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Physical protection of soil organic carbon through aggregates in different land use systems in the semi-arid region of Brazil

机译:巴西半干旱地区不同土地利用系统中土壤有机碳的物理保护

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摘要

The objectives of this work were to quantify the soil organic carbon (SOC) stock and to evaluate the distribution of soil aggregates and their respective SOC and labile carbon (LC) present inside the aggregates in different perennial land use systems in the semi-arid region of Brazil. Soil samples were collected in four land use systems: two forage palm cultivation systems of different ages, a mango orchard, and natural forest. A higher amount of SOC stored in the 0-60 cm layer was observed in the mango orchard, increasing the soil carbon stock by 16.4% in relation to the natural forest. Palm cultivations presented larger amounts of macroaggregates from the 10-20 cm layer until 60 cm depth, while the mango orchard and natural forest presented a similar pattern in all fraction size classes. SOC averages of non-occluded particulate organic matter (POM) and aggregate occluded organic matter (AOM) in the macroaggregates of the 0-10 cm layer were higher in the mango orchard and natural forest compared to palm cultivations; however, the LC of AOM was higher in palm crops. Soil microaggregates were little influenced by land use systems, however this class represented an average of 24% of SOC stock.
机译:这项工作的目标是量化土壤有机碳(SoC)库存,并评估在半干旱地区不同多年生土地使用系统中的聚集体内的土壤聚集体及其各自的SOC和不稳定碳(LC)的分布巴西的。在四种土地使用系统中收集土壤样品:两种牧草棕榈栽培系统,不同年龄,芒果果园和天然林。在芒果果园中观察到储存在0-60cm层中的较高量的SOC,与天然森林的土壤碳储量增加了16.4%。棕榈栽培从10-20cm层呈现较大量的大草凝结,直到60厘米深度,而芒果果园和天然森林在所有分数尺寸类中呈现了类似的模式。与棕榈栽培相比,在0-10cm层的大甲果园和天然森林中,在0-10cm层的大草原中的非闭塞颗粒有机物质(POM)和聚集闭合有机物质(AOM)的SOC平均值;然而,棕榈作物中AOM的LC较高。土壤微烧结几乎没有受到土地利用系统的影响,然而,这一课程的SoC股票平均为24%。

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