有机添加剂对土壤微集料中碳稳定性影响的直接证据

Pavithra S. Pitumpe Arachchige, Ganga M. Hettiarachchi, Charles W. Rice, James J. Dynes, Leila Maurmann, A. L. David Kilcoyne, Chammi P. Attanayake
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引用次数: 0

摘要

以直接证据为基础的方法对于理解非生物/生物因素的参与以及评估新提出的土壤碳(C)稳定理论至关重要。我们分析了从玉米种植系统(22 年,美国堪萨斯州)中采集的微团聚体(150-250 µm),该系统采用免耕和不同的氮(N)处理(氮处理:粪肥/堆肥、尿素、零肥料)。我们直接使用扫描透射 X 射线显微镜和近边缘 X 射线吸收精细结构(STXM-NEXAFS)光谱,研究了自由土壤微团聚体(保留了团聚体结构)中的碳稳定情况。亚微米尺度的研究结果与块体化学分析结果相辅相成。STXM-NEXAFS 分析表明,土壤有机碳(SOC)保存在纳米和微孔内,并与有机矿物质结合,具有不同程度的腐殖化和高度的分子多样性。在添加了粪肥/堆肥的微团聚体中发现了微生物衍生碳,这凸显了有机添加剂在促进微生物多样性方面的贡献。文石状矿物的出现表明微团聚体核心具有生物/化学活性。对游离微团聚体的批量分析表明,与无机肥(3% SOC)和对照组(2.7% SOC)相比,添加了粪肥/堆肥的土壤中 SOC(6.5%)和草酸铵提取物 Fe/Al/Si 的浓度更高,腐殖酸的脂肪族含量也更高。元素(钙[Ca]/C、铁[Fe]/N、Fe/C、铝[Al]/C 和硅[Si]/C)的共存得到了大宗化学分析的部分支持,该分析表明草酸铵提取的铁/铝/硅与 SOC 之间存在密切联系(R2 = 0.63-0.77)。总之,我们的研究为化学、矿物学和生物机制的复杂和互动参与提供了直接/间接证据,而堆肥/粪肥的长期添加可能促进了 SOC 的稳定。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Direct evidence on the impact of organic amendments on carbon stabilization in soil microaggregates

Direct evidence-based approaches are vital in understanding the involvement of abiotic/biotic factors and evaluating the newly proposed theories on soil carbon (C) stabilization. Microaggregates (150–250 µm) collected from a corn system (>22 years; Kansas, USA), which had been under no-till with different nitrogen (N) treatments were analyzed (N treatments: manure/compost, urea, zero fertilizer). We studied C stabilization in free soil microaggregates (with preserved aggregate architecture), directly using scanning transmission X-ray microscopy coupled with near edge X-ray absorption fine structure (STXM-NEXAFS) spectroscopy. Submicron scale findings were complemented with bulk chemical analysis. The STXM-NEXAFS analysis revealed soil organic carbon (SOC) preservation inside nano- and micro-pores and organo–mineral association, various degrees of humification, and high molecular diversity. The presence of microbial-derived C was found in manure-/compost-added microaggregates highlighting the contribution of organic amendments in facilitating microbial diversity. The incidence of aragonite-like minerals suggested the biologically/chemically active nature of microaggregate cores. Bulk analysis of free microaggregates showed a higher concentration of SOC (6.5%), ammonium oxalate extractable Fe/Al/Si), and higher aliphaticity of humic acid in manure-/compost-added soils compared to inorganic fertilizer (3% SOC) and control (2.7% SOC) treatments. The co-existence of elements (calcium [Ca]/C, iron [Fe]/N, Fe/C, aluminum [Al]/C, and silicon [Si]/C) was partially supported by bulk chemical analysis that indicated a strong association between ammonium oxalate extractable Fe/Al/Si and SOC (R2 = 0.63—0.77). Overall, our study provided direct/indirect evidence for the complex and interactive involvement of chemical, mineralogical, and biological mechanisms that may have been stimulated by the long-term addition of compost/manure in stabilizing SOC.

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