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Vegetation that exists in the natural environment often involves a combination of plants with different stalk thicknesses. This combination affects the hydrodynamic properties of the ground surface, which in turn changes the velocity and distribution of run‐off. Current research on the influence of vegetation stalk thickness on water flow resistance is mostly focused on uniform vegetation. There have been few studies on the influence of non‐uniform vegetation on water flow resistance, and most have been qualitative in nature. In order to study the quantitative relationship between combinations of different stalk thicknesses and the water flow resistance of slope vegetation, a laboratory experiment was performed using a flume. The results show that when two different plant stalk thicknesses are staggered and combined, the diameters of the plants exhibit a power function relationship with the Darcy‐Weisbach resistance coefficient. When the diameter of the stem of one of the plants remains constant, at the same water depth, the coefficient of water flow resistance increases with the diameter of the stem of the other plant. Additionally, the coefficient of the vegetation flow resistance increases with increasing water depth. In the non‐submerged state, as the water depth increases, the rate at which the water flow resistance coefficient increases gradually declines, and as the diameter of any plant stem increases, the rate at which the water flow resistance coefficient increases also declines gradually. These findings provide a theoretical basis for the prevention and control of soil erosion and have important practical implications for maintaining water and soil resources. [ABSTRACT FROM AUTHOR]

• Functional decline of subsurface drainage in a rotational paddy field was assessed. • Drainage discharge and water pressure distribution in a flow pathway were measured. • Water flow resistances in the pathway were determined and used for evaluation. • Vertical water flow resistances limited the maximum subsurface drainage rate. • Determination of resistance is useful for the diagnosis of aged subsurface drainage. The functional decline of subsurface drainage systems has become a problem for the cultivation of upland crops in rotational paddy fields, necessitating the development of methods to determine its origin. This study aimed to quantify the water flow resistance (WFR) along the pathway from the plow layer to the drainage canal via aged subsurface drainage in a clayey paddy field. Hydrological monitoring was conducted in a clayey paddy field where subsurface drainage was installed over 20 years ago and soybeans were cultivated during the monitoring. The surface and subsurface drainage rates were measured using flowmeters attached to the drainage outlet. The water pressures along the pathway were measured using tensiometers or pressure transducers installed in the wells. Assuming continuous water flow through the pathway, the time evolution of the sectional WFR was determined from the measured total head gradient and the drainage discharge. Then, potential horizontal and vertical water flow rates, defined as the quotient of the maximum possible driving forces divided by the minimum WFR, were calculated. During rainfall events, the subsurface drainage rate increased rapidly after the start of the drainage, became high and nearly constant with time, and then gradually decreased. When the subsurface drainage rate was high, the total water head gradient in the vertical direction from the plow layer to the collecting drain was large, while the horizontal water head gradient in the plow layer was very small. The potential flow rates of the vertical and horizontal sections ranged from 2.1–5.7 mm/h, and from 6.2 to over 79 mm/h, respectively, indicating that the vertical WFR mainly determined the potential subsurface drainage rate. Our results suggest that simultaneous measurement of the pressure distribution along the water pathway and the subsurface drainage rate is a promising method for the diagnosis of aged subsurface drainage systems. [ABSTRACT FROM AUTHOR]