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Effects of intercropping mulch on the content and composition of soil dissolved organic matter in apple orchard on the loess plateau

机译:黄土高原苹果园间作覆盖对苹果园土壤可溶性有机物含量和组成的影响

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Dissolved organic matter (DOM) is an important parameter that reflects soil fertility and quality. In this study, the effects of intercropping perennial ryegrass and straw mulch on the content, composition and spectral characteristics of soil DOM in orchards in arid and semi-arid areas were investigated by three-dimensional fluorescence excitation-emission matrix (EEM) combined with parallel factor analysis (PARAFAC). Three treatments were applied in a 6-year-old apple orchard on the Loess Plateau: (1) clean tillage (CT); (2) inter-cropping perennial ryegrass mulch (RE); (3) intercropping straw mulch (CS). Soil samples (0-10, 10-20, 20-40, 40-60, 60-80, 80-100 cm) were collected from different treatments. The total soil organic carbon (SOC) and dissolved organic carbon (DOC) content were ranked as CS > RE > CT, and decreased with soil depth. In addition, the vertical distribution of DOC with different soil depth was caused by organic matter input but not leaching. Three humic-like components and two protein-like components were identified by EEM-PARAFAC. Fluorescence spectra showed that humic-like compounds were the dominant fractions in soil DOM in the CS treatment. Fluorescence Index (FI) indicated that the proportion of plant residues and soil organic matter derived DOM ranked as CT > RE > CS and gradually decreased with soil depth. Our results highlight the key role of orchard intercropping mulch in improving the content and compositions of soil DOM through different forms of organic inputs and provide new theoretical support for the evaluation of soil fertility in orchards.
机译:溶解有机物(DOM)是反映土壤肥力和质量的重要参数。本研究利用三维荧光激发-发射矩阵(EEM)结合并行研究了间作多年生黑麦草和秸秆覆盖对干旱和半干旱地区果园土壤DOM的含量,组成和光谱特征的影响。因子分析(PARAFAC)。在黄土高原一个6岁的苹果园中进行了三种处理:(1)清洁耕作(CT); (2)间作多年生黑麦草覆盖物(RE); (3)间作秸秆覆盖物(CS)。从不同处理中收集土壤样品(0-10、10-20、20-40、40-60、60-80、80-100厘米)。土壤总有机碳(SOC)和溶解性有机碳(DOC)含量为CS> RE> CT,并随土壤深度而降低。另外,不同土壤深度的DOC的垂直分布是由有机质输入引起的,而不是淋溶引起的。 EEM-PARAFAC鉴定了三个腐殖质样组分和两个蛋白质样组分。荧光光谱表明,在CS处理中,腐殖质样化合物是土壤DOM中的主要成分。荧光指数(FI)表明,植物残渣和土壤有机质来源DOM的比例为CT> RE> CS,并随土壤深度的增加而逐渐降低。我们的研究结果突出了果园间作覆盖物通过不同形式的有机投入改善土壤DOM含量和组成的关键作用,并为果园土壤肥力的评估提供了新的理论依据。

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