The Use of Grape Pomace as Soil Fertilizer: A Microcosm Study on Available C and N and Consequences for Microbial Biomass, Structure, and Catabolic Responses

Sven Korz, Shamima Parvin, Humberto Aponte, Christian Buchmann, Dörte Diehl and Katherine Muñoz*, 
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Abstract

Grape pomace (GP) is used as a fertilizer in viticulture due to its carbon (C) and nitrogen (N) richness. Its application follows as biologically treated (i.e., vermicompost) or as untreated (fresh), with different nutritional inputs for the soil. But constraints exist regarding the amount and mobility of nutrients as a function of the soil type and the short-term effects on the soil microbiota. In a 6 week microcosm study, we analyzed the C and N dynamics in two agricultural soils (loamy sand and silt loam) after fresh red or white GP application. Microbial responses including biomass, respiration, and ecophysiological indices were recorded at the end of the experiment. White GP increased the available C (dissolved organic carbon) in the soils compared to the control, with a greater availability in sandy loam compared to silt loam soil. Dissolved (available) N in the treated soils did not differ by GP variety or soil type, but values were lower than those in the controls, suggesting a rapid N assimilation. Red GP in the sandy loam soils accounted for the highest total phenolic content (TPC) compared to the white GP. Independently of the GP variety or treatment, values reached control levels after 6 weeks. In the GP treated soils, microbial C/N ratios were narrower compared to the controls. The ergosterol to microbial carbon ratio indicated a higher fungal fraction in the GP treated soils; in particular, in the sandy loam soil, that fits with the availability of nutrients in the respective soils. The GP treatment increased the ratios MBC:TC (microbial C:total C) and MBN:TN (microbial N:total N), independently of the GP variety but with larger ratios in the silt loam soil, indicative of nutrient immobilization. qCO2 metabolic quotients were, in general, higher in the GP treated soils compared to the controls, with the highest values in sandy loam and red GP. The highest substrate utilization (respiration) rate was observed in the silty sandy soil, attributed mainly to the microbial biomass fraction compared to the sandy loam soil. But the functional diversity was not affected by the soil or by the GP treatment. We observed significant correlations between single chemical parameters and microbial indices apart from qCO2, suggesting that the response of the microbiome is multifactorial but driven mainly by the composition of the GP and by the availability of nutrients which in turn depends on the soil properties. This study enables a broader understanding on the consequences of the application of fresh GP varieties in soils with different properties, which is necessary for calculations of optimal nutritional inputs.

Abstract Image

使用葡萄渣作为土壤肥料:关于可用碳和氮及其对微生物生物量、结构和分解反应的影响的微观世界研究
葡萄渣(GP)因富含碳(C)和氮(N)而被用作葡萄栽培的肥料。葡萄渣可以通过生物处理(即蚯蚓堆肥)或未经处理(新鲜)的方式施用,为土壤提供不同的营养。但养分的数量和流动性因土壤类型和对土壤微生物群的短期影响而受到限制。在一项为期 6 周的微观世界研究中,我们分析了两种农用土壤(壤土和粉砂质壤土)在施用新鲜红芝麻或白芝麻后的碳和氮的动态变化。实验结束时记录了微生物的反应,包括生物量、呼吸作用和生态生理指数。与对照组相比,白色 GP 增加了土壤中的可利用碳(溶解有机碳),与淤泥质壤土相比,砂质壤土中的可利用碳更多。经处理的土壤中的溶解(可用)氮不因 GP 品种或土壤类型而异,但数值低于对照组,这表明氮的同化速度很快。与白色 GP 相比,沙壤土中红色 GP 的总酚含量(TPC)最高。无论 GP 品种或处理方法如何,其值在 6 周后都达到了对照组的水平。在经过 GP 处理的土壤中,微生物的 C/N 比值比对照组要小。麦角甾醇与微生物碳的比率表明,GP 处理过的土壤中真菌的比例较高,特别是在沙质壤土中,这与相应土壤中的养分供应情况相吻合。GP 处理增加了 MBC:TC(微生物碳:总碳)和 MBN:TN(微生物氮:总氮)比率,这与 GP 品种无关,但在淤泥质壤土中比率较大,表明养分固定化。与砂质壤土相比,淤泥质砂质土壤中的基质利用(呼吸)率最高,这主要归因于微生物的生物量部分。但功能多样性不受土壤或 GP 处理的影响。除 qCO2 外,我们还观察到单一化学参数与微生物指数之间存在明显的相关性,这表明微生物组的反应是多因素的,但主要受 GP 组成和养分供应的驱动,而养分供应又取决于土壤特性。这项研究使人们能够更广泛地了解在不同性质的土壤中施用新鲜 GP 品种的后果,这对于计算最佳营养投入是必要的。
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