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首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Vertical distribution and regulation of Olsen-phosphorus in 6-m soil profiles after farmland-to-apple orchard conversion on the Chinese Loess Plateau
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Vertical distribution and regulation of Olsen-phosphorus in 6-m soil profiles after farmland-to-apple orchard conversion on the Chinese Loess Plateau

机译:中国黄土高原农田对苹果园6米土壤剖面综合分布与调节

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摘要

Data on the dynamics of Olsen-P in deep soil profiles are crucial for improving P use efficiency but remain scarce worldwide. Hence, we sampled sixty 6-m-deep soil profiles from farmland and in 8-yr, 17-yr, and 25-yr-old apple orchards on China's Loess Plateau, and aimed to investigate the vertical distribution of soil Olsen-P following the farmland-to apple orchard conversion. Land-use change from farmland to apple orchard significantly affected Olsen-P at 0-40 cm soil, with the concentration generally increasing with age of apple orchard. By contrast, Olsen-P at 40-600 cm was not significantly different among the cropping systems. In both farmland and apple orchards, the concentration of Olsen-P decreased at 40-100 cm, compared with that in the 0-40 cm layer, increased with depth from 100 to 400 cm and then stabilized from 400 to 600 cm. The highest accumulation of residual soil Olsen-P in the 6-m profile (RSP0-600) was in the 25-yr orchard, followed by the 17-yr and 8-yr orchards, with the lowest accumulation in farmland. The differences in RSP0-600 cm were primarily associated with RSP0-100 cm, which was significantly positively related to the accumulative application of P fertilizer. The change point in soil Olsen-P against P leaching was 71.2 mg kg(-1), but in farmland and 8-yr, 17-yr, and 25-yr apple orchards, the averaged-depth contents of Olsen-P were all below the critical value, indicating no P leaching risk. Regression analysis revealed that the vertical distribution of soil Olsen-P was regulated by P fertilization at 0-100 cm and by crop roots at 100-600 cm, irrespective of cropping system. The insights gained on Olsen-P accumulation and migration within deep soil profiles after the farmland-to-apple orchard conversion can help to optimize land use and P fertilization management in major apple-producing countries with burgeoning growth in apple production.
机译:关于深层土壤剖面中奥尔森磷动态的数据对于提高磷的利用效率至关重要,但在世界范围内仍然缺乏。因此,我们在中国黄土高原的农田和8年、17年和25年生苹果园中取样了60个6米深的土壤剖面,旨在调查农田转苹果园后土壤Olsen-P的垂直分布。从农田到苹果园的土地利用变化对0-40cm土壤中的Olsen-P有显著影响,其浓度一般随苹果园年龄的增加而增加。相比之下,40-600厘米处的Olsen-P在不同种植制度之间没有显著差异。在农田和苹果园中,Olsen-P的浓度在40-100cm处降低,在0-40cm处降低,在100-400cm处随深度增加,然后在400-600cm处稳定。在6米剖面(RSP0-600)中,残留土壤Olsen-P的最高累积量在25年果园,其次是17年和8年果园,农田中的累积量最低。RSP0-600cm的差异主要与RSP0-100cm有关,与累积施用磷肥显著正相关。土壤中Olsen-P对P淋失的变化点为71.2 mg kg(-1),但在农田和8年、17年和25年苹果园中,Olsen-P的平均深度含量均低于临界值,表明没有P淋失风险。回归分析表明,无论种植制度如何,土壤Olsen-P的垂直分布均受0-100cm施磷量和100-600cm作物根系的调控。在农田转为苹果园后,对Olsen-P在深层土壤剖面中积累和迁移的深入了解有助于在苹果产量迅速增长的主要苹果生产国优化土地利用和磷施肥管理。

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