Supplementing Enhanced Weathering With Organic Amendments Accelerates the Net Climate Benefit of Soil Amendments in Rangeland Soils

IF 8.3 Q1 GEOSCIENCES, MULTIDISCIPLINARY
AGU Advances Pub Date : 2025-04-18 DOI:10.1029/2024AV001480
Tyler L. Anthony, Andrew R. Jones, Whendee L. Silver
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Abstract

Carbon dioxide (CO2) removal (carbon dioxide removal (CDR)) that combines decreased greenhouse gas emissions with atmospheric CO2 reduction is needed to limit climate change. Enhanced rock weathering (ERW) of ground silicate minerals is an emerging CDR technology with the potential to decrease atmospheric CO2. However, there are few multi-year field studies and considerable uncertainty in field-rates of ERW. We explored combining finely ground metabasaltic rock with other soil CDR technologies (compost and biochar amendments) to stimulate carbon (C) sequestration. The combined ground rock (GR), compost, and biochar amendment had the greatest increases in soil C stocks over 3 years (15.3 ± 4.8 Mg C ha−1). All other treatments slowed or reversed background C losses, with GR-only treatments reducing rates of soil C loss relative to the control but still losing soil C over time. Ground rock amendments lowered nitrous oxide (N2O) emissions by 11.0 ± 0.6 kg CO2e ha−1 yr−1 and increased methane (CH4) consumption by 9.5 ± 3.5 to 18.4 ± 4.4 kg CO2e ha−1 yr−1; while noteworthy, emissions reductions were an order of magnitude smaller than organic C sequestration with compost amendments. The combined amendment yielded the greatest estimated net ecosystem benefit (3 year relative changes in soil C, estimated ERW rates, and greenhouse gas emissions) of −86.0 ± 24.7 Mg CO2e ha−1. Benefits were dominated by soil organic C gains, directly from organic amendments and indirectly from increased plant growth. Weathering rates were <10% of the theoretical potential. Combined ERW and organic amendments increased estimated weathering rates and stimulated soil organic C sequestration.

Abstract Image

用有机改进剂补充增强的风化作用加速了牧场土壤改进剂的净气候效益
限制气候变化需要将减少温室气体排放与减少大气二氧化碳相结合的二氧化碳去除(Carbon dioxide removal, CDR)。增强岩石风化(ERW)是一种新兴的CDR技术,具有降低大气CO2的潜力。然而,很少有多年的实地研究和相当大的不确定性的野外剩余物率。我们探索了将细碎的变质玄武岩与其他土壤CDR技术(堆肥和生物炭改良剂)结合起来,以促进碳(C)的固存。土壤碳储量在3年内增加最多的是基岩、堆肥和生物炭复合处理(15.3±4.8 Mg C ha−1)。所有其他处理都减缓或逆转了背景碳的流失,仅gr处理相对于对照降低了土壤碳的流失率,但随着时间的推移,土壤碳仍在流失。地面岩石修正降低了一氧化二氮(N2O)排放量11.0±0.6 kg CO2e ha - 1年−1,增加了甲烷(CH4)消耗量9.5±3.5至18.4±4.4 kg CO2e ha - 1年−1年−1;虽然值得注意,但排放量的减少比通过堆肥修正的有机碳固存要小一个数量级。综合修正产生的最大净生态系统效益(土壤C的3年相对变化,估计的ERW率和温室气体排放)为- 86.0±24.7 Mg CO2e ha - 1。土壤有机碳收益占主导地位,直接来自有机改良,间接来自植物生长的增加。风化率为理论潜势的10%。复合ERW和有机修正增加了估计的风化速率,促进了土壤有机碳的固存。
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CiteScore
2.90
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