当前位置: X-MOL 学术Eur. J. Soil Sci. › 论文详情
Our official English website, www.x-mol.net, welcomes your feedback! (Note: you will need to create a separate account there.)
13C methodologies for quantifying biochar stability in soil: A critique
European Journal of Soil Science ( IF 4.2 ) Pub Date : 2022-05-09 , DOI: 10.1111/ejss.13245
Phillip Chalk 1 , Christopher Smith 2
Affiliation  

Methodologies based on 13C-enrichment (E), 13C-depletion (D) and 13C-natural abundance (NA) to estimate the stability of biochar in soil were critically examined. The stability of 13C-enriched biochar can be estimated by the quantitative recovery of excess 13C, either in the soil or in evolved CO2. Both approaches have advantages and disadvantages. Recovery in the soil is a measure of both residual biochar 13C + 13C immobilised in soil organic matter during biochar decomposition. Variable proportions of organic- and inorganic-C are present in alkaline biochars, and few data exist on the uniformity of labelling, which is a basic requirement of the respired 13CO2 and E methodology. The E technique has had limited application due to the cost and difficulty of obtaining a uniformly-enriched feedstock through continuous labelling of plants with 13CO2 at a constant 13C enrichment. In contrast, the NA technique has been widely applied. The NA and D techniques are in situ methods that involve the addition of C4-derived biochar to a C3-soil or vice versa. Stability is estimated by a two-end-member mixing model that allows the proportion of evolved CO2 derived from the biochar (Cdfb) to be estimated. The mixing model has recently been misused to estimate the Cdfb of 13C-enriched biochar, with 13C-abundance expressed as erroneously large δ values. 13C-based methods provide a yardstick against which rapid stability tests should be evaluated. While numerous laboratory incubation comparisons have been conducted, very few field-based data have been published.

中文翻译:

用于量化土壤中生物炭稳定性的 13C 方法:批评

对基于13 C-富集 ( E )、13 C-消耗 ( D ) 和13 C-自然丰度 ( NA ) 的方法来估计土壤中生物炭的稳定性进行了严格检查。富含13 C 的生物炭的稳定性可以通过定量回收土壤中或释放的 CO 2中的过量13 C 来估计。两种方法都有优点和缺点。土壤中的恢复是衡量残留 biochar 13 C +  13生物炭分解过程中固定在土壤有机质中的 C。碱性生物炭中存在不同比例的有机碳和无机碳,很少有关于标记一致性的数据,这是呼吸13 CO 2E方法的基本要求。由于通过在恒定的13 C 富集下用13 CO 2连续标记植物来获得均匀富集的原料的成本和困难, E技术的应用有限。相比之下,NA技术已被广泛应用。NAD _技术是原位方法,包括将 C 4衍生的生物炭添加到 C 3土壤中,反之亦然。稳定性通过一个两端成员混合模型来估计,该模型允许估计源自生物炭 (Cdfb)的演化 CO 2的比例。混合模型最近被滥用来估计富含 13 C 的生物炭的 Cdfb 其中13 C 丰度表示为错误的大δ值。13基于 C 的方法提供了一个衡量快速稳定性测试的标准。虽然已经进行了许多实验室孵化比较,但很少有基于现场的数据发表。
更新日期:2022-05-09
down
wechat
bug