Net greenhouse gas balance in U.S. croplands: How can soils be part of the climate solution?

Author:

You Yongfa123ORCID,Tian Hanqin12ORCID,Pan Shufen134,Shi Hao5,Lu Chaoqun6ORCID,Batchelor William D.7,Cheng Bo7,Hui Dafeng8ORCID,Kicklighter David9,Liang Xin‐Zhong10ORCID,Li Xiaoyong125,Melillo Jerry9,Pan Naiqing12,Prior Stephen A.11,Reilly John12

Affiliation:

1. Center for Earth System Science and Global Sustainability (CES3), Schiller Institute for Integrated Science and Society Boston College Chestnut Hill Massachusetts USA

2. Department of Earth and Environmental Sciences Boston College Chestnut Hill Massachusetts USA

3. College of Forestry, Wildlife and Environment, Auburn University Auburn Alabama USA

4. Department of Engineering Boston College Chestnut Hill Massachusetts USA

5. State Key Laboratory of Urban and Regional Ecology, Research Center for Eco‐Environmental Sciences, Chinese Academy of Sciences Beijing China

6. Department of Ecology, Evolution, and Organismal Biology Iowa State University Ames Iowa USA

7. Biosystems Engineering Department Auburn University Auburn Alabama USA

8. Department of Biological Sciences Tennessee State University Nashville Tennessee USA

9. The Ecosystems Center, Marine Biological Laboratory Woods Hole Massachusetts USA

10. Department of Atmospheric and Oceanic Science and Earth System Science Interdisciplinary Center University of Maryland College Park Maryland USA

11. USDA‐ARS National Soil Dynamics Laboratory Auburn Alabama USA

12. Joint Program on the Science and Policy of Global Change Massachusetts Institute of Technology Cambridge Massachusetts USA

Abstract

AbstractAgricultural soils play a dual role in regulating the Earth's climate by releasing or sequestering carbon dioxide (CO2) in soil organic carbon (SOC) and emitting non‐CO2 greenhouse gases (GHGs) such as nitrous oxide (N2O) and methane (CH4). To understand how agricultural soils can play a role in climate solutions requires a comprehensive assessment of net soil GHG balance (i.e., sum of SOC‐sequestered CO2 and non‐CO2 GHG emissions) and the underlying controls. Herein, we used a model‐data integration approach to understand and quantify how natural and anthropogenic factors have affected the magnitude and spatiotemporal variations of the net soil GHG balance in U.S. croplands during 1960–2018. Specifically, we used the dynamic land ecosystem model for regional simulations and used field observations of SOC sequestration rates and N2O and CH4 emissions to calibrate, validate, and corroborate model simulations. Results show that U.S. agricultural soils sequestered Tg CO2‐C year−1 in SOC (at a depth of 3.5 m) during 1960–2018 and emitted Tg N2O‐N year−1 and Tg CH4‐C year−1, respectively. Based on the GWP100 metric (global warming potential on a 100‐year time horizon), the estimated national net GHG emission rate from agricultural soils was Tg CO2‐eq year−1, with the largest contribution from N2O emissions. The sequestered SOC offset ~28% of the climate‐warming effects resulting from non‐CO2 GHG emissions, and this offsetting effect increased over time. Increased nitrogen fertilizer use was the dominant factor contributing to the increase in net GHG emissions during 1960–2018, explaining ~47% of total changes. In contrast, reduced cropland area, the adoption of agricultural conservation practices (e.g., reduced tillage), and rising atmospheric CO2 levels attenuated net GHG emissions from U.S. croplands. Improving management practices to mitigate N2O emissions represents the biggest opportunity for achieving net‐zero emissions in U.S. croplands. Our study highlights the importance of concurrently quantifying SOC‐sequestered CO2 and non‐CO2 GHG emissions for developing effective agricultural climate change mitigation measures.

Funder

National Science Foundation

Publisher

Wiley

Subject

General Environmental Science,Ecology,Environmental Chemistry,Global and Planetary Change

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