College of Resources and Environmental Sciences, China Agricultural University, Beijing, China.
College of Agronomy, Anhui Agricultural University, Hefei, China.
Glob Chang Biol. 2021 Oct;27(20):5356-5367. doi: 10.1111/gcb.15731. Epub 2021 Jul 22.
Enhancing soil organic carbon (SOC) through applying animal manure is of interest for both sustaining cereal production and mitigating greenhouse gas (GHG) emissions. Previous syntheses showed that manuring-induced SOC changes varied substantially with agricultural managements and environmental conditions, while their significance and relative importance to such variability are still largely uncertain. Here, we presented a new synthesis using an updated and balanced database integrating the manuring-induced SOC stock changes and their plausible explanatory factors in 250 observations at global 120 sites. Manure application increased SOC stock by 7.41 ± 1.14 (95% confidence interval, CI) and 8.96 ± 1.83 (95% CI) Mg C ha , respectively, compared to their mineral fertilized (REF-min) and unfertilized (REF-zero) references. Of which approx. 72% and 34% were directly contributed by manure-C input, respectively. Following the IPCC (Intergovernmental Panel on Climate Change) approach, these changes corresponded to the manuring-induced SOC change factors of 1.27 ± 0.04 (95% CI) and 1.40 ± 0.08 (95% CI), respectively. Basing on a balanced database, we identified the amount of manure-C input as the most important factor to the global variations in the resultant SOC stock changes. More importantly, our integrative analysis distinguished the significance of soil properties (e.g., soil pH and initial SOC content) in regulating the efficiency of manure application in enhancing SOC stock. These results indicate that, at the similar rate, applying manure could sequestrate much more carbon in alkaline soils than in neutral and acidic soils. By integrating the impacts of agricultural managements and environmental conditions, our findings would help to develop region-specific tailor-made manure application measures in agriculture and to refine the SOC change factors for regional GHG inventories.
通过施用动物粪便来提高土壤有机碳(SOC)含量,对于维持谷物生产和减少温室气体(GHG)排放都具有重要意义。以前的综合研究表明,施肥引起的 SOC 变化因农业管理和环境条件的不同而有很大差异,但其对这种变异性的意义和相对重要性仍在很大程度上不确定。在这里,我们使用一个经过更新和平衡的数据库,该数据库综合了全球 120 个地点的 250 个观测点中施肥引起的 SOC 储量变化及其可能的解释因素,提出了一个新的综合研究。与矿物施肥(REF-min)和未施肥(REF-zero)对照相比,施用有机肥分别使 SOC 储量增加了 7.41±1.14(95%置信区间,CI)和 8.96±1.83(95% CI)Mg C ha 。其中,约 72%和 34%分别直接归因于有机肥-C 的输入。按照政府间气候变化专门委员会(IPCC)的方法,这些变化分别对应于施肥引起的 SOC 变化因子 1.27±0.04(95% CI)和 1.40±0.08(95% CI)。基于一个平衡的数据库,我们确定有机肥-C 的输入量是导致全球 SOC 储量变化的主要因素。更重要的是,我们的综合分析区分了土壤性质(例如土壤 pH 值和初始 SOC 含量)在调节有机肥应用提高 SOC 储量效率方面的重要性。这些结果表明,在相同的速率下,在碱性土壤中施用有机肥可以固存更多的碳,而在中性和酸性土壤中则较少。通过综合考虑农业管理和环境条件的影响,我们的研究结果将有助于制定特定于区域的农业有机肥应用措施,并为区域 GHG 清单修订 SOC 变化因子。