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复垦矿土中的生态系统碳预算与土壤碳固存

Ecosystem carbon budgeting and soil carbon sequestration in reclaimed mine soil.

作者信息

Shrestha Raj K, Lal Rattan

机构信息

Carbon Management and Sequestration Center, OARDC/FAES, School of Natural Resources, 2021 Coffey Road, Columbus, Ohio 43210, United States.

出版信息

Environ Int. 2006 Aug;32(6):781-96. doi: 10.1016/j.envint.2006.05.001. Epub 2006 Jun 21.

Abstract

Global warming risks from emissions of green house gases (GHGs) by anthropogenic activities, and possible mitigation strategies of terrestrial carbon (C) sequestration have increased the need for the identification of ecosystems with high C sink capacity. Depleted soil organic C (SOC) pools of reclaimed mine soil (RMS) ecosystems can be restored through conversion to an appropriate land use and adoption of recommended management practices (RMPs). The objectives of this paper are to (1) synthesize available information on carbon dioxide (CO2) emissions from coal mining and combustion activities, (2) understand mechanisms of SOC sequestration and its protection, (3) identify factors affecting C sequestration potential in RMSs, (4) review available methods for the estimation of ecosystem C budget (ECB), and (5) identify knowledge gaps to enhance C sink capacity of RMS ecosystems and prioritize research issues. The drastic perturbations of soil by mining activities can accentuate CO2 emission through mineralization, erosion, leaching, changes in soil moisture and temperature regimes, and reduction in biomass returned to the soil. The reclamation of drastically disturbed soils leads to improvement in soil quality and development of soil pedogenic processes accruing the benefit of SOC sequestration and additional income from trading SOC credits. The SOC sequestration potential in RMS depends on amount of biomass production and return to soil, and mechanisms of C protection. The rate of SOC sequestration ranges from 0.1 to 3.1 Mg ha(-1) yr(-1) and 0.7 to 4 Mg ha(-1) yr(-1) in grass and forest RMS ecosystem, respectively. Proper land restoration alone could off-set 16 Tg CO2 in the U.S. annually. However, the factors affecting C sequestration and protection in RMS leading to increase in microbial activity, nutrient availability, soil aggregation, C build up, and soil profile development must be better understood in order to formulate guidelines for development of an holistic approach to sustainable management of these ecosystems. The ECBs of RMS ecosystems are not well understood. An ecosystem method of evaluating ECB of RMS ecosystems is proposed.

摘要

人为活动排放温室气体(GHGs)带来的全球变暖风险,以及陆地碳(C)固存的可能缓解策略,增加了识别具有高碳汇能力生态系统的需求。通过转变为适当的土地利用方式并采用推荐的管理措施(RMPs),可以恢复复垦矿土(RMS)生态系统中 depleted 的土壤有机碳(SOC)库。本文的目的是:(1)综合有关煤炭开采和燃烧活动中二氧化碳(CO2)排放的现有信息;(2)了解 SOC 固存及其保护机制;(3)识别影响 RMS 中碳固存潜力的因素;(4)回顾估算生态系统碳预算(ECB)的现有方法;(5)识别知识差距,以提高 RMS 生态系统的碳汇能力并确定研究问题的优先级。采矿活动对土壤的剧烈扰动会通过矿化、侵蚀、淋溶、土壤水分和温度状况的变化以及返回土壤的生物量减少而加剧 CO2 排放。对受到严重扰动的土壤进行复垦会改善土壤质量,并促进土壤成土过程的发展,从而带来 SOC 固存的益处以及通过交易 SOC 信用获得的额外收入。RMS 中的 SOC 固存潜力取决于生物量产量和返回土壤的量以及 C 保护机制。在草地和森林 RMS 生态系统中,SOC 固存速率分别为 0.1 至 3.1 Mg ha(-1) yr(-1) 和 0.7 至 4 Mg ha(-1) yr(-1)。仅适当的土地恢复每年就可以在美国抵消 16 Tg CO2。然而,为了制定全面管理这些生态系统的可持续方法的指导方针,必须更好地理解影响 RMS 中碳固存和保护的因素,这些因素会导致微生物活性增加、养分有效性提高、土壤团聚、碳积累和土壤剖面发育。RMS 生态系统的 ECB 尚未得到很好的理解。本文提出了一种评估 RMS 生态系统 ECB 的生态系统方法。

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