Effects of land reclamation on peatland carbon stability in Sanjiang Plain (Northeast China) over the last century

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Catena Pub Date : 2024-08-26 DOI:10.1016/j.catena.2024.108334
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Abstract

Peatlands store vast amounts of soil carbon and the stability of this carbon pool plays a crucial role in the carbon dynamics under global change. In the Sanjiang Plain, one of the important peatlands distributed region in China, peatlands were seriously affected by the regional land reclamation during the last century. While, there is a scarcity of data evaluating the impact of land reclamation on peatland carbon stability. Here, based on 210Pb dating of the Shenjiadian (SJD) peatland, we reconstructed historical variations in peatland carbon stability and assessed its response on regional land reclamation over the last century in the Sanjiang Plain. The results showed that the highest aromatic content (25.2 ± 0.7 %) and the lowest carbohydrate content (34.7 ± 2.5 %) occurred between 1950 and 1980, coinciding with the period of extensive second land reclamation in the Sanjiang Plain. The increase in regional human activities led to greater accumulation of pyrogenic carbon in the peatland, enhancing carbon stability in the 1950 s. However, as farmland area continued to grow in the 1960 s, local fires caused by agricultural activities led to more frequent peat fires, promoting the accumulation of herbaceous litter in the peatland, which decreased the stability of the peatland carbon pool but increased carbon accumulation rates. With the proportion of shrub litter increasing and regional land reclamation weakening after 1980, the accumulation of shrub litters has increased both carbon stability and carbon accumulation rates in the studied peatland, particularly after 2000.

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上世纪土地开垦对三江平原(中国东北)泥炭地碳稳定性的影响
泥炭地储存着大量的土壤碳,这一碳库的稳定性对全球变化下的碳动态起着至关重要的作用。三江平原是中国重要的泥炭地分布区之一,在上个世纪,泥炭地受到了区域土地开垦的严重影响。然而,评估土地开垦对泥炭地碳稳定性影响的数据却十分匮乏。在此,我们基于沈家店泥炭地的 210Pb 测年,重建了泥炭地碳稳定性的历史变化,并评估了其对上世纪三江平原区域土地开垦的响应。结果表明,1950-1980年间芳烃含量最高(25.2±0.7%),碳水化合物含量最低(34.7±2.5%),与三江平原第二次大规模土地开垦时期相吻合。然而,随着 20 世纪 60 年代农田面积的不断增加,农业活动引起的局部火灾导致泥炭火灾更加频繁,促进了泥炭地中草本枯落物的积累,降低了泥炭地碳库的稳定性,但增加了碳积累率。1980 年后,随着灌木枯落物比例的增加和区域土地开垦力度的减弱,灌木枯落物的积累提高了所研究泥炭地的碳稳定性和碳积累率,尤其是在 2000 年之后。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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