Instituto de Recursos Naturales y Agrobiología de Sevilla, Consejo Superior de Investigaciones Científicas (IRNAS-CSIC), Reina Mercedes Av. 10, 41012 Seville, Spain.
Instituto de Recursos Naturales y Agrobiología de Sevilla, Consejo Superior de Investigaciones Científicas (IRNAS-CSIC), Reina Mercedes Av. 10, 41012 Seville, Spain.
Sci Total Environ. 2018 Feb 1;613-614:969-976. doi: 10.1016/j.scitotenv.2017.09.124. Epub 2017 Sep 26.
The effects of aging on biochar (BC) properties, composition and carbon sequestration are still under debate. This study aimed at illustrating the qualitative alterations of five different BCs aged during a 24-month field experiment located in Southwest Spain. To determine the recalcitrance of each BC, physical fragmentation test, scanning electron microscopy, C NMR spectroscopy and CO-respiration experiments were performed. The physical fragmentation values of all types of BC increased significantly over time at field conditions. FESEM examinations of aged BCs showed collapsed structures and the presence of entrapped soil material and microbial mats into the BC pores. The C NMR spectroscopy demonstrated an increase of the relative abundance of O-alkyl C and alkyl C at expenses of aromatic-C in aged BCs. The C losses of all BCs ranged from 27% to 11% of the initial C. In contrast, the nitrogen (N) content of wood-derived BCs significantly increased probably due to the sorption of nitrogen containing compounds into these highly-porous weathered chars. With the exception of that for the sewage sludge-BC, the pH of all aged BCs decreased from >9 to the soil pH, indicating a short lasting of the liming effect caused by BC addition. The respiration experiment revealed that BC recalcitrance was much lower than expected and, within the range of decades. Only wood-derived BCs significantly increased the mean residence time of the slow C pool of the Cambisol by factors between 3.4 and 7.7. Mediterranean climate conditions and the characteristics of the Cambisol used probably accelerated the microbial degradation of BCs.
衰老对生物炭(BC)性质、组成和碳固存的影响仍存在争议。本研究旨在说明在位于西班牙西南部的为期 24 个月的田间实验中,五种不同 BC 的定性变化。为了确定每种 BC 的抗降解性,进行了物理破碎测试、扫描电子显微镜、C NMR 光谱和 CO 呼吸实验。在田间条件下,所有类型的 BC 的物理破碎值随时间显著增加。老化 BC 的 FESEM 检查显示出坍塌的结构,以及土壤物质和微生物垫被捕获到 BC 孔中的情况。C NMR 光谱表明,在老化的 BC 中,O-烷基 C 和烷基 C 的相对丰度增加,而芳香族-C 的相对丰度减少。所有 BC 的 C 损失范围为初始 C 的 27%至 11%。相比之下,木质素衍生的 BC 的氮(N)含量显著增加,可能是由于含氮化合物被吸附到这些高度多孔的风化炭中。除了污水污泥-BC 外,所有老化的 BC 的 pH 值均从>9 降至土壤 pH 值,表明 BC 添加引起的石灰化作用持续时间很短。呼吸实验表明,BC 的抗降解性远低于预期,并且在几十年的范围内。只有木质素衍生的 BC 显著增加了 Cambisol 慢碳库的平均停留时间,因子在 3.4 到 7.7 之间。地中海气候条件和所用 Cambisol 的特性可能加速了 BC 的微生物降解。