The importance of accounting method and sampling depth to estimate changes in soil carbon stocks

IF 3.9 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Carbon Balance and Management Pub Date : 2024-01-26 DOI:10.1186/s13021-024-00249-1
Anna M. Raffeld, Mark A. Bradford, Randall D. Jackson, Daniel Rath, Gregg R. Sanford, Nicole Tautges, Emily E. Oldfield
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Abstract

Background

As interest in the voluntary soil carbon market surges, carbon registries have been developing new soil carbon measurement, reporting, and verification (MRV) protocols. These protocols are inconsistent in their approaches to measuring soil organic carbon (SOC). Two areas of concern include the type of SOC stock accounting method (fixed-depth (FD) vs. equivalent soil mass (ESM)) and sampling depth requirement. Despite evidence that fixed-depth measurements can result in error because of changes in soil bulk density and that sampling to 30 cm neglects a significant portion of the soil profile’s SOC stock, most MRV protocols do not specify which sampling method to use and only require sampling to 30 cm. Using data from UC Davis’s Century Experiment (“Century”) and UW Madison’s Wisconsin Integrated Cropping Systems Trial (WICST), we quantify differences in SOC stock changes estimated by FD and ESM over 20 years, investigate how sampling at-depth (> 30 cm) affects SOC stock change estimates, and estimate how crediting outcomes taking an empirical sampling-only crediting approach differ when stocks are calculated using ESM or FD at different depths.

Results

We find that FD and ESM estimates of stock change can differ by over 100 percent and that, as expected, much of this difference is associated with changes in bulk density in surface soils (e.g., r = 0.90 for Century maize treatments). This led to substantial differences in crediting outcomes between ESM and FD-based stocks, although many treatments did not receive credits due to declines in SOC stocks over time. While increased variability of soils at depth makes it challenging to accurately quantify stocks across the profile, sampling to 60 cm can capture changes in bulk density, potential SOC redistribution, and a larger proportion of the overall SOC stock.

Conclusions

ESM accounting and sampling to 60 cm (using multiple depth increments) should be considered best practice when quantifying change in SOC stocks in annual, row crop agroecosystems. For carbon markets, the cost of achieving an accurate estimate of SOC stocks that reflect management impacts on soils at-depth should be reflected in the price of carbon credits.

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核算方法和取样深度对估算土壤碳储量变化的重要性。
背景:随着人们对自愿性土壤碳市场的兴趣激增,碳注册机构一直在制定新的土壤碳测量、报告和验证(MRV)协议。这些协议在测量土壤有机碳(SOC)的方法上并不一致。值得关注的两个方面包括 SOC 储量核算方法(固定深度 (FD) 与等效土壤质量 (ESM))和采样深度要求。尽管有证据表明,由于土壤容重的变化,固定深度测量可能会导致误差,而且 30 厘米的取样会忽略土壤剖面的大部分 SOC 储量,但大多数 MRV 协议并未规定使用哪种取样方法,而且只要求取样至 30 厘米。利用加州大学戴维斯分校的世纪试验("Century")和华盛顿大学麦迪逊分校的威斯康星综合耕作系统试验(WICST)的数据,我们量化了 20 年来用 FD 和 ESM 估算的 SOC 储量变化的差异,研究了深度取样(> 30 厘米)对 SOC 储量变化估算的影响,并估算了在不同深度使用 ESM 或 FD 计算储量时,仅采用经验取样入计方法的入计结果有何不同:我们发现,FD 和 ESM 对储量变化的估算可能相差超过 100%,而且正如预期的那样,这种差异很大程度上与表层土壤容重的变化有关(例如,世纪玉米处理的 r = 0.90)。这导致基于 ESM 和基于 FD 的存量之间的入计量结果存在巨大差异,尽管许多处理由于 SOC 存量随时间推移而下降而未获得入计量。虽然土壤在深度上的变异性增加使得准确量化整个剖面上的存量具有挑战性,但在 60 厘米处取样可以捕捉到体积密度的变化、潜在的 SOC 再分布以及整体 SOC 存量的较大比例:结论:在对一年生连作农业生态系统中的 SOC 储量变化进行量化时,ESM 核算和 60 厘米取样(使用多个深度增量)应被视为最佳实践。对于碳市场而言,准确估算 SOC 储量以反映管理对土壤深度的影响所需的成本应反映在碳信用额的价格中。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Carbon Balance and Management
Carbon Balance and Management Environmental Science-Management, Monitoring, Policy and Law
CiteScore
7.60
自引率
0.00%
发文量
17
审稿时长
14 weeks
期刊介绍: Carbon Balance and Management is an open access, peer-reviewed online journal that encompasses all aspects of research aimed at developing a comprehensive policy relevant to the understanding of the global carbon cycle. The global carbon cycle involves important couplings between climate, atmospheric CO2 and the terrestrial and oceanic biospheres. The current transformation of the carbon cycle due to changes in climate and atmospheric composition is widely recognized as potentially dangerous for the biosphere and for the well-being of humankind, and therefore monitoring, understanding and predicting the evolution of the carbon cycle in the context of the whole biosphere (both terrestrial and marine) is a challenge to the scientific community. This demands interdisciplinary research and new approaches for studying geographical and temporal distributions of carbon pools and fluxes, control and feedback mechanisms of the carbon-climate system, points of intervention and windows of opportunity for managing the carbon-climate-human system. Carbon Balance and Management is a medium for researchers in the field to convey the results of their research across disciplinary boundaries. Through this dissemination of research, the journal aims to support the work of the Intergovernmental Panel for Climate Change (IPCC) and to provide governmental and non-governmental organizations with instantaneous access to continually emerging knowledge, including paradigm shifts and consensual views.
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