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Young calcareous soil chronosequences as a model for ecological restoration on alkaline mine tailings

机译:青年石灰质土壤时间序列作为碱性矿山尾矿生态恢复的模型

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摘要

Tailings are artificial soil-forming substrates that have not been created by the natural processes of soil formation and weathering. The extreme pH environment and corresponding low availability of some macro- and rnicronutrients in alkaline tailings, coupled with hostile physical and geochemical conditions, present a challenging environment to native biota. Some significant nutritional constraints to ecosystem reconstruction on alkaline tailings include i) predominant or complete absence of combined nitrogen (N) and poor soil N retention; ii) the limited bioavailability of some rnicronutrients at high soil pH (e.g., Mn, Fe, Zn and Cu); and iii) potentially toxic levels of biologically available soil phosphorus (P) for P-sensitive plants. The short regulatory time frames (years) for mine closure on tailings landforms are at odds with the long time required for natural pedogenic processes to ameliorate these factors (thousands of years). However, there are similarities between the chemical composition and nutrient status of alkaline tailings and the poorly-developed, very young calcareous soils of biodiverse regions such as southwestern Australia We propose that basic knowledge of chronosequences that start with calcareous soils may provide an informative model for understanding the pedogenic processes required to accelerate soil formation on tailings. Development of a functional, stable root zone is crucial to successful ecological restoration on tailings, and three major processes should be facilitated as early as possible during processing or in the early stages of restoration to accelerate soil development on alkaline tailings: i) acidification of the upper tailings profile; ii) establishment of appropriate and resilient microbial communities; and iii) the early development of appropriate pioneer vegetation. Achieving successful ecological restoration outcomes on tailings landforms is likely one of the greatest challenges faced by restoration ecologists and the mining industry, and successful restoration on alkaline tailings likely depends upon careful management of substrate chemical conditions by targeted amendments.
机译:尾矿是人工形成土壤的基质,不是由土壤形成和风化的自然过程产生的。极端的pH环境以及碱性尾矿中某些大量和微量元素的相应利用率较低,再加上不利的物理和地球化学条件,给原生生物群带来了充满挑战的环境。碱性尾矿对生态系统重建的一些重要营养限制包括:i)氮的主要或完全缺乏和土壤氮的保留能力差; ii)在土壤高pH下某些微量营养素(例如Mn,Fe,Zn和Cu)的生物利用度有限; iii)对P敏感植物的生物可利用的土壤磷(P)的潜在毒性水平。在尾矿地貌上关闭矿山的短期监管时间框架(年)与自然成岩过程改善这些因素所需的长时间(数千年)不一致。但是,碱性尾矿的化学成分和养分状况与西南澳大利亚等生物多样性地区的欠发达,非常年轻的钙质土壤之间存在相似之处。我们建议,从钙质土壤开始的时间序列基础知识可以为了解加快尾矿上土壤形成所需的成岩过程。开发功能性,稳定的根区对于尾矿生态修复的成功至关重要,应在加工过程中或恢复的早期阶段促进三个主要过程,以加快碱性尾矿的土壤发育:i)酸化尾矿。上尾矿剖面; ii)建立适当和有弹性的微生物群落; iii)早期开发适当的先锋植被。在尾矿地貌上实现成功的生态恢复结果可能是恢复生态学家和采矿业面临的最大挑战之一,而在碱性尾矿上成功进行恢复可能取决于对目标化学物的有针对性的修正,以对其进行认真的管理。

著录项

  • 来源
    《The Science of the Total Environment》 |2017年第31期|168-175|共8页
  • 作者

    Adam T. Cross; Hans Lambers;

  • 作者单位

    Centre for Mine Site Restoration, Department of Environment and Agriculture, Curnn University, CPO Box U1987, Bentiey, WA 6102, Perth, Australia,School of Biological Sciences, The University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Perth, Australia,Kings Park and Botanic Garden, Kings Park, WA 6005, Perth, Australia;

    Centre for Mine Site Restoration, Department of Environment and Agriculture, Curnn University, CPO Box U1987, Bentiey, WA 6102, Perth, Australia;

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

    Pedogenesis; Mine tailings; Soil acidification; Soil weathering; Plant mineral nutrition;

    机译:成岩作用;矿山尾矿;土壤酸化;土壤风化;植物矿物质营养;

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