College of Water Resource, Shenyang Agricultural University, Shenyang, Liaoning 110866, PR China.
College of Water Resource, Shenyang Agricultural University, Shenyang, Liaoning 110866, PR China.
Sci Total Environ. 2024 May 20;926:172172. doi: 10.1016/j.scitotenv.2024.172172. Epub 2024 Apr 2.
To improve the retention and slow-release abilities of nitrogen (N) and phosphorus (P), an 82 %-purity struvite fertilizer (MAP-BC) was synthesized using magnesium-modified biochar and a solution with a 2:1 concentration ratio of NH to PO at a pH of 8. Batch microscopic characterizations and soil column leaching experiments were conducted to study the retention and slow-release mechanisms and desorption kinetics of MAP-BC. The slow-release mechanism revealed that the dissolution rate of high-purity struvite was the dominant factor of NP slow release. The re-adsorption of NH and PO by biochar and unconsumed MgO prolonged slow release. Mg ionized by MgO could react with PO released from struvite to form Mg(PO). The internal biochar exhibited electrostatic attraction and pore restriction towards NH, while magnesium modification and nutrient loading formed a physical antioxidant barrier that ensured long-term release. The water diffusion experiment showed a higher cumulative release rate for PO compared to NH, whereas in soil column leaching, the trend was reversed, suggesting that soil's competitive adsorption facilitated the desorption of NH from MAP-BC. During soil leaching, cumulative release rates of NH and PO from chemical fertilizers were 3.55-3.62 times faster than those from MAP-BC. The dynamic test data for NH and PO in MAP-BC fitted the Ritger-Peppas model best, predicting release periods of 163 days and 166 days, respectively. The leaching performances showed that MAP-BC reduced leaching solution volume by 5.58 % and significantly increased soil large aggregates content larger than 0.25 mm by 24.25 %. The soil nutrients retention and pH regulation by MAP-BC reduced leaching concentrations of NP. Furthermore, MAP-BC significantly enhanced plant growth, and it is more suitable as a NP source for long-term crops. Therefore, MAP-BC is expected to function as a long-term and slow-release fertilizer with the potential to minimize NP nutrient loss and replace part of quick-acting fertilizer.
为了提高氮(N)和磷(P)的保留和缓释能力,使用镁改性生物炭和 NH 与 PO 的浓度比为 2:1、pH 值为 8 的溶液合成了纯度为 82%的鸟粪石肥料(MAP-BC)。通过批处理微观特性分析和土柱淋溶实验,研究了 MAP-BC 的保留和缓释机制及解吸动力学。缓释机制表明,高纯度鸟粪石的溶解速率是 NP 缓慢释放的主要因素。生物炭对 NH 和 PO 的再吸附以及未消耗的 MgO 延长了缓慢释放。MgO 电离出的 Mg 可与鸟粪石释放的 PO 反应生成 Mg(PO)。内部生物炭对 NH 表现出静电吸引和孔限制作用,而镁改性和养分加载形成物理抗氧化屏障,确保了长期释放。水扩散实验表明,PO 的累积释放率高于 NH,而在土柱淋溶中,趋势相反,表明土壤的竞争吸附促进了 MAP-BC 中 NH 的解吸。在土壤淋溶过程中,MAP-BC 中 NH 和 PO 的累积释放速率比化肥快 3.55-3.62 倍。MAP-BC 中 NH 和 PO 的动态测试数据最符合 Ritger-Peppas 模型,分别预测释放期为 163 天和 166 天。淋溶性能表明,MAP-BC 减少了 5.58%的淋溶溶液体积,显著增加了大于 0.25mm 的土壤大团聚体含量 24.25%。MAP-BC 对土壤养分的保留和 pH 调节降低了 NP 的淋溶浓度。此外,MAP-BC 显著促进了植物的生长,更适合作为长期作物的 NP 源。因此,MAP-BC 有望成为一种长效、缓释肥料,可最大限度地减少 NP 养分损失,并替代部分速效肥料。