首页> 外文期刊>Agriculture, Ecosystems & Environment: An International Journal for Scientific Research on the Relationship of Agriculture and Food Production to the Biosphere >Organic carbon storage potential in deep agricultural soil layers: Evidence from long-term experiments in northeast Italy
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Organic carbon storage potential in deep agricultural soil layers: Evidence from long-term experiments in northeast Italy

机译:深农土壤层中有机碳储存潜力:意大利东北部长实验的证据

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The significant contribution to the global carbon budget made by soil organic carbon (SOC) inspired the "4 per 1000" initiative. It promotes agricultural practices aimed at raising SOC stocks 0.4 % annually over 20 years. However, the response of topsoil and deep soil profiles to agroecosystem changes is largely unknown at present. Our work aims to quantify deep SOC accumulations in stabilized croplands and grasslands of northeast Italy and identify the best management practices to increase those stores. Soil profiles were collected to 70 and 90 cm depths from three well-established long-term experiments. A total of 1242 soil samples were analyzed for SOC concentrations as a function of soil type, soil management practice, and cropping system. SOC stocks were quantified using the equivalent soil mass method. Results show that SOC stocks averaged 23.2 Mg ha(-1) in sandy Arenosol, 59.3 Mg ha(-1) in silty loam Cambisol, 111.6 Mg ha(-1) in clay loam Gleysol, and 383.5 Mg ha(-1) in peaty Histosol. Substantial SOC stocks were found in the subsoil beneath the filled layer, ranging between 59 and 74 % in sandy and clay loam soils. Among the considered managements, the SOC accumulation rate of permanent meadow topsoil was higher than croplands (0.299 Mg ha(-1) yr -1), which fell to 0.256 Mg ha(-1) yr(-1) when estimated along the full soil profile. In contrast, organic carbon added through manures and residues, coupled with minimum tillage practices, led to increased average SOC stock rates in the topsoil (0.205 Mg ha(-1) yr(-1)) and throughout the full soil profile (0.386 Mg ha(-1) yr(-1)), suggesting that some translocation dynamics occurred. The long-term adoption of permanent meadow, along with manure or residue addition under minimum tillage, made it possible to achieve "4 per 1000" goals to great depths in naturally poor-SOC sandy and silty loam soils. In SOC-rich soil, only in the topsoil layer achieved this.
机译:土壤有机碳(SOC)制定的全球碳预算的重大贡献激发了“每1000份4”倡议。它促进了旨在每年筹集0.4%的农业股20多年的农业实践。然而,目前,TOPSOIL和深土壤谱对农业系统变化的响应在很大程度上是未知的。我们的工作旨在量化意大利东北地区稳定的农田和草原的深层SOC积累,并确定增加这些商店的最佳管理措施。从三种良好的长期实验中收集到70和90厘米深度的土壤曲线。作为土壤类型,土壤管理实践和种植系统的函数,分析了共有1242种土壤样品的SOC浓度。使用相同的土壤质量法量化SOC股。结果表明,SoC股在含有粉肥泥棉絮59.3毫克HA(-1)中的23.2毫克HA(-1),粘土壤土胶凝玉米醇的111.6 mg HA(-1),以及383.5 mg HA(-1)泥质组织醇。在填充层下面的底层中发现了大量的SOC股,在桑迪和粘土壤土土壤中的59%至74%之间。在考虑的管理层中,常牙草甸Topsoil的SoC累积率高于农作物(0.299mg HA(-1)YR -1),沿着全额估计,跌至0.256mg ha(-1)Yr(-1)土壤剖面。相比之下,通过粪便和残基加入的有机碳,与最小耕作实践相结合,导致表土中的平均SOC储存率增加(0.205mg HA(-1)Yr(-1))和整个土壤剖面(0.386毫克) HA(-1)YR(-1)),建议发生一些易位动态。长期采用永久性草甸,以及在最小耕作中加入粪肥或残留物,使得可以在自然贫困的沙滩和粉质壤土土壤中实现“每1000”的巨大进球。在富含SoC的土壤中,只有在表土层中才能实现这一点。

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