Hydrological effects of open ditch damming and controlled subsurface drainage in a Nordic agricultural field

Abstract

Controlled drainage (CRD) is an agricultural water management practice designed to adjust the capacity of a drainage system under varying hydrological conditions. This simulation study aimed to quantify the potential of combining a controlled subsurface drainage (CS) with open ditch damming (CD) to manage the water table depth (WTD) and field water balance in Nordic conditions. Simulations with and without controlled drainage were run using a hydrological model that had been set up for a flat loamy field in Northern Ostrobothnia, Finland, for the period 2010–2021. All CRD scenarios reduced the probability of deep WTDs during growing seasons (May–Sep). The impact of CS on WTDs was greater and more uniform than CD. The CRD effects on water balance were seen in water outflow pathways, as CS reduced drain discharge while CD had the opposite effect. When both methods were applied simultaneously, annual evapotranspiration increased 5–12% compared with the free drainage scenario. The effects of CRD on evapotranspiration were greatest during the dry years indicating that CRD has potential to reduce drought in food production areas. None of the CRD scenarios could maintain optimal WTDs during the entire growing season, highlighting the complexity of optimizing field water management using CRD alone. HIGHLIGHTS Combining open ditch damming and controlled subsurface drainage provides flexibility for agricultural water management.; Hydrological modeling provides a holistic view of field hydrology.; Controlled drainage reduces the probability of deep water tables during the growing season.; The impact of drainage design on field water balance was most clearly seen in runoff outflow pathways.;

Keywords

• macropores
• modeling
• water balance
• water management
• water table depth