Liu Xinyu, Yang Yunan, Lin Yangang
School of Space and Earth Sciences, Beihang University, Beijing, 100191, China.
Sci Rep. 2025 Mar 11;15(1):8354. doi: 10.1038/s41598-025-91771-w.
The practice of directly applying unfermented and decomposed organic matter to plants is rare in the growth process of terrestrial plants. The organic matter content at the discharge outlet of shrimp ponds is usually high. Therefore, it is necessary to collect soil from the discharge outlet of shrimp ponds and simulate the migration and transformation pathways of organic acids and related metabolic microorganisms in soil of mangrove wetlands through laboratory soil columns and the HYDRUS-1D model. Results showed that the content of oxalic acid remained relatively stable in the soil column at different depths, citric acid settled downward along the vertical direction, the concentration of acetic acid in the depth range of 30-50 cm increased. The organic acids formed insoluble or slightly soluble precipitates in the form of organic acid calcium, the organic acids in 40-50 cm were completely neutralized on the 18th day. The abundance of acid-producing Acinetobacter Johnsonii increased during the later stages of anaerobic acidification and disappeared after the addition of Ca(OH). The results of HYDRUS-1D simulation showed that the adsorption, deposition and transport of organic acids in the mangrove wetland were poor, the results of vertical infiltration modelling were in agreement with the soil column experiments.
在陆生植物的生长过程中,直接将未发酵和分解的有机物施用于植物的做法很少见。虾塘排水口处的有机物含量通常较高。因此,有必要从虾塘排水口采集土壤,并通过实验室土壤柱和HYDRUS-1D模型模拟红树林湿地土壤中有机酸及相关代谢微生物的迁移转化途径。结果表明,草酸在不同深度的土壤柱中含量相对稳定,柠檬酸沿垂直方向向下沉降,30-50厘米深度范围内乙酸浓度增加。有机酸以草酸钙的形式形成不溶性或微溶性沉淀,40-50厘米处的有机酸在第18天完全中和。产酸约翰逊不动杆菌的丰度在厌氧酸化后期增加,添加Ca(OH)₂后消失。HYDRUS-1D模拟结果表明,有机酸在红树林湿地中的吸附、沉积和迁移较差,垂直入渗模拟结果与土壤柱实验结果一致。