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磷素供应和植物会改变土壤氮素的保持和损失。

Phosphorus availability and plants alter soil nitrogen retention and loss.

机构信息

Sydney Institute of Agriculture, School of Life and Environmental Sciences, The University of Sydney, 380 Werombi Rd, Brownlow Hill, NSW 2570, Australia.

Sydney Institute of Agriculture, School of Life and Environmental Sciences, The University of Sydney, 380 Werombi Rd, Brownlow Hill, NSW 2570, Australia.

出版信息

Sci Total Environ. 2019 Jun 25;671:786-794. doi: 10.1016/j.scitotenv.2019.03.422. Epub 2019 Mar 28.

Abstract

Availability of phosphorus (P) can directly and/or indirectly affect nitrogen (N) retention and loss from soil by stimulating microbial and plant root activities. However, it is not clear how P availability and plant presence interact on nitrous oxide (NO) emission and nitrate (NO) leaching in soil. A mesocosm experiment was conducted to investigate the effect of P addition (0, 10 and 20 mg P kg) with and without plant presence (Phalaris aquatica, C3 grass) on NO emission, NO leaching and N recovery. Our results showed large variation in NO emission with significant increases after leaching events. We observed that initially low but later (after 53 days of sowing) high levels of P addition increased NO emission rates, possibly by stimulating nitrifiers and/or denitrifiers in soil. Plant presence decreased NO emission at times when plants reduced water and NO in the soil, but increased NO emission at times when both water and NO in the soil were abundant, and where plants may have stimulated denitrification through supply of labile organic C. Furthermore, an increase in net N mineralization, possibly due to increased decomposition stimulated by root derived C, may also have contributed to the higher cumulative NO emission with plant presence. P addition increased N recovery in soil, but reduced it in leachates, suggesting increased N fixation in microbial biomass. Our results showed that both P addition and plant presence stimulated N loss as NO, but also increased N retention in the soil-plant system and thus reduced N loss through leaching.

摘要

磷 (P) 的有效性可通过刺激微生物和植物根系活动,直接和/或间接影响土壤中氮 (N) 的保留和损失。然而,目前尚不清楚 P 的有效性和植物的存在如何影响土壤中一氧化二氮 (NO) 的排放和硝酸盐 (NO) 的淋失。本中尺度实验研究了添加磷 (0、10 和 20mg P kg) 以及是否存在植物 (水生雀稗,C3 草) 对 NO 排放、NO 淋失和 N 回收的影响。结果表明,NO 排放存在较大的变化,淋溶事件后有明显的增加。我们观察到,最初低但后来 (播种后 53 天) 高浓度的 P 添加增加了 NO 排放速率,可能是通过刺激土壤中的硝化作用和/或反硝化作用。当植物减少土壤中的水分和 NO 时,植物的存在会降低 NO 的排放,但当土壤中的水分和 NO 都很丰富时,植物会通过供应易分解的有机 C 来增加 NO 的排放,此时植物的存在会增加 NO 的排放。此外,由于根衍生的 C 刺激的分解增加,可能会导致净 N 矿化增加,这也可能导致植物存在时累积的 NO 排放增加。P 添加增加了土壤中的 N 回收,但减少了淋出液中的 N 回收,这表明微生物生物量中的 N 固定增加。我们的结果表明,P 添加和植物的存在都刺激了作为 NO 的 N 损失,但也增加了土壤-植物系统中的 N 保留,从而减少了通过淋失的 N 损失。

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