Abstract
Background 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. Methods We implemented a field experiment (200 m 2) 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. Results The results showed that N-NH 4+, P-PO 43- 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 (P<0.001), with the exception of N-NO 3-, which was insignificant (P>0.05). When comparing the wet and dry seasons, nutrient concentrations exhibited minor differences (P>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 4+, total N, yet larger P fertilizer amounts substantially enhanced soil total P (P<0.001). Conclusions Under conventional rice cultivation, N-NH 4+, P-PO 43- and total P losses mainly occur through runoff rather than leaching. While N-NO 3- 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.
Highlights
The Mekong Delta (MD) is the biggest rice-producing region in Vietnam (Clauss et al, 2018), accounting for approximately 55% of total national rice (Oryza sativa L.) outputs through intensive rice production systems (Uno et al, 2021)
The effects of synthetic fertilizer topdressing on the total N, soil organic matter (SOM), and total P were negligible in the soil
It is noted that the concentration of N-NH4+, P-PO43À and Total P (TP) in the surface water (SW) was consistently higher than that in the SbW (P < 0.05), while the value of N-NO3À was insignificant between the SW and SbW (P > 0.05)
Summary
The Mekong Delta (MD) is the biggest rice-producing region in Vietnam (Clauss et al, 2018), accounting for approximately 55% of total national rice (Oryza sativa L.) outputs through intensive rice production systems (Uno et al, 2021). For conventional rice cultivation in the MD’s paddy fields, the amount of fertilizer application in the wet season (WS) and dry season (DS) has been found to vary from 82–97 kg N haÀ1, 22.64– 22.69 kg P haÀ1, and 29–32 kg K haÀ1 (Stuart et al, 2018). It has been suggested that higher amounts of fertilizer application under conventional rice cultivation and local water management regimes would largely result in increased nutrients in adjacent environments. This paper aims to explore the temporal-spatial dynamics of nutrients in the SW, SbW and soil of triple rice-cropping models both during the WS and DS under conventional local farming practices. We assessed the nutrient dynamics in surface, subsurface water and soil under local water management and conventional rice cultivation practices in the Vietnamese Mekong. Eight samples of surface water, subsurface water (30–45 cm), and topsoil (0–20 cm) were collected and analysed during the rice-growing seasons
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