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Eolian Deposition and Soil Fertility in a Prehistoric Agricultural Complex in Central Arizona, USA

机译:美国亚利桑那州中部史前农业综合体的风积和土壤肥力

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摘要

Prehistoric farmers in arid and semiarid ecosystems commonly used rock alignments to concentrate water and sediments on their fields. Previous research has emphasized the importance of runoff from organic matter-rich uplands as a mechanism for soil nutrient replenishment. However, eolian inputs to these dryland ecosystems might also contribute substantially to mineral-derived nutrient pools. We explored the relative importance of eolian deposition, prehistoric agriculture, and the presence of rock alignments on soil properties in a semiarid grassland in Arizona. Subsurface soils behind natural rock alignments are finer in texture than soils unbound by rock alignments, while subsurface soils behind agricultural rock alignments coarsen relative to unbound soils. Neither rock alignments nor estimated crop yields had detectable effects on mineral-derived nutrient pools. In contrast, eolian deposition is an important source of soil mass and nutrients to modern soils. While dust deposition likely reduced soil heterogeneity across this landscape, it could have also contributed to the sustainability of prehistoric agriculture.
机译:干旱和半干旱生态系统中的史前农民通常使用岩石排列来将水和沉积物集中在他们的田地上。先前的研究强调了富含有机物的高地径流作为补充土壤养分的机制的重要性。但是,对这些旱地生态系统的风积投入也可能极大地促进了矿物来源的营养库。我们探讨了风积作用,史前农业以及亚利桑那州半干旱草原土壤性质对岩石排列的相对重要性。天然岩石准线后的地下土壤质地要比未受岩石准线约束的土壤细,而农业岩石准线后的地下土壤则相对于未结合的土壤要粗糙。岩石定线和估计的农作物收成对矿物质来源的营养库都没有可检测到的影响。相反,风积是现代土壤中土壤质量和养分的重要来源。尽管尘埃沉积可能会降低整个景观中土壤的异质性,但它也可能有助于史前农业的可持续发展。

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