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首页> 外文期刊>Soil Science Society of America Journal >Phosphorus Loss Potential and Phosphatase Activity under Phosphorus Fertilization in Long-Term Paddy Wetland Agroecosystems
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Phosphorus Loss Potential and Phosphatase Activity under Phosphorus Fertilization in Long-Term Paddy Wetland Agroecosystems

机译:长期稻田湿地农业生态系统施磷条件下的磷损失势和磷酸酶活性

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Phosphorus fertilization may lead to increased P runoff and leaching, contributing to surface water and groundwater pollution. Plots of a 25-yr field study in subtropical China representing eight P fertilization treatments were sampled to determine the effects of P fertilization on P loss potential and correlations among soil test P, soil neutral phosphatase activity, and water P content. Phosphorus fertilization increased soil test P and neutral phosphatase activity in the plow layer compared with P-free fertilization. Total P content of paddy surface water increased with P fertilization, from <0.01 to 0.35 mg L(-1). Phosphorus fertilization created P runoff loss risk, especially with the combined application of both inorganic fertilizers and organic amendments. The P runoff loss potential could be reduced or avoided by utilizing physical barriers on field margins to reduce or eliminate runoff. Soil neutral phosphatase activity, soil test P in the 0- to 5-cm layer, and surface water P content were significantly and positively correlated. Soil neutral phosphatase activity contributed to soil test P and the potential of P runoff loss. Fertilization did not affect soil test P or neutral phosphatase activity beneath the plow layer or total P of paddy groundwater at the 100-cm depth. The P content of paddy groundwater was not related to that of surface water, indicating that downward movement of P and P leaching did not occur. The results suggest that paddy wetland ecosystems can store P with proper management, especially for organic amendments.
机译:磷肥可能导致磷流失和淋溶增加,导致地表水和地下水污染。在中国亚热带地区进行的为期25年的田间研究的地块(代表8种磷肥处理)被采样,以确定磷肥对磷损失潜力的影响以及土壤试验磷,土壤中性磷酸酶活性和水分P含量之间的相关性。与无磷肥料相比,磷肥提高了耕作层的土壤试验磷和中性磷酸酶活性。稻田地表水的总磷含量随施磷量的增加而增加,从<0.01增加到0.35 mg L(-1)。磷肥造成磷径流损失的风险,特别是在无机肥料和有机改良剂共同施用的情况下。通过利用场边界上的物理屏障来减少或消除径流,可以减少或避免P径流损失的可能性。土壤中性磷酸酶活性,0至5 cm层中的土壤测试P和地表水P含量均呈显着正相关。土壤中性磷酸酶活性有助于土壤测试磷和磷径流损失的潜力。施肥不会影响耕作层下的土壤试验磷或中性磷酸酶活性,也不会影响100 cm深度的水稻地下水的总磷。稻田地下水的磷含量与地表水无关,表明磷和磷的浸出并未发生向下运动。结果表明,稻田湿地生态系统可以通过适当的管理来储存磷,特别是对于有机改良剂。

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