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Oxidation is Key for Black Carbon SurfaceFunctionality and Nutrient Retention in AmazonAnthrosols

机译:氧化是亚马逊炭黑表面活性炭和养分保留的关键

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Aims: Soil black carbon (BC) has been shown to possess large amounts of cation exchange sites and surface charge, and is viewed as a potential soil amendment to improve nutrient retention and for pollutant remediation. This study investigated the nano-scale distribution of reactive functional groups and the binding of cations on the surface of micron-size BC particles, identified the key processes, and explored the sources of surface functionality and their relative contribution to cation exchange capacity (CEC). Materials and Methods: Elemental microprobe and synchrotron-based Scanning Transmission X-ray Spectromicroscopy (STXM) coupled with Near Edge X-ray Absorption Fine Structure (NEXAFS) spectroscopy were used for nano-scale mapping of cations and reactive functional groups, and further distinction of the sources of reactive functional groups generated either by oxidation of BC surfaces or by adsorption of non-BC organic matter onto the BC surfaces. Their respective contribution to cation adsorption was obtained using a depth profile of a BC-rich Anthrosol from the central Amazon, Brazil. Results and Discussion: Adsorption of Non-BC organic matter is more dominant on the surface of BC particle in topsoil as evidenced by a stronger signal of microbial biomass and humic substances extracts. In comparison, a greater level of oxidation was found on the outerlayer of BC particles in subsoil horizons. Organic C in subsoils was found to generate 23-42% more CEC per unit C than topsoil. Based on CEC per unit C, the capacity of BC in creating CEC was 6-7 times higher than Non-BC, and the BC in deeper horizons had up to 20% higher CEC than the topsoil horizon. Near BC surfaces, higher ratios of Ca/C and K/C in subsoil than topsoil horizons reinforce the observation that BC in subsoil horizons had a higher capacity in binding cations and creating CEC than in the topsoil horizon. Conclusions: Oxidation of BC is suggested to be more efficient and important for creating CEC than the adsorption of non-BC onto BC surfaces, thus identified as being key for BC surface functionality and nutrient retention in Amazon Anthrosols.
机译:目的:已证明土壤黑碳(BC)具有大量的阳离子交换位点和表面电荷,被视为潜在的土壤改良剂,可改善养分保持力并修复污染物。这项研究调查了反应性官能团的纳米级分布以及微米级BC颗粒表面上阳离子的结合,确定了关键过程,并探讨了表面官能度的来源及其对阳离子交换能力(CEC)的相对贡献。材料和方法:元素微探针和基于同步加速器的扫描透射X射线光谱(STXM)结合近边缘X射线吸收精细结构(NEXAFS)光谱用于阳离子和反应性官能团的纳米级标测,并进一步区分通过BC表面的氧化或通过将非BC有机物质吸附到BC表面上而产生的反应性官能团的来源。它们各自对阳离子吸附的贡献是使用来自巴西中部亚马逊的富含BC的Anthrosol的深度曲线获得的。结果与讨论:表层土壤中BC颗粒表面非BC有机物的吸附更为明显,这是由微生物生物量和腐殖质提取物的较强信号所证明的。相比之下,在地下土壤层中,BC颗粒的外层发现了更高水平的氧化。发现底土中的有机碳每单位C产生的CEC比表土高23-42%。基于每单位C的CEC,BC产生CEC的能力是Non-BC的6-7倍,而在较深层的BC的CEC则比表土层高出20%。在BC表层附近,地下土壤中Ca / C和K / C的比例高于表层土壤,这表明以下观点:地下土壤中的BC具有比阳离子表层更高的结合阳离子和产生CEC的能力。结论:与将非BC吸附到BC表面相比,BC的氧化被认为对创建CEC更为有效和重要,因此被确定为BC表面功能和养分在亚马逊人烟中的关键。

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