Soil organic carbon response to global environmental change depends on its distribution between mineral-associated and particulate organic matter: A meta-analysis

被引:200
|
作者
Rocci, Katherine S. [1 ,2 ,3 ]
Lavallee, Jocelyn M. [2 ]
Stewart, Catherine E. [4 ]
Cotrufo, M. Francesca [2 ,3 ]
机构
[1] Colorado State Univ, Grad Degree Program Ecol, Ft Collins, CO 80523 USA
[2] Colorado State Univ, Soil & Crop Sci Dept, Ft Collins, CO 80523 USA
[3] Colorado State Univ, Nat Resource Ecol Lab, Ft Collins, CO 80523 USA
[4] ARS, USDA, Ft Collins, CO USA
基金
美国国家科学基金会;
关键词
Soil organic matter; Global change; Soil physical fractionation; Nitrogen fertilization; Warming; Elevated CO2; CO2 ENRICHMENT FACE; ELEVATED CO2; NITROGEN ADDITIONS; LITTER DECOMPOSITION; AGRICULTURAL SOILS; ATMOSPHERIC CO2; USE-EFFICIENCY; CLIMATE-CHANGE; PLANT-GROWTH; COVER CROPS;
D O I
10.1016/j.scitotenv.2021.148569
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soil organic carbon (SOC), as the largest terrestrial carbon pool, plays an important role in global carbon (C) cycling, which may be significantly impacted by global changes such as nitrogen (N) fertilization, elevated carbon dioxide (CO2), warming, and increased precipitation. Yet, our ability to accurately detect and predict the impact of these global changes on SOC dynamics is still limited. Investigating SOC responses to global changes separately for mineral-associated organic carbon (MAOC) and the particulate organic carbon (POC) can aid in the understanding of overall SOC responses, because these are formed, protected, and lost through different pathways. To this end, we performed a systematic meta-analysis of the response of SOC, MAOC, and POC to global changes. POC was particularly responsive, confirming that it is a better diagnostic indicator of soil C changes in the short-term, compared to bulk SOC and MAOC. The effects of elevated CO2 and warming were subtle and evident only in the POC fraction (+5.11% and -10.05%, respectively), while increased precipitation had no effects at all. Nitrogen fertilization, which comprised the majority of the dataset, increased SOC (+5.64%), MAOC (+4.49%), and POC (+13.17%). Effect size consistently varied with soil depth and experiment length, highlighting the importance of long-termexperiments that sample the full soil profile in global change SOC studies. In addition, SOC pool responses to warming were modified by degree of warming, differently for air and soil warming manipulations. Overall, we suggest that MAOC and POC respond differently to global changes and moderators because of the different formation and loss processes that control these pools. Coupled with additional plant and microbial measurements, studying the individual responses of POC and MAOC improves understanding of the underlying dynamics of SOC responses to global change. This will help inform the role of SOC in mitigating the climate crisis. (C) 2021 Elsevier B.V. All rights reserved.
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页数:12
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