–70. Selected papers from the Food and Agriculture Organization of the United Nations, Rome.
Dwyer, L. M., Stewart, D. W., and Balchin, D. (1988). “Rooting characteristics of corn, soybeans and barley as function of available water and soil physical characteristics.” Can. J. Soil Sci., 68, 121–132.
Haverkamp, R., Vauclin, M., Touma, J., Wierenga, P., and Vachaud, G. (1977). “Comparison of numerical simulation models for one dimensional infiltration.” Soil Sci. Soc. Am. J., 41, 285–294.
Hinz, C. (1998). “Analysis of unsaturated/saturated water flow near a fluctuating water table.” J. Contam. Hydrol., 33, 59–80.
Hopmans, J. W., Roy, K. C., and Wallender, W. W. (1991). “Irrigation water management and soil-water hysteresis–A computer modeling study with stochastic soil hydraulic properties.” Trans. ASAE, 34, 449–459.
Huang, K., Mohanty, B. P., Leij, F. L., and van Genuchten, M. Th. (1996). “Solution of the nonlinear transport equation using modified Picard iteration.” Adv. Water Resour., 21, 237–249.
Jaynes, D. B. (1984). “Comparison of soil-water hysteresis models.” J. Hydrol., 75, 287–299.
Jaynes, D. B. (1992). “Estimating hysteresis in the soil water retention function.” Proc., Int. Workshop on Indirect Methods for Estimating the Hydraulic Properties of Unsaturated Soils, M. Th. van Genuchten, F. J. Leij, and L. J. Lund, eds., Univ. of California, Riverside, Calif., 219–232.
Klute, A., and Heermann, D. F. (1974). “Soil water development under a periodic boundary condition.” Soil Sci., 117, 265–271.
Kool, J. B., and Parker, J. C. (1987). “Development and evaluation of closed form expressions for hysteretic soil hydraulic properties.” Water Resour. Res., 23, 105–114.
Lehmann, P., Stauffer, F., Hinz, C., Dury, O., and Fluhler, H. (1998). “Effect of hysteresis on water flow in a sand column with a fluctuating capillary fringe.” J. Contam. Hydrol., 33, 81–100.
Li, K. Y., De Jong, R., and Boisvert, J. B. (1999). “Comparison of root water uptake models.” Sustaining the global farm, 2001, D. E. Scott, R. H. Mohtar, and G. E. Steinhardt, eds., 1112–1117. Selected papers from the Tenth International Soil Conservation Organization Meeting, Purdue Univ. and the USDA-ARS National Soil Erosion Research Laboratory, West Lafayette, Ind.
Li, K. Y., De Jong, R., and Boisvert, J. B. (2001). “An exponential root water-uptake model with water stress compensation.” J. Hydrol., 252, 189–204.
Mualem, Y. (1984). “A modified dependent domain theory of hysteresis.” Soil Sci., 137, 283–291.
Scott, P. S., Farquhar, G. J., and Kouwen, N. (1983). “Hysteretic effects on net infiltration.” Advances in infiltration, ASAE, St. Joseph, Mich., 163–170.
Stauffer, F., and Dracos, T. (1986). “Experimental and numerical study of water and solute infiltration in layered porous media.” J. Hydrol., 84, 9–34.
Stauffer, F., and Kinzelbach, W. (2001). “Cyclic hysteretic flow in porous medium column: Model, experiment, and simulations.” J. Hydrol., 240, 264–275.
van Dam, J. C., and Feddes, R. A. (2000). “Numerical simulation of infiltration, evaporation and shallow ground water levels with the Richards equation.” J. Hydrol., 233, 72–85.
van Genuchten, M. Th. (1980). “A closed form equation for predicting the hydraulic conductivity of unsaturated soils.” Soil Sci. Soc. Am. J., 44, 892–898.
Werner, A. D., and Lockington, D. A. (2003). “Influence of hysteresis on tidal capillary fringe dynamics in a well-sorted sand.” Adv. Water Resour., 26, 1199–1204.

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Published In

Go to Journal of Irrigation and Drainage Engineering
Journal of Irrigation and Drainage Engineering
Volume 133Issue 2April 2007
Pages: 100 - 109

History

Received: Apr 11, 2005
Accepted: Aug 7, 2006
Published online: Apr 1, 2007
Published in print: Apr 2007

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Authors

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C. P. Krishnamoorthy
Research Scholar, Dept. of Chemical Engineering, Indian Institute of Technology, Madras, Chennai-600 036, India.
Abhijit P. Deshpande
Assistant Professor, Dept. of Chemical Engineering, Indian Institute of Technology, Madras, Chennai-600 036, India.
S. Pushpavanam
Professor, Dept. of Chemical Engineering, Indian Institute of Technology, Madras, Chennai-600 036, India (corresponding author). E-mail: [email protected]

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