当前位置: X-MOL 学术Earth Syst. Sci. Data › 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.)
An investigation of the global uptake of CO2 by lime from 1963 to 2020
Earth System Science Data ( IF 11.4 ) Pub Date : 2022-11-02 , DOI: 10.5194/essd-2022-327
Longfei Bing , Mingjing Ma , Lili Liu , Jiaoyue Wang , Le Niu , Fengming Xi

Abstract. Lime is responsible for the continuous and stable absorption of CO2 from the atmosphere during its cycle via the carbonation reaction. However, the magnitude of the global uptake of CO2 by lime under natural conditions remains unclear. Here, existing data on materials associated with the production, utilisation, and disposal stages of lime-containing materials were analysed using a comprehensive model to obtain regional and global estimates for the sequestration of carbon from 1963 to 2020. The CO2 emissions linked to the production of lime during the investigated period were also estimated. The results reveal that the global uptake of CO2 by lime increased from 38.25 Mt (95 % confidence interval, CI:27.85-51.38 Mt) in 1963 to 134.33 Mt (95 % CI:90.37-139.29 Mt) in 2020. Cumulatively, approximately 4.05 Gt of CO2 (95 % CI:3.02-5.25 Gt CO2) were sequestered by lime produced between 1963 and 2020, and this amount corresponds to 38.79 % of CO2 emissions from the associated process during the period. Lime-containing materials in China accounted for 63.12 % of the total uptake, and among the three stages of the lime cycle, the utilisation stage accounted for the highest CO2 sequestration (~74.05 %). The results also demonstrate that lime, which is usually omitted from emission inventories as a carbon sink, is very important to the carbon cycle. The present study indicates that the CO2 uptake by lime can reduce the carbon footprint of lime production process and provide scientific proof for further research of the potential of lime-containing materials in carbon capture and storage. The ** data utilised in the present study can be accessed at https://doi.org/10.5281/zenodo.7112485 (Ma, 2022)

中文翻译:

1963 年至 2020 年全球石灰吸收 CO2 的调查

摘要。石灰负责在其循环过程中通过碳酸化反应从大气中持续稳定地吸收 CO 2 。然而,在自然条件下石灰对 CO 2的全球吸收量仍不清楚。在这里,使用综合模型分析了与含石灰材料的生产、利用和处置阶段相关的材料的现有数据,以获得 1963 年至 2020 年碳封存的区域和全球估计值。还估算了调查期间的石灰产量。结果表明,全球对 CO 2的吸收石灰从 1963 年的 38.25 Mt(95 % 置信区间,CI:27.85-51.38 Mt)增加到 2020 年的 134.33 Mt(95 % CI:90.37-139.29 Mt)。累计约 4.05 Gt CO 2(95 % CI: 3.02-5.25 Gt CO 2 ) 被 1963 年至 2020 年间生产的石灰封存,这一数量相当于该期间相关工艺产生的 CO 2排放量的 38.79%。我国含石灰物料占总吸收量的63.12%,在石灰循环的三个阶段中,利用阶段CO 2占比最高封存(~74.05%)。结果还表明,通常作为碳汇从排放清单中省略的石灰对碳循环非常重要。本研究表明石灰吸收CO 2可以减少石灰生产过程的碳足迹,并为进一步研究含石灰材料在碳捕获和储存中的潜力提供科学依据。本研究中使用的**数据可在 https://doi.org/10.5281/zenodo.7112485 (Ma, 2022) 访问
更新日期:2022-11-02
down
wechat
bug