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Visualizing land‐use and management complexity within biogeochemical cycles of an agricultural landscape

机译:在农业景观的生物地球化学周期内可视化土地利用和管理复杂性

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摘要

Abstract Crop fields are cultivated across continuities of soil, topography, and local climate that drive biological processes and nutrient cycling at the landscape scale; yet land management and agricultural research are often performed at the field scale, potentially neglecting the context of the surrounding landscape. Adding to this complexity is the overlap of ecosystems and their biogeochemical legacies, as a patchwork of crops fields, natural grasslands, and forests develops across the landscape. Furthermore, as new technologies and policies are introduced, management practices change, including fertilization strategies, which further alter biological productivity and nutrient cycling. All of these environmental, biological, and historical legacies are potentially recorded in the isotopic signal of plant, soil, and sediment organic matter across the landscape. We mapped over 1500 plant, soil, and sediment isotopic values and generated an isotopic landscape (isoscape) over a 40‐km2 agricultural site in NE Germany. We observed distinct patterns in the isotopic composition of organic matter sampled from the landscape that clearly reflect the landscape complexity. C3 crop intrinsic water‐use efficiency reflected a precipitation gradient, while native forest and grassland plant species did not, suggesting that native plants are more adapted to predominant climatic conditions. δ13Csoil patterns reflected both the long‐term input of plant organic matter, which was affected by the local climate conditions, and the repeated cultivation of corn. Soil organic matter 15N isotopic values also revealed spatial differences in fertilization regimes. Forest fragments, in which the nitrogen cycle was relatively open, were more water‐use efficient. Sediments from small water bodies received substantial inputs from surrounding field vegetation but were also affected by seasonal drying. These isotopic maps can be used to visualize large spatial heterogeneity and complexity, and they are a powerful means to interpret past and current trends in agricultural landscapes.
机译:摘要植物田间越过土壤,地形和局部气候的连续性,可以在景观量表上驱动生物过程和养分循环;然而,土地管理和农业研究通常在现场规模上进行,可能忽视周围景观的背景。添加到这种复杂性是生态系统和他们的生物地球化学遗址的重叠,作为农作物领域,天然草原和森林的拼凑而成的景观。此外,由于介绍了新技术和政策,管理实践改变,包括施肥策略,进一步改变生物生产力和营养循环。所有这些环境,生物学和历史遗产都可能在植物,土壤和沉积物有机物的同位素信号中记录在整个景观中。我们映射了1500多种植物,土壤和沉积物同位素值,并在Ne德国的一个40平方公里的农业遗址上产生了同位素景观(Isoscape)。我们观察到从景观中取样的有机物质的同位素组成中的明显模式,清楚地反映了景观复杂性。 C3作物内在用水效率反映了沉淀梯度,而原生林和草原植物物种没有,表明本土植物更适应主要的气候条件。 Δ14CSOIL模式反映了受局部气候条件影响的植物有机物的长期输入,以及玉米的反复培养。土壤有机物15N同位素值也揭示了受精制度的空间差异。森林碎片,其中氮循环相对开放,更有吸水性有效。小水体的沉积物从周围的田间植被接受了大量输入,但也受季节性干燥的影响。这些同位素地图可用于可视化大的空间异质性和复杂性,并且它们是一种强大的方法,可以解释农业景观的过去和当前趋势。

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