Abstract
Mostly the swamps in Rwanda are surrounded by volcanic hills with small streams flowing to discharge runoff and seepage water. Mugogo swamp is located in Busogo sector, Musanze district, North province. Total area of the swamp is approximately 50 ha. The swamp is surrounded by hills and elevated volcanic rocky terrains. Potato is the main crop cultivated in the swamp. The average production rate of potato is 7 MT/ha which is very low compared to 12 MT/ha in well drained areas. During rainy season seepage water and runoff water from the surrounding hills cause the waterlogged condition of the swamp and affecting the potato cultivation and land productivity.
The remedial measure for this swamp is to divert separately the runoff and seepage water from surrounding catchment area and then remove the recharge water by pumping through a system of subsurface drains. Hydraulic head–drain discharge relationship can be fitted with quadratic equation. Equivalent drainable porosity and equivalent hydraulic conductivity are determined as 0.105 m/day and 0.34% respectively for drain depth of 40 cm from soil surface. Effective hydraulic conductivity in the soil profile shows that its average value in the top 15 cm of soil layer is 0.17 m/day and that in the remaining depth up to impermeable layer is 0.015 m/day. Third degree polynomial expressions are made for Head–hydraulic conductivity and head–drainable porosity relationships. The nonlinear relation of hydraulic conductivity and drainable porosity with drawdown shows that the proximity of Kinoni stream does not affect drainage parameters of the area because of less seepage from the stream. The study also reveals that adoption of 7 m drain spacing is very less if crop parameter is not considered and will result higher drain cost.
Drainage coefficient of 5 mm/day is arrived considering the rainfall distribution, infiltration rate of soil, allowable water logging tolerance of potato crop. Required drain spacings are calculated for different drainage coefficients of 1, 2, 3, 4 and 5 mm/day under different drawdown conditions to plot subsurface drainage characteristic curves of the swamp. These curves are useful to directly read the drain spacing and drain depth for the required drainage coefficient without going for tedious calculations. Cost analysis shows that the ratio of drain spacing to drain depth can be a decisive factor to select best combination of drain depth and drain spacing. For drainage coefficient of 5 mm/day, optimum drain spacing-depth ratio is found as 7.2 with a cost of 0.689 million Frw/ha. For different drainage coefficients in the swamp, the drain depth of 1.5 m is crucial and optimum cost occurs at this depth. It is also found that any increase in drawdown beyond the drawdown at critical drain depth will not reduce the cost significantly.
Similar content being viewed by others
References
Ahuja LR, Naney JW, Nielsen DR (1984) Scaling soil water properties and infiltration modeling. Soil Sci Soc Am J 48:970–973
Braun HMH, Kruijne R (1994) Soil conditions. In: Ritzema HP (ed) Drainage principles and applications, ILRI Publication 16, International Institute for Land Reclamation and Improvement, The Netherlands, Wageningen
Feyen JD, Jacques D, Timmerman A, Vanderborgt J (1998) Modelling water flow and solute transport in heterogenous soils: A review of recent approaches. J Agric Eng 70:231–256
Jhorar RK (2002) Estimation of effective soil hydraulic parameters for water management studies in semi-arid zones: integral use of modeling, remote sensing and parameter estimation. Doctoral Thesis, Wageningen University
Li W, Li B, Shi Y, Jacques D, Feyen J (2001) Effect of spatial variation of textural layers on regional field water balance. Water Resour Res 37:1209–1219
Mathew EK, Vos J (2003) Determination of drainage parameters in the low-lying acid sulphate coastal wetlands of Kerala, India. In: 9th International Drainage Workshop, The Netherlands, Paper No. 011
Ritzema HP (ed) (1994) Drainage principles and applications. The Netherlands, Wageningen
Taylor GS (1960) Drainable porosity evaluation from outflow measurements and its use in drawdown equations. Soil Sci 90:338
Wildenschild D, Jensen KH (1999) Numerical modeling of observed effective flow behaviour in unsaturated heterogeneous sands. Water Resour Res 35:29–42
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Kannan, N. Study of Drawdown–Drain Discharge Relationship and its Application in Design of Cost Effective Subsurface Drainage System in Mugogo Swamp, Busogo, Rwanda. Water Resour Manage 22, 1113–1125 (2008). https://doi.org/10.1007/s11269-007-9215-7
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11269-007-9215-7