Gunathunga Samadhi U, Gagen Emma J, Evans Paul N, Erskine Peter D, Southam Gordon
School of Earth & Environmental Sciences, The University of Queensland, St. Lucia 4072, Australia.
School of Earth & Environmental Sciences, The University of Queensland, St. Lucia 4072, Australia.
Sci Total Environ. 2023 Sep 20;892:164515. doi: 10.1016/j.scitotenv.2023.164515. Epub 2023 Jun 1.
The primary solid waste product of surface coal mining is overburden (also known as spoil), the material that is moved to access the underlying coal seams. Once removed, this material is generally stored in large (>100 m in height) piles until it is re-contoured in preparation for post-mining rehabilitation, often remaining there for decades. Under ideal conditions, these new landforms would have at least 30 cm veneer of topsoil applied as a growth medium for plants. However, topsoil deficit conditions are common in coal mines, so the forced use of overburden that possess poor chemical, biological, and physical properties as the growth medium hinders plant establishment. To reach the characteristics of a functional soil that can support plants, it is necessary to dramatically improve spoil quality, i.e., accelerate pedogenesis, as an integral part of the rehabilitation process. For decades, overburden rehabilitation has often taken the traditional approach of using the agricultural practice of fertilizer application or focusing primarily on the types of plants used to stabilize these young landforms. In contrast, success improved when the rehabilitation procedures employed a more holistic approach to establishing self-sustaining plant-soil ecosystems. Here we identify constraints that impede spoil-to-soil transformation, discuss the global treatment options practiced post-mining for coal spoils, and describe how a comprehensive biogeochemical approach can be implemented in spoil reclamation processes going forward. Integrating the revitalization of soil organisms, reclamation of soil chemistry, soil structure, and landform into rehabilitation procedures can accelerate the transformation of coal spoils to functional soils. We believe that a shift in the nature of the question from "what chemicals and seeds should we add to coal spoil during site rehabilitation?" to something fundamentally more specific: "How do we induce pedogenic functions in coal spoils to develop fertile soils?" is needed.
露天煤矿开采产生的主要固体废弃物是表土(也称为废石),即开采煤层时移除的物料。这些物料一旦被移除,通常会被堆积成大型(高度超过100米)的土堆,直至重新整形以准备进行开采后复垦,往往会在那里留存数十年。在理想条件下,这些新形成的地貌会覆盖至少30厘米厚的表土,作为植物生长的介质。然而,表土短缺的情况在煤矿中很常见,因此被迫使用化学、生物和物理性质较差的表土作为生长介质会阻碍植物的生长。为了使土壤具备支持植物生长的功能特性,有必要大幅提高废石质量,即加速土壤形成过程,这是复垦过程中不可或缺的一部分。几十年来,表土复垦通常采用传统方法,即施用化肥或主要关注用于稳定这些新形成地貌的植物种类。相比之下,当复垦程序采用更全面的方法来建立自我维持的植物 - 土壤生态系统时,成功率会提高。在这里,我们确定了阻碍废石向土壤转化的限制因素,讨论了全球范围内煤矿废石开采后采用的处理方法,并描述了如何在未来的废石复垦过程中实施综合生物地球化学方法。将土壤生物的复苏、土壤化学、土壤结构和地形的复垦整合到复垦程序中,可以加速煤矿废石向功能性土壤的转化。我们认为,问题的性质需要从“在场地复垦期间,我们应该向煤矿废石中添加哪些化学物质和种子?”转变为更具根本性的具体问题:“我们如何诱导煤矿废石中的成土功能以形成肥沃的土壤?”