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Pore characteristics regulate priming and fate of carbon from plant residue

机译:从植物残留物中调节碳的灌注和命运

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Decomposition of the plant residue added to soil affects fate of native soil organic matter (SOM) via magnitude and direction of priming effect (PE). Soil pore characteristics, namely, pore size distribution (PSD), regulate air and liquid fluxes, as well as transport of solubilized decomposing residue to microorganisms. The goal of this study was to assess the effect of PSD on plant residue decomposition and PE as modulated by i) residue quality, ii) soil moisture status, and iii) long-term management history. We combined labeling and imaging approaches to visualize loss of decomposing residue and link it to PE in soils with two contrasting PSDs, dominated by small (5-10 mu m) pores and by a combination of very small (5 mu m) and large (>30 mu m) pores, respectively. The microcosms were incubated with C-13-labeled corn and soybean leaves, in soils from long-term conventional and biologically based managements. X-ray computed micro-tomography scanning was utilized to visualize loss of intact leaves at early stages (7, 14, 24 d) of decomposition. We found that PSD of soil adjacent to the decomposing plant residue played a major role in the fate of the residue and of its decomposition products. In microcosms with prevalence of small (5-10 gm) pores decomposition of corn leaves was slower, movement of decomposition products into the adjacent soil was greater, and proportion of CO2 that originated from the residue was lower than in the microcosms with prevalence of large pores. Greater positive PE took place in microcosms with small than with large pores. While these tendencies were observed in all studied soil moisture levels, management practices, and plant residue substrates, they were most pronounced in microcosms with more labile residue (soybean) in the soil from long-term biologically based management. Across treatments, the intensity of PE was greater for soils under conventional than biologically-based management. The findings emphasize importance of accounting for soil PSD when assessing processes of soil C accrual and priming. (C) 2017 Elsevier Ltd. All rights reserved.
机译:添加到土壤中的植物残留物的分解影响天然土壤有机物质(SOM)的命运(PE)的初始和方向影响天然土壤有机物(SOM)。土壤孔隙特性,即孔径分布(PSD),调节空气和液体助熔剂,以及溶解的分解残留物与微生物的运输。本研究的目的是评估PSD对植物残留物分解和PE的影响,通过I)残留物质量,ii)土壤水分状况和III)长期管理历史。我们组合标签和成像方法以使分解残留物的丧失和将其连接到具有两个对比的PSD的土壤中的PE,由小(5-10μm)孔主导,并通过非常小(<5μm)的组合来实现。分别大(>30μm)毛孔。将微观与C-13标记的玉米和大豆叶一起温育,在长期传统和生物基础管理的土壤中。 X射线计算的微型断层扫描扫描用于在分解的早期阶段(7,14,24d)处可视化完整叶片的损失。我们发现与分解植物残留物相邻的土壤PSD在残留物的命运和其分解产物中发挥了重要作用。在患有小(5-10克)的微观速度的微观(5-10克)分解玉米叶子较慢,分解产物进入相邻的土壤的运动越大,源于残留物的二氧化碳比例低于微观的微观毛孔。更大的阳性PE在小于大毛孔的微观体积中进行。虽然在所有研究的土壤水分水平,管理实践和植物残留基材中观察到这些趋势,但在长期生物学管理中,在土壤中具有更加不稳定的残留物(大豆),它们最明显的微观态度。在治疗中,常规的土壤比基于生物学的管理更大的土壤更大。调查结果强调在评估土壤C应计和灌注过程时对土壤PSD核算的重要性。 (c)2017 Elsevier Ltd.保留所有权利。

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