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Critical review on soil phosphorus migration and transformation under freezing-thawing cycles and typical regulatory measurements

机译:冻融循环下土壤磷迁移和转化的批判性综述及典型调节测量

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摘要

Freezing-thawing period plays an important role in the soil nutrient cycling. The frequency of freezing-thawing cycles (FTCs) can directly affect the supply of effective soil nutrients, further influences the growth and development of crops. Phosphorus is one of the essential nutrients for crop growth, and almost no compounds in gas form in nature, which is non-renewable resources. In modern agricultural production, phosphorus required by plants is mainly from the soil, but the utilization rate of phosphorus fertilizer in soil is generally only 10%-25%. Therefore, it is of great significance to study phosphorus migration and transformation behavior of soil in the non-growth period and related interfacial processes for improving the utilization efficiency of phosphorus fertilizer, increasing crop yield, reducing excessive application of phosphorus fertilizer, and subsiding environmental pollution. This paper systematically concludes key interfacial process of soil phosphorus in freezing-thawing soil system and relative mechanisms describing migration and transformation behavior of soil phosphorus. Besides, it summarizes the mediating effects of widely used soil conditioner on phosphorus cycling. The results show that freezing- thawing will destroy the structure of the soil, causing phosphorus to migrate along with runoff, soil water and heat movement. It also affects the types of microorganisms, the activity of microbial communities and the oxidation-reduction reaction of related minerals, making the phosphorus in soil from an unstable form to an active form. Biochar and humic substances can improve the physical and chemical properties of the soil, and have favorable effects on soil during freezing-thawing period. This review has important significance for the rational utilization of existing phosphorus resources, the maintenance of soil phosphorus cycle balance and the sustainable development of agriculture, meanwhile, has guiding significance for the reasonable utilization of agricultural wastes.
机译:冷冻后期在土壤养分循环中起着重要作用。冻融循环循环(FTCS)的频率可以直接影响有效的土壤营养素的供应,进一步影响作物的生长和发育。磷是作物生长的基本营养素之一,并且在自然界中几乎没有气体形式的化合物,这是不可再生的资源。在现代农业生产中,植物所需的磷主要来自土壤,但土壤中磷肥的利用率通常仅为10%-25%。因此,在非生长期和相关界面过程中研究土壤的磷迁移和转化行为具有重要意义,提高磷肥的利用效率,增加作物产量,减少磷肥的过度适用,以及消退环境污染。本文系统地结束了冰川土壤系统中土壤磷的关键界面过程及描述土壤磷的迁移和转化行为的相对机制。此外,它总结了广泛使用的土壤调节剂对磷循环的调解作用。结果表明,冻融将破坏土壤的结构,导致磷迁移以及径流,土壤水和热运动。它还影响微生物的类型,微生物群落的活性以及相关矿物的氧化还原反应,使土壤中的磷从不稳定的形式到活性形式。生物炭和腐殖质物质可以改善土壤的物理和化学性质,并在冻融期间对土壤具有良好影响。本综述对现有磷资源的合理利用具有重要意义,对土壤磷循环平衡和农业可持续发展的维护,同时对农业废物合理利用的指导意义。

著录项

  • 来源
    《The Science of the Total Environment》 |2021年第10期|141614.1-141614.14|共14页
  • 作者

    Ying Zhao; Yuelei Li; Fan Yang;

  • 作者单位

    Joint Laboratory of Northeast Agricultural University and Max Planck Institute of Colloids and Interfaces (NEAU-MPICI). Harbin 150030 China School of Water Conservancy & Civil Engineering Northeast Agricultural University Harbin 150030 China;

    Joint Laboratory of Northeast Agricultural University and Max Planck Institute of Colloids and Interfaces (NEAU-MPICI). Harbin 150030 China School of Water Conservancy & Civil Engineering Northeast Agricultural University Harbin 150030 China;

    Joint Laboratory of Northeast Agricultural University and Max Planck Institute of Colloids and Interfaces (NEAU-MPICI). Harbin 150030 China School of Water Conservancy & Civil Engineering Northeast Agricultural University Harbin 150030 China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Phosphorus; Freezing-thawing; Migration and transformation; Interfacial process; Regulatory effect;

    机译:磷;冷冻解冻;迁移和转型;界面过程;监管效果;

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