Abdulhamid Yusuf, Duan Lei, Yaqiao Sun, Hu Jinmei
School of Water and Environment, Chang'an University, Xi'an, 710054, China.
Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region, Ministry of Education, Chang'an University, Xi'an, 710054, China.
Sci Rep. 2024 Feb 17;14(1):3954. doi: 10.1038/s41598-024-54571-2.
This study investigates the impact of water levels and soil texture on the migration and transformation of nitrate (NO-N) and ammonium (NH-N) within a soil column. The concentrations of NO-N gradually decreased from an initial concentration of 34.19 ± 0.86 mg/L to 14.33 ± 0.77 mg/L on day 70, exhibiting fluctuations and migration influenced by water levels and soil texture. Higher water levels were associated with decreased NO-N concentrations, while lower water levels resulted in increased concentrations. The retention and absorption capacity for NO-N were highest in fine sand soil, followed by medium sand and coarse sand, highlighting the significance of soil texture in nitrate movement and retention. The analysis of variance (ANOVA) confirmed statistically significant variations in pH, dissolve oxygen and oxidation-reduction potential across the soil columns (p < 0.05). Fluctuating water levels influenced the migration and transformation of NO-N, with distinct patterns observed in different soil textures. Water level fluctuations also impacted the migration and transformation of NH-N, with higher water levels associated with increased concentrations and lower water levels resulting in decreased concentrations. Among the soil types considered, medium sand exhibited the highest absorption capacity for NH-N. These findings underscore the significant roles of water levels, soil texture, and soil type in the migration, transformation, and absorption of nitrogen compounds within soil columns. The results contribute to a better understanding of nitrogen dynamics under varying water levels and environmental conditions, providing valuable insights into the patterns of nitrogen migration and transformation in small-scale soil column experiments.
本研究调查了水位和土壤质地对土壤柱内硝酸盐(NO-N)和铵(NH-N)迁移转化的影响。NO-N浓度从初始浓度34.19±0.86mg/L在第70天逐渐降至14.33±0.77mg/L,呈现出受水位和土壤质地影响的波动和迁移。较高水位与较低的NO-N浓度相关,而较低水位则导致浓度升高。细砂土对NO-N的保留和吸附能力最高,其次是中砂和粗砂,突出了土壤质地在硝酸盐迁移和保留中的重要性。方差分析(ANOVA)证实了各土壤柱间pH值、溶解氧和氧化还原电位存在统计学显著差异(p<0.05)。水位波动影响了NO-N的迁移转化,在不同土壤质地中观察到明显的模式。水位波动也影响了NH-N的迁移转化,较高水位与浓度增加相关,较低水位则导致浓度降低。在所考虑的土壤类型中,中砂对NH-N的吸附能力最高。这些发现强调了水位、土壤质地和土壤类型在土壤柱内氮化合物迁移、转化和吸附中的重要作用。研究结果有助于更好地理解不同水位和环境条件下的氮动态,为小规模土壤柱实验中氮迁移和转化模式提供有价值的见解。