在关键来源区域的牧场土壤短期浸泡下释放
Janani Palihakkara1, Lucy Burkitt2, Paramsothy Jeyakumar2
1Environmental Sciences Group, School of Agriculture and Environment, Massey University, Palmerston North, 4442, New Zealand; Department of Soil Science, Faculty of Agriculture, University of Peradeniya, Peradeniya, 20400, Sri Lanka.
Journal of environmental management
|January 29, 2025
概括
新西兰的关键来源区域 (CSA) 在频繁降雨期间释放 (P). 最近的土壤对P的释放风险高于可以吸收P的Pallic或Allophanic土壤,这可以吸收P.
科学领域:
- 环境科学 环境科学
- 土壤科学 土壤科学
- 水质管理水质管理
背景情况:
- 关键来源区域 (CSAs) 是表面水中 (P) 的重要贡献者.
- 频繁的降雨事件可能导致CSA土壤中的P释放.
- 短期,频繁的潜水对新西兰CSA中P释放的影响需要进行系统研究.
研究的目的:
- 为了研究三个对比的新西兰农田土壤 (新鲜的,pallic,allophanic) 在短期,频繁的潜水下释放的P潜力.
- 为了在不同类型的土壤中比较孔水和池水中的P释放动态.
- 确定P释放的机制,并评估与CSA不同类型土壤相关的风险.
主要方法:
- 收集了近期土壤,地土壤和地土壤类型的未被干扰的土壤块.
- 模拟了6个短期潜水事件,控制水位.
- 在孔水和池水中测量了溶解反应 (DRP),pH,溶解有机碳和其他水质参数.
- 分析了土壤P分数,并使用热力学建模来理解P矿物动力学.
主要成果:
- 最近的土壤释放了大量的P到孔水和池水中.
- 棕色土壤将P释放到孔水中,但没有显著改变池水 DRP.
- 化土壤吸收了P,减少了DRP在孔水和池水中.
- 沉浸期间的平均池水DRP水平远高于新西兰的目标度.
结论:
- 最近的土壤具有较高的风险,因为在频繁的潜水下释放P,导致P流失到地表水中.
- 性土壤和性土壤显示了保留的潜力,性土壤作为吸附材料.
- 这些发现强调了土壤类型在管理CSAs中的P损失方面的重要性,并表明Allophanic土壤可以减轻P流失.
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