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。
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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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Issue Information Proceedings of the 14th North American Forest Soils Conference Soil chemical properties affecting grain yield and oil content of crambe biofuel crop Particulate organic carbon and nitrogen and soil-test biological activity under grazed pastures and conservation land uses Determining microbial metabolic limitation under the influence of moss patch size from soil extracellular enzyme stoichiometry
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