School of Environment, Tsinghua University, Beijing 100084, China.
University of Wuppertal, School of Architecture and Civil Engineering, Institute of Foundation Engineering, Water- and Waste-Management, Laboratory of Soil- and Groundwater-Management, Pauluskirchstraße 7, Wuppertal, 42285, Germany.
Environ Sci Technol. 2020 Dec 1;54(23):14797-14814. doi: 10.1021/acs.est.0c04033. Epub 2020 Nov 2.
Biochar has triggered a black gold rush in environmental studies as a carbon-rich material with well-developed porous structure and tunable functionality. While much attention has been placed on its apparent ability to store carbon in the ground, immobilize soil pollutants, and improve soil fertility, its temporally evolving in situ performance in these roles must not be overlooked. After field application, various environmental factors, such as temperature variations, precipitation events and microbial activities, can lead to its fragmentation, dissolution, and oxidation, thus causing drastic changes to the physicochemical properties. Direct monitoring of biochar-amended soils can provide good evidence of its temporal evolution, but this requires long-term field trials. Various artificial aging methods, such as chemical oxidation, wet-dry cycling and mineral modification, have therefore been designed to mimic natural aging mechanisms. Here we evaluate the science of biochar aging, critically summarize aging-induced changes to biochar properties, and offer a state-of-the-art for artificial aging simulation approaches. In addition, the implications of biochar aging are also considered regarding its potential development and deployment as a soil amendment. We suggest that for improved simulation and prediction, artificial aging methods must shift from qualitative to quantitative approaches. Furthermore, artificial preaging may serve to synthesize engineered biochars for green and sustainable environmental applications.
生物炭作为一种富碳材料,具有发达的多孔结构和可调的功能,在环境研究中引发了一场“黑金热”。虽然人们已经注意到它在土壤中储存碳、固定土壤污染物和提高土壤肥力方面的明显能力,但它在这些作用中的时空演变性能不容忽视。田间应用后,温度变化、降水事件和微生物活动等各种环境因素会导致生物炭的破碎、溶解和氧化,从而使理化性质发生剧烈变化。直接监测添加生物炭的土壤可以提供其时空演变的良好证据,但这需要长期的田间试验。因此,设计了各种人工老化方法,如化学氧化、干湿循环和矿物改性,以模拟自然老化机制。在这里,我们评估了生物炭老化的科学,批判性地总结了老化对生物炭性质的影响,并提供了人工老化模拟方法的最新进展。此外,还考虑了生物炭老化对其作为土壤改良剂的潜在发展和应用的影响。我们建议,为了提高模拟和预测的准确性,人工老化方法必须从定性方法转变为定量方法。此外,人工预老化可以用于合成用于绿色和可持续环境应用的工程生物炭。