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首页> 外文期刊>Agricultural Water Management >Spent coffee grounds as organic amendment modify hydraulic properties in a sandy loam Brazilian soil
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Spent coffee grounds as organic amendment modify hydraulic properties in a sandy loam Brazilian soil

机译:作为有机修正的咖啡渣改变砂土巴西土壤中的液压特性

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Soil physical and chemical properties can be amended by application of organic residues, such as spent coffee grounds (SCG). In this work we examined SCG effects on the modification of some soil physical-hydraulic properties, such as soil water retention and aeration, investigating beneficial uses for this waste product. Soil properties were evaluated using pots filled with a mixture of a sandy loam soil with the contents of 0, 5, 10, 15 and 20% of SCG. The most relevant soil properties to the purposes were the moisture at container capacity (theta(cc)), readily available water capacity (RAWC) and drainable porosity (phi(D)). Additionally, under the hypothesis that SCG can be used as soil conditioner, lettuce crop, cultivar "Mimosa Roxa Roxanne", was transplanted to the pots where the leaf area index and the cumulative biomass throughout the growing cycle were examined. Comparing to the absence of SCG (0%), soil SCG contents of 5, 10, 15 and 20% presented larger values of theta(cc) and consequently larger RAWC and smaller phi(D). Although the increase of soil water storage from 43.2 (0%) to 53.3 (20%) mm, crop development was prejudiced by the reduction on phi(D) from 0.1595 (0%) to 0.0827 (20%) m(3) m(-3), which affected soil aeration. This greater water availability, obtained with the increase of theta(cc), was promoted by the residue addition pointing out for a possible use of SCG to increase water retention for other crops.
机译:土壤物理和化学性质可以通过施用有机残留物而修改,例如废咖啡渣(SCG)。在这项工作中,我们研究了对一些土壤物理 - 液压性能的改变的SCG效应,例如土壤水保留和曝气,调查这种废物产品的有益用途。使用填充有砂土土壤混合物的罐评估土壤性质,其含量为0,5,10,15和20%的SCG。目的最相关的土壤性质是容量(θ(CC))的水分,易于使用的水容量(RawC)和可排水孔隙率(PHI(D))。另外,在SCG可用作土壤调理剂的假设下,莴苣作物,栽培品种“含羞草ROXA ROXANNE”被移植到叶片区域指数和在整个生长循环中的累积生物量的罐中。比较不存在SCG(0%),土壤SCG含量为5,10,15和20%呈现较大的θ(CC)值,因此较大的RawC和较小的PHI(D)。虽然从43.2(0%)的土壤储存量增加至53.3(20%)mm,作物发育的含量从0.1595(0%)降低至0.0827(20%)m(3)米(-3),影响土壤曝气。通过增加θ(cc)的这种较大的水可用性由指出可能使用SCG以增加其他作物的水潴留来促进促进。

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