严重土壤退化的遗留问题阻碍了矿物相关土壤有机碳的积累

IF 8.2 1区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES
Otávio dos Anjos Leal, Rüdiger Reichel, Holger Wissel, Nicolas Brüggemann
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引用次数: 0

摘要

全球努力的目标是农业土壤表层30厘米土壤有机碳(SOC)增加率达到2.4‰y - 1,以解决与土壤有机碳储量下降相关的土壤生产力下降问题。为了研究土壤有机碳的保护机制和累积限制,我们对德国矿区开采后形成的均匀土壤进行了独特的时间序列研究,这些土壤为传统农业服务,具有较大的有机碳储存空间,但有机碳积累有限。我们假设有限的有机碳积累与氮不足有关,而不是与矿物质饱和度有关。土壤样本(0-30 cm和30-60 cm)按时间顺序(0-56年)收集,并与原始未开采土壤(OS)进行比较。通过土壤培养、有机质密度分馏和δ13C测量,研究了有机碳的平均停留时间(MRT)及其保护机制。56年后,总SOC和矿物相关SOC (MAOC)储量仍比0-30 cm的OS低18%和28%,估计补充时间分别为93年和129年。矿物相关氮(MAN)存量在恢复时间低于OS水平时停滞不前。MAOC与总有机碳和MAN储量呈显著的线性相关,表明限制有机碳积累的不是矿物饱和度,而是氮。事实上,MAOC储量亏缺至饱和的估计值为316.4 Mg ha−1。在30 ~ 60 cm处,由于初始损失相对较小,土壤有机碳和氮储量在30年内得到恢复。SOC在0-30 cm和30-60 cm处的初始MRT(15.3年和27.9年)下降,最终与OS相当(11.7年和7.7年)。这反映了进入土壤的新碳最初主要含有MAOC(78 - 82%),随后稳定为MAOC。由于退化土壤易受氮流失的影响,因此需要有针对性的氮管理来恢复有机碳储量,并符合欧洲法律对农业有机碳积累的要求。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Legacy of severe soil degradation hinders the buildup of mineral-associated soil organic carbon

Legacy of severe soil degradation hinders the buildup of mineral-associated soil organic carbon
Global efforts target a soil organic carbon (SOC) enhancement rate of 2.4 ‰ y−1 in the upper 30 cm of agricultural soils to address declining soil productivity associated with declining SOC stocks. We explored a unique chronosequence of homogeneous soils formed after mining in Germany, which serve conventional agriculture and exhibit a large margin for SOC storage, but limited SOC accrual, to study SOC protection mechanisms and accrual constraints. We hypothesized that limited SOC accrual is associated to insufficient nitrogen rather than to minerals saturation. Soil samples (0–30 and 30–60 cm) were collected across the chronosequence (0–56 years) and compared to an original non-mined soil (OS) managed similarly. The mean residence time (MRT) of SOC and its protection mechanisms were studied using soil incubation, organic matter density fractionation, and δ13C measurements. After 56 years, total and mineral-associated SOC (MAOC) stocks remained 18 % and 28 % lower than in the OS at 0–30 cm, with estimated replenishment times of 93 and 129 years, respectively. Mineral-associated nitrogen (MAN) stocks stagnated along recultivation time below OS level. Together with significant linear correlation of MAOC with total SOC and MAN stocks, these results indicate that nitrogen rather than saturation of minerals limits SOC accrual. In fact, the MAOC stock deficit to saturation was estimated at 316.4 Mg ha−1. At 30–60 cm, SOC and nitrogen stocks were restored within 30 years, due to comparatively lower initial losses. The initial MRT of SOC at 0–30 and 30–60 cm (15.3 and 27.9 years) declined before finally becoming comparable to OS (11.7 and 7.7 years). This reflected new carbon entering the soil that initially contained predominantly MAOC (78–82 %), followed by its stabilization as MAOC. Due to their susceptibility to nitrogen losses, degraded soils require tailored nitrogen management to restore SOC stocks and comply with European laws requiring agricultural SOC accrual.
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来源期刊
Science of the Total Environment
Science of the Total Environment 环境科学-环境科学
CiteScore
17.60
自引率
10.20%
发文量
8726
审稿时长
2.4 months
期刊介绍: The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere. The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.
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