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首页> 外文期刊>Global change biology >The influence of time, soil characteristics, and land-use history on soil phosphorus legacies: a global meta-analysis
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The influence of time, soil characteristics, and land-use history on soil phosphorus legacies: a global meta-analysis

机译:时间,土壤特征和土地利用历史对土壤磷的影响:全球荟萃分析

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Agriculturally driven changes in soil phosphorus (P) are known to have persistent effects on local ecosystem structure and function, but regional patterns of soil P recovery following cessation of agriculture are less well understood. We synthesized data from 94 published studies to assess evidence of these land-use legacies throughout the world by comparing soil labile and total P content in abandoned agricultural areas to that of reference ecosystems or sites remaining in agriculture. Our meta-analysis shows that soil P content was typically elevated after abandonment compared to reference levels, but reduced compared to soils that remained under agriculture. There were more pronounced differences in the legacies of past agriculture on soil P across regions than between the types of land use practiced prior to abandonment (cropland, pasture, or forage grassland). However, consistent patterns of soil P enrichment or depletion according to soil order and types of post-agricultural vegetation suggest that these factors may mediate agricultural legacies on soil P. We also used mixed effects models to examine the role of multiple variables on soil P recovery following agriculture. Time since cessation of agriculture was highly influential on soil P legacies, with clear reductions in the degree of labile and total P enrichment relative to reference ecosystems over time. Soil characteristics (clay content and pH) were strongly related to changes in labile P compared to reference sites, but these were relatively unimportant for total P. The duration of past agricultural use and climate were weakly related to changes in total P only. Our finding of reductions in the degree of soil P alteration over time relative to reference conditions reveals the potential to mitigate these land-use legacies in some soils. Better ability to predict dynamics of soil nutrient recovery after termination of agricultural use is essential to ecosystem management following land-use change.
机译:众所周知,由农业驱动的土壤磷(P)的变化对当地生态系统的结构和功能具有持续性影响,但是对农业停止后土壤磷回收的区域模式知之甚少。我们通过比较94个已发表研究的数据,通过比较废弃农业地区的土壤不稳定和总磷含量与农业中剩余的参考生态系统或地点的土壤不稳定度和总P含量,来评估这些土地使用遗产的证据。我们的荟萃分析表明,弃耕后土壤磷含量通常比参考水平要高,但与农业条件下残留的土壤相比,磷含量要低。与过去放弃耕作的土地利用类型(耕地,牧场或草场)相比,过去农业在土壤P上的遗产跨地区的差异更为明显。然而,根据土壤顺序和农业后植被类型的不同,土壤磷富集或枯竭的模式一致,表明这些因素可能介导了农业对土壤磷的影响。我们还使用混合效应模型研究了多个变量对土壤磷恢复的作用跟随农业。自停耕以来的时间对土壤磷的遗传有很大影响,相对于参考生态系统而言,磷的不稳定程度和总磷富集度明显降低。与参考地点相比,土壤特征(粘土含量和pH)与不稳定磷的变化密切相关,但对总磷的影响相对不重要。过去农业使用和气候的持续时间仅与总磷的变化弱相关。我们发现,相对于参考条件,土壤磷的变化程度随时间的推移而降低,这揭示了减轻某些土壤中这些土地利用遗留现象的潜力。终止农业用途后,更好的预测土壤养分恢复动态的能力对于土地用途变化后的生态系统管理至关重要。

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