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首页> 外文期刊>Revista ciencia agronomica >Interferências dos pedoambientes nos atributos do solo em uma topossequência de transi??o Campos/Floresta
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Interferências dos pedoambientes nos atributos do solo em uma topossequência de transi??o Campos/Floresta

机译:在Campos / Floresta向正序过渡中,人为环境对土壤属性的干扰

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摘要

The pedoenvironmental conditions promote changes in soil properties, so the aim of this work was to study Interference of the pedoenvironment on soil properties in a topossequence of the Grassland/Forest transition in the Humaitá region, AM. Was picked up a topossequence characteristic sequence Grassland/Forest, then a pathway was established, from a field environment to the natural forest environment. These pedoambients were identified and defined as the expression patterns of vegetation. Were collected 20 samples at the representative side of the profiles in each one of the pedoambiental units of the topossequence (top grassland: 0.0-14 and 0.30-0.66 m;low grassland : 0.0-0.15 and 0.27-0.80 m; ecotone zone: 0.0-0.15 and 0.32-0.50 m; forest: 0.0-0.15 m 0.67-100 as a total of 80 samples) being the criteria for sampling depths the coincidence with the surface and subsurface diagnostic horizons determined by the morphological description of the profiles. Were performed physical analysis of texture, clay dispersion and flocculation, soil bulk density and particle porosity and hydraulic conductivity. In the chemical analysis were determined pH in water and KCl, Ca, Mg, K, Na and Al contents, available P, H + Al and organic carbon. The physical and chemical soil were dependent on the pedoambients. With the use of multivariate statistical techniques was possible to distinguish three different environments that are equivalent to three pedoambients.
机译:人为环境条件促进土壤性质的变化,因此本研究的目的是研究AM于Humaitá地区的草地/森林过渡带之后人为环境对土壤性质的干扰。从后序特征序列草原/森林中选取了一个,然后建立了一条从田间环境到天然森林环境的途径。这些古生物被识别并定义为植被的表达模式。在后序的每个土壤环境单元中,在剖面的代表性侧收集了20个样品(顶部草原:0.0-14和0.30-0.66 m;低草原:0.0-0.15和0.27-0.80 m;生态交错带:0.0 -0.15和0.32-0.50 m;森林:0.0-0.15 m 0.67-100,共80个样品)是采样深度的标准,与通过轮廓的形态描述确定的地表和地下诊断层一致。进行了质地,粘土分散和絮凝,土壤容重和颗粒孔​​隙度以及水力传导率的物理分析。在化学分析中,测定水中的pH值以及KCl,Ca,Mg,K,Na和Al的含量,可用的P,H + Al和有机碳。物理和化学土壤取决于土壤环境。通过使用多元统计技术,有可能区分出等同于三个教育环境的三个不同环境。

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