Nutrient dynamics in water and soil under conventional rice cultivation in the Vietnamese Mekong Delta.

The evaluation of nutrient variability plays a crucial role in accessing soil potentials and practical intervention responses in rice production systems. Synthetic fertilizer applications and cultivation practices are considered key factors affecting nutrient dynamics and availability. Here, we assessed the nutrient dynamics in surface, subsurface water and soil under local water management and conventional rice cultivation practices in the Vietnamese Mekong Delta. We implemented a field experiment (200 m ) in the 2018 wet season and the 2019 dry season in a triple rice-cropping field. Eight samples of surface water, subsurface water (30-45 cm), and topsoil (0-20 cm) were collected and analysed during the rice-growing seasons. The results showed that N-NH , P-PO and total P peaks were achieved after fertilizing. Irrespective of seasons, the nutrient content in surface water was always greater than that of subsurface water ( < 0.001), with the exception of N-NO , which was insignificant ( > 0.05). When comparing the wet and dry seasons, nutrient concentrations exhibited minor differences ( > 0.05). Under conventional rice cultivation, the effects of synthetic fertilizer topdressing on the total N, soil organic matter (SOM), and total P were negligible in the soil. Higher rates of N fertilizer application did not significantly increase soil N-NH , total N, yet larger P fertilizer amounts substantially enhanced soil total P ( < 0.001). Under conventional rice cultivation, N-NH , P-PO and total P losses mainly occur through runoff rather than leaching. While N-NO loss is similar in surface water and subsurface water. Notably, nutrient content in soil was high; whilst SOM was seen to be low-to-medium between seasons. Future work should consider the nutrient balance and dynamic simulation in the lowland soil of the Vietnamese Mekong Delta's paddy fields.