在基于土壤柱实验的红树林土壤中对有机酸迁移和转化的模拟
Xinyu Liu1, Yunan Yang2, Yangang Lin1
1School of Space and Earth Sciences, Beihang University, Beijing, 100191, China.
Scientific reports
|March 12, 2025
概括
池土壤有机酸在红树林湿地不同迁移. 酸缩在30-50厘米深处,而其他酸则沉或被中和,微生物活动影响了这一过程.
科学领域:
- 环境科学 环境科学
- 土壤科学 土壤科学
- 微生物学 微生物学
背景情况:
- 对于陆地植物来说,未分解的有机物质的直接应用并不常见.
- 池排放出口通常具有高有机物质含量.
研究的目的:
- 研究在红树林湿地土壤中有机酸和相关微生物的迁移和转化.
- 用实验室土壤柱和HYDRUS-1D模型来模拟这些过程.
主要方法:
- 实验室土壤柱实验模拟红树林湿地条件.
- 使用HYDRUS-1D模型进行有机酸运输的数值模拟.
- 分析不同土壤深度的有机酸度和微生物社区动态.
主要成果:
- 氧化酸水平在深度上稳定;酸垂直向下移动.
- 酸度在30-50厘米深度之间增加.
- 有机酸形成沉物,导致在18天内在更深层 (40-50厘米) 的土壤层中完全中和.
- 产生酸的细菌Acinetobacter Johnsonii在无氧酸化过程中增加,但在添加氧化后减少.
- 液体-1D模拟表明有机酸的吸附,沉积和运输很差,与实验结果一致.
结论:
- 在红树林土壤中有机酸的行为是复杂的,受深度,化学降水和微生物活动的影响.
- 这项研究为管理沿海生态系统中池排放的有机物提供了有价值的数据.
- 模型模拟证实了实验观测,增强了对湿地土壤中的有机酸命运的理解.
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